Salt in Dutchess Co Waters – Where, when, so what?
-
Upload
katelyn-hogan -
Category
Documents
-
view
16 -
download
1
description
Transcript of Salt in Dutchess Co Waters – Where, when, so what?
CARTI Presentation April 2010 1
Salt in Dutchess Co Waters –Where, when, so what?
Stuart Findlay and Vicky Kelly – Cary Institute of Ecosystem Studies
Don Siegel and Li Jin – Syracuse University
Some Chloride Reference Points• Background - ~ 10 mg/L or less [Catskill Reservoirs]
• Sublethal – 50-100 mg/L Subtle yet Significant
– Biotic Indices
– Microbial processes
– Associations
• EPA Chronic – 230 mg/L
• Drinking Water Std – 250 mg/L
• EPA Acute – 860 mg/L
• Lethal - 1000 or higher
SIMPLER
• REFERENCE <10 mg/L
• ENVIRONMENTAL EFFECTS ~ 100 mg/L
• LETHAL > 1000 mg/L
DUTCHESS COUNTY WATERS80 mg/L (+/- 79 SD)
Ten Mile10-40
Crum Elbow15-50
Casperkill100-300(Cunningham et al 2009)
Dutchess CountyChloride(mg/L)
Wappinger10-45
Fishkill10-100
Mullaney et al., USGS
DC WC
CARTI Presentation April 2010 6
Karraker et al. 2008
CARTI Presentation April 2010 7NaCl (mg/L)
0 10000 20000 30000 40000 50000
Pe
rce
nt
Su
rviv
al
0
20
40
60
80
100
120
AdultEmbryo
THE UNEXPECTED
• Long-term increases in concentration
• High concentrations in summer
• Higher concentrations downstream (in summer)
Long-term IncreaseSaw Kill Creek
HRNERR• Low-density residential
• Yearly mean Cl-
concentrations have doubled since 1991 (20 to 40 mg/L)
• Similar Cl- concentrations throughout year
Year
1990 1992 1994 1996 1998 2000 2002 2004
Chl
orid
e (m
g/L)
0
10
20
30
40
50
60
High concentrations
in summer
0
20
40
1 2 3 4 5 6 7 8 9 10 11 12
MONTH
CH
LOR
IDE
(mg/
L)
East Branch Wappinger Creek, Millbrook
No decline in summer concentrations
DISTANCE FROM MOUTH (km)
0 5 10 15 20 25 30 35
Chl
orid
e (m
g/L)
0
20
40
60
80
100
120
140
160
FISHKILL CREEKSummer 2005
Popul
atio
n
New York State
Downstream increases insummer
HeadwatersMouth
Groundwater / Surfacewater
05
1015202530354045
25 50 75 100 125 150 175 200 225 More
Chloride (mg/L)
% o
f Sam
ples
WELL
SURF
Fig. 4: Frequency distribution of chloride concentrations in surface and well samples from Dutchess County.
A few wells have Cl > surface water concentration – Could support high baseflow concentrations
Private drinking-water wellsNon-random but widely distributed
Residential Land Cover and Chloride (M. Essery)
Subwatersheds in the Fishklill Basin
Percent Residential
5 10 15 20 25 30 35 40 45
Chlo
ride (
mg/L
)
20
40
60
80
100
120
140
160
180
200
220
Sources of Chloride(% of flux in Fishkill Creek)
(>80%)
(~1%)
(5-10%)
CHLORIDE IS NOT ALONE – ASSOCIATED WITH
OTHER CONTAMINANTS
0 30 60 90 120 150 180 210
CL (mg/L)
0
4
8
12
16
20
24
NO
3 (
mg/L
)
D. Burns - EMC
Event – Dec 24-27, 2008Fishkill Creek at Beacon
Exposure at “peak” concentration equivalent to about twice as long at “baseline” concentration
An Engaging Problem?• Everyone understands “salt”-opportunity for
education
• Not viewed as a threatening issue -not (presently) a health hazard or regulated material
• Point sources don’t always seem to be the problem (no finger-pointing, low media attention)
• Chloride is associated with nitrate so trend may suggest presence of other contaminants
The Future? Scenario Tests• Scenario 1--Reducing road salt application by half
– Cl decreases up to 20.7% at mouth
• Scenario 2- --Doubling road salt application– Cl increases up to 34.2% at mouth
0
20
40
60
80
100
120
06/01/08 08/31/08 11/30/08 03/01/09 05/31/09
Cl c
once
ntr
atio
ns (
mg/
L)
Modeled Cl
Scenario1 Cl
Scenario2 Cl
Fishkill Creek Reach 7 (mouth)
Base
-50%
2X
Jin et al. 2011