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2011  Northeast  Private Well  Water  Symposium   ,[object Object],[object Object],[object Object],[object Object],[object Object]
Getting The Waters Tested  The Marcellus Shale Factor Old Issues New Issues Environment Water Resources Private Wells In PA
B.F. Environmental  Consultants Inc. ,[object Object],[object Object],[object Object],[object Object]
Water-Research Center ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Carbon County Groundwater Guardians
Document Notice ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Goals ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],What ? 95 % drilled wells 5 % hand-dug and other
PA -Private Wells Not Regulated ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Lets Be Honest – We have Problems in Pennsylvania with Private Wells ,[object Object],[object Object],[object Object]
Properly Constructed Wells and Poorly Constructed Wells Confining Bed Sea Level Stagnant Water – no to little flow Saline Water Proper  Construction Brine Water 600 to 1200 ft Fresh Water Poorly Constructed
Some Private Well Photos
What is the Marcellus Shale Factor and Why a Citizen Database? ,[object Object],[object Object],[object Object],[object Object],[object Object],WE  Support the Citizen Groundwater Database at  Wilkes University !
This is Drinking Water in PA? Iron / Manganese Bacteria Sediment / Gases Corrosion 50% Other 50%
Before Marcellus Shale Development What was the Quality of Private Well Water? ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Not Just a Marcellus  Shale Issue
[object Object],Corrosive Water Low pH Soft Water (low hardness) to Moderate Hardness Iron and Manganese  Total Coliform Bacteria Sulfur Odors and  Methane- Biogenic and Thermogenic Gas (Tends to be < 10 mg/L) Some over 28 mg/L Contamination by VOCs, SOCs,  Glycols, Saline Water, and Radionuclides are NOT COMMON, but  saline water may influence  1 to 3 % of wells – This is 12,000 to  36,000 households in PA!
Goal of the Database ,[object Object],[object Object],[object Object],[object Object],[object Object]
Image Source: Luzernecounty.org Recent Baseline Testing in Luzerne County, PA 320 Private Wells Tested Conducted by Certified Laboratories Third Party Samplers Not Wilkes University Study Area
The Source of the Data I am Presenting Today Certified – Third Party Samplers All Testing Completed by Certified Laboratories Using  Approved Methods Samples include rigorous QC/QA including Blanks/ Duplicates All wells purged using Standards of Practice Purging Time Based on Stabilized Well Parameters (pH, conductivity, and temperature) The data is the baseline data that was done by EnCana. Homeowners had to approve releasing the data – over 90 % said  Yes.
Up to 3% influenced by Saline Water – These same samples have methane approaching 7 mg/L or more.  Source – Wilkes University Database Total Coliform (49%) 20%  E Coli. Positive Lead (22 %) Plasticizers (8%) Arsenic (6%)
Most Contamination appears to be associated with Total Coliform Bacteria ,[object Object],[object Object],[object Object],[object Object],[object Object],Therefore – In some cases - the Private Wells  are Facilitating Groundwater Contamination.
What are Phthalates? ,[object Object],[object Object],[object Object],[object Object],8 % have plasticizers above the drinking water standards
How ?  Not Sure – Here are Some Ideas ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Arsenic- up to 6 % Elevated Levels ,[object Object],[object Object],[object Object],[object Object],[object Object]
More Facts- Private Wells Issues Can / Does Impact Citizens Health ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Methane in Water ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Methane Gas Video from Salt Springs State Park – Fall 2010, by Brian Oram http:// www.friendsofsaltspringspark.org “At the base of the gorge is a bubbling salt spring, traces of an  1850s woolen mill, and mid-19th century farmhouses and barns.”  Go to: http://youtu.be/2QugRgXGdIQ
Methane Gas Migration- Not Related to Marcellus Shale Private Well Landfill Wetland 600 to  1200 ft 1200 to 3000+ ft Gas from Non-Marcellus Shale Groundwater Flow Lake
Rock Sample from Quarry – West of Dimock Sandstone Unit – Containing Plant Materials, Organic Muds – Possible Shallow Methane Source
Duke Study- “ Gas Well Drilling and   Hydraulic Fracturing&quot; by Osborn   ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Title is spin. If I told you your grade was 26.8 +/- 30 – Did you get a zero?
It looks like background methane levels may follow a linear/ curvilinear trend. Cabot – Quick Look
Bedrock Fractures and Fractured Zones High Yielding Well (High Methane ?) Fractured  Zone Lower Yielding Well (Low Methane?)
Purge Time, minutes C O N C E N T R A T I O N Methane Increases with Purge Time. How Many Private Well Owner Normally Let Water Run for 45 minutes
Methane Gas Migration Videos (2009 – Prior to Regulatory Change) ,[object Object],[object Object],[object Object],[object Object]
Some Marcellus Shale Issues ,[object Object],[object Object],[object Object],[object Object]
Marcellus Shale - Cartoons ,[object Object]
PSU Study -Migration and Disturbance During Drilling-  losing circulation Proper Construction Poor Construction Key Points 1. Proper Casing and Cement of Marcellus Shale Wells 2. Knowing How Private Wells Are Constructed 3. Isolation Distances will not Solve This Problem. 4. Fixing Private Wells has to be part of the Solution. 5. This may account for the data on bromide from PSU. 6. The issue may not be well radial distance, but construction and drilling issue. 7. Recommend closed loop drilling with water within freshwater aquifer (no muds) or water-based muds. up to 2000 ft Lined Pit Could this explain the  Bromide Issue??
Catskill Formation “ Bluestone Quarry – West of Dimock” Note – Preferential Flow Pathways Along Joints and Bedding Planes 80 feet
Migration Concepts- Multiple Casements and Recreate Confining Layers- Need Good Cement Bonds- Cement up to Deepest Casement or Surface Older Younger Water Table Private Well Confining Layer More Conventional  Reservoir Target
Could Radon Gas be a Good Surrogate for Methane Migration?  It cost less to test for Radon than Methane- Not Suggesting we Eliminate Methane- add Radon 9000 psi 4000 psi Is this Possible ? Very Deep Private Well- We have some that are 900 + feet deep
Note ,[object Object],[object Object]
Related to Marcellus Shale ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Problem – This does nothing to fix the Problems we have in  PA with Private Wells that is not caused by the Marcellus Shale Development.
What We Need in PA ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Things We Tried ,[object Object],[object Object],[object Object],[object Object]
DRASTIC Model
Correlation of DRASTIC and Incidences of Contamination Comparison of Relative DRASTIC index vulnerabilities to frequencies of the occurrence of Total Coliform contamination of Buda and Salansky well water samples- Thanks to Encana and the local private well owners. Poor Correlation. – I think poor well construction making wells more vulnerable than anticipated.
Again ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
New Community Resource Download a Free Copy (pdf) – email  [email_address] ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Add Your Data to the Citizen Database- Contact Mr. Brian Oram at  [email_address]  or  [email_address]
Announcements ,[object Object],[object Object],[object Object],[object Object],[object Object]
Baseline Testing- Critical Issues ,[object Object],[object Object],[object Object],[object Object]
Facebook Sites ,[object Object],[object Object],[object Object],[object Object]
Presented by: ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]

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Testing Private Wells for Contaminants in Northeast PA

  • 1.
  • 2. Getting The Waters Tested The Marcellus Shale Factor Old Issues New Issues Environment Water Resources Private Wells In PA
  • 3.
  • 4.
  • 5.
  • 6.
  • 7.
  • 8.
  • 9.
  • 10. Properly Constructed Wells and Poorly Constructed Wells Confining Bed Sea Level Stagnant Water – no to little flow Saline Water Proper Construction Brine Water 600 to 1200 ft Fresh Water Poorly Constructed
  • 12.
  • 13. This is Drinking Water in PA? Iron / Manganese Bacteria Sediment / Gases Corrosion 50% Other 50%
  • 14.
  • 15. Not Just a Marcellus Shale Issue
  • 16.
  • 17.
  • 18. Image Source: Luzernecounty.org Recent Baseline Testing in Luzerne County, PA 320 Private Wells Tested Conducted by Certified Laboratories Third Party Samplers Not Wilkes University Study Area
  • 19. The Source of the Data I am Presenting Today Certified – Third Party Samplers All Testing Completed by Certified Laboratories Using Approved Methods Samples include rigorous QC/QA including Blanks/ Duplicates All wells purged using Standards of Practice Purging Time Based on Stabilized Well Parameters (pH, conductivity, and temperature) The data is the baseline data that was done by EnCana. Homeowners had to approve releasing the data – over 90 % said Yes.
  • 20. Up to 3% influenced by Saline Water – These same samples have methane approaching 7 mg/L or more. Source – Wilkes University Database Total Coliform (49%) 20% E Coli. Positive Lead (22 %) Plasticizers (8%) Arsenic (6%)
  • 21.
  • 22.
  • 23.
  • 24.
  • 25.
  • 26.
  • 27. Methane Gas Video from Salt Springs State Park – Fall 2010, by Brian Oram http:// www.friendsofsaltspringspark.org “At the base of the gorge is a bubbling salt spring, traces of an 1850s woolen mill, and mid-19th century farmhouses and barns.” Go to: http://youtu.be/2QugRgXGdIQ
  • 28. Methane Gas Migration- Not Related to Marcellus Shale Private Well Landfill Wetland 600 to 1200 ft 1200 to 3000+ ft Gas from Non-Marcellus Shale Groundwater Flow Lake
  • 29. Rock Sample from Quarry – West of Dimock Sandstone Unit – Containing Plant Materials, Organic Muds – Possible Shallow Methane Source
  • 30.
  • 31. It looks like background methane levels may follow a linear/ curvilinear trend. Cabot – Quick Look
  • 32. Bedrock Fractures and Fractured Zones High Yielding Well (High Methane ?) Fractured Zone Lower Yielding Well (Low Methane?)
  • 33. Purge Time, minutes C O N C E N T R A T I O N Methane Increases with Purge Time. How Many Private Well Owner Normally Let Water Run for 45 minutes
  • 34.
  • 35.
  • 36.
  • 37. PSU Study -Migration and Disturbance During Drilling- losing circulation Proper Construction Poor Construction Key Points 1. Proper Casing and Cement of Marcellus Shale Wells 2. Knowing How Private Wells Are Constructed 3. Isolation Distances will not Solve This Problem. 4. Fixing Private Wells has to be part of the Solution. 5. This may account for the data on bromide from PSU. 6. The issue may not be well radial distance, but construction and drilling issue. 7. Recommend closed loop drilling with water within freshwater aquifer (no muds) or water-based muds. up to 2000 ft Lined Pit Could this explain the Bromide Issue??
  • 38. Catskill Formation “ Bluestone Quarry – West of Dimock” Note – Preferential Flow Pathways Along Joints and Bedding Planes 80 feet
  • 39. Migration Concepts- Multiple Casements and Recreate Confining Layers- Need Good Cement Bonds- Cement up to Deepest Casement or Surface Older Younger Water Table Private Well Confining Layer More Conventional Reservoir Target
  • 40. Could Radon Gas be a Good Surrogate for Methane Migration? It cost less to test for Radon than Methane- Not Suggesting we Eliminate Methane- add Radon 9000 psi 4000 psi Is this Possible ? Very Deep Private Well- We have some that are 900 + feet deep
  • 41.
  • 42.
  • 43.
  • 44.
  • 46. Correlation of DRASTIC and Incidences of Contamination Comparison of Relative DRASTIC index vulnerabilities to frequencies of the occurrence of Total Coliform contamination of Buda and Salansky well water samples- Thanks to Encana and the local private well owners. Poor Correlation. – I think poor well construction making wells more vulnerable than anticipated.
  • 47.
  • 48.
  • 49.
  • 50.
  • 51.
  • 52.

Hinweis der Redaktion

  1. The Marcellus Shale Factor is the reality that private wells in PA provide 1.5 Million citizens with water that does not meet a drinking water standard and as a state we have no real licensing program for well drillers, private well constructions standards, or the ability to fix wells that have been poortly cited and constructed – Part One – The Private Well Factor
  2. Water-soluble products that are placed on the land surface and in streams or surface impoundments Land Disposal Stockpiles and mine tailings Disposal of sewage and sludge Salt spreading Animal feedlots Fertilizers and pesticides Accidental spills Particulate matter from airborne sources Substances that are deposited in the ground above the water table Septic systems, cesspools, and privies. Surface impoundments and lagoons Landfills Waste disposal in excavations Leakage from underground storage tanks Leakage from underground pipelines Artificial recharge Sumps and dry wells Grave yards Disposal, storage, or extraction of materials below the water table Waste disposal in wet excavations Drainage wells and canals Abandoned and exploration wells Water supply wells Waste disposal wells Mines
  3. DRASTIC is a groundwater quality model for evaluating the pollution potential of large areas using the hydrogeologic settings of the region (Aller et al., 1985, Aller et al., 1987, Deichert et al., 1992). This model was developed by EPA and NWWA in the 1980&apos;s. A hydrogeologic setting is defined as a mappable unit with common hydrogeologic characteristics. This model employs a numerical ranking system that assigns relative weights to various parameters that help in the evaluation of relative groundwater vulnerability to contamination. DRASTIC is an acronym for the seven hydrogeologic weighted factors used in a rating system that produces a numerical value called the DRASTIC index. The seven parameters are depth to water (D), net recharge (R), aquifer media (A), soil media (S), topography (T), impact of the vadose zone media (I), and hydraulic conductivity of the aquifer (C). Higher DRASTIC index values relate to a specific area of greater potential to pollution and contamination while lower DRASTIC index values indicate a specific area of lower potential to pollution and contamination. DRASTIC includes various hydrogeologic settings which influence the pollution potential of a region. The higher the DRASTIC index, the greater the relative pollution potential. The DRASTIC index can be further divided into four categories: low, moderate, high, and very high. The sites with high and very high categories are more vulnerable to contamination and consequently need to be managed more closely. The weights assigned are relative, therefore a site with a low pollution potential may still be susceptible to groundwater contamination but it is less susceptible to contamination compared to the sites with high DRASTIC ratings.
  4. If there is a positive correlation, then we should s