Information regarding air emissions from shale gas development and production is critically important given production is now occurring in highly urbanized areas across the United States. Methane, the primary shale gas constituent, contributes substantially to climate change; other natural gas constituents are known to have adverse health effects. This study goes beyond previous Barnett Shale field studies by encompassing a wider variety of production equipment (wells, tanks, compressors, and separators) and a wider geographical region. The principal components analysis, unique to this study, provides valuable information regarding the ability to anticipate associated shale gas chemical constituents.
Soil and water (sludge) obtained from reserve pits used in unconventional natural gas mining was analyzed for the presence of technologically enhanced naturally occurring radioactive material (TENORM). Samples were analyzed for total gamma, alpha, and beta radiation, and specific radionuclides: beryllium, potassium, scandium, cobalt, cesium, thallium, lead-210 and -214, bismuth-212 and -214, radium-226 and -228, thorium, uranium, and strontium-89 and -90. Laboratory analysis confirmed elevated beta readings recorded at 1329 ± 311 pCi/g. Specific radionuclides present in an active reserve pit and the soil of a leveled, vacated reserve pit included 232Thorium decay series (228Ra, 228Th, 208Tl), and 226Radium decay series (214Pb, 214Bi, 210Pb) radionuclides. The potential for impact of TENORM to the environment, occupational workers, and the general public is presented with potential health effects of individual radionuclides. Current oversight, exemption of TENORM in federal and state regulations, and complexity in reporting are discussed.
An increasing number of children are born with intersex variation (IV; ambiguous genitalia/hermaphrodite, pseudohermaphroditism, etc.). Evidence shows that endocrine-disrupting chemicals (EDCs) in the environment can cause reproductive variation through dysregulation of normal reproductive tissue differentiation, growth, and maturation if the fetus is exposed to EDCs during critical developmental times in utero. Animal studies support fish and reptile embryos exhibited IV and sex reversal when exposed to EDCs. Occupational studies verified higher prevalence of offspring with IV in chemically exposed workers (male and female). Chemicals associated with endocrine-disrupting ability in humans include organochlorine pesticides, poly-chlorinated biphenyls, bisphenol A, phthalates, dioxins, and furans. Intersex individuals may have concurrent physical disorders requiring lifelong medical intervention and experience gender dysphoria. An urgent need exists to determine which chemicals possess the greatest risk for IV and the mechanisms by which these chemicals are capable of interfering with normal physiological development in children.
Carbon disulfide (CS2) has been historically associated with the
production of rayon, cellophane, and carbon tetrachloride. This study identifies
multiple mechanisms by which CS2 contributes to the formation of
CO2 in the atmosphere. CS2 and other associated
sulfide compounds were found by this study to be present in emissions from
unconventional shale gas extraction and processing (E&P) operations. The
breakdown products of CS2; carbonyl sulfide (COS), carbon monoxide
(CO), and sulfur dioxide (SO2) are indirect greenhouse gases (GHGs)
that contribute to CO2 levels in the atmosphere. The heat-trapping
nature of CO2 has been found to increase the surface temperature,
resulting in regional and global climate change. The purpose of this study is to
identify five mechanisms by which CS2 and the breakdown products of
CS2 contribute to atmospheric concentrations of CO2.
The five mechanisms of CO2 formation are as follows: Chemical Interaction of CS2 and hydrogen sulfide
(H2S) present in natural gas at high temperatures,
resulting in CO2 formation;Combustion of CS2 in the presence of oxygen producing
SO2 and CO2;Photolysis of CS2 leading to the formation of COS, CO, and
SO2, which are indirect contributors to
CO2 formation;One-step hydrolysis of CS2, producing reactive
intermediates and ultimately forming H2S and
CO2;Two-step hydrolysis of CS2 forming the reactive COS
intermediate that reacts with an additional water molecule,
ultimately forming H2S and CO2. CS2
and COS additionally are implicated in the formation of
SO2 in the stratosphere and/or troposphere.
SO2 is an indirect contributor to CO2
formation and is implicated in global climate change.
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