On June 24, 2013, Robert Jackson, the Nicholas Professor of
Global Environmental Change at Duke University, published a study that detailed
the relationship between methane, propane and ethane found in drinking water
wells, and the proximity of the well to hydraulic fracturing sites. The 2013
study followed a 2011 study of sixty drinking water wells in the northeast Pennsylvania
Marcellus region. After it was published, the 2011 study received criticism
from the gas industry for not testing enough wells, and failing to
demonstrate that the increased levels of methane were a given consequence of
drilling, rather than faulty well casing or cementing. The 2013 study surveyed
an additional 81 wells in the region, including wells from Ostego County in New
York (where fracking has not been conducted).
The study showed an increased concentration of methane gas
in drinking water from wells closer to a drilling site. Specifically, water
wells within one kilometer of gas wells exhibited six times the concentration
of methane of other wells. The methane gas in the water wells consistently bore
a thermogenic signature (which matches signatures of methane trapped in the
deeper shale formations currently being drilled), rather than a biogenic
signature (which matches shallower pockets of methane).
The study offered two explanations for the increased
presence of methane. First, it acknowledged the possibility of inadequate steel
casings in gas wells; and second, it suggested imperfections in cement sealings
between casings in gas wells could be responsible for the methane’s presence in
water wells.
For more information on the study, visit the website
for the Proceedings of the National Academy of Sciences (PNAS).
Written by: Garrett Lent, Research Assistant
Written by: Garrett Lent, Research Assistant
Agricultural Law Resource and Reference Center
June 2013
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