Download presentation
Presentation is loading. Please wait.
Published byDylan McCarthy Modified over 9 years ago
1
Shingle Creek Chloride TMDL Abby Morrisette and Josh Kuhn 9/10/11
2
Shingle Creek
3
Why is Chloride a Problem? TMDL focuses on Chloride Inhibits osmo- regulatory processes – “Pickles” organism Evidence of decreased invertebrate IBI
4
Chloride Limit Shingle Creek is Class 2 water for protection of aquatic life Limits: – Acute: 860 mg/L for one hour duration – Chronic: 230 mg/L over four day average
5
Major Sources: Road Deicing Private Industrial and Residential Deicing Salt piles Railway and Airport Deicing Minor Sources/Transport Mechanisms: Groundwater Discharge From Infiltration Natural Sources Water Softeners and Septic Systems Landfills Fertilizer Sources of Chloride
6
The TMDL Study
7
Sampling Sampled from Dec 2002-August 2003 Assessed historical data – Flows at USGS Queen Avenue Bridge station from May 1996 to December 1998 – Groundwater chloride concentrations from a 1996 USGS study
8
Conductivity and flow recorded every 15 minutes Chloride samples collected biweekly and during runoff events.
9
Quality Control Conductivity loggers calibrated 3x/year – measurements within 10% of conductivity standards. Duplicate samples demonstrated <10% difference.
10
Data Filling Gaps in data due to frozen conditions and broken data loggers Gaps filled using regression equations relating the site with the USGS Queen Avenue station Summer and fall data used to estimate winter discharge. – Spring equations run separately.
11
GIS Area of roads calculated using GIS. Salt applications recorded by Municipality plow drivers used to calculate total salt applications.
12
Salt Piles Evaluated for runoff and salt composition.
13
All point sources are de minimis thus not assigned a waste load allocation.
14
Conclusions from the Study
17
Source Allocation 87% Road Salt!!!!
19
“MPCA believes using the 71% target is a conservative assumption that overestimates the chloride reduction needed to achieve WQSs.”
20
TMDL critiques Places where we thought assumptions and methods were unsound
21
Chloride-Conductivity Correlation This is a questionable relationship, with R=0.80 The graphical fit appears to underestimate high chloride R values are lower in winter
22
Lack of Groundwater Analysis “…groundwater interactions with surface waters in the Shingle Creek watershed have not been thoroughly studied.” ~Page 6.10 of TMDL report
23
Lack of Groundwater Analysis Load duration curves indicate that groundwater chloride is at standard
24
Lack of Groundwater Analysis USGS study of shallow wells indicates temporally variable chloride concentrations from 4.3-370 mg/L Relationship between surface chloride and groundwater chloride is assumed linear – No data or calculations
25
Sampling Gaps No data collected from September to November For broken data loggers, flows were interpolated from Queen Avenue station, assuming linear regression Almost all winter flows interpolated, not measured
26
Queen Avenue Station Analysis Flow from Queen Ave Station does not account for ~6 mi 2 of the watershed – Exclusion accounts for highly developed areas – Flow at Queen Ave may not be linearly related to other flows in the watershed, as assumed
27
TMDL Summary
28
Shingle Creek is seasonally impaired for Chloride
29
Recommended Chloride Reduction 71% reduction of chloride, allocated according to source analysis – Over-estimate
30
Is this realistic?
31
Big Task 71% reduction will require significant resources Reducing road salt could be a public safety hazard – Alternatives salts could be more hazardous than chloride
32
Questionable Data? We need a better understanding of groundwater transport in the watershed A lot of major assumptions and interpolations were made Link between IBI and chloride is weak
33
Questions?
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.