Groundwater Conditions in Carbonate Bedrock Areas ... · 12/13/2016 · • Groundwater in...
Transcript of Groundwater Conditions in Carbonate Bedrock Areas ... · 12/13/2016 · • Groundwater in...
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Madeline Gotkowitz Hydrogeologist
Groundwater Conditions in Carbonate Bedrock Areas, Southwest Wisconsin
NR 151 Technical Advisory Committee December 13, 2016
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Outline
• Southwest Wisconsin Hydrogeology • Pathogen transport in fractured rock • groundwater quality
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Karst is a type of landscape
• Formed when soluble rocks, such as limestone and dolomite, dissolve
• Dissolution occurs because percolating rainwater is slightly acidic, pH about 5.7
• Spectacular, well-developed karst systems feature large caves and sinkholes (Kentucky, New Mexico, Cave of the Mounds)
• Wisconsin’s karst features are relatively muted, with small sinkholes, enlarged fracture networks and conduits
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20% of U.S. land surface is karst
Weary and Doctor, 2014
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crystalline rock
sandstone
carbonate
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Carbonate rocks Silurian
Sinnipee
Prairie du Chien
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sandstone
Mount Simon sandstone
Sinnipee
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Wisconsin River Valley
Sinnipee dolomite
Galena
sandstone
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St. Peter sandstone
Prairie du Chien dolomite
Cross section of geologic strata in Driftless Area
Galena dolomite
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Bedding plane fractures, Iowa County
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Horizontal
Vertical
Platteville Fm, Hwy 151 Lafayette County
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southwest
northeast
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Near Cave of the Mounds, Dane County
Easy to see…
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Or not so easy to see…
Sinnipee dolomite, Iowa County
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Lafayette County Fracture traces in field
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• Cause acute illness • Survival depends on
temperature, moisture, and absence of UV light
• Present in large numbers in human and animal waste
• Septic systems, sewer systems, and manure
• Remain infectious on the order of 10s of months in groundwater
Pathogens: bacteria, protozoa and viruses
Bacteria: Campylobacter, Salmonella, E. coli O157:H7,
Aeromonas
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Pathogen transport
Particulates and common diameters: (1 micron = 1 millionth of a meter)
Human hair (~50-100 um) Rock fracture (1 – 1,000s um)
Colloids (<0.2 um) Bacteria (~.2 – 20 um) Viruses (~0.005 um)
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Porous media: slows groundwater transport, filters pathogens, dilutes dissolved contaminants (e.g. nitrate)
Fractures: rapid transport, no filtration or contaminant decay
Pore spaces filled with water
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Dodgeville Fleet Farm
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Bacteria, private residential wells
Well water quality viewer, Center for Watershed Science and Education, UW Extension; Accessed 12/9/2016
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Well water quality viewer, Center for Watershed Science and Education, UW Extension; Accessed 12/9/2016
27% 34 of 126
27% 351 of 958
16% 5 of 31
19% 33 of 171 35%
40 of 115
41% 128 of 312
23% 253 of 1,087
32% 37 of 114
20% 106 of 536
14% 332 of 2,381
20% 229 of 1,167
11% 42 of 374
19% 100 of 525
28% 101 of 355
21% 553 of 2681
17% 16 of 96
22% 22 of 102
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Summary • Karst is a landscape typified by large openings in
carbonate bedrock • Wisconsin geology is not uniform: karst forms a
V-shaped band across the state • Groundwater in carbonate rock with thin soil
cover is very vulnerable to contamination because of rapid flow pathways from the land surface
• Southwest Wisconsin has ridge and valley topography with thin soil on uplands
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Summary
• Sinnipee and Platteville formations are highly fractured and karst features are common
• The layered geology leads to perched groundwater in some areas
• 15 to 40% of tested private residential wells are positive for coliform bacteria (an indicator bacteria)
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sandstone
shale
dolomite
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Water levels respond to precipitation.
Galena aquifer Mt Simon aquifer
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Prairie du Chein Dolomite underlain by Cambrian sandstone and siltstone layers(up to 1,000 feet thick in this area)
WELL CONSTRUCTION IN IOWA COUNTY UPLANDS
Soil and clay
Galena Dolomite
Decorah Shale
Platteville Dolomite
St. Peter Sandstone
regional water table
YF365new well
UG327old well
Septictank
perched water table
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Karst landscapes are characterized by sinkholes, caves, and underground drainage
Runkel, et al., 2003
In Wisconsin, fracture networks are the predominant expression of karst
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Well design and construction support groundwater quality in deep aquifers.