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Evaluation of Geology and Water Well Data Associated with the EPA Hydraulic Fracturing
Retrospective Case Study, Bradford County, PA
Deborah Watkins, P.E. and Thomas Cornuet, P.G. July 24, 2012
12M-0159
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Background Information
Hydrogeology and Historical Water Quality in Bradford Co., PA
Historical and Baseline Groundwater Data Evaluation
Study Well Evaluation
Conclusions
Discussion Topics for Today’s Presentation
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EPA is conducting a retrospective hydraulic fracturing study in Bradford and Susquehanna Cos. - During the first sampling event, EPA collected samples from
37 groundwater locations in October and November of 2011 - A second sampling event was conducted in April 2012; data are
currently being evaluated and are not included in this presentation
A third party contractor collected split samples with the EPA for accessible sample locations; many sample locations could not be accessed because:
- EPA deemed confidential - Property owner would not allow access
Certified commercial laboratories used EPA approved analytical methods
Background Information
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Objective: - Evaluation of analytical data for 15 Bradford Co, PA groundwater
sample locations to determine if they have been impacted by unconventional shale gas development
Scope: - Evaluate hydrogeology and summarize historical water quality data
in Bradford Co.
- Compare EPA Study Well data to historical water quality and available pre-drill/baseline data sets
- Identify exceedances of EPA and PADEP water quality screening criteria for historical and baseline data sets
Presentation: - Provides a brief overview of evaluation including methane
WESTON Evaluation
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Hydrogeology and Historical Water Quality
in Bradford Co, PA
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Bradford County Geology
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Prepared prior to commercial unconventional shale gas development in Bradford Co.
A comprehensive study of the hydrogeology and groundwater quality of Bradford, Potter, and Tioga Cos. conducted by the USGS beginning in 1983
Describes hydrogeologic conceptual model and provides a large and thorough historical/background database of water quality data for unconsolidated stratified drift glacial deposits and the Lock Haven and Catskill bedrock formations
Bradford Co. Hydrogeology and Geochemistry USGS Report (Williams et al, 1998)
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Catskill Formation : 9 EPA split sample locations Lock Haven Formation: 6 EPA split sample locations
Devonian-age interbedded shale, siltstone, and sandstone
Catskill underlies much of the uplands of Bradford Co. and Lock Haven underlies most of the major valleys
Lock Haven water typically considered hard and often naturally high in arsenic, barium, chloride, iron, manganese, sodium, and TDS
Catskill and Lock Haven Formations
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Restricted groundwater flow zones: - Naturally occurring
- Water quality is affected by aquifer formation geochemistry, water residence time, recharge, and depth of occurrence
- Highly mineralized or poor water quality (often Na-Cl or Na-HCO3 water types)
- Often exhibits elevated hydrogen sulfide and methane concentrations
Typically found in major stream and river valleys, mostly in Catskill and Lock Haven bedrock formations
Water quality typically contains barium, chloride, iron, manganese, radium, sodium, strontium, and TDS which commonly exceed screening criteria
Bradford Co. Hydrogeology “Restricted Groundwater Flow Zones”
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Historical and Baseline Groundwater Data Evaluation
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Database No. of Wells* Sample Dates Classifications**
National Water Information System (NWIS) – inorganics
169 1935-2006 Catskill, Lock Haven Formations
National Uranium Resource Evaluation (NURE) - inorganics
160 October 1977 Catskill, Lock Haven Formations
USGS Water Resources Report 68 (Wms 1998) - inorganics
108 1935-1986 Detailed geologic classifications***
Baseline Data (near sample locations) – inorganics and BTEX
3,773 9/17/2009 – 1/10/2012
Divided into Central, Eastern, and
Western Regions
Databases
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*Includes only wells in Bradford Co. in the Catskill and Lock Haven Formations. **Geologic units assigned based on bedrock occurrence; geographic regions used for
retrospective study wells. ***Includes Catskill Formation, Lock Haven Formation, stratified drift (confined
and unconfined), and restricted flow zone.
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Baseline Sampling Program Near Retrospective Wells
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PA Statewide Groundwater Information System (PAGWIS) query cross referenced 83% of NWIS wells
PA Geologic Survey (PGS) spatial query used to classify remaining wells (17% of NWIS; all of NURE)
PGS spatial query used to identify wells potentially within stratified drift (within stratified drift footprint and < 120 feet deep)
If depth not known, defaulted to bedrock formation
Geologic Classification for NURE, NWIS, and Study Wells
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Screening Levels for Select Parameters
Parameter PADEP Act 2* EPA MCL EPA SMCL EPA
Regional**
Aluminum (mg/L) 0.2 15.5
Arsenic (mg/L) 0.01 0.01 0.000045
Chloride (mg/L) 250
Iron (mg/L) 0.3 10.9
Lead (mg/L) 0.005 0.015***
Lithium (mg/L) 0.073 0.031
Manganese (mg/L) 0.3 0.05 0.322
pH (pH units) 6.5-8.5
TDS (mg/L) 500
Turbidity (NTU) 5
Total Coliform (col/100 ml) 1
*Residential use wells < 2,500 mg/l TDS **Screening levels for tap water (chronic) ***Action level
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Parameters Historical USGS Databases
Baseline Database
Aluminum √ √ Arsenic √ √ Barium √ √ Chloride/TDS(1) √ √ Iron √ √ Lead √ √ Lithium Limited data √ Manganese √ √ pH √ √ Sodium √ √ Strontium(1) Limited data √ Turbidity Limited data √
Parameters that Frequently Exceeded Water Quality Screening Criteria in Historical and Regional Baseline Databases (pre 2006)
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(1) In the Restricted Flow Zone
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Region N
umbe
r of S
ampl
es
Num
ber o
f Det
ectio
ns
% o
f Det
ectio
ns
Max
imum
(mg/
L)
Mea
n (m
g/L)
Med
ian
(mg/
L)
Tota
l Num
ber >
3 m
g/L
Tota
l Num
ber >
7 m
g/L
Tota
l Num
ber >
20
mg/
L
Central Region 1965 526 26.8% 43.3 3.27 0.36 233 98 25
Eastern Region 570 157 27.5% 40.7 4.14 0.52 45 30 11
Western Region 1238 504 40.7% 72.1 4.12 0.70 274 125 30
Comparison of Baseline Methane Levels with Screening Levels of 3 mg/L, 7 mg/L, and 20 mg/L
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Study Well Evaluation
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Study well data included pre-drill baseline samples, additional post-drill samples, and EPA retrospective split samples
All study well data were compared to Applicable Water Quality Criteria
- Heavy Metals (As, Ba, Fe, Mn, etc.)
- Inorganics (Cl, TDS, Na, SO4, etc.)
- Organics (VOCs, SVOCs, etc.)
For 12 groundwater locations, post-drill data were compared to regional baseline data for those sample locations
For all 15 groundwater locations, available data were compared to historical USGS databases and regional baseline data
Study Well Parameters Evaluated
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Time Plot of Chloride - Property Owner E (115 ft. Well)
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Time Plot of Iron - Property Owner E (115 ft. Well)
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Time Plot of Manganese - Property Owner E (115 ft. Well)
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Time Plot of Sodium - Property Owner E (115 ft. Well)
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Time Plot of TDS - Property Owner E (115 ft. Well)
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Time Plot of Barium - Property Owner E (115 ft. Well)
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Time Plot of Methane - Property Owner G
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Time Plot of Methane - Property Owner H
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Time Plot of Methane – Property Owner I
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Conclusions
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The 15 groundwater sample locations do not appear to be impacted by natural gas drilling or production activities - For all 15 groundwater sample locations, water quality data was typical of
water quality concentrations in historical USGS databases and regional baseline data
- There are no significant increases in inorganic and other water quality parameters when comparing data from each of the 12 study wells with available baseline data
- There are no significant increases in dissolved methane when comparing data from each of the 12 study wells with available baseline data
- Few organics were detected - None of these are attributable to natural gas production activities or exceeded applicable drinking water standards
Similar to the historical/baseline databases, the15 sample locations contained aluminum, arsenic, barium, chloride, iron, lead, lithium, manganese, pH, sodium, strontium, and turbidity; in several instances, these naturally occurring concentrations exceeded EPA and/or PADEP screening criteria
Conclusions
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Boyer, EW, Swistock, BR, Clark, J, Madden, M and DE Rizzo, 2011. The Impact of Marcellus Gas Drilling on Rural Drinking Water Supplies, Center for Rural Pennsylvania, March 2012.
Focazio, MJ, Welch, AH, Watkins, SA, Helsel, DR and MA Horn, 2000. A Retrospective Analysis on the Occurrence of Arsenic in Ground-Water Resources of the United States and Limitation in Drinking-Water-Supply Characterizations, Water Resources Investigations Report 99-4270, USGS.
Low, DJ. and DG Galeone, 2007. Reconnaissance of Arsenic Concentrations in Ground Water from Bedrock and Unconsolidated Aquifers in Eight Northern-Tier Counties of Pennsylvania, Open-File Report 2006-1376, USGS.
Swistock, BR, Clemens, S and WE Sharpe, 2009. Drinking Water Quality in Rural Pennsylvania and the Effect of Management Practices, Center for Rural Pennsylvania, January 2009.
Watkins, DM, and TS Cornuet, 2012. Evaluation of Geology and Water Well Data Associated with the EPA Hydraulic Fracturing Retrospective Case Study, Bradford County, Pennsylvania, April 2012. http://www.chk.com/News/Articles/Documents/ 20120529_CHK_WestonStudy_BradfordPA.pdf
Williams, JE, Taylor, LE and DJ Low, 1998. Hydrogeology and Groundwater Quality of the Glaciated Valleys of Bradford, Tioga, and Potter Counties, Pennsylvania, PA Geological Survey and USGS, Water Resources Report 68.
Williams, JH, 2010. Evaluation of Well Logs for Determining the Presence of Freshwater, Saltwater and Gas above the Marcellus Shale in Chemung, Tioga, and Broome Counties, New York, USGS, Scientific Investigations Report 2010-5224.
References
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Thank You!
Questions?
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