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Effects of Precipitation on the Acid Mine Drainage Impacted Hewett Fork Watershed Understanding Storm Response Ze b Ma rtin Ohio Unive rsity Contents Project Overview Objectives of the Research Project Area Background of


  1. Effects of Precipitation on the Acid Mine Drainage Impacted Hewett Fork Watershed Understanding Storm Response Ze b Ma rtin Ohio Unive rsity

  2. Contents Project Overview • Objectives of the Research • Project Area • Background of Literature • Methodology • Results • Conclusion • Recommendations •

  3. Project Overview • Examination of storm response in an AMD impacted streams using new and emerging auto-sampler technologies, to track and analyze the changing geochemical environment within AMD receiving streams over the course of selected storm events.

  4. Objectives of the Research • Study the storm response of water quality in AMD impacted streams. • Determine if flushing events impair water quality and go untreated by remediation efforts. • Provide data that reflects how the water chemistry is changing in real time during a storm. • Fill a knowledge gap in current theories of what is limiting biological recovery.

  5. Project Area

  6. Hewett Fork • Drainage area of 104.89 square kilometers • 79.6 percent forest cover • Headwater stream and second largest tributary to Raccoon Creek at 24.8 km long. • The headwaters of Raccoon Creek are among the worst mine-related problems in Ohio • Approximately 1,200 acres of abandoned mines and coal refuse piles are located within the drainage basin. • Currently being actively remediated by lime doser

  7. Selected Field Sites • Three major AMD inputs are treated at a single location in Carbondale, OH., and discharges into Hewett Fork at field site HF129 . • HF090 is 4.5 km downstream of HF129, and represents the downstream extent of the mixing zone where limited biological recovery can be seen. • HF039 is 11.4 km downstream of HF129, and represents the zone in which water quality and biological metrics are both being met

  8. Field Sites HF039 HF129 HF090

  9. Background • What does the literature say? o Most research based on annual loading • Does not account for geochemical changes during storms • High flows are critical because they are associated with high loads o Grab samples • Does not account for geochemical changes during storms • Safety risk • Cost o Limited biological recovery • Episodic events • Extended mixing zone

  10. Methods: Data Collection • HF129 – Diver and Baro o Depth, pH, conductivity, and temperature • HF090, HF039 - two auto-samplers paired with YSI data sondes o pH, conductivity, temperature, TDS • HF190, HF120, HF090, HF039 - Flow measurements o Marsh-McBirney Model 2000 Flo-Mate o Recorded in feet per second

  11. Auto-Samplers

  12. Methods: Storm Sampling • 8 sampling events sampled from 5/1/16 – 12/6/16 Seasons based on water year o • 4 spring storms 2 summer storms • 2 Fall storms • • Sampling was triggered by a predicted precipitation event =< 1cm o EPA recommends 72 hours in between sampling • Collected 1 sample every hour for 24 hours using auto- samplers o Collected a total of 216 samples at HF039 o Collected a total of 192 samples at HF090

  13. Methods: Discharge • USGS Bolins Mills gauge station data used to create hydrograph for 2016 o Used to determine water year seasons • Flow measurements were collected 7 times at HF039 and HF090 o Discharge calculated using velocity-area method o Equipment failure at HF039

  14. Water Year 2016

  15. Discharge

  16. Methods: Lab Analysis • Collected water samples were split o Analyzed at ISEE Lab at OU • Preserved in 20% nitric acid at <4°C • Analyzed for total Al, As, Ba, Ca, Cd, Co, Cr, Cu, Fe, K, Mg, Mn, Na, Ni, Pb, Sr, and Zn on ICP-OES (iCAP 6300 Duo) o Analyzed in Watershed Lab at OU • Purged of air and stored at <4°C • Analyzed for Acidity (Hach 8202), Alkalinity (820), Sulfate (8051)

  17. What is Storm Response? • Purging and Sparing ~ Lewis & Grant 1979 • Sparing – removal of oxygen from the reaction site due to flooding • Purging – flushing of accumulated oxidation products by storm run-off • Is that it? o Mixed o Consistent

  18. Storm Response: F=Flushing, D=Dilution, M=Mixed, & C=Consistent

  19. Similar Responses • Primary Response Groups o Flushing • Al, Fe, K, & Mn o Dilution • Ca, Mg*, Na, Sr, & Sulfate o Consistent • Ba o Mixed • Net Acidity

  20. Net Acidity Response

  21. Net Acidity Response

  22. Net Acidity Response

  23. Primary Flush: 4/30/16 – 5/1/16 Fe HF039 Al HF039 10 4000 3 4000 3500 2.5 8 Discharge (L/s) 3000 3000 Al (mg/L) Fe (mg/L) 2 2500 6 1.5 2000 2000 4 1500 1 1000 1000 2 0.5 500 0 0 0 0 0 5 10 15 20 25 0 5 10 15 20 25 Time Time Fe2+ Discharge L/s Al3+ Discharge L/s Fe HF090 Al HF090 10 500 3 500 8 400 Discharge (L/s) 2.5 400 Al (mg/L) Fe (mg/L) 2 6 300 300 1.5 4 200 200 1 2 100 100 0.5 0 0 0 0 0 5 10 15 20 25 0 5 10 15 20 25 Time Time Al3+ Discharge L/s Fe2+ Discharge L/s

  24. Primary Dilution: 4/30/16 – 5/1/16 Mg HF039 Ca HF039 4000 12 4000 45 3500 3500 11 Discharge (L/s) 3000 3000 40 Ca (mg/L) Mg (mg/L) 10 2500 2500 2000 35 9 2000 1500 1500 8 1000 30 1000 7 500 500 25 0 6 0 0 5 10 15 20 25 0 5 10 15 20 25 Time Time Ca HF090 Mg HF090 Ca2+ Discharge L/s Mg2+ Discharge L/s 500 12 500 45 11 400 400 Discharge (L/s) 40 Mg (mg/L) Ca (mg/L) 10 300 300 9 35 200 200 8 30 100 100 7 6 0 25 0 0 5 10 15 20 25 0 5 10 15 20 25 Time Time Ca2+ Discharge L/s Mg2+ Discharge L/s

  25. Diverging response: 6/4/16 – 6/5/16 HF039 HF039 3 1350 0.45 1340 Discharge (L/s) 0.4 1320 2.5 Fe (mg/L) Al (mg/L) 1300 0.35 1300 2 0.3 1280 0.25 1260 1.5 1250 0.2 1240 1 0.15 1220 1200 0.1 1200 0.5 0.05 1180 0 1160 0 1150 HF090 HF090 0.45 3.0 3 3.0 Discharge (L/s) 0.4 2.5 2.5 2.5 Fe (mg/L) Al (mg/L) 0.35 2.0 2.0 0.3 2 1.5 1.5 0.25 1.5 1.0 0.2 1.0 1 0.15 0.5 0.5 0.1 0.5 0.0 0.0 0.05 0 -0.5 0 -0.5 Fe Discharge l/s Al Discharge l/s

  26. Diverging response: 6/4/16 – 6/5/16 HF039 Mg HF039 1340 80 1350 12 Discharge (L/s) 1320 Mg (mg/L) 1300 10 Ca (mg/L) 60 1300 1280 8 1260 40 1250 6 1240 1220 4 20 1200 1200 2 1180 0 1160 0 1150 HF090 HF090 3.0 80 3.0 Discharge (L/s) 12 2.5 2.5 Ca (mg/L) 10 60 2.0 Mg (mg/L) 2.0 8 1.5 1.5 40 6 1.0 1.0 4 0.5 0.5 20 2 0.0 0.0 0 -0.5 0 -0.5 Mg Discharge l/s Ca Discharge l/s

  27. Inconsistent Metals • No primary response displayed o As – only detected at HF039 during 9/28/16 – 9/29/16 o Cu – 4/30/16 – 5/1/16, 9/28/16 – 9/29/16, & 10/20/16 – 10/22/16 o Ni – only detected during 10/20/16 – 10/22/16 o Pb - only detected at HF039 during 9/28/16 – 9/29/16 o Zn – 7/28/16 – 7/29/16, 9/28/16 – 9/29/16, 10/20/16 – 10/22/16, & 12/5/16 – 12/6/16

  28. Critical Conditions • Acidic flushes were seen in the spring and fall storms downstream at the downstream site • Al and Fe also flush during the early spring and early fall storms at the downstream site • Al and Fe consistently flushed at the upstream site throughout the study

  29. Conclusions • Storm response in AMD impacted watersheds is important to understand • Precipitation is not the ultimate driver of response pattern • Response patterns differ between parameters, seasons, sites, and antecedent conditions • Antecedent soil conditions may be responsible for determining response patterns

  30. Recommendations • Watershed managers working in AMD impacted streams should implement storm flow monitoring to better understand the fate and transport of pollutant materials through their watersheds • Further studies should be completed to understand the interactions of precipitation run-off events and soil moisture content

  31. Questions?

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