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Blas L. Valero-Garcés Kathleen R. Laird Sherilyn C. Fritz Kerry Kelts Emi Ito Eric C. Grimm 《Quaternary Research》1997,48(3):359-369
Seismic stratigraphy, sedimentary facies, pollen stratigraphy, diatom-inferred salinity, stable isotope (δ18O and δ13C), and chemical composition (Sr/Ca and Mg/Ca) of authigenic carbonates from Moon Lake cores provide a congruent Holocene record of effective moisture for the eastern Northern Great Plains. Between 11,700 and 950014C yr B.P., the climate was cool and moist. A gradual decrease in effective moisture occurred between 9500 and 710014C yr B.P. A change at about 710014C yr B.P. inaugurated the most arid period during the Holocene. Between 7100 and 400014C yr B.P., three arid phases occurred at 6600–620014C yr B.P., 5400–520014C yr B.P., and 4800–460014C yr B.P. Effective moisture generally increased after 400014C yr B.P., but periods of low effective moisture occurred between 2900–280014C yr B.P. and 1200–80014C yr B.P. The data also suggest high climatic variability during the last few centuries. Despite the overall congruence, the biological (diatom), sedimentological, isotopic, and chemical proxies were occassionally out of phase. At these times the evaporative process was not the only control of lake-water chemical and isotopic composition. 相似文献
123.
Water wells were sampled near North Madison, Ohio, following a gas well blow out that injected large amounts of CH4 into near-surface groundwater Chemical analyses showed elevated levels of Fe+2, Mn+2, Ca+2, sulfide, alkalinity, and pH, and low levels of dissolved oxygen, SO4
−2, and NO3
− in CH4-affected wells compared to unaffected wells. Sulfate reduction is quantitatively the most important vehicle for CH4 oxidation Equilibrium thermodynamic computer models were used to simulate groundwaters from the North Madison area Model
results showed that CH4 is oxidized to HCO3
−, SO4
−2 is reduced, iron and manganese oxides are reduced and dissolved, and pH increases These simulations are in excellent agreement
with trends observed in the field data A laboratory experiment was designed to simulate CH4
− perturbed groundwater in the methane-perturbed system, sulfide increased significantly, providing direct evidence for methane
oxidation by sulfate reduction
Although suitable anaerobic methane-oxidizing bacteria have not been isolated from groundwater aquifers, the combination of
field data, laboratory experiment, and computer simulation form a convincing argument that CH4 perturbation of aquifers can and does affect groundwater chemistry 相似文献
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Ajay Jasra David A. Stephens Kerry Gallagher Christopher C. Holmes 《Mathematical Geology》2006,38(3):269-300
In this paper we develop a generalized statistical methodology for characterizing geochronological data, represented by a distribution of single mineral ages. The main characteristics of such data are the heterogeneity and error associated with its collection. The former property means that mixture models are often appropriate for their analysis, in order to identify discrete age components in the overall distribution. We demonstrate that current methods (e.g., Sambridge and Compston, 1994) for analyzing such problems are not always suitable due to the restriction of the class of component densities that may be fitted to the data. This is of importance, when modelling geochronological data, as it is often the case that skewed and heavy tailed distributions will fit the data well. We concentrate on developing (Bayesian) mixture models with flexibility in the class of component densities, using Markov chain Monte Carlo (MCMC) methods to fit the models. Our method allows us to use any component density to fit the data, as well as returning a probability distribution for the number of components. Furthermore, rather than dealing with the observed ages, as in previous approaches, we make the inferences of components from the “true” ages, i.e., the ages had we been able to observe them without measurement error. We demonstrate our approach on two data sets: uranium-lead (U-Pb) zircon ages from the Khorat basin of northern Thailand and the Carrickalinga Head formation of southern Australia. 相似文献
126.
Kerry L. Sublette J. Bryan Tapp J. Berton Fisher Eleanor Jennings Kathleen Duncan Greg Thoma Josh Brokaw Tim Todd 《Applied Geochemistry》2007
For almost a decade the Tallgrass Prairie Preserve in Oklahoma has been used as a field laboratory for the investigation of aspects of the remediation and restoration of oil and brine spills. Objectives of this work have included: (1) simplification of the remediation process and lowering the cost of remediation; (2) the development of methods to accelerate or jump-start the restoration process; and (3) determining appropriate metrics for assessing the status of soil ecosystem recovery. This research has resulted in a number of lessons learned that will be presented here which can be exported to other exploration and production sites, especially sites located in sensitive ecosystems. Key observations have included the role of a fertilizer amendment in linking the remediation and restoration process at an oil-impacted site, the use of nematodes as ecological indicators in the restoration of oil- and brine-impacted sites, and the development of a two-stage process for remediation of brine impacted sites that does not include significant use of gypsum. 相似文献
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Juan Armando Flores de la Torre Kerry Mitchell Magdalena Samantha Ramos Gómez Alma Lilian Guerrero Barrera Laura Yamamoto Flores Francisco Javier Avelar González 《Environmental Earth Sciences》2018,77(10):386
Concentrations of Pb and Zn, plant uptake of these metals, the influence of the plants’ growth on the physicochemical properties and metal concentrations in the tailings of an abandoned 300-year-old mine tailing dam in Zacatecas, Mexico were investigated. Tailings were found to be heavily contaminated, with average levels of 2621 ± 53 and 3827 ± 83 mg/kg for Pb and Zn, respectively (maximum concentrations of 8466 ± 116 and 12,475 ± 324 mg/kg, respectively), exceeding international standards. Though physico-chemical conditions (pH, conductivity, redox potential, moisture, organic matter, nitrate, nitrite, ammonium nitrogen, total nitrogen, phosphorus and sulfates) do not favor the development of vegetation, some plants have adapted to these adverse conditions. Moreover, there was a significant reduction of Pb and Zn concentration in the rhizosphere (between 10–78% for Pb and 18–62% for Zn, depending on plant species). Sporobolus airoides showed average biomass concentrations of 173 ± 2 and 313 ± 6 mg/kg, for Pb and Zn, respectively; which implies a risk for mobility and possible incorporation into the food chain. Barcleyanthus salicifolius, Asclepsias linaria and Cortaderia selloana on the other hand, showed average biomass concentrations of 28 ± 3 and 121 ± 5 mg/kg of Pb and Zn, respectively, thus representing a lower biomagnification risk. The effect of these plants to reduce metal concentrations in the rhizosphere, improve physico-chemical conditions in metal polluted substrates, but with limited metal accumulation in biomass, suggests that they can be evaluated for use in stabilizing metal polluted tailings. 相似文献
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