ZUSGSZUSGS science fora changing world Sedimentation and Sediment Chemistry, Neopit Mill Pond,...
Transcript of ZUSGSZUSGS science fora changing world Sedimentation and Sediment Chemistry, Neopit Mill Pond,...
ZUSGSscience fora changing world
Sedimentation and Sediment Chemistry, Neopit Mill Pond, Menominee Indian Reservation, Wisconsin, 2001
Prepared in cooperation with the Menominee Indian Tribe of Wisconsin
Open File Report 03-23
U.S. Department of the Interior U.S. Geological Survey
Sedimentation and Sediment Chemistry, Neopit Mill Pond, Menominee Indian Reservation, Wisconsin, 2001
By Faith A. Fitzpatrick and Marie C. Peppier
Prepared in cooperation with the Menominee Indian Tribe of Wisconsin
Open-File Report 03-23Middleton, Wisconsin: 2003
U.S. Department of the Interior U.S. Geological Survey
U.S. Department of the InteriorGale A. Norton, Secretary
U.S. Geological SurveyCharles G. Groat, Director
For additional information about this report, write to:District ChiefU.S. Geological Survey8505 Research WayMiddleton, Wl 53562-3586World Wide Web: http://wi.water.usgs.gov/
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Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government.
Although this report is in the public domain, it contains copyrighted materials that are noted in the text. Permission to reproduce those items must be secured from the individual copyright owners.
Cover photograph shows the Menominee Enterprises, Inc. sawmill at Neopit, Wisconsin. From Milfred, C.J., Olson, G.W., and Hole, F.D., 1967, Soil resources and forest ecology of Menominee County, Wisconsin: University of Wisconsin, Geological and Natural History Survey, Soil Survey Division, Bulletin 85, Soil Series No. 60, fig. 7, p. 25. Date of photo and photographer unknown.
Ill
Contents
Abstract.................................................................................................................................................... 1Introduction .................................................. 1
Purpose and scope............................................................................................................................ 1Description of study area................................................................................................................. 2Acknowledgments............................................................................................................................. 2
Study methods............................................................................................................................................ 2Review of historical documents...................................................................................................... 2Transect surveying and sediment coring....................................................................................... 2Sediment laboratory analyses......................................................................................................... 2
Physical characteristics.............................................................................................................. 2Radiometric age dating............................................................................................................... 3Minor and trace elements........................................................................................................... 3Organic compounds..................................................................................................................... 3Quality control............................................................................................................................... 3
Pre-dam topography and channel characteristics................................................................................. 3Post-dam sedimentation.............................................................................................................................Sediment chemistry.................................................................................................................................... 5
Minor and trace elements............................................................................................................... 5Organic compounds.......................................................................................................................5
Conclusions................................................................................................................................................... 6References cited.............................................................................................................................. 7Figures........................................................................................................................Tables . .. ... .. ..... ..... ........ ......... . .. . . ...... .. ........ .... . ......... . ....... ................ 19Appendix Tables............................................................................................................................... 23
A. Transect survey and sounding data......................................................................................... 24B. Core descriptions..................................................................................................................... 36C. Bulk density and organic content data.................................................................................... 49D. Radiometric dating results......................................................................................................... 50E. Minor- and trace-element data................................................................................................. 51F. Organic compound data................................................................................................... 55
IV
Figures1. Transect lines and core locations, Neopit Mill Pond, Neopit, Wis...................................... 82. Estimated location of pre-dam channel, Neopit Mill Pond.................................................... 93. Geologic cross sections, Neopit Mill Pond, November 2001 through July 2002
A. Cross section 2.................................................................................................................. 10B. Cross section 3.................................................................................................................. 10C. Cross section 4.................................................................................................................. 10D. Cross section 5.................................................................................................................. 11E. Cross section 7.................................................................................................................. 12F. Cross section 8.................................................................................................................. 12G. Cross section 9.................................................................................................................. 13H. Cross section 10................................................................................................................ 14I. Cross section 11................................................................................................................ 15J. Cross section 12................................................................................................................ 16K. Cross section 13................................................................................................................ 17L Cross section 14................................................................................................................ 17
4. Post-dam sediment thickness at core locations, Neopit Mill Pond, 2001......................... 18
Tables1. General Land Office Survey Notes from 1854 for the Neopit Mill Pond area................... 192. Worksheet for calculating volume and weight of post-dam sediment in
Neopit Mill Pond......................................................................................................................... 203. Organic compounds detected in Neopit Mill Pond sediment (concentrations
normalized to 1 percent total organic carbon) and consensus-based sediment quality guidelines........................................................................................................................ 21
Appendix TablesA. Transect survey and sounding data
A1. Altitudes of land surface and hard and soft.bottom and descriptive notesfor transect 2............................................................................................................................... 24
A2. Altitudes of land surface and hard and soft bottom and descriptive notesfor transect 3............................................................................................................................... 25
A3. Altitudes of land surface and hard and soft bottom and descriptive notesfor transect 4............................................................................................................................... 26
A4. Altitudes of land surface and hard and soft bottom and descriptive notesfor transect 5............................................................................................................................... 27
A5. Altitudes of land surface and hard and soft bottom and descriptive notesfor transect 7...............................................................................................................................28
A6. Altitudes of land surface and hard and soft bottom and descriptive notesfor transect 8............................................................................................................................... 29
A7. Altitudes of land surface and hard and soft bottom and descriptive notesfor transect 9............................................................................................................................... 30
A8. Altitudes of land surface and hard and soft bottom and descriptive notesfor transect 10............................................................................................................................ 31
A9. Altitudes of land surface and hard and soft bottom and descriptive notesfor transect 11............................................................................................................................. 32
A10. Altitudes of land surface and hard and soft bottom and descriptive notesfor transect 12.............................................................................................................................33
All. Altitudes of land surface and hard and soft bottom and descriptive notesfor transect 13.............................................................................................................................34
A12. Altitudes of land surface and hard and soft bottom and descriptive notesfor transect 14.............................................................................................................................35
B. Core descriptionsB1. Core descriptions for core 1..................................................................................................... 36B2. Core descriptions for core 2..................................................................................................... 37B3. Core descriptions for core 3..................................................................................................... 39B4. Core descriptions for core 4..................................................................................................... 40B5. Core descriptions for core 5..................................................................................................... 41B6. Core descriptions for core 6..................................................................................................... 42B7. Core descriptions for core 7..................................................................................................... 44B8. Core descriptions for core 8..................................................................................................... 46B9. Core descriptions for core 9..................................................................................................... 47
BIO. Core descriptions for core 10................................................................................................... 48C. Bulk density and organic content data
C1. Bulk density and organic matter data for core samples collected from NeopitMill Pond, Neopit, Wis., 2001.................................................................................................... 49
D. Radiometric dating resultsD1. Radiometric dating results for core samples collected from Neopit Mill Pond,
Neopit, Wise., 2001..................................................................................................................... 50E. Minor- and trace-element data
E1. Minor and trace element results for core samples from Neopit Mill Pond,Neopit, Wise., 2001..................................................................................................................... 51
F. Organic compound dataF1. Organic compounds detected in core samples collected from Neopit Mill
Pond, Neopit, Wise., 2001.......................................................................................................... 55F2. Organic compounds not detected in core samples collected from Neopit Mill
Pond, Neopit, Wise., 2001.......................................................................................................... 58
VI
Conversion Factors, Vertical Datum, and Abbreviated Units of Measurement
Multiplyinch (in.)inch (in.)
foot (ft)acre
mile (mi)square foot (ft2)
square mile (mi2)cubic foot (ft3)
cubic yard (yd3)pound (Ib)pound (Ib)ton (short)
By25.4
2.540.30480.40481.6090.092942.590
35.3141.308
453.6.4536
0.9072
To Obtainmillimetercentimetermeterhectarekilometersquare metersquare kilometercubic metercubic metergramkilogrammegagram
Temperature, in degrees Celsius (°C) can be converted to degrees Fahrenheit (°F) by use of the following equation: °F=1.8(°C) + 32.
Vertical datum: In this report, "sea level" refers to the National Geodetic Vertical Datum of 1929 (NGVD of 1929), a geodetic datum derived from a general adjustment of the first-order level nets of both the United States and Canada, formerly called Sea Level Datum of 1929.
Abbreviated units of measurement used in this report: Sediment sample weight is given in grams. Bulk density is given in pounds per cubic foot (lb/ft3) and grams per cubic centimeter (g/cm3). Sediment chemical concentration is given in micrograms per gram (/ig/g), grams per kilogram (g/kg), or percent.
Sedimentation and Sediment Chemistry, Neopit Mill Pond, Menominee Indian Reservation, Wisconsin, 2001
by Faith A. Fitzpatrick and Marie C. Peppier
Abstract
The volume, texture, and chemistry of sediment deposited in a mill pond on the West Branch of the Wolf River at Neopit, Wis., Menominee Reservation, were studied in 2001-2002. The study was accomplished by examining General Land Office Survey Notes from 1854, establishing 12 transects through the mill pond, conducting soundings of the soft and hard bottom along each transect, and collecting core samples for preliminary screening of potential contaminants. Com bined information from transects, cores, and General Land Office Survey notes were used to reconstruct the pre-dam location of the West Branch of the Wolf River through the mill pond. Neopit Mill Pond contains approximately 253 acre-ft of organic-rich muck, on average about 1.2 ft thick, that was deposited after the dam was built. Elevated concentrations of polycyclic aromatic hydrocarbons (PAHs) associated with cre osote and pentachlorophenol were found in post-dam sediment samples collected from Neopit Mill Pond. Trace-element con centrations were at or near background concentrations. Further study and sampling are needed to identify the spatial extent and variability of the PAHs, pentachlorophenol, and other byprod ucts from wood preservatives.
Photograph of the Menominee Enterprise, Inc. sawmill at Neopit, Wis. Date and photographer unknown (Milfred and others, 1967, p. 25).
Introduction
Neopit Mill Pond is located on the West Branch of the Wolf River at Neopit, Wis., Menominee Reservation (fig. 1). The dam for the mill pond was constructed in 1907 and the mill pond has been used in the past to store logs used in the Menom inee Enterprise, Inc. sawmill located on the northeast side of the pond. A severe storm in 1905 damaged about 40 million board ft of hardwood-hemlock west of Neopit along the West Branch (Milfred and others, 1967). An Act of 1906 allowed the Menominee Tribe to log the timber under supervision of Gov ernment experts, create lumber mills, and sell lumber (Milfred and others, 1967). The lumber mill and mill pond at Neopit were constructed soon after these events. At the time of this study, the future of the dam is not known, and there is some possibility that the dam may be removed or upgraded and the stream restored or rehabilitated. Knowledge of the volume and chemical characteristics of the impounded sediment are needed prior to the removal of the dam or stream restoration. A cooperative study between the U.S. Geological Survey (USGS) and the Menominee Indian Tribe of Wisconsin was done in 2001-2002 to estimate the volume, texture, and chem istry of sediment deposited in Neopit mill pond. The objectives of this study were to: (1) identify and describe the pre-dam channel of the West Branch of the Wolf River; (2) estimate the volume and describe the texture of post-dam sediment in Neopit Mill Pond; and (3) describe the chemistry of post-dam sediment in the mill pond.
Purpose and Scope
The purpose of this report is to describe the findings from the study of sedimentation and sediment chemistry of Neopit Mill Pond. This report presents the results of the analysis of General Land Office Survey Notes, an estimate of pre-dam channel planform through the pond, results from soundings and surveys, core descriptions, estimates of post-dam sediment
2 Sedimentation and Sediment Chemistry, Neopit Mill Pond, Menominee Indian Reservation, Wisconsin, 2001
volume and weight, and results from preliminary screening of minor and trace elements and organic compounds in post-dam sediment.
Description of Study Area
Neopit Mill Pond is on the north side of Neopit, Wis., in the Menominee Indian Reservation. The pond has an area of 202 acres and a maximum depth of 10 ft. Two main tributaries enter the pond from the north (West Branch of the Wolf River) and the west (Little West Branch of the Wolf River). Neopit Mill Pond is surrounded by sandy glacial outwash and till and the topography is rolling to hilly (Milfred and others, 1967). Soils near the pond and in the watershed are composed of loams, sandy loams, and peat (Milfred and others, 1967). Vegetation in the watershed upstream of the pond mainly consists of northern hardwoods, hemlock-hardwoods, and swamp conifers (Milfred and others, 1967).
Acknowledgments
The authors thank Heather Arthur, Douglas Cox, and Jeremy Pyatskowit of the Environmental Services Department of the Menominee Indian Tribe of Wisconsin for their exhaus tive field data collection efforts. They collected all the sound ing data and greatly assisted with collecting cores and survey ing. Matt Diebel (USGS) assisted with surveying and coring. Technical reviewers were Douglas Cox (Menominee Tribe Environmental Services), Herbert Gam (USGS), and Thomas Janisch (Wisconsin Department of Natural Resources). Janisch also provided insight on potential contaminants associated with wood preservatives and lumber mills in Wis consin. Michelle Greenwood (USGS), Susan Jones (USGS), and Jen Bruce (USGS) provided editorial and graphic support.
Study Methods
This study involved examining historical documents, surveying 12 transects in the mill pond, determining the pre- dam land surface through soundings, collecting several cores along the transects, and analyzing subsamples of cores for analysis of organic content, minor and trace elements, organic compounds, and radiometric dating. Data were collected from November 2001 through July 2002.
Review of Historical Documents
Copies of original General Land Office (GLO) Survey Notes were obtained from the State of Wisconsin, Board of Commissioners of Public Lands for two townships: Township 29 North, Range 14 East and Township 29 North, Range 13 East. Notes for both townships are from 1854.
Transect Surveying and Sediment Coring
Data from transect surveys and sediment coring pro vided quantitative information on sedimentation and sediment geochemistry. Twelve transects (fig. 1) were placed along the pond at a spacing of about 1,000 ft. Depths to soft and hard sediment were measured by use of a sounding pole in impounded areas. An auto level was used to extend the transect data from below the water surface along the shoreline of the pond. Each transect end was marked with a semi-perma nent marker such as rebar or pipe or painted trees. A "total sta tion" surveying level was used to determine the elevations of the markers at each transect end point. Transect elevation data were referenced to a Wisconsin Department of Transportation benchmark on the railroad bed at Neopit (the benchmark has an altitude of 1,068 ft based on the 1982 USGS 7.5-minute quadrangle map, fig. 2). A global positioning system was used to verify the location of each transect and core.
The thickness, texture, geochemistry, and age of sedi ment in the pond were examined in cores collected with two devices a geoprobe (2-in. diameter) and a piston corer (3-in. diameter). Ten cores were collected in March 2001 when the mill pond was frozen. The cores were examined in the field or at the USGS laboratory in Middleton, Wis. for color (Munsell Color, 1975), and field determination of texture was done by rubbing sediment between the fingers and use of the U.S. Department of Agriculture textural triangle (Soil Survey Staff, SCS, 1951). Samples were taken from a subset of side-by-side cores collected at sites 1,2, 6, and 7 for preliminary analysis of water content, organic matter, minor and trace elements, organic compounds, and radiometric dating at USGS labora tories. Subsamples and cores were chilled or frozen during transport from the mill pond to the USGS in Middleton, where they were immediately frozen and archived upon arrival.
Sediment Laboratory Analyses
Physical Characteristics
Physical characteristics measured included water content and organic matter content (loss on ignition) for two samples
Pre-Dam Topography and Channel Characteristics 3
from core 1, one sample from core 2, and eight samples from core 7 (table Cl). Water and organic matter content were ana lyzed at the USGS laboratory in Middleton. Water content was measured by use of standard American Society for Testing and Materials Procedure D2216-92, except that sample sizes were less than 20 g wet weight due to the small sample size. Percent age dry weight was determined by measuring weight loss after24 hours at 105°C. Organic matter content was determined by weight loss after ashing at 550°C for 1 hour (methods described in Dean, 1974). Dry bulk density was calculated by use of the formula:
p = (D(2.5IX + 1.6CX ))/(D + (1-D) (2.5IX + 1.6CX)),(1)
where p is dry bulk density (g cm"3), x is depth in the core, D is the proportion dry weight of unit wet volume, I is inorganic proportion of dry material (assuming a density of
^
2.5 g cm ), and C is organic proportion of dry material
(assuming a density of 1.6 g cm"3).
Radiometric Age Dating
Radiometric age dating included the analysis of six samples for 210Pb, 137Cs, and 226Ra (table Dl). The 210Pb dating technique is based on the escape of radon from the Earth and the subsequent decay of this radioactive gas into 210Pb. This technique is most suitable for dating material up to a maximum age of about 150 years because the half-life of 210Pb is approximately 22 years (Olsson, 1986). To account for some of the variability associated with possible fluctuation in the sources of lead or inhomogeneous sediment, 226Ra also was analyzed in each of the samples. Optimally, samples from sed iment more than 150 years old are collected to measure local background concentrations of 210Pb supplied to the sediment from decay of uranium minerals (Olsson, 1986). 137Cs was first detected in 1945, and in 1954 the first increase occurred in the Northern Hemisphere, corresponding to increased nuclear weapon testing (Krishnaswami and Lal, 1978). In 1960 a minimum occurred, followed by a maximum in 1963. With the signing of the atmospheric nuclear test ban treaty, atmospheric contributions have dropped off substantially (Olsson, 1986).
1 "^"7
A date of 1963 is assigned to the sample with the highest Cs activity.
Minor and Trace Elements
Two samples from core 1 and one sample each from cores 2 and 7 were submitted to the USGS National Water- Quality Laboratory, Denver, Colo. for analyses of minor and trace elements in sediment (table El). The piston core tube was composed of Lexane and the geoprobe cores had plastic liners.
The cores were subsampled with plastic equipment and sam ples stored in plastic jars. Samples were not sieved. Samples were frozen prior to shipping. All elements except sulfur were analyzed by use of inductively coupled plasma-mass spec- trometry (Briggs and Meier, 1999). Sulfur was anaylzed by methods described in Jackson and others (1985) and Jackson and others (1987). Total digestions were done.
Organic Compounds
Four samples from core 1, two samples from core 2, and 1 sample from core 7 were analyzed for organic compounds at the USGS National Water-Quality Laboratory (tables Fl and F2). Compounds analyzed for included pesticides and metabo lites, semi-volatile organic substances, polycyclic aromatic hydrocarbons (PAHs), chlorinated and nonchlorinated phe nols, benzenes, ethanes, polychlorinated biphenyls (PCBs), DOT and metabolites, phthalate esters, nitrosamines, and halomethanes. Subsamples were collected from the cores by use of stainless steel equipment and samples were stored in glass jars. Jars were frozen after subsampling. Samples were not sieved. Laboratory methodology is detailed in Fishman (1993), Foreman and others (1995), and Furlong and others (1996).
Quality Control
Quality control procedures included collecting duplicate cores and approximately 15 percent replicate samples for lab oratory analysis. Quality control measures at the USGS labo ratories included comparisons to standard reference materials, spikes, and duplicates (Pirkey and Glodt, 1998).
Pre-Dam Topography and Channel Characteristics
A combination of the 1854 GLO notes and transect and core data (figs. 1 and 3; tables A1-A12, B1-B10) were used to reconstruct the location of the West Branch of the Wolf River. Estimated planforms for the West Branch and its tributary, the Little West Branch, are shown on figure 2. Three section lines bisect the mill pond. There was generally good agreement between the location of the channel from the GLO notes and the lowest elevation for the hard bottom (interpreted to be channel bottom) found along transects nearest to the section lines (fig. 3). There are some potential alternative locations for the channel or possibility that the channel was braided or con tained islands. The presence of peat-like sediment in some of
4 Sedimentation and Sediment Chemistry, Neopit Mill Pond, Menominee Indian Reservation, Wisconsin, 2001
the cores suggests that part of the mill pond was previously wetland or lowland, making it difficult to pinpoint the exact location of the channel, especially where the two tributaries join.
The GLO notes give some indication of the width, depth, and type of sediment in the pre-dam channel in 1854 observed along section lines (table 1). The West Branch of the Wolf River through the impounded section was about 46-66 ft wide, 1-2 ft deep, and most likely gravel bottom. The Little West Branch was about 40 ft wide and is noted as having rapid current and high banks near the upstream end of the mill pond along the section line between sections 24 and 19. Down stream of the mill pond, the West Branch of the Wolf River was 109 ft wide, 1-2 ft deep, and had a sandy bottom.
The altitude of the pre-dam channel bottom of the West Branch of the Wolf River ranged from about 1,038 ft near the location of the dam (transects 13 and 14), to 1,049 ft near the north side of the mill pond at transect 7 (figs. 3E, 3K, and 3L). The Little West Branch pre-dam channel bottom ranged from an altitude of about 1,043 ft at its confluence with the West Branch of the Wolf River near transect 9 to about 1,046 ft near the west end of the mill pond at transect 2. The value of 1,046 ft for the west end is uncertain because of the lack of core data from transects 2 and 3. The hard bottom altitude for these transects can be used as an approximate indicator of the pre-dam topography because the sounding pole penetrated the pre-dam peat deposits that were present in this area, as shown in core 7 from transect 4.
Post-Dam Sedimentation
Figure 4 shows the estimated thickness of post-dam sediment at each of the core locations. Post-dam sediment is composed of organic-rich muck with or without wood pieces. Characteristics of the pre- and post-dam deposits at each core location are shown along the transects in figures 3A-L. A common stratigraphic sequence of the deposits is about 1 ft of organic-rich muck with large wood pieces near the base of the unit, underlain by pre-dam deposits of peat, sand, or sand and gravel. Large wood pieces were most prevalent in cores nearest to the lumber mill. The pre-dam peat deposit is thickest toward the western side of the pond near core 7.
The presence of wood pieces in loamy sand sometimes found below the organic muck in cores 2, 3, 6, 7, 9, and 10 was somewhat confusing because the sand is interpreted to have been deposited before the mill pond and lumber mill were constructed. The wood found in sandy deposits below the organic-rich muck may be related to the 1905 storm and
related damaged timber in the West Branch drainage basin but also may be related to earlier logging, log drives, or older storms. Buried A horizons were also identified in cores 2 and 10 and likely represent old flood-plain surfaces. It is likely that during floods some of the organic-rich muck was eroded in the narrow reach of the pond upstream of the dam (for example transects 12, 13, and 14).
As stated in the previous section, the hard bottom alti tudes based on soundings are sometimes deeper than inter preted pre-dam land surface based on core data (fig. 3). The sounding pole tended to extend into pre-dam deposits if they were composed of peat or loamy, organic-rich sand. However, sometimes the sounding pole would stop because of the pres ence of large wood pieces typically found at the base of the post-dam sediment, associated with debris coming off of the logs as they were stored in the mill pond prior to use at the lumber mill. The sounding pole correctly marked the altitude of the pre-dam surface if the muck was directly underlain by sand and gravel, such as in cores 4 and 5.
Cores collected in shallow water (cores 4 and 7) showed some disagreement between the top of sediment as measured by coring (February and March 2001) and that determined from sounding (summer 2001). It is thought that this is because the water was shallow enough that the entire water column was frozen down to the soft bottom. This means that there was potential for some of the top of the core to be lost from augering a hole in the ice.
The results from analysis of 210Pb, 137Cs, and 226Ra for samples from core 7 were not helpful for determining sedi mentation rates in the mill pond (table Dl). The lack of a Cs peak most likely indicates that the sediment at this site possi bly was subjected to mixing by wave action or bioturbation. Also, it is not known how much water levels varied in the mill pond historically.
A very rough estimate of the volume and weight of organic-rich muck associated with post-dam sedimentation can be made by averaging the depth of post-dam sediment at each transect (based mainly on the core data) and multiplying it by the average width of each transect and the length of mill pond that it represents (table 2). Dry bulk density of the organic-rich muck is estimated to be about 6.9 lbs/ft3 based on the average of bulk density calculated from subsamples (table Cl). The bulk density is quite low because of the high water content of the muck (generally about 90 percent) and substan tial amount of organic matter (34-58 percent) (table Cl). The sum of areas calculated for each transect is 211 acres, in close approximation to the listed size of 202 acres by the Wisconsin Department of Natural Resources. The mill pond is estimated to contain about 253 acre-ft (408,700 yds3 or 38,000 tons) of post-dam related sediment. This estimate could be further
Sediment Chemistry 5
refined by collecting additional core data and refining the sounding techniques to only penetrate the organic-rich muck.
Sediment Chemistry
A small set of archived subsamples (four samples from three cores for analysis of minor and trace elements and seven samples from three cores for analysis of organic compounds) was submitted for laboratory analysis of minor and trace ele ments and synthetic organic chemicals for preliminary identi fication of potential contaminants in the impounded sediment. The results from these analyses do not represent a complete range of concentrations of potential contaminants within Neo- pit Mill Pond. Instead, they are useful for preliminary screen ing and to help guide future sediment-chemistry sampling.
Minor and Trace Elements
Concentrations of the minor and trace-element in organic- rich muck (post-dam sediment) from Neopit Mill Pond were generally within the range of concentrations observed for stre- ambed sediment samples collected from eight sites along the Wolf River and its tributaries, although there are a few excep tions (Scudder and others, 1997; Gam and others, 2001). Table El contains a comparison of element concentrations in Neopit Mill Pond and other Wolf River tributaries, as well as consensus-based sediment guidelines for aquatic life (thresh old and probable effects concentrations, TEC and PEC, respec tively) for arsenic, cadmium, chromium, copper, lead, mer cury, nickel, and zinc (MacDonald and others, 2000). Concentrations of arsenic, copper, mercury, and nickel in all Neopit Mill Pond sediment samples were within the concentra tion range for Wolf River streambed sediment and below the TECs. Cadmium and zinc concentrations were slightly higher in Neopit Mill Pond than in Wolf River streambed sediment, and two samples (core 1 and core 7) had concentrations just above the TEC. A chromium concentration from a core 7 sample was above the range of concentrations from Wolf River streambed sediment and above the TEC. Lead concentrations were within the range of concentrations from Wolf River stre ambed sediment, but one sample from core 1 was above the lead TEC. All sediment concentrations were below the PECs for the same eight elements.
Organic Compounds
Several organic compounds were detected in Neopit Mill Pond (table Fl). Table F2 contains the list of organic
compounds that were analyzed for but not detected in the Neo pit Mill-Pond samples. Unlike minor and trace elements, these compounds were not analyzed previously by the USGS for streambed sediment at other sites in the Wolf River basin. The minimum reporting limits for some of the compounds are high because the sample size was smaller than the optimum sample size required by the laboratory (for example, fluorene). Detected concentrations are given as estimates if sample size was smaller than that required by the laboratory to meet quality-assurance guidelines.
Several of the organic compounds have sediment quality guidelines for aquatic life (Washington State, 1991; Persaud and others, 1993; Canadian Council of Ministers of the Envi ronment, 1999; MacDonald and others, 2000; Janisch and oth ers, 2002). The TECs and PECs for these compounds are listed in table 3. Janisch and others (2002) contains a compendium of TECs and PECs for PAHs and other organic compounds that are used to assess sediment quality in Wisconsin lakes and streams based on previous studies by Washington State (1991), Persaud and others (1993), Canadian Council of Ministers of the Environment (1999), and MacDonald and others (2000). In order to compare organic compounds to the TECs and PECs on a common basis, compound concentrations shown in table 3 are normalized to 1 percent total organic carbon. Samples from Neopit Mill Pond ranged from 18 to 29 percent organic carbon, which has a significant effect on lowering the normal ized concentrations (and potential toxicity) of some of the organic compounds to values below TECs and PECs.
Concentrations of four organic compounds in sediment were above the consensus-based sediment quality guidelines for aquatic life (table 3). Concentrations of acenapthene and acenapthylene were above the TEC in samples from cores 1 and 2. One sample from core 1 had a napthalene concentration slightly above the TEC. This same sample from core 1 had concentrations of pentachlorophenol almost twice that of the draft Wisconsin PEC from Janisch and others (2002). This sample came from the core interval of 0.50-0.55 ft, or an actual depth of 1.06-1.22 ft when corrected with core recovery ratio, and also contained the highest concentrations of acenaphthene, acenaphthylene, anthracene, benz[a]anthracene, benzo[a]pyrene, benzo[b]fluoranthene, benzo[ghi]perylene, benzo[k]fluoranthene, carbazole, chrysene, fluoranthene, indeno[l,2,3-cd]pyrene, naphthalene, phenanthrene, bis(2-ethylhexyl)phthalate, and di-n-butyl phthalate (table Fl). Although no sediment guidelines are available, p-cresol concentrations in the bottom of core 2 were over twice the concentrations in core 1 and the top of core 2, and in core 7 p-cresol concentrations were over 10 times higher than in core 1 (table Fl).
6 Sedimentation and Sediment Chemistry, Neopit Mill Pond, Menominee Indian Reservation, Wisconsin, 2001
Most of the organic compounds detected in sediment from the pond are polycyclic aromatic hydrocarbons (PAHs) and are found, along with a number of other organic com pounds, in creosote, a common wood preservative (Awata and others, 1998; Brooks, 2000). Creosote is a distillate derived from coal tar produced by the carbonization of coal, and con sists of at least 160 liquid and solid aromatic hydrocarbon compounds (Brooks, 2000). PAHs are also are released during forest fires and home wood burning and may be naturally found in high concentrations in peat. When released to water, many PAHs readily sorb to particulate matter and dissolved organic matter (Awata and others, 1998). The environmental fate of the compounds is determined by rates of adsorption, volatilization, and biodegradation. Some are carcinogenic, are listed by the Resource Conservation and Recovery Act (RCRA) as toxic hazardous waste, and may bioaccumulate in aquatic life. Some studies have shown that aquatic life and ani mals (including humans) may rapidly metabolize or excrete PAHs, thus confounding the relations between more persistent PAHs and biomagnification through the food chain (Brooks, 2000). Concentrations of the PAHs associated with wood pre servatives and burning would be expected to be highest in cores 1 and 2 near the lumber mill, because historically, wood preservatives were used at the lumber mill and the mill cur rently burns wood. It is not known why a sample from core 7 had higher concentrations of p-cresol than samples from cores 1 and 2.
Pentachlorophenol (penta) is another commonly used wood preservative that was used at the Neopit lumber mill in the 1970s. It is not thought to occur naturally (Brooks, 2000). Penta may be dissolved in water or sorb onto particulate mat ter. It degrades through chemical, microbiological, and photo chemical processes, thus the ultimate fate, toxicity, and bioac- cumulation potential are highly dependent on local physical, chemical, and biological conditions. The complex processes involved in the persistence of penta in sediment may be why only one sample from this study contained detectable concen trations of the preservative, and why it had elevated concentra tions. Alternatively, this sampled interval may represent the period when penta was used at the lumber mill. There seems to be more complexity to the spatial distribution of penta com pared to the distribution of PAHs detected in sediment from the mill pond. Dioxins and furans have been found in dis charges from other wood treatment facilities that used penta (Janisch and others, 2002). Samples were not analyzed for dioxin and furans in this study.
Additional analyses of organic compounds in sediment from Neopit Mill Pond are needed to better determine the spatial extent and concentration of PAHs, penta, and possibly other contaminants and byproducts that are associated with
wood preservatives. The possible occurrence of dioxin and furans needs investigation. The potential transport of organic compounds to the water column and aquatic life also needs investigation and fish tissue should be analyzed. It would also be helpful to have more information on the history of the wood preservatives used at the lumber mill.
Conclusions
The following conclusions can be made from this study of sedimentation and sediment chemistry at Neopit Mill Pond:
Combined information from transects, cores, and General Land Office Survey Notes were useful for reconstructing the pre-dam location of the West Branch of the Wolf River through Neopit Mill Pond. The probable pre-dam location of the channel was mapped by use of a combination of the above three sources of data. Core data indicated that pole soundings overestimated the depth to the pre-dam land surface (hard bottom) if pre-dam deposits were composed of peat or loamy sand.
Approximately 253 acre-ft (408,700 yds3) of sediment have been deposited in Neopit Mill Pond after the dam was constructed in 1907. Post-dam sediment is composed of organic-rich muck, on average about 1.2 ft thick. Post-dam sediment has a water content of about 79-93 percent and an organic matter content of about 35-58 percent. The mill pond contains about 38,000 tons (dry weight) of post-dam sediment. Large pieces of wood are abundant in the sedi ment, especially near the dam and lumber mill.
Elevated concentrations of polycyclic aromatic hydrocar bons (PAHs) associated with creosote and pentachlo- rophenol (both commonly used wood preservatives) were found in samples from three cores from Neopit Mill Pond. Trace-element concentrations were at or near background concentrations.
Further study is needed to identify the spatial extent and variability of the PAHs, pentachlorophenol, and other byproducts from wood preservatives. Potential effects of these contaminants on the water column and aquatic life need more investigation to guide future restoration efforts.
References Cited 7
References Cited
Awata, H., Bates, S., Knaub, D., and Popelka, R., 1998, Poly nuclear aromatic hydrocarbons: properties and environ mental fate an EXAMS model simulation: Environmental Engineering and Science, Clemenson University, accessed (2002) at URL http://entweb.clemson.edu/pesticid/docu- ment/leeorgl/leeorg4.htm.
Briggs, P.H., and Meier, A.L., 1999, The determination of forty two elements in geological materials by inductively coupled plasma-mass spectrometry: U.S. Geological Survey Open-File Report 99-0166, 15 p.
Brooks, K.M., 2000, Assessment of the environmental effects associated with wooden bridges preserved with creosote, pentachlorophenol, or chromated copper arsenate: U.S. Department of Agriculture, Forest Service, Forest Products Laboratory Research Paper FP-RP-587, 100 p.
Canadian Council of Ministers of the Environment, 1999, Canadian sediment quality guidelines for the protection of aquatic life: Winnipeg, Canadian Council of Ministers of the Environment Report.
Dean, W.E., Jr., 1974, Determination of carbonate and organic matter in calcareous sediments and sedimentary rock by loss on ignition comparison with other methods: Journal of Sedimentary Petrology, v. 44, p. 242-248.
Foreman, W.T., Connor, B.F., Furlong, E.T., Vaught, D.G., and Merten, L.M., 1995, Methods of analysis by the U.S. Geological Survey National Water Quality Labora tory determination of organochlorine pesticides and polychlorinated biphenyls in bottom sediment by dual capillary-column gas chromatography with electron-capture detection: U.S. Geological Survey Open-File Report 95-140, 78 p.
Furlong, E.T., Vaught, D.G., Merten, L.M., Foreman, W.T., and Gates, P.M., 1996, Methods of analysis by the U.S. Geological Survey National Water Quality Labora tory determination of semivolatile organic compounds in bottom sediment by solvent extraction, gel permeation, chromatographic fractionation, and capillary-column gas chromatography/mass spectrometry: U.S. Geological Survey Open-File Report 95-719, 67 p.
Garn, H.S., Scudder, B.C., Richards, K.D., and Sullivan, D.J., 2001, Characteristics of water, sediment, and benthic com munities of the Wolf River, Menominee Indian Reservation, Wisconsin, water years 1986-98: U.S. Geological Survey Water-Resources Investigations Report 01-4019, 54 p.
Jackson, L.L., Brown, F.W., and Neil, ST., 1987, Major and minor elements requiring individual determinations, classi cal whole rock analysis, and rapid rock analysis, in Bae- decker, P.A., ed., Methods for geochemical analysis: U.S. Geological Survey Bulletin 1770, p. G12-G17.
Jackson, L.L., Engleman, E.E., and Peard, J.L., 1985, Determi nation of total sulfur in lichens and plants by combustion- infrared analysis: Environmental Science and Technology, v. 19, p. 437-441.
Janisch, T., Liebenstein, L., Galarneau, S., and others, 2002, Consensus-based sediment quality guidelines; recommen dations for use and application: Madison, Wis., Wisconsin Department of Natural Resources WT-732-2002, February 2002, 32 p.
Krishnaswami, S., and Lal, D., 1978, Radionuclide limnochro- nology, in Lerman, A., ed., Lakes: Chemistry, Geology, Physics: Springer-Verlag, NY, p. 153-177.
MacDonald, D.D., Ingersoll, C.D., and Berger, T. A., 2000, Development and evaluation of consensus-based sediment quality guidelines for freshwater ecosystems: Archive of the Environmental Contamination Toxicologists, v. 39, p. 20-31.
Milfred, C.J., Olson, G.W., and Hole, F.D., 1967, Soil resources and forest ecology of Menominee County, Wis consin: University of Wisconsin, Geological and Natural History Survey, Soil Survey Division, Bulletin 85, Soil Series No. 60, Madison, Wis.., 203 p. and 3 plates.
Munsell Color, 1975, Munsell soil color charts, Baltimore, Munsell Color Division of Kollmorgen Corp., variable pagination.
Olsson, I.U., 1986, Radiometric dating, in Berglund, B.E., ed., Handbook of Holocene Paleoecology and Paleohydrology: Chichester, John Wiley and Sons, p. 273-312.
Persaud, D.R., Jaagumagi, R., and Hayton, A., 1993, Guide lines for the protection and management of aquatic sediment quality in Ontario: Toronto, Ontario Ministry of Environ ment and Energy Report, 27 p.
Pirkey, K.D., and Glodt, S.R., 1998, Quality control at the U.S. Geological Survey National Water Quality Laboratory: U.S. Geological Survey Fact Sheet FS-026-98, 6 p.
Scudder, B.C., Sullivan, D.J., Fitzpatrick, F.A., and Rheaume, S.J., 1997, Trace elements and synthetic organic compounds in biota and streambed sediment of the Western Lake Mich igan Drainages, 1992-1995: U.S. Geological Survey Water- Resources Investigations Report 97-4192, 34 p.
Soil Survey Staff, SCS, 1951, Soil Survey Manual, in USDA Agricultural Handbook No. 18.
Washington State, Department of Ecology, 1991, Sediment management standards: Washington State Department of Ecology, Chapter 173-204 WAC, 61 p.
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n 10
, (I)
cro
ss
sect
ion
11,
(J)
cros
s se
ctio
n 12
, (K
) cr
oss
sect
ion
13,
(L)
cros
s se
ctio
n 14
. D
ots
repr
esen
t so
undi
ng l
ocat
ions
, lin
es r
epre
sent
cur
rent
(20
01-2
002)
bot
tom
(so
ft bo
ttom
) an
d pr
e-da
m
(190
7) b
otto
m (
hard
bot
tom
).
Cro
ss s
ectio
n an
d co
re l
ocat
ions
are
sho
wn
on f
ig.
1.
EX
PL
AN
AT
ION
Sof
t bot
tom
gg]
Org
anic
-ric
h m
uck
Har
d bo
ttom
W
7^ S
and
xxxx
Woo
d
Bur
ied
soil
W
ater
sur
face
jo t
.
. I
['. ;'
.?j
San
d an
d gr
avel
Pea
t
NO
RTH
I cro
ss s
ectio
n 11
SO
UT
H1,
060
1,05
5
tH
1,05
0LJ
J
LU
Q Z) jE
1,04
5
1,04
0
1,03
5
Org
anic
-ric
h m
uck
Loam
y or
gani
c-ric
h m
uck
San
d an
d gr
avel
Org
anic
-r
Bar
k, l
ea\
Cla
yey
sa
h m
uck
s an
d tw
igs
d an
d gr
avel
, ro
ots
NA
TIO
NA
L G
EO
DE
TIC
VE
RT
ICA
L D
AT
UM
OF
192
9 V
ER
TIC
AL
SC
ALE
GR
EA
TLY
EX
AG
GE
RA
TE
D
500
1,00
0 1,
500
DIS
TA
NC
E F
RO
M L
EF
T R
EF
ER
EN
CE
PO
INT
, IN
FE
ET
(LO
OK
ING
DO
WN
ST
RE
AM
)
2,00
0
Figu
re 3
. G
eolo
gic
cros
s se
ctio
ns,
Neo
pit
Mill
Pon
d, N
ovem
ber
2001
thr
ough
Jul
y 20
02.
(A)
cros
s se
ctio
n 2,
(B
) cr
oss
sect
ion
3, (
C)
cros
s se
ctio
n 4,
(D
) cr
oss
sect
ion
5, (
E)
cros
s se
ctio
n 7,
(F)
cro
ss s
ectio
n 8,
(G
) cr
oss
sect
ion
9, (
H)
cros
s se
ctio
n 10
, (I)
cro
ss
sect
ion
11,
(J)
cros
s se
ctio
n 12
, (K
) cr
oss
sect
ion
13,
(L)
cros
s se
ctio
n 14
. D
ots
repr
esen
t so
undi
ng lo
catio
ns,
lines
rep
rese
nt c
urre
nt (
2001
-200
2) b
otto
m (
soft
botto
m)
and
pre-
dam
(1
907)
bot
tom
(ha
rd b
otto
m).
Cro
ss s
ectio
n an
d co
re lo
catio
ns a
re s
how
n on
fig
. 1.
EX
PL
AN
AT
ION
- S
oft
botto
m
- H
ard
botto
m-
Wat
er s
urfa
ce
Org
anic
-ric
h m
uck
San
d an
d gr
avel
Loam
y m
uck
Woo
d
1,06
0
1,05
5
ffi
1,05
0LL
NO
RTH
J cr
oss
sect
ion
12S
OU
TH
LU
Q D
1,04
5
1,04
0
1,03
5
rgsr
iic-r
ich
muc
k
^yrg
anic
-ric
h m
uck
Peat
ana
roo
tlets
Sand
Woo
dS
and
with
org
anic
laye
rsW
ood
Sand
, lo
am a
nd r
ootle
tsN
AT
ION
AL
GE
OD
ET
IC V
ER
TIC
AL
DA
TUM
OF
192
9 V
ER
TIC
AL
SC
ALE
GR
EA
TLY
EX
AG
GE
RA
TE
D
500
1,00
01,
500
2,00
0
DIS
TA
NC
E F
RO
M L
EF
T R
EF
ER
EN
CE
PO
INT
, IN
FE
ET
(LO
OK
ING
DO
WN
ST
RE
AM
)
Figu
re 3
. G
eolo
gic
cros
s se
ctio
ns,
Neo
pit
Mill
Pon
d, N
ovem
ber
2001
thr
ough
Jul
y 20
02.
(A)
cros
s se
ctio
n 2,
(B
) cr
oss
sect
ion
3, (
C)
cros
s se
ctio
n 4,
(D
) cr
oss
sect
ion
5, (
E)
cros
s se
ctio
n 7,
(F)
cro
ss s
ectio
n 8,
(G
) cr
oss
sect
ion
9, (
H)
cros
s se
ctio
n 10
, (I)
cro
ss
sect
ion
11,
(J)
cros
s se
ctio
n 12
, (K
) cr
oss
sect
ion
13,
(L)
cros
s se
ctio
n 14
. D
ots
repr
esen
t ~
so
undi
ng l
ocat
ions
, lin
es r
epre
sent
cur
rent
(20
01-2
002)
bot
tom
(so
ft bo
ttom
) an
d pr
e-da
m
(190
7) b
otto
m (
hard
bot
tom
). C
ross
sec
tion
and
core
loca
tions
are
sho
wn
on fi
g. 1
.
EX
PL
AN
AT
ION
Sof
t bo
ttom
£r^
Org
anic
-ric
h m
uck
FM
I S
and
xxxx
W
ood
chip
laye
r
Har
d bo
ttom
W
ater
sur
face
San
dy lo
am
Pea
t
1,05
5NO
RTH
cros
s se
ctio
n 1 3
L C
ross
sec
tion
14S
OU
TH
1,05
0
1,04
5
LLJ
LU LU §
1,04
0 t h-
1,03
5
1,03
0
Cor
es
. 2e
1,2e
2 /
I IV\
/I zH
$s?s
« -4
~ Lo
amy,
org
anic
-ric
h m
uck
XXXX
*= *-
>__
Larg
e w
ood
chun
ks
*x£
x* "
-CT
^ S
andy
org
anic
-ric
h m
uck,
roo
ts,
if*, f
^^ W
ood
cnun
kssj
rx-x
' ^"
"~~"
San
d, g
rave
l, an
d w
ood
chun
ks
e?£*
'- O
rgan
ic d
ebris
, ro
otle
ts
««x>
^~
-~- S
and,
gra
vel,
and
woo
d ,.\g
r' *
~^T
~- W
ood
and
sand
woo
d
r~ ,
?.
- ^7
'- S
and
and
grav
el
-t^Z
^--
Gra
velly
loam
with
woo
d, r
ootle
ts a
nd
^ S
andy
cla
y lo
am w
ith g
rave
l and
roo
tlets
Org
anic
-ric
h lo
amy
muc
k w
ith w
ood
chip
s "W
ood
chip
laye
r
500
0
DIS
TA
NC
E F
RO
M L
EF
T R
EF
ER
EN
CE
PO
INT
, IN
FE
ET
(LO
OK
ING
DO
WN
ST
RE
AM
)
Figu
re 3
. G
eolo
gic
cros
s se
ctio
ns,
Neo
pit
Mill
Pon
d, N
ovem
ber
2001
thr
ough
Jul
y 20
02.
(A)
cros
s se
ctio
n 2,
(B
) cr
oss
sect
ion
3, (
C)
cros
s se
ctio
n 4,
(D
) cr
oss
sect
ion
5, (
E)
cros
s se
ctio
n 7,
(F)
cro
ss s
ectio
n 8,
(G
) cr
oss
sect
ion
9, (
H)
cros
s se
ctio
n 10
, (I)
cro
ss
sect
ion
11,
(J)
cros
s se
ctio
n 12
, (K
) cr
oss
sect
ion
13,
(L)
cros
s se
ctio
n 14
. D
ots
repr
esen
t so
undi
ng l
ocat
ions
, lin
es r
epre
sent
cur
rent
(20
01-2
002)
bot
tom
(so
ft bo
ttom
) an
d pr
e-da
m
(190
7) b
otto
m (
hard
bot
tom
). C
ross
sec
tion
and
core
loca
tions
are
sho
wn
on fi
g. 1
.
500
NA
TIO
NA
L G
EO
DE
TIC
VE
RT
ICA
L D
ATU
M O
F 1
929
VE
RT
ICA
L S
CA
LE G
RE
ATL
Y E
XA
GG
ER
AT
ED
EX
PL
AN
AT
ION
Sof
t bo
ttom
H
ard
botto
m
Wat
er s
urfa
ce
San
d an
d gr
avel
San
d
\~^\
Org
anic
-ric
h m
uck
Loam
y m
uck
xxxx
Woo
d
Bur
ied
soil
horiz
on
[g^|
Org
anic
-ric
h lo
amy
muc
k
88°
51'
44°
59
44
°58
'
yr
,1.6
EX
PL
AN
AT
ION
Pos
t-dam
sed
imen
t th
ickn
ess
at c
ore
loca
tions
, in
fee
t
0.5 I
1 M
ILE
S
J
0.5
1 K
ILO
ME
TE
RS
Bas
e fr
om 1
:24,
000
U.S
. G
eolo
gica
l S
urve
y to
pogr
aphi
c m
ap,
Neo
pit Q
uadr
angl
e, 1
982,
T
owns
hip
29 N
orth
Figu
re 4
. Pos
t-da
m s
edim
ent t
hick
ness
at c
ore
loca
tions
, N
eopi
t Mill
Pon
d, N
eopi
t, 20
01.
Tabl
e 1.
Gen
eral
Lan
d O
ffice
Sur
vey
Not
es fr
om 1
854
for t
he N
eopi
t M
ill P
ond
area
[ft,
feet
; *,
cal
cula
ted
from
sur
vey
unit
of m
easu
re li
nks
whe
re 1
lin
k =
0.66
fee
t; --
, no
info
rmat
ion
give
n]
Sect
ion
line
T29N
, R14
E, s
ectio
ns 2
0 an
d 21
T29N
, R14
E, s
ectio
ns 1
9 an
d 20
T29N
, R14
E, s
ectio
ns 1
7 an
d 20
T29N
, R14
E, s
ectio
ns 1
8 an
d 19
T29N
, R13
E, s
ectio
n 24
, and
T29
N, R
14E,
Stre
am n
ame
Wes
t Bra
nch
Wol
f Riv
er
Wes
t Bra
nch
Wol
f Riv
er
Tour
tillo
tte C
reek
Wes
t Bra
nch
Wol
f Riv
er
Littl
e W
est B
ranc
h
Cha
nnel
w
idth
(ft*
)
108.
9
46.2 9.9
66.0
39.6
Cha
nnel
de
pth
(ft)
1-2
1-2 - 1-2
Stre
ambe
d _
, se
dim
ent
Rcm
arks
sand
y
--
sand
y
grav
elly
rapi
d cu
rren
t, hi
gh b
anks
sect
ion
19
T29N
, R13
E, s
ectio
n 13
, and
T29
N, R
14E,
se
ctio
n 18
Wes
t Bra
nch
Wol
f Riv
er39
.6
Tab
le 2
. Wor
kshe
et fo
r ca
lcul
atin
g vo
lum
e an
d w
eigh
t of
post
-dam
sed
imen
t in
Neo
pit
Mill
Pon
d [ft
, fe
et;
g, g
ram
; cm
, ce
ntim
eter
; Ib
s, p
ound
s]P
ost-
dam
M
ap
Sou
ndin
g A
vera
ge
sedi
men
t tr
anse
ct
tran
sect
tr
anse
ct
Tra
nsec
tT
rans
ect
num
ber
2 3 4 5 9 10 11 12 13 14
Tot
als
for
impo
undm
ent
Are
a (a
cres
)V
olum
e of
sed
imen
t (ft
3)V
olum
e of
sed
imen
t (a
cre-
ft)V
olum
e of
sed
imen
t (y
ds3)
Ave
rage
dry
bul
k de
nsity
(g/
cm3)
Ave
rage
dry
bul
k de
nsity
(Ib
s/ft3
) ,
Wei
ght o
f dry
sed
imen
t (to
ns)
dept
h (f
t)
wid
th (
ft)
wid
th (
ft)
wid
th (
ft)
leng
th (
ft)2.
02.
01.
61.
01.
80.
70.
71.
42.
32.
3
212
1 1
,034
,875
253
408,
699
0.11
04
6.89
338
,033
300
400
650
1,60
01,
700
1,90
01,
600
450
250
300
450
600
650
1,60
01,
800
na1,
550
500
250
300
375
500
650
1,60
01,
750
1,90
01,
575
475
250
300
463
513
850
975
1,22
51,
250
1,20
01,
175
725
450
Tra
nsec
tar
ea (
ft2)
173,
438
256,
250
552,
500
1,56
0,00
02
,14
3,7
50
2,3
75
,00
01,
890,
000
558,1
25
181,
250
135,
000
Isla
ndT
rans
ect
area
, no
Tra
nsec
tar
ea (
ft2)
is
land
s (f
t2)
volu
me
(ft3
)0 0
22,5
00 0
160,
000
225,0
00
200,0
00 0 0 0
173,
438
256,
250
530,
000
1,56
0,00
01,
983,
750
2,1
50
,00
01
,690
,000
558,
125
181,
250
135,
000
346,
875
512,
500
848,
000
1 ,56
0,00
03,
570,
750
1,50
5,00
01,
183,
000
781
,375
416,
875
310,
500
Tabl
e 3.
Org
anic
com
poun
ds d
etec
ted
in N
eopi
t M
ill P
ond
sedi
men
t (c
once
ntra
tions
nor
mal
ized
to
1 pe
rcen
t to
tal o
rgan
ic c
arbo
n) a
nd c
onse
nsus
-bas
edse
dim
ent q
ualit
y gu
idel
ines
[ft,
feet
; g,
gra
m;
kg, k
ilogr
am; |
ug, m
icro
gram
; E, e
stim
ated
; na
, not
ava
ilabl
e; U
SGS,
U.S
. Geo
logi
cal
Surv
ey. I
nter
val
top
and
botto
m d
epth
s ar
e no
t cor
rect
ed f
or r
ecov
ery
ratio
Thr
esho
ld a
nd p
roba
ble
effe
ct c
once
ntra
tions
are
fro
m J
anis
ch a
nd o
ther
s (2
002)
, w
hich
are
pri
mar
ily b
ased
on
guid
elin
es in
Mac
Don
ald
and
othe
rs (
2000
),C
anad
ian
Cou
ncil
of M
inis
ters
of t
he E
nvir
onm
ent (
1999
), Pe
rsau
d an
d ot
hers
(19
93),
and
Was
hing
ton
Stat
e (1
991)
.Pe
ntac
hlor
ophe
nol T
EC
s an
d PE
Cs
are
draf
t gu
idel
ines
.Se
e ta
ble
Fl
for
full
list o
f det
ecte
d co
mpo
unds
with
unn
orm
aliz
ed c
once
ntra
tions
.]
0) JD Ew
. 3
C
,2
3
'«C
CO
£ o
0
COO
D
lc
4458
5108
8495
000
lc
4458
5108
8495
000
lc
4458
5108
8495
000
lc
4458
5108
8495
000
2c
4458
5008
8495
600
2c
4458
5008
8495
600
7c
4459
0588
5127
00T
hres
hold
eff
ect
conc
entr
atio
nPr
obab
le e
ffec
t co
ncen
trat
ion
~f a o 4
-1^~ 5 0) 4-1
JC
0.00
0.05
0.50
0.55
0.10
0.15
0.20
E o "o JD 15 a> j: 0.05
0.10
0.55
0.60
0.15
0.20
0.30
T3 a O 0) JJJJJJ o o 0) 4-1 (Q 0
2/13
/200
12/
13/2
001
2/13
/200
12/
13/2
001
2/13
/200
12/
13/2
001
3/1/
2001
o> c o «5
O 0 'E «5 ff O JC 8 5 1 1 2 2 1
3 c o .Q (5 o 3 o h- 190
180
240
240
170
180
290
"o Q.
C
O fi (Q 0 O 'E (0 E? 6 18 18 23 24 17 18 29
o>
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*TTi
O
J «\
J £
c £
0>
J=a 5
"o
c>
R5 « o
ci j
=t a
na na 10 3 na na na na na
5* 1 0) c £ o 3 U. 7 7 na 6 na 10 na 77.4
536
1 0) c 0) 4-1 .c a (Q c a> < na 11 13 4 6 12 na 6.7 89
i 0) J9? .c 4-<
J= a (Q c a> < 18 49 55 17 29 51 na 5.9
128
I 0) c 0) o 15 4-< C < 6 9 18 6 6 7 na 57.2
845
s 1 0)
0) o 1 4-1 c (0 r i
.(C.
"N*
0) .a 8 9 30 9 7 7 7 108
1,05
0
f
1 0) c £ a trt
."*
. o N C 0) m 11 14 39 14 8 13 na 150
1,45
0
"3 I 0) c 0) .c E o 3 «*- A ?**. O N C 0) m 14 17 50 14 11 17 na 240
13,4
00
1 0) c JB £» 0)
£ !E . o N C 0) m 15 16 49 20 12 19 na 170
3,20
0
1 0) c 0) ^ 5 o H^ 2] "o* N c 0) CD na 3 27 11 2 6 na 240
13,4
00
3 1 0) c 0) (A JC O 5 10 36 11 4 7 7 166
1,29
0
Tabl
e 3.
Org
anic
com
poun
ds d
etec
ted
in N
eopi
t M
ill P
ond
sedi
men
t (c
once
ntra
tions
nor
mal
ized
to 1
per
cent
tota
l org
anic
car
bon)
and
con
sens
us-b
ased
sedi
men
t qua
lity
guid
elin
es C
ontin
ued
[ft,
feet
; g,
gra
m;
kg, k
ilogr
am;
jug,
mic
rogr
am;
E, e
stim
ated
; na
, not
ava
ilabl
e; U
SGS,
U.S
. G
eolo
gica
l Su
rvey
. In
terv
al t
op a
nd b
otto
m d
epth
s ar
e no
t cor
rect
ed f
or r
ecov
ery
rat
Thr
esho
ld a
nd p
roba
ble
effe
ct c
once
ntra
tions
are
fro
m J
anis
ch a
nd o
ther
s (2
002)
, w
hich
are
pri
mar
ily b
ased
on
guid
elin
es i
n M
acD
onal
d an
d ot
hers
(20
00),
Can
adia
n C
ounc
il of
Min
iste
rs o
f th
e E
nvir
onm
ent
(199
9), P
ersa
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nd o
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s (1
993)
, an
d W
ashi
ngto
n St
ate
(199
1).
Pent
achl
orop
heno
l T
EC
s an
d PE
Cs
are
draf
t gu
idel
ines
.Se
e ta
ble
Fl
for
full
list o
f de
tect
ed c
ompo
unds
with
unn
orm
aliz
ed c
once
ntra
tions
.]
l_
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32
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4458
5108
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5108
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Ic
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5108
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5108
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5008
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445850088495600
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resh
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effe
ct con
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onPr
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ect co
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ion
3 0) c 0) .c + » c (0 1_ 0 3 u. 19 39 100
30 26 28 11 423
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2 3 na na na na na na na
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22 24 16 5 8 18 22 na na
3 0) c 0) (0 £ * > a (0 z 78 172
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(0 c Q) £ Q. 28 72 106
31 24 46 na 204
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200
12,0
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3 1 "o c Q) £ Q. s o .c o (0 * > c Q) Q. na na 367
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200
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1 Q) + » JS (0 * > £ a 3
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200
1 7,000
3 JS (0 * > £ a £"S a na na na 4 5 na na 610
1,10
0
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869
293
280
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51 1.61
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23
Appendix Tables
24
Table A1 . Altitudes of land surface and hard and soft bottom and descriptive notes for transect 2.Based on survey and sounding data collected in 2001 and 2002.[ft, feet; LEW, left edge of water; REW, right edge of water]
Distance from left side (ft)
0.066.0129.0171.0219.0453.0
Altitude of soft bottom
(ft)
1,049.71,048.51,048.41,049.71,050.0
Altitude of hard bottom
(ft)1,050.01,044.41,046.51,044.91,045.11,050.0
DescriptionLEW
REW
25
Table A2. Altitudes of land surface and hard and soft bottom and descriptive notes for transect 3.Based on survey and sounding data collected in 2001 and 2002.[ft, feet; LEW, left edge of water; REW, right edge of water]
Distance from left side (ft)
0.00.02.411.072.6134.3195.9257.6319.2380.9442.5504.1565.8584.3642.5631.8631.8
Altitude of soft bottom
(ft)
1,048.81,049.31,047.61,049.21,049.31,049.21,049.01,049.31,049.41,048.0
Altitude of hard bottom
(ft)1,053.61,052.91,052.71,050.01,044.01,040.71,042.51,043.71,043.71,041.01,041.01,043.01,049.41,044.71,050.01,052.01,053.6
DescriptiontopofrebaratRP3-lground surface at RP3-1top of bankLEWfairly softvery soft (muck)in channelsolid bottomvery solid bottombottom becoming softer
hard bottomall gravel, old railroad bed
REWground and top of bank at RP3-2top of rebar at RP3-2
26
Table A3. Altitudes of land surface and hard and soft bottom and descriptive notes for transect 4.Based on survey and sounding data collected in 2001 and 2002.[ft, feet; LEW, left edge of water; REW, right edge of water]
Distance from left side (ft)
0.030.730.788.9147.1205.2263.4321.6379.8437.9496.1554.3612.5670.7692.3699.7728.7728.7
Altitude of soft bottom
(ft)
1,047.11,047.31,047.71,047.61,047.61,047.41,047.41,047.61,047.11,047.91,049.4
Altitude of hard bottom
(ft)1,053.21,052.71,050.11,040.81,041.11,041.01,041.61,041.51,040.61,041.31,042.11,042.31,043.91,045.81,050.11,052.01,052.61,053.3
DescriptiontopofrebaratRP4-ltop of bankLEW
REWtop of bankground at RP4-2topofrebaratRP4-2
27
Table A4. Altitudes of land surface and hard and soft bottom and descriptive notes for transect 5.Based on survey and sounding data collected in 2001 and 2002.[ft, feet; LEW, left edge of water; REW, right edge of water]
Distance from left side (ft)
0.00.013.4
103.4193.4283.5373.5463.5553.5643.5733.6823.6913.6
1,003.61,093.61,183.71,243.71,333.71,423.71,513.71,603.81,674.41,682.71,682.7
Altitude of soft bottom
(ft)
1,043.91,043.61,044.11,043.91,044.01,044.01,043.91,044.91,046.11,046.91,047.41,047.51,048.31,048.31,048.41,048.81,048.41,048.3
Altitude of hard bottom
(ft)1,054.01,053.71,049.91,040.11,039.91,040.41,040.41,040.91,040.71,038.91,039.71,041.21,042.61,043.41,043.91,040.81,044.01,042.01,042.51,043.81,045.91,049.91,053.61,054.0
DescriptiontopofrebaratRP5-lground surface at RP5-1 and top of bankLEWsoft
hard bottom
peaty layer
hard bottom
very softmore solid
hard brush layer (over old railroad bed)hard brush layer (over old railroad bed)REWground surface at RP5-2top of rebar at RP5-2
28
Table A5. Altitudes of land surface and hard and soft bottom and descriptive notes for transect 7.Based on survey and sounding data collected in 2001 and 2002.[ft, feet; LEW, left edge of water; REW, right edge of water]
Distance from left side (ft)
0.00.09.717.726.741.756.771.786.7101.7116.7131.7146.7161.7176.7176.7176.7
Altitude of soft bottom
(ft)
1,049.61,049.61,049.61,049.51,049.41,049.21,048.71,049.11,049.41,049.4
Altitude of hard bottom
(ft)1,056.21,054.61,052.31,050.41,048.31,048.61,049.41,048.71,049.01,048.51,048.51,048.91,048.31,048.81,050.41,053.61,054.6
DescriptiontopofrebaratRP7-lground surface at RP7-1top bankLEW
muck
sand bar in middlesand bar in middlegravelgravelgravelgravelREWtop of bankground surface at RP7-2
29
Table A6. Altitudes of land surface and hard and soft bottom and descriptive notes for transect 8.Based on survey and sounding data collected in 2001 and 2002.[ft, feet; LEW, left edge of water; REW, right edge of water]
Distance from left side (ft)
0.00.015.394.8198.6302.3406.0509.8613.5717.2820.9924.7
1,028.41,132.11,235.91,339.61,443.31,547.11,560.11,564.11,564.1
Altitude of soft bottom
(ft)
1,046.61,047.11,046.31,045.91,046.11,046.11,046.01,045.71,045.61,045.11,044.51,044.11,044.61,044.2
Altitude of hard bottom
(ft)1,054.11,052.81,050.11,041.01,044.51,040.61,040.11,040.91,041.21,040.81,041.81,042.51,040.31,040.01,040.91,039.81,040.61,050.11,053.01,053.31,054.1
DescriptiontopofrebaratRP8-lground surface at RP8-1LEWsoftmore solid bottomspongyspongy
spongyspongy
solidvery soft bottom
REWtop bankground surface at RP8-2topofrebaratRP8-2
30
Table A7. Altitudes of land surface and hard and soft bottom and descriptive notes for transect 9.Based on survey and sounding data collected in 2001 and 2002.[ft, feet; LEW, left edge of water; REW, right edge of water]
Distance from left side (ft)
0.00.011.0
100.3189.7279.0368.4457.7547.1636.4725.8815.1904.5993.8
1,083.21,172.51,261.91,351.21,440.51,529.91,619.21,708.61,797.91,822.71,837.71,837.7
Altitude of soft bottom
(ft)
1,049.61,048.41,046.51,047.41,046.21,045.91,046.01,044.81,044.51,044.21,044.21,043.91,042.91,043.51,043.91,044.41,044.61,044.91,045.41,047.4
Altitude of hard bottom
(ft)1,053.51,052.91,049.91,045.41,040.41,041.81,041.81,042.91,041.91,041.81,041.81,040.31,040.91,039.41,039.31,039.91,039.81,040.01,039.31,040.61,037.91,042.81,043.81,049.91,052.41,053.5
DescriptiontopofrebaratRP9-lground surface at RP9-1 and top of bankLEWvery softspongysolid (gravel)
very solid (sand)
stopped, very solidsolid stopspongyspongysoft
solidsoft(peat like bottom)spongy
very softsandy-gravel
REWground surface at RP9-2topofrebaratRP9-2
31
Table A8. Altitudes of land surface and hard and soft bottom and descriptive notes for transect 1 0.Based on survey and sounding data collected in 2001 and 2002.[ft, feet; LEW, left edge of water; REW, right edge of water]
Distance from left side (ft)
0.00.02.623.469.8116.2162.6208.9255.3301.7348.1394.5440.9487.3533.6533.6539.9541.9541.9
Altitude of soft bottom
(ft)
1,048.51,047.91,050.01,043.91,041.91,041.41,041.91,041.41,042.41,043.91,046.8
Altitude of hard bottom
(ft)1,056.41,055.41,053.71,050.41,045.21,043.21,049.91,040.31,039.71,039.41,040.21,039.11,039.11,040.21,044.41,050.41,052.91,054.41,055.7
DescriptiontopofrebaratRPlO-1ground surface at RP10-1top of bankLEW
REWtop of bankground surface at RP10-2topofrebaratRP10-2
32
Table A9. Altitudes of land surface and hard and soft bottom and descriptive notes for transect 1 1 .Based on survey and sounding data collected in 2001 and 2002.[ft, feet; LEW, left edge of water; REW, right edge of water]
Distance from left side (ft)
0.00.01.55.0
94.1183.2272.3361.3450.4539.5628.6717.7806.8895.9
1,014.61,133.41,252.21,371.01,489.81,549.21,569.21,572.21,580.71,580.7
Altitude of soft bottom
(ft)
1,042.21,041.11,041.31,041.91,042.61,042.01,042.91,042.81,046.31,048.31,048.31,047.41,047.71,048.91,048.9
Altitude of hard bottom
(ft)1,055.41,055.41,051.21,050.31,041.01,038.41,039.01,041.21,041.71,040.41,038.91,039.11,044.81,046.11,046.41,044.51,045.31,047.21,046.91,050.31,052.31,052.91,054.41,055.8
DescriptiontopofrebaratRPll-1ground surface at RP1 1-1 (boulder)bottom of slopeLEW
REWold shoreline
ground surface at RP1 1-2topofrebaratRPll-2
33
Table A10. Altitudes of land surface and hard and soft bottom and descriptive notes for transect 12.Based on survey and sounding data collected in 2001 and 2002.[ft, feet; LEW, left edge of water; REW, right edge of water]
Distance from left side (ft)
0.00.02.34.812.842.672.4102.2132.0161.8191.6221.4
Altitude of soft bottom
(ft)
1,045.31,043.11,042.71,042.51,041.81,041.61,040.4
251.2 | 1,039.6281.0310.8340.6370.4400.2430.0459.8489.6525.3552.2565.2566.2567.7567.7
1,039.41,041.51,041.91,043.21,044.01,044.01,044.11,045.21,048.1
Altitude of hard bottom
(ft)1,055.81,055.61,055.21,051.21,050.31,042.41,041.61,041.21,041.31,038.81,038.21,038.51,037.81,036.91,040.31,039.91,041.01,041.91,042.21,042.51,043.41,047.51,050.31,051.61,052.61,052.91,053.4
DescriptiontopofrebaratRP12-lground surface at RP 12-1top of left slopebottom of bankLEW
REWold shoreline bottomold shoreline topground surface at RP12-2topofrebaratRP12-2
34
Table A1 1 . Altitudes of land surface and hard and soft bottom and descriptive notes for transect 13.Based on survey and sounding data collected in 2001 and 2002.[ft, feet; LEW, left edge of water; REW, right edge of water]
Distance from left side (ft)
0.00.07.0
24.469.5104.2138.9173.6208.3236.0251.0251.0
Altitude of soft bottom
(ft)
1,041.91,040.41,038.81,040.61,042.41,042.7
Altitude of hard bottom
(ft)1,053.31,053.31,049.91,038.11,039.21,035.91,038.01,038.01,038.51,049.91,051.91,052.2
DescriptiontopofrebaratRP13-lground surface at RP13- 1LEWvery sudden hardvery soft, firm stopvery soft, firm stopvery soft, firm stopvery solid bottom
REWground surface at RP13-2topofrebaratRP13-2
35
Table A12. Altitudes of land surface and hard and soft bottom and descriptive notes for transect 14.Based on survey and sounding data collected in 2001 and 2002.[ft, feet; LEW, left edge of water; REW, right edge of water]
Distance from left side (ft)
0.00.07.039.371.6103.8136.1168.4200.7233.0265.2300.2308.2308.2
Altitude of soft bottom
(ft)
1,043.41,041.41,040.41,039.31,040.31,040.21,040.51,042.1
Altitude of hard bottom
(ft)1,053.91,052.91,049.91,039.91,038.21,037.91,037.81,037.51,036.61,037.21,039.71,049.91,051.81,052.3
DescriptiontopofrebaratRP14-lground surface at RP14-1LEWbarky layer then hardvery soft, firm stopvery soft, firm stopvery soft, firm stopvery soft, firm stopslight middle resistace layervery soft, firm stopvery soft, firm stopREWground surface at RP14-2topofrebaratRP14-2
Tab
le B
1 . C
ore
desc
riptio
ns f
or c
ore
1 at
cro
ss s
ectio
n 1 4
, ap
prox
imat
ely
1 35
ft fr
om l
eft
edge
of
wate
r an
d rig
ht e
dge
of w
ater
.C
ore
loca
tion
is 4
4°,
58.8
44';
88°,
49.
838'
.I
[ft, f
eet;
in.,
inch
; v.,
very
; f.,
fine
; m
., m
ediu
m;
c.,
coar
se;
occa
s.,
occa
sion
al]
! I
Core
1 a
co
llect
ed
on
2/1
3/01
with
a p
isto
n c
ore
rW
ate
r d
ep
th =
9.8
5 ft
jC
ore
de
pth
= 0
to 0
.9 ft
jC
orr
ect
ed
R
eco
very
j
Alti
tude
Dep
th (
ft)
de
pth
(ft
)*
ratio
I
(ft)
**0
I 0.
0 1.
6 !
1,04
0.5
0.45
j
0.7
| 1,
039.
70.
55
| 0.
9 |
1,03
9.6
1 1
Cor
e 1b
co
llect
ed
on
2/1
3/01
with
a p
isto
n c
ore
rW
ate
r d
ep
th =
10.
1 ft
|C
ore
de
pth
= 0
to 0
.9 ft
i1
Co
rre
cte
d
Reco
very
j
Alti
tude
Dep
th (
ft)
[ d
ep
th (
ft)*
ra
tio
| (f
t)**
6 |
6.0
| 1.
5 j
1,04
0.2
0.6
I 0.
9 1
1,03
9.3
~~
~~
H ~
n~
~~
T~
~~
~C
ore
1c c
olle
cted o
n 2
/13/
01 w
ith a
pis
ton c
ore
rW
ate
r d
ep
th =
9.8
ft
[C
ore
de
pth
= 0
to 1
.7 ft
jC
orr
ect
ed
R
eco
very
j
Alti
tude
Dep
th (
ft)
de
pth
(ft)*
ra
tio
[ (f
t)**
6 I
6.6
| 2.
1 1
1,04
0.5
0.8
! 1.
7 1
1,03
8.8
..........
..........
. .........
. ^-^^^^^. ----^-^^^^
..........
.
*Dep
th c
orre
cted
with
rec
over
y ra
tios
j
Desc
riptio
n3
ft n
orth
of c
ore
1m
uck
and
sand
, hom
ogen
ous
10Y
R2/
1 , w
ood
chip
s co
mm
onsa
me,
woo
d ch
ips
abun
dant
, mor
e sa
nd, l
ess
muc
k, 1
0YR
2/1
...
......
..
...
......
..._.
......
.....
......
......
......
.. ...
......
......
.....
..^. ,
...
....
, ..
....
..,_
.., .
......
......
......
......
......
......
. ..
...
_ .
..._.
......
......
......
......
......
......
......
......
.....
......
. ....
....
....._
......
._...
......
......
....
......
. ...
. ...
... .
.. ...
...
... .
......
......
Desc
riptio
n3
ft e
ast o
f core
lsu
bsam
pled
for t
race
ele
men
ts
Desc
riptio
n6ft e
ast o
f cor
e 1
subs
ampl
ed fo
r org
anic
che
mic
als
|**
Alti
tude
ass
umed
fro
m w
ater
leve
l at t
rans
ect
12 a
nd g
iven
wat
er d
epth
Tab
le B
2. C
ore
desc
ript
ions
for
cor
e 2
at c
ross
sec
tion
1 3,
appr
oxim
atel
y 96
ft f
rom
lef
t edg
e of
wat
er a
nd 1
08
ft fr
om r
ight
edg
e of
wat
erC
ore
loca
tion
is 4
4°, 5
8.83
8';
88°,
49.
931'
.[ft
, fee
t; in
., in
ch; v
, ver
y; f.
, fin
e; m
., m
ediu
m;
c., c
oars
e; o
ccas
., oc
casi
onal
]
IC
ore
2a c
olle
cted
2/1
3/01
with
a p
isto
n co
rer
Wat
er d
epth
= 9
.25
ft (lo
g on
top)
Har
d bo
ttom
= 1
1 .8
ftC
ore
dept
h =
0 to
1 .3
ft
jC
orre
cted
i
Rec
over
y
6 1
0.0
2.6
0.5
1.3
! |
! j
Alti
tude
(ft)
Des
crip
tion
1,04
1.1
13 f
t so
uth
of c
ore
21 ,
039.
8 ! s
ampl
e fe
ll o
ut o
f tu
be-
muc
k, s
and
and
woo
d co
mm
on, l
iqui
fied
Cor
e 2b
col
lect
ed 2
/13/
01 w
ith a
pis
ton
core
rW
ater
dep
th =
10 ft
|
Cor
e de
pth
= 0
to 1
.3 ft
Cor
rect
ed
Rec
over
y D
epth
(ft)
dept
h (ft
)*
ratio
OJ
0.0
5.2
0.25
! 1.
3
Alti
tude
(ft)
1 D
escr
iptio
n1,
041.
1 j3
ft n
orth
of c
ore
21,
039.
8 H
ost s
ome
sam
ple
from
the
top,
sub
sam
pled
eve
ry 0
.5 in
. for
trac
e el
emen
ts
Cor
e 2c
col
lect
ed 2
/14/
01 w
ith a
pis
ton
core
r j
Wat
er d
epth
= 1
0 f
tC
ore
dept
h =
0 to
1 .2
ft
Cor
rect
ed
Rec
over
y
0 0.
0 4
0.3!
1.
2j
i
Alti
tude
(ft)
j D
escr
iptio
n1,
041.
1 16
ft w
est o
f cor
e 2
1 ,03
9.9
1 sub
sam
pled
for o
rgan
ic c
hem
ical
s
Cor
e 2d
1 co
llect
ed 3
/9/0
1 w
ith a
9 eo
pro b
e co
rer
{W
ater
dep
th =
1 0
ftH
ard
botto
m =
11.
5 ft
Cor
e de
pth
= 0
to 4
.0 ft
j
Cor
rect
ed
Rec
over
y D
epth
(ftL
_ de
pth
(ft)*
ra
tio0!
0.
0!
2.5
6.9!
2.
3!
1.3
3.3
1.6J
4.
0
. ....
. i I
Alti
tude
(ft)
Des
crip
tion
1,04
0.3!
1,03
8.1
jloam
y sa
ndy,
org
anic
-ric
h m
uck
with
woo
d ch
ips
at b
ase,
unk
now
n sm
ell,
10Y
R2/
1 (s
harp
bou
ndar
y)po
orly
sor
ted
m.
sand
with
com
mon
bar
k w
ood
piec
es ~
1",
som
e 3
mm
lam
inat
ion
of o
rgan
ic m
atte
r fro
m 0
.75-
1. 00
ft,
f. gr
avel
inc
reas
es a
t 1,
037.
1 ba
se,
10Y
R4/
2 (m
oder
ate b
ound
ary)
1,03
6.3
jpoo
rly s
orte
d m
. to
v.c.
san
d w
ith (
-40
perc
ent)
pea
grav
el a
nd g
rave
l up
to 1
", ro
unde
d, 1
0YR
3/2
CJ
00
Tab
le B
2. C
ore
desc
ript
ions
for c
ore
2 at
cro
ss s
ectio
n 13
, app
roxi
mat
ely
96 ft
from
left
edge
of w
ater
and
108
ft f
rom
rig
ht e
dge
of w
ater
C
ontin
ued
Cor
e lo
cati
on i
s 44
*. 5
8.83
8';
88°,
49.
931
'. [
[ft, f
eet;
in.,
inch
; v.,
very
; f.,
fine;
m.,
med
ium
; c.,
coar
se; o
ccas
., oc
casio
nal]
! I
Cor
e 2e
1 , c
olle
cted
3/9
/01
with
a g
eopr
obe
core
rW
ater
dep
th =
10
ft
jC
ore
dept
h =
1 .0
to 5
.0 ft
\
Dep
th (
ft)0
0.35 0.
60.
75 1.1
Cor
rect
ed
| R
ecov
ery
dept
h (f
t)"
ratio
0.0
1.3
2.2
3.6
2.7
4.0
Alti
tude
(ft)
Des
crip
tion
1,03
9.3;
1,03
8.0
1,03
7.1
muc
k, o
rgan
ic ri
ch m
uck,
san
d gr
adua
lly in
crea
sing
tow
ard
base
, 10Y
R3/
2, la
rge
chun
ks o
f woo
d at
0.3
5 ft
loam
y- sa
nd o
rgan
ic-r
ich
muc
k, s
and
incr
easi
ng to
war
d ba
se, 1
OY
R3/2
, sm
all p
iece
s of
woo
d, c
hips
, mor
e bro
wn
than
abo
ve, r
oots
abu
ndan
t1,
036.
6 [w
ood
piec
es in
loam
y- sa
nd o
rgan
ic-r
ich
muc
k, 1
0YR
3/2
(abr
upt b
ound
ary)
1,03
5.3
Cor
e 2e
2 co
llec
ted
3/9/
2001
with
geo
prob
e co
rer
Wat
er d
epth
s 10
ftC
ore
dept
h =
5.0
to 9
.0 ft
Dep
th (
ft)0
0.15
0.45 0.5
0.55
0.65 0.
70.
750.
95
11.
4
Cor
rect
ed
dept
h (ft
)* 0.0
6.4
1.3
1.4
1.6
1.9
2.0
__________._
__..__
Rec
over
y ra
tio2.
9
.
2.7
2.9
4.6
1_
_*D
epth
cor
rect
ed w
ith re
cove
ry ra
tios
Alti
tude
(ft)
1,03
5.3
1,03
4.9
1,03
4.0
1,03
3.9
1,03
3.7
1,03
3.5
1,03
3.3
1,03
3.2
1,03
2.6
1,03
2.5
1,03
1.3
poor
ly s
orte
d, m
. to
v. c.
sand
and
gra
vel u
p to
0.5
" ab
unda
nt p
ink
feld
spar
, woo
d co
mm
on, 1
.5 in
. pie
ce o
f woo
d, 2
.5Y
4/2
Des
crip
tion
grav
el a
nd c
hunk
s of
bar
k an
d w
ood
(mod
erat
e bo
unda
ry)
wel
l sor
ted
m.
sand
, 2.
5YR
5/2
(gra
dual
bre
ak)
grav
el a
nd p
oorl
y so
rted
c.
sand
, 2.
5Y4/
2 (a
brup
t bou
ndar
y)1m
m o
rgan
ic d
ebri
s la
yer p
lus
root
lets
, 10
YR
2/1
(abr
upt b
ound
ary)
m. t
o c.
san
d, o
ccas
iona
l 1/
4" f
elds
par p
ebbl
es, 2
.5Y
3/2
(mod
erat
e w
ith 1
/4"
woo
dchi
p la
yer)
mai
nly
1/4"
bar
k w
ith s
and,
10Y
R3/
1 (m
oder
ate)
m.
to c
. sa
nd, 2
.5Y
4/2
(abr
upt b
ound
ary)
mor
e gr
ay m
. to
c. sa
nd w
ith f
elds
par p
ebbl
es (
-1/4
"), c
omm
on ro
otle
ts, o
ccas
iona
l sm
all b
ark
piec
es, 2
.5Y
3/2
( abr
upt b
ound
ary)
orga
nic
rich
loam
with
occ
as.
1/4"
woo
d ch
ips,
abu
ndan
t roo
tlets
, 1/
4" p
ebbl
es c
omm
on, (
old
A h
oriz
on??
) so
ft,
10Y
R2/
1 (a
brup
t bou
ndar
y)sa
ndy
clay
loam
with
-20
% g
rave
l, po
orly
sor
ted
but u
p to
3/4
" di
amet
er,
occa
s. r
ootle
ts,
10Y
R4/
1
....
.. .
..
........
.......
... ....
......
. .
__.
..........
..........
..........
.......
.........
Tab
le B
3. C
ore
desc
ript
ions
for c
ore
3 at
cro
ss s
ectio
n 1 2
, app
roxi
mat
ely
1 91
ft fr
om le
ft ed
ge o
f wat
er.
Cor
e lo
cati
on i
s 44
1, 58
.879
'; 88
°, 5
9.12
7'.
][ft
, fee
t; in.
, inc
h; v
., ve
ry; f
., fin
e; m
., m
ediu
m; c
., co
arse
; occ
as.,
occa
siona
l]
I I
Cor
e 3a
col
lect
ed 3
/1/2
001
with
a p
isto
n co
rer
Wat
er d
epth
= 8
.0 f
eet
Cor
e de
pth
= 0.
0 to
1 .6
ft
Dep
th (
ft)0
0.2
0.8
1.1
Cor
rect
ed
dept
h (ft
)* 0.0
0.3
1.2
1.6
Rec
over
y ra
tio1.
5
Cor
e 3b
col
lect
ed 3
/9/2
001
with
a g
eoW
ater
Dep
th =
8.0
fee
tC
ore
dept
h =
0.0
to 4
.0 f
t
Dep
th (
ft)0
0.2
0.3
0.65
0.85
1.15
1.25 1.
41.
51.
55 i.7 1.8
Cor
rect
ed
dept
h (f
t)* 0.0
0.4
0.7j
1.4
1.9
2.6
2.8
3.1
3.3
3.4
3.8
4.0
Rec
over
y ra
tio2.
2
*Dep
th c
orre
cted
with
rec
over
y ra
tios
Alti
tude
(f
t)1,
042.
31,
042.
0
1,04
1.1
1,04
0.7
prob
e
Alti
tude
..........
....(ft).
..........
.....1,
042.
31,
041.
91,
041.
61,
040.
91,
040.
41,
039.
81,
039.
51,
039.
21,
039.
01,
038.
91,
038.
51,
038.
3
Des
crip
tion
3 ft
sou
th o
f site
loca
tion
orga
nic
fluf
f, hi
gh w
ater
con
tent
, 10
YR
2/1
orga
nic-
rich
muc
k, 1
0YR
2/1,
1 i
n. b
ark
piec
es to
war
ds b
ase
com
mon
, silt
loam
orga
nic
rich
muc
k, 1
-3"
abun
dant
larg
e ba
rk p
iece
s, 1
0YR
2/1,
leav
es c
omm
on,
silt
loam
to lo
am, s
and
cont
ent i
ncre
ases
tow
ard
the
base
Des
crip
tion
orga
nic-
rich
muc
k, f
luff
y, n
o vi
sibl
e pi
eces
of o
rgan
ic m
ater
ial,
very
pun
gent
sm
ell,
5 Y3/
2 (g
radu
al b
ound
ary)
larg
e pi
ece
of b
ark
in o
rgan
ic-r
ich
muc
k, 1
0YR
2/2
(gra
dual
bou
ndar
y)or
gani
c-ri
ch m
uck,
bro
wni
sh,
1 OY
R2/
2 (m
oder
ate
boun
dary
)pe
at, b
row
nish
, loa
my
muc
k, o
rgan
ic-r
ich,
abu
ndan
t roo
tlets
, roo
t mas
s, b
urie
d A
hor
izon
? (m
oder
ate
boun
dary
)po
orly
sor
ted
f. to
rn,
sand
, 10Y
R3/
2 (m
oder
ate
boun
dary
)la
rge
chun
k of
woo
d w
ith f.
to m
. sa
nd m
atri
x, ro
otle
ts 1
0YR
3/1
(mod
erat
e bou
ndar
y)c.
to
v.c.
san
d, p
oorl
y so
rted
with
dar
k or
gani
c m
atte
r, 1
0YR
4/1
(gra
dual
bou
ndar
y)po
orly
sor
ted
m.
sand
with
1/8
" or
gani
c la
min
atio
n, s
and
10Y
R4/
2, o
rgan
ic la
min
atio
n 10
YR
2/1
(mod
erat
e bou
ndar
y)1/
4" w
ood
chun
k, d
ark
on o
utsi
de, s
mal
ler c
hunk
s of
woo
d, 1
0YR
2/1
(sha
rp b
ound
ary)
poor
ly s
orte
d lo
amy
m. t
o f.
sand
, occ
asio
nal r
ootle
ts,
10Y
R3/
1 (m
oder
ate
boun
dary
)si
lt lo
am, u
noxi
dize
d, ra
re ro
otle
ts, 2
.5Y
3/2
Tab
le B
4. C
ore
desc
riptio
n fo
r co
re 4
at c
ross
sec
tion
1 1 ,
appr
oxim
atel
y 1 ,
200
ft fr
om le
ft ed
ge o
f wate
r and
354
ft
from
rig
ht e
dge
of w
ater
.
[ft, f
eet;
in.,
inch
; v
, ver
y; <
., fin
e; m
., m
ediu
m;
c., c
oars
e; o
ccas
., oc
casi
onal
]
Cor
e 4b
col
lect
ed 3
/1/2
001
with
a p
isto
n co
rer
Wat
er d
epth
= 3
.7 ft
....
........
........
........
.......,
........
.._H
ard
bott
om =
4.7
ft
thro
ugh
grav
el a
nd w
eeds
jC
ore
dept
h =
0.0
to 1
.0 ft
|
,.... , .. ,. . ......-
, ^
mm
mm
m^
m.m
..m.m
mnm
m,m
^,^
^..
..»
..^
Cor
rect
ed
Dep
th (
ft)
dept
h (f
t)*
Rec
over
y j
Alti
tude
ratio
(ft)
Des
crip
tion
........
0.0.
40.
31,
046.
3 jo
rgan
k m
uck,
si
l.l
0.7
l,045
.9jo
rgai
ucin
iiack
;^i].
tloam
, in
c^1 ,
045 .
6 j s
and
and
grav
el, 0
. lia
, 1 O
YR
3/3,
top
of u
nit m
arks
pre
-dam
bou
ndar
y ___
____
_1.
6J1.
0*D
epth
cor
rect
ed w
ith re
cove
ry ra
tios
Tab
le B
5. C
ore
desc
ript
ion
for c
ore
5 at
cro
ss s
ectio
n 1 1
, ap
prox
imat
ely
500
ft fr
om le
ft ed
ge o
f wat
er a
nd 6
99 ft
fro
m c
ore
4.[ft
, fee
t; in
., in
ch; v
., ve
ry; f
., fin
e; m
., m
ediu
m;
c., c
oars
e; o
ccas
., oc
casi
onal
]
i I
IC
ore
5a c
olle
cted
3/1
/200
1 w
ith a
pis
ton
core
rW
ater
dep
th =
7.5
ft
jH
ard
bott
om =
9.0
ft
{C
ore
dept
h =
0.0
to 1
.2ft
Dep
th (
ft)0
0.4
0.7
1.4
Cor
rect
ed !
Rec
over
y de
pth
(ft)*
| ra
tio6.6
i 6.9
0.3
i6.
6! 1.2!
* Dep
th c
orre
cted
with
rec
over
y ra
tios
Alti
tude
(f
t)1,
042.
81,
042.
41,
042.
2
1,04
1.6
Des
crip
tion
3 ft
sou
th o
f cor
e 5
orga
nic
muc
k, s
ilt, s
ilt-l
oam
, 10
YR
2/1
orga
nic
muc
k w
ith b
ark,
leav
es a
nd tw
igs,
silt
loam
, 10
YR
2/1
(sha
rp b
ound
ary)
clay
ey s
and
and
grav
el, 0
.5 in
. , ro
ots
com
mon
, loa
my
sand
, gra
vel c
omm
on, 2
.5 Y
R4/
2, tw
o cl
ayey
loam
lens
es a
bout
0.0
5 ft
thic
k
Tab
le B
6. C
ore
desc
riptio
ns for
core
6 a
t cr
oss
sect
ion
9, a
ppro
xim
atel
y 1 ,
440
ft fr
om le
ft ed
ge o
f wat
er_a
nd^_
65_f
tjrom
rig
ht
Cor
e lo
catio
n is
44"
, 59
.098
'; 88
°, 5
0.96
7'.
|[ft
, fee
t; in
., in
ch;
v., v
ery;
f.,
fine;
m.,
med
ium
; c.
, coa
rse;
occ
as.,
occa
sion
al]
9.9 r
6...6.3
..??.
!!?.?
!?^
on[^
J^
^^
^^
J^
^o
njD
ore
rW
ater
Dep
th =
5.6
ft
HjitM
bw
tto
n ^
JO
^__
t C
ore
dept
h =
0.0
to 3
.0 ft
jI
Cor
rect
ed
j Rec
over
y D
epth
(ft
) I
dept
h (f
t)*
ratio
Alti
tude
(f
t)D
escr
iptio
nO
j__
!1.
7
0.0 _. 3.0
3 ft
sou
th o
f cor
e 6
! org
anic
muc
k, h
igh
wat
er c
onte
nt, a
quat
ic v
eget
atio
n m
atte
r com
mon
, gra
ss b
lade
s, r
ootle
ts, m
aybe
wild
rice
, si
lt or
gani
cs, l
ow
1,04
1.3
i sed
imen
t con
tent
, mos
tly o
rgan
ics,
10Y
R2/
1
9.9r
.e.. 6.
9. 99
!!®9J
*i*?.
on
3/2/
2001
with
a p
isto
n co
rer
Wat
er d
epth
= ,
^ou
^5^
^
............
............
............
............
......
Har
d bo
ttom
= a
bout
10.
0 ft
1.7|
1,
044.
3 3
ft e
ast o
f cor
e 6
0.9!
1.5
.l.>P
^;i.l
.E!!
}s.:
¥^^
Cor
e 6d
col
lect
ed o
n 3/
2/20
01 w
ith a
pis
ton
core
r W
'ate
7'd'
e'pt
h""^
ab'o
'ui5
'jft''
"""
""""""
""j" - - p
-
Har
d bo
ttom
= a
bout
10.
0 ft
Cor
e de
pth
= 0.
0 to
1.5
ft
Dep
th (
ft)
Cor
rect
ed
dept
h (f
t)*
Rec
over
y i
Alti
tude
ra
tio
I (f
t)D
escr
iptio
n0
O.O
j1.
71
1,04
4.3
i 6 f
t nor
th o
f cor
e 6
1,04
2.8
[sub
sam
pled
for
org
anic
che
mic
als
ever
y 0.
1 ft
fro
m 0
.2-0
.7 f
t
Tab
le B
6. C
ore
desc
ript
ions
for c
ore
6 at
cro
ss s
ectio
n 9,
app
roxi
mat
ely
1 ,44
0 ft
from
left
edge
of w
ater
and
865
ft fr
om r
ight
edg
e of
wat
er C
ontin
ued
Cor
e lo
catio
n is
44°
, 59
.098
'; 88
°, 5
0.96
7'.
|[ft
, fee
t; in.
, inc
h; v.
, ver
y; f.
, fin
e; m
., m
ediu
m; c
., co
arse
; occ
as.,
occa
sion
al]
!___
1__
_C
ore
6e c
olle
cted
on
3/9/
2001
with
a g
eopr
obe
core
rW
ater
dep
th =
abo
ut 5
.6 ft
j
jH
ard
botto
m =
abo
ut 1
0.0
ft
j j
Cor
e de
pth
= 0.
0 to
4.0
ft j
Dep
th (
ft)0
0.3
0.7
Cor
rect
ed
dept
h (f
t)* 0.0
0.6
1.4
Rec
over
y ra
tio2.
0
6.9J
l.
§|
1.45 1.
51.
61.
71.
83 2
2.9
3.0
13.
23.
4
iA
ltitu
de j
(ft)
Des
crip
tion
1,04
4.3
1,04
3.7
1,04
2.9
1,04
2.5
1,04
1.4
1,04
1.3
1,04
1.1
| 1,
040.
93.
7 1
4.0
orga
nic-
rich
muc
k, f
luff
, fin
e-gr
aine
d, n
o vi
sibl
e or
gani
c m
atte
r, 1
0YR
2/2,
org
anic
sm
ell,
(abr
upt b
ound
ary)
larg
e pi
eces
of w
ood/
bark
(up
to 2
"+)
with
muc
k m
atri
x 10
YR
2/1,
slig
ht p
unge
nt s
mel
l, (m
oder
ate
boun
dary
)or
gani
c m
atte
r with
abu
ndan
t sm
all w
ood
chip
s -1
/4",
10Y
R2/
2, o
rgan
ic s
mel
l, (m
oder
ate
boun
dary
)f.
sand
y lo
am to
loam
y m
. sa
nd,
occa
s. 1
/4"
woo
d ch
ips,
occ
as.
gras
s bl
ades
1/1
6" w
ide
rare
, 3/
4" c
hunk
s of
woo
d, o
ccas
. roo
tlets
, 10
YR
3/1
(mod
erat
e bo
unda
ry)
brow
n pe
at, s
andy
(m
ay h
ave
mix
ed in
), 1/
16-i
n. p
iece
s of
org
anic
deb
ris,
10Y
R2/
2 (s
harp
bou
ndar
y)m
. sa
nd, m
oder
ate
sort
ing,
cle
an, 2
.5Y
4/2
(mod
erat
e bo
unda
ry)
mix
of c
. sa
nd (
30%
), f.
grav
el (
30%
), la
rge
bark
chi
ps u
p to
1 1
/4"
(30%
), 2.
5Y4/
2 (m
oder
ate
boun
dary
)1,
040.
7 jc
. sa
nd w
ith v
.c.
sand
, mod
erat
e so
rtin
g, n
o or
gani
c m
ater
ial,
2.5Y
4/2
I 1,
040.
3 jm
. sa
nd, w
ell
sort
ed, n
o or
gani
cs, e
xcep
t in
core
tip,
rar
e ch
arco
al c
hips
-1/
8-1/
4",
2.5Y
4/2
*Dep
th c
orre
cted
with
reco
very
ratio
s j
Tab
le B
7. C
ore
desc
riptio
ns f
or
core
7 a
t cr
oss
sect
ion
4, a
ppro
xim
atel
y 22
5 ft
from
left
edge
of w
ate
r an
d 48
9 ft
from
rig
ht e
dge
of w
ater
.C
ore
loca
tion
is 4
4°,
59.0
79';
88°,
51
.449
'. j
[ft, f
eet;
in.,
inch
; v.,
very
; (.,
fine;
m.,
med
ium
; c,
coa
rse;
occ
as.,
occa
sion
al]
Core
7a
colle
cte
d o
n 3
/1/0
1 w
ith a
pis
ton c
ore
r j
Wate
r d
ep
th =
3.4
ft
Har
d bottom
= 9
.1 f
tC
ore
de
pth
= 0
.0 to
2.4
ft
Co
rre
cte
d
0!
0.0
0.5
0.7
1.8
1 2
.4
..........
..........
..........
.... .._
. .....
..........
..........
..........
..........
..........
..........
..........
..........
..........
..........
.....
I i iR
eco
very
A
ltitu
de
j ra
tio
(ft)
[
1.3
1, 04
6.7
j 6 ft
sout
h of c
ore
7D
esc
riptio
n
1,04
6.1
jorg
anic
muc
k, h
igh
wat
er c
onte
nt, s
ilt, n
o sa
nd, o
ccas
. fin
e ro
otle
ts,
10Y
R2/
1, n
o w
ood
1,04
4.3
jorg
anic
muc
k, le
ss w
ater
, silt
, no
sand
gra
ins,
no
woo
d, u
nifo
rm,
10Y
R2/
1i
i i
Core
7b
colle
cte
d o
n 3
/2/0
1 w
ith a
pis
ton c
ore
r j
Wate
r d
ep
th =
ab
ou
t 3.
4 ft
j j
Har
d bottom
= a
bo
ut
9.1
ft
[ !
Core
de
pth
= 0
.0 to
1 .2
ft
i j
| C
orr
ect
ed
D
epth
(ft)
i d
ep
th (
ft)*
0 0
.0
Re
cove
ry
Alti
tude
i ra
tio
(ft)
i
6.9
1,04
6.7
16 ft e
ast o
f cor
e 7
Desc
riptio
n
1.45
! 1.
21
1,04
5.5!
(lost
org
anic
flu
ff fr
om
top)
subs
ampl
ed fo
r tr
ace
ele
men
ts a
nd r
adio
metr
ic d
atin
gf
:
Cor
e 7c
colle
cte
d o
n 3
/2/0
1 w
ith a
pis
ton c
ore
r \
Wate
r d
ep
th =
about
3.4
ft
i !
Har
d bottom
= a
bo
ut
9.1
ft
! i
Core
de
pth
= 0
.0 to
1 .7
ft
jC
orr
ect
ed
{Reco
very
A
ltitu
de
j D
epth
{ft^_
de
pth
(ft
)*
ratio
(f
t)
|0{
0.
0 1.
0 1,
046.
7 J6
ft w
est o
f cor
e 7
Desc
riptio
n
1.7
1 1.
7 1
1,04
5.0
! sub
sam
pled
for
orga
nic
chem
ical
si
!C
ore
7d1
co
llect
ed
on
3/9
/01
with
a g
eo
pro
be
core
rW
ater
dep
th =
abo
ut 3
.4 ft
i
iH
ard
bottom
= a
bo
ut
9.1
ft
jC
ore
de
pth
= 0
.0 to
4.0
ft
j!
Co
rre
cte
d
Dep
th (
ft)
de
pth
(ft
)*0
0.0
0.2
0.3
i.il
1.62
2.9
2.75
4.
0
Reco
very
A
ltitu
de j
ra
tio
(ft)
!
1.5
1 ,04
6. 1
j * *
all v
ery
grad
ual b
ound
arie
s* *
Desc
riptio
n
1,04
5.8
1 org
anic
muc
k 10
YR
2/1
1,04
4.5
(org
anic
muc
k w
ith o
ccas
iona
l roo
tlets
,mor
e to
war
ds th
e to
p of t
he u
nit
10Y
R2/
1 "s
mel
ls li
ke P
AH
s"1 ,
043.
2 ip
eat,
occa
sion
al ra
re s
tick
root
s, fi
brou
s, b
row
nish
10
YR
3/2
1 ,04
2. 1
jpea
t occ
asio
nal r
are
stic
ks a
nd ro
ots,
fibr
ous,
mor
e br
own,
occ
asio
nal b
its o
f 1/
8" w
ood
piec
es
10Y
R4/
4i
Tab
le B
7. C
ore
desc
riptio
ns f
or
core
7 a
t cr
oss
sect
ion
4, a
pjpr
oxim
atel
y 22
5 ft
from
lef
t ed
ge o
f wat
er a
nd 4
89 f
t fr
om r
ight
edg
e of
wa
ter
Co
ntin
ue
d
9.9
!?.!
99
a^'?
..!J
^[ft
, fee
t; in
., in
ch;
v , v
ery;
(.,
fine;
m.,
med
ium
; c.
, coa
rse;
occ
as.,
occa
sion
al]
_________i_
________I_
______j_
______I
Cor
e 7d
2 co
llect
ed o
n 3/
9/01
with
a g
eop
rob
e co
rer
.VM
!!Ld.
e$ll
^^H
ard
bott
om =
abo
ut 9
.1 f
t j_
___________|
__......
..........
..........
..........
..........
..........
..........
..........
..........
..........
..........
..........
......
Cor
rect
ed
Rec
over
y A
ltitu
de
dej_
th_ I
ffiP
_H*!
?L_.
. $
) ....
. -
- -
-^
j^~
~~
^
0.65
1 0.
9 j
1,04
1.3
|loam
j[ o
rgan
ic-r
ich
muc
k (m
ay h
ave
been
som
e sa
nd m
ixin
g in
from
cor
e ex
trus
ion)
, rar
e ro
otle
ts,
10Y
R2/
1 (g
radu
al b
ound
ary)
_______0.9
j_______l_
.2j_
_____
1,04
0.9
j wel
l sor
ted
f. to
m.
sand
, ra
re o
rgan
ic d
ebri
s, 2
.5 Y
4/4
(gra
dual
bou
ndar
y)
11 1.3
J .....
........1
>MP_:
8jf:
t.9 :
. .s.^
...w
!tll...
^'9.9.
^..B£
c.?.s.
1/8..'
1/1"
^ ?i
.?e..> a
l.s..9
E^:M
^I?.
.^.e£
?.?...1
9Xl?:
?/2.. (
SB.^.^
..k9.]S
!?^)...
..........
..........
..........
..........
..........
......
__
__
__
LO
S]_
__
__
__
1.4
1_
__
__
_
1,04
0.8
!lar
gc w
ood
chun
ks in
org
anic
-ric
h f.
sand
, 10
YR
3/2
(mod
erat
e bo
unda
ry)
1.6j
2.
1 j
1,04
0.0
jf. t
orn,
san
d[co
arse
ning
gra
dual
ly to
^c.
sand
^ith
: dep
th,^
no w
ood.
or] o
rgan
ic m
atte
r, c
lean
, 2.5
Y4/
2
1.75
! 2.
3j
....L
.9.?
?-?i
ii^Y
eLan
.dY-
c.- s.^
4.?.
P99£
fe ?
9^?d
'S^?
.?9^
n.de
4.j 9
c.c.a.
?- ^?
"liy
."^9
94.E
^.?.
s..'P
^.^
4.s
.E^
c..9I^
9^
______1.8
21_______2.4
i_
__
__
_
1,03
9.7
jwoo
d pi
eces
, dec
ompo
sed
orga
nic
mat
ter i
n m
. sa
nd,
10Y
R2/
2 (m
oder
ate
boun
dary
)2.
05!
2.7]
L
9?9:
4]v.
c. s
andj
oj/.l
f: g
rave
l (2-
4 m
^
__
____2.1
SJ_
___
__
_2
^8
]__
__
__
__
_1
,03
9.3
[lar
ge (
2 in
.) ch
unk
of w
ood,
roo
ts a
nd w
ood
piec
es in
mat
rix
of v
.c.
sand
and
v.f.
gra
vel (
grad
ual b
ound
ary)
____
____
____
____
___
| !
I v.c
. sa
nd to
v.f.
gra
vel (
2-4
mm
), a
bund
ant p
ink
feld
spar
, sub
roun
ded,
10Y
R,
1/8"
and
sm
alle
r bits
of d
ecom
pose
d or
gani
c m
atte
r (m
oder
ate
__
__
__
_2
_3
J__
__
__
_3
.0J_
__
__
__
__
l,0
39
.ljb
ou
nd
ary
)
I j
i_
__
__
_2
.52
J__
__
__
_3
.3J_
__
__
_
1,03
8.8
jaltc
mat
ing
f. to
m.
sand
with
laye
rs o
f par
tially
dec
ompo
sed
orga
nic
mat
ter
and
woo
d bi
ts <
l/8"
, roo
tlets
, 10
YR
2/1
(sha
rp b
ound
ary)
2.75
! 3.6
1 i
l?9.
38-5
jorg
anic
deb
ris
(pos
sibl
y sl
ackw
ater
dep
osit)
, ste
ms
root
s an
d w
ood
piec
es, b
ark
1/16
-1",
10Y
R3/
2 (s
harp
bou
ndar
y)______3.O
S j_
__
__
__
4.0
)__
__
__
1,
038.
1 [r
ank
feld
spar
£ g
ravc
i and
sm
alle
r with
v.f.
gra
vel a
nd v
.c.
sand
, 10
YR
3/3
1 I
i 1
*Dcp
th c
orre
cted
with
reco
very
rati
os_
___I_
_____)
Tab
le B
8. C
ore
desc
rifrt
jons
fo
r co
re 8
at
cros
s se
ctio
ns 8
and
9,
appr
oxim
atel
y 49
8 ft
from
left
edge
of w
ate
r al
ong
cros
s se
ctio
n 9
and
and
678
ft fr
om le
ft ed
ge o
f wate
r al
ong
cros
s se
ctio
n 8.
C
ore
loca
tion
is 4
4°,
59.1
69';
88°,
50.
966'
(!!.;!
.?.?
!' )!]
.'. In?
!?-. V
-'. V?
^.! .
! . !'
n?.i
T '
T!®
l'yi)!
? ;
?~
~~
T~
~^^
Cor
e 8a
col
lect
ed o
n 3/
2/20
01 w
ith a
pis
ton
core
r
= 6.
6 ft
^..
^.__
^.
Cor
rect
ed
Rec
over
y j
Alti
tude
D
epth
(ft
) de
pth
(ft)
* ra
tio
| (f
t)
____________________________D
escri
pti
on
........
........
........
J:0].
........
........
........
^ ___
! or
gani
c-ric
h m
uck,
silt
, hig
h w
ater
con
tent
, she
lls c
omm
on fr
om 0
.8-1
.0, l
eave
s, g
rass
bla
des
and
root
lets
com
mon
thro
ugho
ut,
1.2}
___.
......
......
L?.!.
....
......
......
......
......
......
......
J..^?
Jeaf
^ma^
*Dep
th c
orre
cted
with
reco
very
ratio
s
Tab
le B
9. C
ore
desc
ript
ions
for
cor
e 9
at c
ross
sec
tion
5,
appr
oxim
atel
y 31
5 f
t fro
m l
eft e
dge
of w
ater
and
1 ,3
53 f
t fro
m r
ight
edg
e of
wat
er.
Cor
e lo
catio
n is
4f,
59.
079'
; 88
°, 5
1 .1
95'.
][ft
, fee
t; in
., in
ch; v
., ve
ry; f
., fin
e; m
., m
ediu
m;
c., c
oars
e; o
ccas
., oc
casi
onal
]|
Cor
e 9a
1 co
llect
ed o
n 3/
9/01
with
a g
eopr
obe
Wat
er d
epth
= a
bout
6.8
ftC
ore
dept
h =
0.0
to 4
.0 ft
Cor
rect
ed
Dep
th (
ft)
dept
h (ft
)40!
0.
00.
4 0.
70.
6J
1.0
0.85
1.
51.
02J
1.8
1.18
2.
11.
6|
2.8
1.93
1 3.
42.
05!
3.6
2.3
1 4.
0I
Rec
over
y ra
tio
1.7
*Dep
th c
orre
cted
with
rec
over
y ra
tios
Alt
itud
e (f
t)1,
043.
11,
042.
41,
042.
11,
041.
71,
041.
4
1,04
1.1
1,04
0.3
1,03
9.8
1,03
9.6
1,03
9.1
Des
crip
tion
orga
nic
rich
muc
k, f
luff
y, p
unge
nt s
mel
l, 10
YR
2/2
(mod
erat
e bo
unda
ry)
orga
nic
rich
muc
k w
ith w
ood
chun
ks a
nd p
iece
s, p
unge
nt s
mel
l, 10
YR
2/2
(mod
erat
e bo
unda
ry)
orga
nic
rich
muc
k w
ith p
eat -
gra
ss b
lade
s an
d ro
otle
ts,
10Y
R2/
2 (a
brup
t bou
ndar
y)f.
to m
. sa
nd, o
ccas
. roo
tlets
, occ
as.
deco
mpo
sed
orga
nic
mat
ter,
wel
l so
rted
, 10
YR
3/3
(mod
erat
e bo
unda
ry)
f. to
m.
sand
with
org
anic
mat
ter,
laye
red
1/8
in. w
ood
piec
es, r
ootle
ts, d
ecom
pose
d de
bris
, bar
k sl
ight
ly p
unge
nt s
mel
l, 10
YR
3/2
(mod
erat
e bo
unda
ry)
f. to
m.
sand
, zon
e w
ith o
rgan
ic m
atte
r an
d bi
ts fr
om 1
.45-
1.5
ft, w
ell s
orte
d, 1
0YR
3/3
(gra
dual
bou
ndar
y)al
tern
atin
g la
yers
of v
.c.
sand
and
f. g
rave
l, pi
nk f
elds
par o
ccas
iona
lly, r
are,
2.5
Y4/
2 (s
harp
bou
ndar
y)al
tern
atin
g la
min
atio
ns o
f dec
ompo
sed
ogan
ic m
atte
r and
f. s
and,
2.5
Y3/
2 (g
radu
al b
ound
ary)
f. sa
nd, w
ell s
orte
d, r
are
orga
nic
mat
ter,
2.5Y
4/2
Tab
le B
1 0.
Cor
e de
scri
ptio
ns f
or c
ore
1 0 a
t cr
oss
sect
ion
1 0, a
ppro
xim
atel
y 26
2 ft
from
lef
t edg
e of
wat
er.
Cor
e lo
catio
n is
4/f
, 58
.960
'; 88
°, 5
0.62
0'.
][ft
, fee
t; in
., in
ch; v
., ve
ry; f
., fin
e; m
., m
ediu
m; c
., co
arse
; oc
cas.
, occ
asio
nal]
i I
. I
Cor
e 10
a1 c
olle
cted
on
3/9/
01 w
ith a
geo
prob
eW
ater
dep
th =
8.9
ftC
ore
dept
h =
0.0
to 4
.0 ft
I C
orre
cted
D
epth
(ft)
j
dept
h (ft
)*o|
o.o0.
25 1
0.4
0.5
1 0.
7i
0.9
1 1.
3il
j 1.7
1.25
'! 1.
81.
65|
2.4
1.75
1 2.
51.
951
2.8
2.3
1 3.
32.
5 !
3.6
2.6!
3.
72.
8)
4.0
i
Rec
over
y ra
tio1.
4
*Dep
th c
orre
cted
with
reco
very
ratio
s
Alti
tude
(ft
)1,
041.
5
1,04
1.2
1,04
0.8
1,04
0.3
1,03
9.8
1,03
9.8
1,03
9.2
1,03
9.0
1,03
8.8
1,03
8.3
1,03
8.0
1,03
7.8
1,03
7.5
Des
crip
tion
orga
nic-
rich
muc
k, p
unge
nt s
mel
l, 10
YR
2/1
(gra
dual
bou
ndar
y)or
gani
c-ri
ch m
uck
with
1/8
" w
ood
chip
s, 1
0YR
2/1
(mod
erat
e bo
unda
ry)
peat
, tin
y ro
otle
ts a
bund
ant,
occa
s. b
lade
-lik
e pi
eces
, 7.5
YR
2/1
(sha
rp b
ound
ary)
m.
to v
.c.
sand
, poo
rly
sort
ed, 2
.5Y
4/2
(mod
erat
e bo
unda
ry)
brow
n pe
at,
7.5Y
R3/
2 (m
oder
ate
boun
dary
)fi
ne g
rave
l (1/
16-1
/8 in
.) an
d ve
ry c
oars
e sa
nd, p
ink
feld
spar
com
mon
, cle
an n
o or
gani
cs,
10Y
R4/
3 (m
oder
ate
boun
dary
)pe
aty
(fib
ers
and
root
lets
) ra
san
d, 1
0YR
3/3
(mod
erat
e bo
unda
ry)
f. gr
avel
(1/
16-1
/8 in
.) an
d v.
c. s
and,
pin
k fe
ldsp
ar c
omm
on, c
lean
no
orga
nics
, 10
YR
4/3
(sha
rp b
ound
ary)
orga
nic-
rich
ra
sand
, slig
htly
fibr
ous,
bur
ied
A h
oriz
on 1
0YR
3/2
(ver
y gr
adua
l bou
ndar
y)v.
c. s
and
to v
.f. g
rave
l, cl
ean
10Y
R4/
2 (v
ery
shar
p bo
unda
ry)
woo
d bi
ts, r
oots
, org
anic
deb
ris,
10
YR
2/2
f. to
ra
sand
, cle
an, g
ray,
2.5
Y4/
2
Tabl
e C1
. Bu
lk d
ensi
ty a
nd o
rgan
ic m
atte
r dat
a fo
r cor
e sa
mpl
es c
olle
cted
from
Neo
pit M
ill P
ond,
Neo
pit,
Wis.
, 200
1[ft
, fee
t; g,
gra
ms;
cm
, cen
timet
er;
USG
S, U
.S. G
eolo
gica
l Sur
vey;
sed
, sed
imen
t. In
terv
al to
p an
d bo
ttom
dep
ths
are
not c
orre
cted
for r
ecov
ery
ratio
.]
Cor
e nu
mbe
rIb Ib 2b 7b 7b 7b 7b 7b 7b 7b 7b
USG
S si
te
num
ber
4458
5108
8495
000
4458
5108
8495
000
4458
5008
8495
600
4459
0588
5127
0044
5905
8851
2700
4459
0588
5127
0044
5905
8851
2700
4459
0588
5127
0044
5905
8851
2700
4459
0588
5127
0044
5905
8851
2700
Inte
rval
to
p (ft
)0.
000.
350.
100.
050.
200.
250.
450.
750.
750.
95 1.40
Inte
rval
bo
ttom
(f
t)0.
100.
450.
200.
100.
250.
300.
500.
800.
801.
001.
45
Dat
e co
llect
ed2/
13/2
002
2/13
/200
22/
13/2
002
3/1/
2001
2/13
/200
23/
1/20
013/
1/20
013/
1/20
013/
1/20
013/
1/20
013/
1/20
01
Plat
e (g
)1.
1184
31.
1151
61.
1080
81.
1183
01.
1151
71.
1013
51.
1181
91.
1174
91.
1096
31.
1142
31.
1040
8
Plat
e +
wet
sed
(g)10
.822
694.
3259
610
.306
045.
6861
47.
3732
77.
6713
79.
7186
58.
5729
810
.988
0714
.568
339.
2847
5
Plat
e +
dry
sed
(g)1.
7810
61.
7856
22.
5567
31.
3479
41.
6482
51.
6643
11.
8490
51.
8271
52.
0481
32.
4237
1.99
696
Afte
r 550
° pl
ate
+ dr
y se
d (g
)1.
5509
11.
5324
92.
0160
71.
2183
41.
3515
61.
3485
51.
4327
81.
4247
31.
5185
1.65
925
1.48
685
Dry
sed
(g)0.
6626
30.
6704
61.
4486
50.
2296
40.
5330
80.
5629
60.
7308
60.
7096
60.
9385
1.30
947
0.89
288
Wet
sed
(g)9.
7042
63.
2108
9.19
796
4.56
784
6.25
816.
5700
28.
6004
67.
4554
99.
8784
413
.454
18.
1806
7
Afte
r 55
0° s
ed(g)
0.43
248
0.41
733
0.90
799
0.10
004
0.23
639
0.24
720.
3145
90.
3072
40.
4088
70.
5450
20.
3827
7
Wat
er
cont
ent
_Jp
ctl
93.2
79.1
84.3
95.0
91.5
91.4
91.5
90.5
90.5
90.3
89.1
Org
anic
m
atte
r (p
et)
34.7
37.8
37.3
56.4
55.7
56.1
57.0
56.7
56.4
58.4
57.1
Cal
cula
ted
bulk
den
sity
(g/c
m5_
..0.
071
0.24
0.17
0.05
20.
089
0.09
00.
089
0.10
0.10
0.10
0.12
Tab
le D
1 . R
adio
met
ric d
atin
g re
sults
for
core
sam
ples
col
lect
ed f
rom
Neo
pit
Mill
Pon
d, N
eopi
t, W
is.,
2001
[ft, f
eet;
pCi/g
, pi
coC
urie
s pe
r gr
am;
US
GS
, U
.S.
Geo
logi
cal S
urve
y. I
nter
val t
op a
nd b
otto
m d
epth
s ar
e no
t cor
rect
ed f
or r
ecov
ery
ratio
.]
Cor
e nu
mbe
r7b 7b 7b 7b 7b 7b
US
GS
site
num
ber
4459
0588
5127
0044
5905
8851
2700
4459
0588
5127
0044
5905
8851
2700
4459
0588
5127
0044
5905
8851
2700
Inte
rval
to
p (
ft)0.
050.
250.
450.
750.
951.
40
Inte
rval
bo
ttom
(f
t)0.
100.
300.
500.
801.
001.
45
Dat
e co
llect
ed3/
1/20
013/
1/20
013/
1/20
013/
1/20
013/
1/20
013/
1/20
01
210R
b
(PC
i/g)
13 12 13 11 11 9.9
210P
b2-
sigm
a2.
41.
61.
81.
41.
51.
9
137C
s (p
Ci/g
)2.
01.
62.
32.
62.
43.
0
137C
s2-
sigm
a0.
69 .77
.72
.48
.56
.79
226R
a (p
CI/g
)0.
06 .13
.59
.88
.42
.64
226R
a2-
sigm
a2.
01.
21.
0.7
81.
31.
7
Tabl
e E1
. M
inor
and
tra
ce e
lem
ent
resu
lts fo
r co
re s
ampl
es c
olle
cted
fro
m N
eopi
t M
ill P
ond,
Neo
pit,
Wis
., 20
01[ft
, fee
t; pe
t, pe
rcen
t; ug
/g,
mic
rogr
ams
per
gram
;na
, no
t ava
ilabl
e; U
SG
S,
U.S
. G
eolo
gica
l S
urve
y. I
nter
val t
op a
nd b
otto
m d
epth
s ar
e no
t cor
rect
ed f
or r
ecov
ery
ratio
,Th
resh
old
and
prob
able
effe
ct c
once
ntra
tions
are
from
Mac
Don
ald
and
othe
rs,
2000
.]
Cor
e nu
mbe
rIb Ib 2b 7b
US
GS
site
num
ber
4458
5108
8495
000
4458
5108
8495
000
4458
5008
8495
600
Inte
rval
to
p (f
t)0.
000.
35L
d.io
4459
0588
5127
00
0.20
Ran
ge in
con
cent
ratio
n fro
m e
ight
Wol
f R
iver
bas
in s
ites
(Scu
dder
and
oth
ers,
1 9
97;
Gar
n an
d ot
hers
, 20
01 )
|T
hres
hold
effe
ct c
once
ntra
tion
Pro
babl
e ef
fect
con
cent
ratio
nr
Inte
rval
bo
ttom
(f
t)0.
100.
450.
20
Dat
e co
llect
ed2/
13/2
001
2/13
/200
12/
13/2
001
0.25
!
3/1/
2001
i - -
Inor
gani
c ca
rbon
(p
et)
0.99
0.16
Org
anic
ca
rbon
(p
et)
19
Tot
al
carb
on
(pet
)20
22
220.
15
T 19
0.48
28
^_
.4
.. .
0.06
-0.3
1 11
.6-2
2.3
na
nana na
19
Cal
cium
(p
et)
3.1
1.4
1.3
29
j 3.
6
....
... .J
.
11.9
-22.
4 na
1.5-
1.9
Mag
nesi
um
(pet
)1.1 0.53
0.49
0.37
0.53
-0.7
4
Pot
assi
um
(pet
)1.1 1.
01.
10.
44
0.80
-0.9
8
Sod
ium
(p
et)
0.34
0.41
0.42
0.18
0.37
-0.5
9
Sul
fur
(pet
)0.
740.
940.
72
i0.
6
0.28
-0.3
8na
|
na
j na
na
nana
na
na
na
i
na
na
Pho
spho
rus
(pet
)0.
110.
048
0.04
30.
13
0.17
-0.2
3na na
Tab
le E
1. M
inor
and
tra
ce e
lem
ent
resu
lts f
or c
ore
sam
ples
col
lect
ed f
rom
Neo
pit
Mill
Pon
d, N
eopi
t, W
is.,
2001
C
ontin
ued
[ft,
feet
; pe
t, pe
rcen
t; ug
/g,
mic
rogr
ams
per
gram
; na
, no
t av
aila
ble;
US
GS
, U.S
. G
eolo
gica
l S
urve
y. I
nter
val t
op a
nd b
otto
m d
epth
s ar
e no
t co
rrec
ted
for
reco
very
rat
io.
Thr
esho
ld a
nd p
roba
ble
effe
ct c
once
ntra
tions
are
fro
m M
acD
onal
d an
d ot
hers
, 20
00.]
Cor
e num
ber
Ib Ib 2b 7b
US
GS
site
num
ber
4458
5108
8495
000
4458
5108
8495
000
4458
5008
8495
600
4459
0588
5127
00
Ran
ge in
con
cent
ratio
n fr
om e
ight
W
olf
Riv
er b
asin
site
s (S
cudd
er a
nd
othe
rs,
1997
; G
arn
and
othe
rs,
2001
)
Alu
min
um
(p
et)
2.4
An
timo
ny
(ng/
g)0.
5
Ars
enic
(ng/
g)7.
82.
6 0.
6 j
7.9
2.6
0.4
1.6
: 0.
2
2.3-
3.0
na
__
5.6 ^
3.4
5.6-
20Th
resh
old
effe
ct c
once
ntra
tion
na
na
9.79
Pro
babl
e ef
fect
con
cent
ratio
n na
na
33
Ba
riu
m
(ng/
g)27
0
Bery
llium
(ng/
g)0.
830
0 j
0.6
Cadm
ium
... (n
g/g)
_j0.
8
Cerium
Oig/
g)45
1.7
| 35
310
0.7
0.9
3422
0 0.
5I.
I 36
Ch
rom
ium
(ng/
g)50 41 39 87
_J
i
300-
380
! |
< 1-
0.81
0.
4-0.
9 31
-58
, 33
-66
" i
na
, na
na
, na
0.99
Cobalt
(ng/
g)5 4 4 4
Co
pp
er
(ng/
g)28 22
_18 20
5.2-
8.0
13-2
3
Galli
um
(^g/
g)7 6 7 4
<4-1
0
Iron
(ng/
g)1.
81.
71.
41.
4
h -J
2.3-
3.2
na
43.4
na
j
31.6
|
na
; na
La
nth
an
um
(^g/
g)23 18 17 21
18-3
2na
4.98
na
'
111
na
149
na
j na
na
Tab
le E
1. M
inor
and
tra
ce e
lem
ent
resu
lts f
or c
ore
sam
ples
col
lect
ed f
rom
Neo
pit
Mill
Pon
d, N
eopi
t, W
is.,
20
01
Con
tinue
d I
[ft,
feet
; pe
t, pe
rcen
t; ug
/g,
mic
rogr
ams
per
gram
; na
, no
t av
aila
ble;
US
GS
, U
.S.
Geo
logi
cal
Sur
vey.
Int
erva
l top
and
bot
tom
dep
ths
are
not
corr
ecte
d fo
r re
cove
ry r
atio
.T
hres
hold
and
pro
babl
e ef
fect
con
cent
ratio
ns a
re f
rom
Mac
Don
ald
and
othe
rs,
2000
.] |
Cor
e num
ber
Ib Ib 2b 7b
US
GS
site
num
ber
4458
5108
8495
000
4458
5108
8495
000
4458
5008
8495
600
Lead
(ng/
g)4
0
h " 26
4459
0588
5127
00
22
...
| .....
_..
_._
._!
Ran
ge in
con
cent
ratio
n fr
om e
ight
W
olf
Riv
er b
asin
site
s (S
cudd
er a
nd
othe
rs,
1997
; G
arn
and
othe
rs,
2001
)16
-40
Lith
ium
(ng'g
)M
anga
nese
fog/
g)15
'
350
13 13 10
270
250
Me
rcu
ry
Mo
lyb
de
nu
m
(ng/
g)
j (m
g/g)
0.13
J
5.7
0.1
; 6.
5
0.1
i 2.
6
320
i 0.
17
' 0.
7i i
10-1
31,
600-
3,50
0
Thr
esho
ld e
ffect
conce
nin
itioii
[ 35
.8
I na
|
na
0.04
-6.1
0.
5-<
2.0
Neodym
ium
(Mi/g
)20 15
r
M- ~
"
18
16-2
7
Nic
kel
1 (^
g/g)
13 10 10
Nio
biu
m
(ng/
g)9 8 7
Sca
ndiu
m
{u-g
/g)
5 4 4
8 5
i 4
1 L 7-
14
Sel
enui
m_
(Mg/g
)2.
0
1.7
1.4
Silv
er
fog/
g)0.
1
0.1
0.1
4.6
| <
.l1
i
<4-
84.
8-7.
0 ,
0.9-
5.3
0.18
na
!
na
22.7
na
na
na
Pro
babl
e ef
fect
coi
K'L
-ntia
tioii
| 12
8 '
na
\ na
1.06
na
0.2-
0.7
na
na
i 48
.6
na
na
na
! na
Str
on
tium
(Ml/g
)61 59 60 48
63-8
7
na na
Tabl
e E1
. M
inor
and
tra
ce e
lem
ent r
esul
ts f
or c
ore
sam
ples
col
lect
ed f
rom
Neo
pit
Mill
Pon
d, N
eopi
t, W
is.,
2001
C
ontin
ued
[ft,
feet
; pe
t, pe
rcen
t; ug
/g,
mic
rogr
ams
per g
ram
; na
, no
t ava
ilabl
e; U
SG
S,
U.S
. G
eolo
gica
l S
urve
y. I
nter
val t
op a
nd b
otto
m d
epth
s ar
e no
t cor
rect
ed f
or r
ecov
ery
ratio
.Th
resh
old
and
prob
able
effe
ct c
once
ntra
tions
are
from
Mac
Don
ald
and
othe
rs,
2000
.]
Cor
e nu
mbe
rIb Ib 2b 7b
US
GS
site
num
ber
4458
5108
8495
000
4458
5108
8495
000
4458
5008
8495
600
4459
0588
5127
00
Ran
ge in
con
cent
ratio
n fro
m e
ight
W
olf R
iver
bas
in s
ites
(Scu
dder
and
ot
hers
, 19
97;
Gar
n an
d ot
hers
, 20
01)
Tho
rium
(ng/
g)6 5
H-^
4
3.6-
11
Tin
(ng/
g)3 3 2 1
1.4-
<5
Tita
nium
(ng/
g)0.
14
0.16
Ura
nium
(ng/
g)15 15
0.16
7
0.08
2 4.
5
Van
adiu
m(n
g/g)
38 40 38 25
Yttr
ium
(>g/
g)r
13 10 10
Zin
c(n
g/g)
140
110
9014
13
0
i :
<1
Thr
esho
ld e
ffect
con
cent
ratio
n |
na
na
j na
2.4-
4.7
-
-ina
Pro
babl
e ef
fect
con
cent
ratio
n na
;
na
na
na
.
42-6
0
na na
14-2
261
-130
na
! 12
1
-
na
459
'
Tabl
e F1
. Org
anic
com
poun
ds d
etec
ted
in co
re s
ampl
es c
olle
cted
from
Neo
pit M
ill P
ond,
Neo
pit,
Wis
., 20
01[f
t, fe
et;
g, g
ram
; kg,
kilo
gram
; jig
, mic
rogr
am; E
, est
imat
ed; U
SGS,
U.S
. Geo
logi
cal S
urve
y;<,
les
s th
an; i
nter
val t
op a
nd b
otto
m d
epth
s ar
e no
t cor
rect
ed f
or re
cove
ry r
atio
.]
o .Q 3 C 2 o o lc lc lc lc 2c 2c 7c
0)
.Q 3 C
0) w CO 0 CO D44
5851
0884
9500
044
5851
0884
9500
044
5851
0884
9500
044
5851
0884
9500
044
5850
0884
9560
044
5850
0884
9560
044
5905
8851
2700
_.
Q.
O ? O £ 0.00
0.05
0.50
0.55
0.10
0.15
0.20
0 £
0
.Q 15 Z c0.
050.
100.
550.
600.
150.
200.
30
o
o o o 0 o 15 Q2/
13/2
001
2/13
/200
12/
13/2
001
2/13
/200
12/
13/2
001
2/13
/200
13/
1/20
01
c o .Q 8 o c I? j
?C
O
)
7.7
4.7
0.9 1 2.2
2.3
1.2
I O .Q £ Q 1-
190
180
240
240
170
180
290
c 0 8 0 c x-
s
1_
*^f
o 3
180
180
230
240
170
180
290
3L
If «
c c
Q)
O
o £
73
c <~
>g,
to
o>G*
c .
*T
f
^"
^
Q. -^
<250
<250
E18
0E
60<2
50<3
00<6
20
o c o c '5 u- _
2 S
«S
c »
< 3
<250
<250
<250
210
<250
<300
<620
"3 ^
o c 2 o 3 U.
E12
013
0<2
50E
100
<250
E18
0<6
20
0) c o Q.
^^
(0
O)
c .*
O
O)
<
>2?
<50
190
E24
0^"
E80
E11
0E
210
<620
Q)
0> £ Q.
x-s
(0
O)
<»
"^
o o*
< -^
330
880
990
300
520
910
<620
2 3 o o o 2 £ C <
E10
016
032
0E
100
E10
0E
130
<620
o 8 2 £ C
(0 i j
O)
N ^
£ "&
QJ
^**
m 3
E14
016
054
017
0E
120
E13
0E
120
0) 2 JO.
t<5L O
O)
CO
<3;
200
250
710
250
E15
0E
240
<620
Tabl
e F1
. Org
anic
com
poun
ds d
etec
ted
in c
ore
sam
ples
col
lect
ed fr
om N
eopi
t Mill
Pon
d, N
eopi
t, W
is.,
2001
C
ontin
ued
[ft,
feet
; g,
gra
m;
kg, k
ilogr
am; u
g, m
icro
gram
; E, e
stim
ated
; USG
S, U
.S. G
eolo
gica
l Sur
vey;
<, l
ess
than
; int
erva
l top
and
bot
tom
dep
ths
are
not c
orre
cted
for
rec
over
y ra
tio.]
& 3 C 2 0 0 lc lc lc lc 2c 2c 7c
o> A E 3
C 0) 'w C/)
O (/) 1344
5851
0884
9500
044
5851
0884
9500
044
5851
0884
9500
044
5851
0884
9500
044
5850
0884
9560
044
5850
0884
9560
044
5905
8851
2700
o>i
0)JQ
£ 'slf
C
O
**3k
0)
3 5
CQ ^ s3
250
300
900
250
E20
031
0<6
20
O)
^c
^ ^iT
S c PI
o> o>
m
a.27
029
088
036
0E
210
340
<620
o> c
.* £
o §
3N
£
.*
CO
"??
03?
m ^ s
=<2
50 50 480
190
E40
El 1
0<6
20
3 ^ ^
o> o N (C (C O<2
50<2
50E
150
E50
<250
<300
<620
3 B)
^
o> 0) M r~ O E90 18
065
020
0E
70E
120
E13
0
o> o> S o)
O
!*3
O>LL
s3
?
350
710
1,80
054
047
050
0E
190
lj_1 V 3
CM" "
5>L
__
l """"'
O
Oc
c0
0)
TJ
^£
CLE
140
220
640
270
E11
0E
200
<620
3 1£
o> P? 5 £
1 O
T-
C
E50 10
0E
10<1
50E
30E
50<6
20
J>
>» -
3£
o> o>
c'Z
«
^
^3*^
"o.
CO
(Q
CM
CE
40 60 <250
<150
<250
<300
<620
o> >^M
^
fll
^^ c
£
o> P? Q £
<o
nCM
C
400
440
290
E90
E14
033
0E
400
o> c 0) (C .C
V
*-
O)
z s
31,
400
3,10
03,
300
1,20
01,
800
2,30
0<6
20
3 1 UJ
Q Q Q.
Q.
<4 E2 <9 <3 E4
E4
E7
^^ O)
X 1 o W 2 o Q.
440
500
<250
300
1,10
02,
300
5,70
0
o 2_e*
£
*i
<o o
T-
O. 3
<250 80
E22
0E
80<2
5040
0<6
20
o> 2 c ^
<C
O)
Q. 3
510
1,30
01,
900
560
440
820
<620
Tabl
e F1
. Org
anic
com
poun
ds d
etec
ted
in co
re s
ampl
es c
olle
cted
from
Neo
pit M
ill P
ond,
Neo
pit,
Wis
., 20
01 C
ontin
ued
[ft,
feet
; g, g
ram
; kg,
kilo
gram
; ng,
mic
rogr
am; E
, est
imat
ed; U
SGS,
U.S
. Geo
logi
cal S
urve
y;<,
les
s th
an; i
nter
val t
op a
nd b
otto
m d
epth
s ar
e no
t cor
rect
ed f
or re
cove
ry r
atio
.]
Core
number
Ic Ic Ic Ic 2c 2c 7c
USGS
site
number
4458
5108
8495
000
4458
5108
8495
000
4458
5108
8495
000
4458
5108
8495
000
4458
5008
8495
600
4458
5008
8495
600
4459
0588
5127
00
3) ^
"o 0
Q.
E15
019
029
016
0E
l 80
330
<620
Pentachlorophenol (ng/kg
)
<250
<250
E6,
600
<150
<250
<300
<620
bis(2-Ethylhexyl) phthala
te (jxg/k
g)
<250
240
360
<150
<250
230
E28
0
Butylbenzyl phthala
te (jxg/k
g)
<250
240
<250
<150
<250
<300
E38
0
0) To a 3
^>
Xt
O)
5 s^
<250
<250
E50
<150
<250
<300
<620
0) 5 <0
Xj a. ^^
O)
5 .
3<2
50<2
50<2
50E
70E
90<3
00<6
20
3) 3 0) C a. 380
740
1,60
047
053
059
0E
80
Dibenzothiophene (ng/kg
)
<250
<250
<250
E60
<250
<300
<620
58
Table F2. Organic compounds (micrograms per kilogram) not detected incore samples collected from Neopit Mill Pond, Neopit, Wis., 2001
2,2'-Biquinoline
3,5'-Xylenol
4-Bromophenylphenylether
4-Chlorophyenyl phenyl ether
l-Methyl-9H-fluorene
Acridine
Aldrin
alpha-HCH
2-Methylanthracene
Dibenz[a,h]anthraceneAzobenzene1 ,2,4-Trichlorobenzene
Hexachlorobenzene
1 ,3-Dichlorobenzene
Nitrobenzene
1 ,2-Dichlorobenzene
1 ,4-Dichlorobenzene
Pentachloronitrobenzene
Benzo[c]cinnoline
Beta-HCH
bis(2-Chloroisopropyl) ether
bis(2-Chloroethyl) ether
Hexachlorobutadiene
Chloroneb
cis-Chlordane
cis-Nonachlor
cis-Permethrin
Hexachlorocyclopentadiene
Dacthal
Dieldrin
N-Nitrosodiphenylamine
N-Nitrosodi-n-propylamine
alpha-Endosulfan
Endrin
Hexachloroe thane
Heptachlor epoxide
Heptachlor
Isodrin
Isophorone
Isoquinoline
Lindane
4-Chloro-3-methylphenol
2,4,6-Trimethylphenolbis(2-Chloroethoxy)methane
o,p' -Methoxychlor
p,p' -Methoxychlor
Mirex
1 ,2-Dimethylnaphthalene
2-Chloronaphthalene
2-Ethyhiaphthaleneo,p'-DDD
o,p'-DDE
o,p'-DDT
Oxychlordanep,p'-DDD
p,p'-DDT
Polychlorinated biphenyls
Pentachloroanisole
Phenanthridine2,4-Dichlorophenol
2,4-Dinitrophenol
4,6-Dinitro-2-methylphenol
C8-Alkylphenol
4-Nitrophenol
2-Chlorophenol
2-Nitrophenol
2,4,6-Trichlorophenol
Dimethyl phthalateDi-n-octyl phthalate
1-Methylpyrene
Quinoline2,4-Dinitrotoluene
2,6-Dinitrotoluene
Toxaphenetrans-Chlordane
trans-Nonachlor
trans-Permethrin