Unconventional oil
and gas development (UOGD) sometimes impacts
water resources, including incidents of methane (CH4) migration
from compromised wells and spills that degrade water with salts, organics,
and metals. We hypothesized that contamination may be more common
where UOGD overlaps with legacy coal, oil, and gas extraction. We
tested this hypothesis on ∼7000 groundwater analyses from the
largest U.S. shale gas play (Marcellus), using data mining techniques
to explore UOGD contamination frequency. Corroborating the hypothesis,
we discovered small, statistically significant regional correlations
between groundwater chloride concentrations ([Cl]) and UOGD proximity
and density where legacy extraction was extremely dense (southwestern
Pennsylvania (SWPA)) but no such correlations where it was minimal
(northeastern Pennsylvania). On the other hand, legacy extraction
of shallow gas in SWPA may have lessened today’s gas leakage,
as no regional correlation was detected for [CH4] in SWPA.
We identify hotspots where [Cl] and [CH4] increase by 3.6
and 3.0 mg/L, respectively, per UOG well drilled in SWPA. If the [Cl]
correlations document contamination via brines leaked from wellbores,
impoundments, or spills, we calculate that thallium concentrations
could exceed EPA limits in the most densely developed hotspots, thus
posing a potential human health risk.
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