Our study revealed a type of saline water
in shallow aquifers, particularly along valleys in northeastern Pennsylvania, that resemble the unique geochemical composition of the Marcellus brine.
As expected, the youngest water is concentrated
in the shallowest aquifer layers and the proportion of young water decreases with depth.
Not exact matches
But Clarens says fracking fluids could theoretically leak into
aquifers, because the wells must be dug through
shallow layers where the
aquifers lie
in order to reach shales.
«The requirements weren't as rigorous, the testing wasn't as rigorous and
in some cases the
shallow aquifers were contaminated,» Kobelski said.
The hydraulic fracturing process — pushing gallons upon gallons of chemical - laden water into shale rock
in order to bubble up natural gas — takes place deep
in the ground, thousands of feet below the earth's surface and thousands of feet below the
shallow aquifers that provide drinking water.
Groundwater studies
in shallow, porous
aquifers using CFCs were conducted by, for example, Busenberg and Plummer, Cook et al., and Oster et al..
Active biogenic methanogenis is widespread
in shallow fresh water
aquifers thoughout the planet.
My concern is that many will read the title, «Geochemical evidence for possible natural migration of Marcellus Formation brine to
shallow aquifers in Pennsylvania,» and immediately infer that residual treatment water (i.e., frack fluid) is most likely to leak into groundwater from depths of several thousand feet.
A large percentage of the 20 + million engine pump wells
in operation
in India were drilled manually and pump from
shallow aquifers that are refilled each monsoon.
In contrast to La Nina induced
shallow -
aquifer effects, deep
aquifers have been filled with meltwater from the last Ice Age, and that water is slowly and steadily seeping back into the oceans today.
In some parts of the coastal area having very
shallow immobile and continuous fresh water
aquifers and scat - tered population, drinking water supply by means very low cost VSST and SST has been proved successful.
But
in the coastal area, the salinity distributions
in ground water and replenishment of water
in deep and
shallow aquifers are regulated by complex hydrogeolog - ical phenomena.
In some cases, difficulty arises in determining the safe yield capacity of the shallow aquifer
In some cases, difficulty arises
in determining the safe yield capacity of the shallow aquifer
in determining the safe yield capacity of the
shallow aquifers.
The
shallowest aquifer is usually not used because of contamination risks, but it has a lot of advantages
in terms of receiving recharge and requiring less energy to use, as long as you don't drink it.
Mean values ± standard deviation of methane concentrations (as milligrams of CH4 L - 1) and carbon isotope composition
in methane
in shallow groundwater δ13C - CH4 sorted by
aquifers and proximity to gas wells (active vs. nonactive)
Given the intimate connection between river water and widespread alluvial
aquifers it is clear that there must be stong seasonal change
in «
shallow groundwater» temperature many metres below the surface.