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-Road Salt In The Lake George Basin- A Long-term Watershed Case Study
& Current Basin-wide Research
http://www.wildernessphotographs.com/photo.php?id=1056
Why is the focus on road salt in the Lake George drainage basin important?
▪ There has been a 3-fold increase in the concentration of NA+ and CL- in Lake George during the past 30 years
▪ Winter highway deicing practices are the primary source of these compounds
▪ Direct correlation between the surface area of watershed roads and [Cl-] of the stream draining the watershed (Swinton et al 2015)
The State of the Lake: Thirty Years of Water Quality Monitoring on Lake George. Lake George, New York, 1980 – 2009. (Boylen et al 2014)
Volume-weighted annual concentration of chloride in wet precipitation at Huntington Forest, NY (from NADP (2016) http://nadp.sws.uiuc.edu/data/ntn/plots/ntntrends.html?siteID=NY20)
2009 mean annual [Cl-] in Lake George was >350xs the volume-weighted [Cl-] in wetfall
-Long-term Watershed Case Study-
Finkle Brook Watershed
▪ Located on the west side of Lake
George (Town of Bolton) ▪ 7th largest watershed in the Lake
George drainage basin
Finkle Brook Watershed Case Study
▪ Surface area = 4.2 mi2
▪ Length of channel = 4.65 mi
▪ Mean basin slope = 903 ft/mi
▪ Mean annual ppt = 37 inches
▪ Mean annual runoff = 18 inches
Finkle Brook Watershed Case Study
▪ Began studying Finkle Brook and watershed in 1992
▪ Instrumented channel near outflow for continuous flow and automatic sample collection
▪ Collected base-flow and storm event samples for chemistry
▪ 1992-2005 – monitored 89 storm events and collected numerous base-flow chemistry samples
-Historical Information- Lake George Urban Runoff Study
▪ 3 Year Study (1980-1982) ▪ US EPA Nationwide Study (28 sites) ▪ South end of Lake George ▪ 7 Stream/Stormsewer Stations ▪ Direct drainage along shoreline ▪ 40+ Storm Events Sampled
-Historical Information- Lake George Urban Runoff Study
There is a direct relationship between areal loading and percent development
-Winter Road Maintenance- Lake George Drainage Basin
In the beginning (1960s-1970s), the primary winter de-icing compound was sand…..
…..and this was the result
By 2002, the volume of the Finkle Brook delta was
estimated to be >13,000 yd3
Finkle Brook Watershed Case Study Sources of Data
Fuhs - NYSDOH (1972)
LGUR Study- NYSDEC (1980-82)
Sutherland - NYSDEC (1991-2006)
Swinton - DFWI (2007-2010)
Sutherland and Navitsky (2013-16)
Finkle Brook Watershed Case Study Long-term Increase in Base-flow [Chloride]
Flow-weighted Base-flow [Cl-] at Outlet since 1970 Baseflow [Cl-] - Source & Outflow
R² = 0.7649
0
20
40
60
80
100
120
140
160
1970 1975 1980 1985 1990 1995 2000 2005 2010 2015
Conc
entr
atio
n in
mg/
L
Year
0.72
106.62
22.0
0.1
1.0
10.0
100.0
1000.0
EDGECOMB POND(above)
FINKLE AT OUTFLOW(below)
FUHS AT OUTFLOW(1970-71)
Conc
entr
atio
n in
mg/
L Sampling Station
Finkle Brook Watershed Case Study The Finkle Brook Corridor - Edgecomb Pond to Sawmill Bay
▪ DELINEATED 1,000-FT CORRIDOR FROM EDGECOMB POND TO SAWMILL BAY
▪ LENGTH OF CORRIDOR FROM POND TO SAWMILL BAY IS ~12,000 FEET
▪ SURFACE AREA OF CORRIDOR (EXCLUSIVE OF CHANNEL) = 260 ACRES
▪ ROADS WITHIN CORRIDOR = 15.5 ACRES, OR ~6 PERCENT OF TOTAL CORRIDOR AREA
Summary of Finkle Brook Watershed Case Study
▪ Roads adjacent to FB corridor are having an impact (sediment/nutrients) on the water quality of Finkle Brook and, ultimately, Lake George
▪ Sedimentation basins placed strategically along stream corridor will reduce the impact of sediment and adsorbed contaminants
▪ However, salt reduction only can occur through strict adherence to BMPs such as The S.A.V.E. Lake George Partnership
Current Basin-wide Research
▪ During the winter of 2015-2016, a greatly reduced snowpack and reduced application of road deicing material provided the opportunity to study the response of streams and their watersheds to these reductions
▪ Currently studying 14 watersheds; all 14 streams are sampled for [anions:cations] prior to flowing into Lake George; 11 streams also sampled above the developed area to provide base-flow [anions:cations]
▪ The FUND For Lake George is sponsoring this study
Finkle Brook - 2016
▪ Fuhs (1972) dataset most robust for meaningful statistics
▪ Sutherland (2001) data above Fuhs regressions, with S&N 2016 well above 2001 data for flow equivalent conditions
▪ 2016 base-flow (<2 cfs) [Cl-], [Na+] and [Ca+] are increasing
Current Basin-wide Research
0
0.5
1
1.5
2
2.5
0 5 10 15 20 25 30 35
meq
/L
flow, ft3/sec
meq Cl/L (Fuhs 1972)
meq Na/L (Fuhs 1972)
meq Ca/L (Fuhs 1972)
meq Cl/L (Sutherland 2001)
meq Ca/L (Sutherland 2001)
meq Cl/L (S&N 2016)
meq Na/L (S&N 2016)
meq Ca/L (S&N 2016)
THE FUTURE OF ROAD SALT IN THE LAKE GEORGE BASIN
• REDUCE THE USE • JOIN THE S.A.V.E. LAKE GEORGE PARTNERSHIP