Hemlock-Canadice UMP – NYS Dept. of Environmental Conservation

Hemlock-Canadice UMP – NYS Dept. of Environmental Conservation.

Putting Local Aquifer Protections in Place in New York

Putting Local Aquifer Protections in Place in New York.

 

 

March 16, 2013

Putting Local Aquifer Protections in Place

A USGS report released this week on the hydrogeology of the aquifer system in the Susquehanna River Valley in parts of Broome and Chenango Counties, New York highlights the role of aquifer protection in the context of gas drilling impacts. In the section, “Considerations for Aquifer Protection,” the report states:

“Aquifer protection in the study area is a topic of public concern in relation to the potential for natural gas drilling in this part of New York. Aquifer protection efforts likely will focus on currently used resources. Information provided in this report may help managers prioritize protection of largely unused aquifers whose characteristics suggest that they are capable of providing large public or commercial water supplies.” p. 17.

In the press release accompanying the report, the author of the report, USGS scientist Paul Heisig, states,”This study is intended to put basic facts into the hands of those tasked with making decisions on future groundwater use and protection. We have identified and mapped a variety of aquifer types and described their current use and their potential as groundwater sources.”

Local officials and concerned citizens in the study area now have excellent information to assist efforts to put appropriate aquifer protections in place. Because the study area is located in an area that is likely to be the target of some of the first high volume horizontal hydrofracking (HVHF) activity in New York if HVHF is allowed to go forward in the state, if local aquifer protections are sought in the area, such efforts should be initiated quickly.

The report and accompanying maps are among the most detailed and comprehensive reports and maps yet produced in the ongoing effort of USGS and the DEC to issue detailed maps of New York’s aquifers. The report fills a gap in that effort. The report maps the section of the Susquehanna River Valley shown between sections 10 and 33 on the map below of the detailed reports produced so far. Another report recently released by USGS on the Cayuta Creek and Catatonk Creek valley aquifers, fills the gap above sections 32 and 27 on the map below.

One of the most important aspects of the newly released Susquehanna River valley aquifer report is the detailed consideration given to the upland watersheds and the fractured bedrock aquifers in those watersheds. The report points out the close connections between the uplands and the valley aquifers:

“If water quality in those streams [flowing from the uplands] is compromised by activites in the upland watershed, groundwater quality in the valley may, in turn, be degraded; therefore, the maintenance of good water quality in the upland watersheds that are the source of these streams is an important aspect of protecting the Susquehanna River valley-fill aquifer system.”

While a number of communities in New York have put aquifer protection strategies in place, many more communities are becoming aware of the need to do so and are looking at protection options. I spoke about watershed protection options recently at a program in Elmira on Feb. 22, 2013, and am scheduled to speak again on the topic at a program in Candor on March 27, 2013. Some of the options I discussed were zoning to create aquifer protection districts, establishing critical environmental areas under the State Environmental Quality Review Act regulations, obtaining sole source aquifer status from the federal EPA, establishing municipal compacts and setting up watershed protection associations. Slides and notes from my presentation in Elmira are posted on my law office website.

Posted by Rachel Treichler at 03/16/13 12:30 PM

Copyright 2013, Rachel Treichler

USGS Scientific Investigations Report 2012-5282: Hydrogeology of the Susquehanna River Valley-Fill Aquifer System and Adjacent Areas in Eastern Broome and Southeastern Chenango Counties, New York

USGS Scientific Investigations Report 2012-5282: Hydrogeology of the Susquehanna River Valley-Fill Aquifer System and Adjacent Areas in Eastern Broome and Southeastern Chenango Counties, New York.

Prepared in cooperation with New York State Department of Environmental Conservation

Hydrogeology of the Susquehanna River Valley-Fill Aquifer System and Adjacent Areas in Eastern Broome and Southeastern Chenango Counties, New York

By Paul M. Heisig

Thumbnail of and link to report PDF (3.56 MB)Abstract

The hydrogeology of the valley-fill aquifer system along a 32-mile reach of the Susquehanna River valley and adjacent areas was evaluated in eastern Broome and southeastern Chenango Counties, New York. The surficial geology, inferred ice-marginal positions, and distribution of stratified-drift aquifers were mapped from existing data. Ice-marginal positions, which represent pauses in the retreat of glacial ice from the region, favored the accumulation of coarse-grained deposits whereas more steady or rapid ice retreat between these positions favored deposition of fine-grained lacustrine deposits with limited coarse-grained deposits at depth. Unconfined aquifers with thick saturated coarse-grained deposits are the most favorable settings for water-resource development, and three several-mile-long sections of valley were identified (mostly in Broome County) as potentially favorable: (1) the southernmost valley section, which extends from the New York–Pennsylvania border to about 1 mile north of South Windsor, (2) the valley section that rounds the west side of the umlaufberg (an isolated bedrock hill within a valley) north of Windsor, and (3) the east–west valley section at the Broome County–Chenango County border from Nineveh to East of Bettsburg (including the lower reach of the Cornell Brook valley). Fine-grained lacustrine deposits form extensive confining units between the unconfined areas, and the water-resource potential of confined aquifers is largely untested.

Recharge, or replenishment, of these aquifers is dependent not only on infiltration of precipitation directly on unconfined aquifers, but perhaps more so from precipitation that falls in adjacent upland areas. Surface runoff and shallow groundwater from the valley walls flow downslope and recharge valley aquifers. Tributary streams that drain upland areas lose flow as they enter main valleys on permeable alluvial fans. This infiltrating water also recharges valley aquifers.

Current (2012) use of water resources in the area is primarily through domestic wells, most of which are completed in fractured bedrock in upland areas. A few villages in the Susquehanna River valley have supply wells that draw water from beneath alluvial fans and near the Susquehanna River, which is a large potential source of water from induced infiltration.

First posted February 20, 2013

  • Appendix 1 XLS (864 kB)
    Well data for Susquehanna River valley and adjacent uplands, eastern Broome and southeastern Chenango Counties, New York.
  • Plate 1 html
    Hydrogeology of the Susquehanna valley-fill aquifer system and adjacent areas in eastern Broome and southeastern Chenango Counties, New York

For additional information contact:
Director
U.S. Geological Survey
New York Water Science Center
425 Jordan Road
Troy, NY 12180
(518) 285-5600
http://ny.water.usgs.gov

COMMENTS
What the USGS are saying is that these three regions/locations are prime for “developers” (AKA drillers) to sink MAJOR water wells to supply frack operations. This paper relates to what I heard a Senior SRBS scientist present last year, that SRBC was quite concerned that as gas drilling moved North from PA it would be getting to the “headwaters regions (low water volume) of the Susq and other rivers and thus they anticipated more emphasis by the drillers to use groundwater for their fracking uses.
This directly goes to the issue of impacts on water quantity of residential and public water wells; that is what will a big mother of a “comercial” well by a driller do to the QUANTITY of water available from your private well.  In other words, will your water well dry up?
This is an issue that is NOT adressed at all in NYS draft regs OR the rdSGEIS – only pre-drill baseline testing of wells near(1000ft) a proposed well pad need be tested by the driller for QUALITY.
The potential impact on private property values is clear; mitigation by drilling a private well deeper would probably work, although I dont know enoug hydrology to float a boat, so to speak.
————————————
“Unconfined aquifers with thick saturated coarse-grained deposits are the most favorable settings for water-resource development, and three several-mile-long sections of valley were identified (mostly in Broome County) as potentially favorable: (1) the southernmost valley section, which extends from the New York–Pennsylvania border to about 1 mile north of South Windsor, (2) the valley section that rounds the west side of the umlaufberg (an isolated bedrock hill within a valley) north of Windsor, and (3) the east–west valley section at the Broome County–Chenango County border from Nineveh to East of Bettsburg (including the lower reach of the Cornell Brook valley).”
————————————
Finally, this water source/quantity issue will apply equally to regions further north of the NY/PA border, and one hope USGS is studying such; remember, drilling a bit north likely wont be marcellus but rather the deeper Utica Shale.
S
Stan Scobie, Binghamton, NY, 607-669-4683

Putting Local Aquifer Protections in Place in New York. Rachel Treichler

Injection Wells: The Poison Beneath Us – ProPublica

Injection Wells: The Poison Beneath Us – ProPublica.

Poisoning the Well: How the Feds Let Industry Pollute the Nation’s Underground Water Supply – ProPublica

Poisoning the Well: How the Feds Let Industry Pollute the Nation’s Underground Water Supply – ProPublica.

Oil and gas: Water flows to money in drought-stricken drilling regions — 07/30/2012 — www.eenews.net

Oil and gas: Water flows to money in drought-stricken drilling regions — 07/30/2012 — www.eenews.net.

Water supplies OK, despite Ohio drought | Mansfield News Journal | mansfieldnewsjournal.com

Water supplies OK, despite Ohio drought | Mansfield News Journal | mansfieldnewsjournal.com.

Drought strains U.S. oil production – Jul. 31, 2012

Drought strains U.S. oil production – Jul. 31, 2012.

The Fight Over Fracking in Colorado’s North Fork Valley – Businessweek

The Fight Over Fracking in Colorado’s North Fork Valley – Businessweek.

Pacific Institute: Hydraulic Fracturing and Water Resources: Separating the Frack from the Fiction

Pacific Institute: Reports.

Hydraulic Fracturing and Water Resources: Separating the Frack from the Fiction

 

fracking_cover_small.jpgHydraulic fracturing, or “fracking,” has generated growing controversy in the past few years. New research from the Pacific Institute finds the real issues around its impacts on water are shared by stakeholders from government to industry to environmental groups – and point to the need for better and more transparent information in order to clearly assess the key water-related risks and develop sound policies to minimize those risks.

Much of the public attention on hydraulic fracturing has centered on the use of chemicals in the fracturing fluids and the risk of groundwater contamination. But the new study finds that while chemical disclosure can be useful for tracking contamination, risks associated with fracking chemicals are not the only issues that must be addressed. The massive water requirements for fracking and the potential conflicts with other water needs, including for agriculture and for ecosystems, pose major challenges. Methane contamination of drinking water wells is also a concern according to some field studies, as are the serious challenges associated with storing, transporting, treating, and disposing of wastewater.

The report Hydraulic Fracturing and Water Resources: Separating the Frack from the Fiction is a detailed assessment and synthesis of existing research on fracking as well as the results of interviews with representatives from state and federal agencies, industry, academia, environmental groups, and community-based organizations from across the United States. Interviewees identified a broad set of social, economic, and environmental concerns, foremost among which are impacts of hydraulic fracturing on the availability and quality of water resources.

“Despite the diversity of viewpoints among the stakeholders interviewed, there was surprising agreement about the range of concerns associated with hydraulic fracturing. Among the most commonly cited were concerns about spills and leaks, wastewater management, and water withdrawals,” said Heather Cooley, co-director of the Pacific Institute Water Program. “In addition to concerns about impacts on water resources, social and economic concerns were identified as well, such as worker health and safety and community impacts associated with rapidly industrializing rural environments.”

Hydraulic fracturing refers to the process by which fluid is injected into wells under high pressure to create cracks and fissures in rock formations that improve the production of these wells. Energy analysts, including the Energy Information Administration (EIA), project that the United States will become increasingly reliant on natural gas, with production projected to increase by nearly 30% over the next 25 years.

The growth in natural gas production is driven by a dramatic increase in domestic shale gas production, and by 2021, the United States is projected to be a net exporter of natural gas ( U.S. EIA 2012). The rapid development of unconventional natural gas resources – such as shale – has been largely facilitated through the use of directional (horizontal) drilling and hydraulic fracturing.

Hailed by some as a game-changer that promises increased energy independence, job creation, and lower energy prices, fracking has led others to call for a temporary moratorium or a complete ban due to concern over potential environmental, social, and public health impacts. The research finds that the lack of credible and comprehensive data and information is a major impediment to a robust analysis of the real concerns associated with hydraulic fracturing.

“Much of what has been written about the interaction of hydraulic fracturing and water resources is either industry or advocacy reports that have not been peer-reviewed, and the discourse around the issue to date has been marked by opinion and obfuscation,” said Cooley. “More and better research is needed to clearly assess the key water-related risks associated with hydraulic fracturing and develop sound policies to minimize those risks.”

Based in Oakland, California, the Pacific Institute is a nonpartisan research institute that works to create a healthier planet and sustainable communities. Through interdisciplinary research and partnering with stakeholders, the Institute produces solutions that advance environmental protection, economic development, and social equity – in the West, nationally, and internationally. www.pacinst.org.

Download the full report.
Download the Executive Summary.
Download the press release.