Unconventional natural gas resources offer an opportunity to access a relatively clean fossil fuel that could potentially lead to energy independence for some countries. Horizontal drilling and hydraulic fracturing make the extraction of tightly bound natural gas from shale formations economically feasible. These technologies are not free from environmental risks, however, especially those related to regional water quality, such as gas migration, contaminant transport through induced and natural fractures, wastewater discharge, and accidental spills. We review the current understanding of environmental issues associated with unconventional gas extraction. Improved understanding of the fate and transport of contaminants of concern and increased long-term monitoring and data dissemination will help manage these water-quality risks today and in the future.
The dynamics of granular activated carbon (GAC) adsorbers
for the uptake of gas-phase mercury was evaluated as a
function of temperature, influent mercury concentration,
and empty bed contact time. Sulfur-impregnated
carbons
exhibited enhanced mercury removal efficiency over virgin
carbon due to the formation of mercuric sulfide on the
carbon
surface. The effect of the sulfur impregnation method
on mercury removal efficiency was examined through experi
ments conducted on commercially available sulfur-impregnated carbon (HGR) and carbon impregnated with
sulfur in our laboratory (BPL-S). Although HGR and
BPL-S
possess similar sulfur contents, BPL-S is impregnated at a
higher temperature, which promotes a more uniform
distribution of sulfur in the GAC pore structure. At
low
influent mercury concentrations and low temperatures,
HGR and BPL-S performed similarly in the removal of
mercury
gas. However, as the temperature was increased above
the melting point of sulfur, the performance of HGR
deteriorated significantly, while the performance of BPL-S
slightly improved. At high influent mercury
concentrations,
HGR performed better than BPL-S, regardless of
temperature.
For both HGR and BPL-S, the observed dynamic mercury
adsorptive capacities were far below the capacities
predicted by the stoichiometry of mercuric sulfide
formation.
In HGR carbon the sulfur is very accessible, but ag
glomeration that occurs at high temperatures causes the
sulfur to be relatively unreactive. In BPL-S carbon,
on
the other hand, the sulfur remains in a highly reactive
form,
but its location deep in the internal pores makes it
relatively
inaccessible and prone to blockage by HgS formation.
Microbial communities associated with produced water from hydraulic fracturing are not well understood, and their deleterious activity can lead to significant increases in production costs and adverse environmental impacts. In this study, we compared the microbial ecology in prefracturing fluids (fracturing source water and fracturing fluid) and produced water at multiple time points from a natural gas well in southwestern Pennsylvania using 16S rRNA gene-based clone libraries, pyrosequencing, and quantitative PCR. The majority of the bacterial community in prefracturing fluids constituted aerobic species affiliated with the class Alphaproteobacteria. However, their relative abundance decreased in produced water with an increase in halotolerant, anaerobic/facultative anaerobic species affiliated with the classes Clostridia, Bacilli, Gammaproteobacteria, Epsilonproteobacteria, Bacteroidia, and Fusobacteria. Produced water collected at the last time point (day 187) consisted almost entirely of sequences similar to Clostridia and showed a decrease in bacterial abundance by 3 orders of magnitude compared to the prefracturing fluids and produced water samplesfrom earlier time points. Geochemical analysis showed that produced water contained higher concentrations of salts and total radioactivity compared to prefracturing fluids. This study provides evidence of long-term subsurface selection of the microbial community introduced through hydraulic fracturing, which may include significant implications for disinfection as well as reuse of produced water in future fracturing operations.
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