Relevant bibliographies by topics / Environmental biogeochemistry

Academic literature on the topic 'Environmental biogeochemistry'

Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Environmental biogeochemistry"

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Osborn, D. "Environmental biogeochemistry." Biological Conservation 32, no. 2 (1985): 189–90. http://dx.doi.org/10.1016/0006-3207(85)90085-0.

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Poorter, R. P. E. "Environmental biogeochemistry." Palaeogeography, Palaeoclimatology, Palaeoecology 52, no. 1-2 (November 1985): 179–80. http://dx.doi.org/10.1016/0031-0182(85)90049-5.

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Tardy, Y. "Environmental biogeochemistry." Earth-Science Reviews 22, no. 3 (November 1985): 243. http://dx.doi.org/10.1016/0012-8252(85)90065-0.

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Inskeep, William P. "Diversity of Environmental Biogeochemistry." Journal of Environmental Quality 21, no. 3 (July 1992): 513. http://dx.doi.org/10.2134/jeq1992.00472425002100030038x.

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Greenland, D. J. "Diversity of Environmental Biogeochemistry." Geoderma 58, no. 3-4 (October 1993): 245. http://dx.doi.org/10.1016/0016-7061(93)90045-m.

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Bianchi, Thomas S., Madhur Anand, Chris T. Bauch, Donald E. Canfield, Luc De Meester, Katja Fennel, Peter M. Groffman, Michael L. Pace, Mak Saito, and Myrna J. Simpson. "Ideas and perspectives: Biogeochemistry – some key foci for the future." Biogeosciences 18, no. 10 (May 19, 2021): 3005–13. http://dx.doi.org/10.5194/bg-18-3005-2021.

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Abstract. Biogeochemistry has an important role to play in many environmental issues of current concern related to global change and air, water, and soil quality. However, reliable predictions and tangible implementation of solutions, offered by biogeochemistry, will need further integration of disciplines. Here, we refocus on how further developing and strengthening ties between biology, geology, chemistry, and social sciences will advance biogeochemistry through (1) better incorporation of mechanisms, including contemporary evolutionary adaptation, to predict changing biogeochemical cycles, and (2) implementing new and developing insights from social sciences to better understand how sustainable and equitable responses by society are achieved. The challenges for biogeochemists in the 21st century are formidable and will require both the capacity to respond fast to pressing issues (e.g., catastrophic weather events and pandemics) and intense collaboration with government officials, the public, and internationally funded programs. Keys to success will be the degree to which biogeochemistry can make biogeochemical knowledge more available to policy makers and educators about predicting future changes in the biosphere, on timescales from seasons to centuries, in response to climate change and other anthropogenic impacts. Biogeochemistry also has a place in facilitating sustainable and equitable responses by society.
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Ashraf, Muhammad Aqeel, and Muhammad Faheem. "Environmental toxicology and biogeochemistry of ecosystems." Environmental Science and Pollution Research 27, no. 30 (April 12, 2020): 37173–75. http://dx.doi.org/10.1007/s11356-020-08699-z.

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Xia, Xuelian, Yanguo Teng, and Yuanzheng Zhai. "Biogeochemistry of Iron Enrichment in Groundwater: An Indicator of Environmental Pollution and Its Management." Sustainability 14, no. 12 (June 9, 2022): 7059. http://dx.doi.org/10.3390/su14127059.

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Iron (Fe) is one of the most biochemically active and widely distributed elements and one of the most important elements for biota and human activities. Fe plays important roles in biological and chemical processes. Fe redox reactions in groundwater have been attracting increasing attention in the geochemistry and biogeochemistry fields. This study reviews recent research into Fe redox reactions and biogeochemical Fe enrichment processes, including reduction, biotic and abiotic oxidation, adsorption, and precipitation in groundwater. Fe biogeochemistry in groundwater and the water-bearing medium (aquifer) often involves transformation between Fe(II) and Fe(III) caused by the biochemical conditions of the groundwater system. Human activities and anthropogenic pollutants strongly affect these conditions. Generally speaking, acidification, anoxia and warming of groundwater environments, as well as the inputs of reducing pollutants, are beneficial to the migration of Fe into groundwater (Fe(III)→Fe(II)); conversely, it is beneficial to the migration of it into the media (Fe(II)→Fe(III)). This study describes recent progress and breakthroughs and assesses the biogeochemistry of Fe enrichment in groundwater, factors controlling Fe reactivity, and Fe biogeochemistry effects on the environment. This study also describes the implications of Fe biogeochemistry for managing Fe in groundwater, including the importance of Fe in groundwater monitoring and evaluation, and early groundwater pollution warnings.
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Hmielowski, Tracy. "Synchrotron Radiation-Based Methods for Environmental Biogeochemistry." CSA News 62, no. 11 (November 2017): 10–16. http://dx.doi.org/10.2134/csa2017.62.1110.

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Bargagli, Roberto, Fabrizio Monaci, and Charlie Bucci. "Environmental biogeochemistry of mercury in Antarctic ecosystems." Soil Biology and Biochemistry 39, no. 1 (January 2007): 352–60. http://dx.doi.org/10.1016/j.soilbio.2006.08.005.

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Dissertations / Theses on the topic "Environmental biogeochemistry"

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Frost, Thomas. "Environmental controls of air-water gas exchange." Thesis, University of Newcastle Upon Tyne, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.299423.

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Rebecca, Steely L. "BIOGEOCHEMISTRY OF LAKE ERIE SEDIMENT AND PORE WATER." Case Western Reserve University School of Graduate Studies / OhioLINK, 2015. http://rave.ohiolink.edu/etdc/view?acc_num=case1429549600.

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Park, Eun Joo. "Metal Speciation, Mixtures and Environmental Health Impacts." Thesis, Harvard University, 2015. http://nrs.harvard.edu/urn-3:HUL.InstRepos:23205169.

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Numerous applications of heavy metal have caused to their wide contamination in the environmental system and raised serious concerns over potential harmful effects on public health and the environment. Water, sediment, and dietary food are the main exposure media of heavy metal pollution and key determinants of adverse human and environmental health effects. Heavy metal(s) toxicity and speciation involve various mechanistic features with specific media and some of them are not clearly investigated. In particular, biological effects such as toxicity are not related to the total concentration of heavy metals in media, and many laboratory and field studies have supported this supposition. Organisms respond to the bioaccessible and bioavailable fraction of metals only, not the total concentration. The bioaccessibility and bioavailability of toxicants are dependent on chemical properties of the contaminant, the many exposure pathways, and temporal variability of these variables with respect to uptake by the target organism. Usually, bioavailable fractions are estimated using chemical or biological approaches. For this study, biological approaches were performed to better ascertain the toxic effects of heavy metals on organisms. A better understanding of bioaccessibility and bioavailability can be a useful tool in exposure and risk assessment. Therefore, this study presents experimental designs focusing on assessing of the bioaccessibility and bioavailability of metals in aquatic, benthic organisms and dietary food. This study also examines the role of metal mixtures on the adverse effects of metals.
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Morrissey, Ember. "Environmental regulation of tidal wetland microbial communities and associated biogeochemistry." VCU Scholars Compass, 2013. http://scholarscompass.vcu.edu/etd/3300.

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Microbial communities play an essential role in carrying out the biogeochemical cycles that sustain life on Earth, yet we know very little about their ecology. One question of particular interest is how environmental conditions shape microbial community structure (i.e., the types of organisms found in the community and their relative abundance), and whether such changes in structure are related to biogeochemical function. It is the aim of this dissertation to address this question via the examination of carbon (C) and nitrogen (N) cycling in wetland ecosystems, which due to their diverse hydrology have a profound influence on biogeochemical cycles. With respect to N cycling, the community structure of denitrification- and dissimilatory nitrate reduction to ammonium (DNRA)-capable organisms was evaluated in response to changes in resource availability, specifically organic matter (OM) and nitrate (NO3-), using an in situ field manipulation. Interactive regulation of microbial community composition was exhibited in both groups, likely due to variation in C substrate preferences and NO3- utilization efficiency. Subsequent experimentation considering only denitrification revealed that resource regulation of activity rates was mediated through changes in denitrifier community composition. The resource regulation of wetland C cycling also was evaluated using an in situ OM manipulation. OM characteristics (e.g., degree of decomposition) affected microbial extracellular enzyme activity (EEA) and changed the community structure of bacteria, archaea, and methanogens. These changes were linked with carbon dioxide and methane production via a conceptual model diagramming the importance of microbial community structure and EEA in greenhouse gas production. The investigation of C cycling in wetlands was extended to consider an important global change threat: saltwater intrusion into freshwater tidal wetlands. Bacterial community structure and EEA were examined along a natural salinity gradient. Salinity was strongly associated with bacterial community structure and positively correlated with EEA. These results suggested that salinity-induced increases in decomposition were responsible for reduced soil OM content in more saline wetlands. This work demonstrates that microbial communities in wetlands are structured by environmental conditions including resource availability and salinity. Further, the research provides evidence that environmental regulation of important biogeochemical processes in wetlands (e.g., methanogensis, denitrification, etc.) is mediated through changes in microbial community structure.
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Zang, Xu. "Encapsulation of Proteinaceous materials in Macromolecular Organic Matter as a mechanism for environmental preservation /." The Ohio State University, 2001. http://rave.ohiolink.edu/etdc/view?acc_num=osu1486400446370061.

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Li, Miling. "Environmental Origins of Methylmercury in Aquatic Biota and Humans." Thesis, Harvard University, 2016. http://nrs.harvard.edu/urn-3:HUL.InstRepos:27201754.

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Methylmercury (MeHg) is a neurotoxin found in fish and shellfish, that poses risks to human and ecological health. Exposure to MeHg adversely affects neurodevelopment of children and cardiovascular health in adults. Seafood consumption is the primary exposure route to MeHg in North America. An understanding of the link between environmental MeHg sources and human exposures is needed to determine the impacts of ongoing environmental change. However, few data exist for relating environmental exposures to human health outcomes. Imprecision in dietary recall data on fish consumption and variability in MeHg concentrations within and across seafood species consumed have made it challenging to accurately identify sources of human MeHg exposure. In addition, the diverse environmental sources of MeHg production in ecosystems make it more difficult to quantitatively attribute human exposures to specific environments where methylation is taking place. My doctoral dissertation uses naturally occurring mercury (Hg) stable isotopes to characterize sources of MeHg exposure in aquatic biota and human populations. The objectives of my work are to (1) explore the utility of Hg stable isotopes in human hair as a novel method for tracing sources of MeHg exposure to humans; (2) examine drivers of the internal body burden of MeHg in frequent seafood consumers; (3) refine understanding of environmental MeHg sources for estuarine fish. My first dissertation chapter characterizes the magnitude of mass-dependent fractionation between seafood and consumers and shows Hg stable isotopes in human hair is a promising tool for estimating different Hg exposure sources (e.g., coastal vs. oceanic fish). My second chapter uses dietary survey data and Hg isotopes in hair from high-frequency seafood consumers to show that differences in in vivo demethylation do not explain variability in biomarker concentrations. I infer that absorption efficiencies for MeHg in seafood are very low for some high-frequency fish consumers and hypothesize that this is caused by interactions with co-ingested foods. The last chapter investigates diverse Hg stable isotope signatures in benthic, riverine and pelagic estuarine fish and uses these signatures to better characterize the relative importance of different environmental MeHg sources.
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Blodau, Christian. "Carbon biogeochemistry in northern peatlands : regulation by environmental and biogeochemical factors." Thesis, McGill University, 2001. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=38154.

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Nitrogen and sulfur deposition and water table level fluctuations have the potential to influence the C biogeochemistry in peatlands. Processes in peatland mesocosms were examined under steady state and dynamic conditions at different rates of N and S deposition, and water table levels. Net turnover rates were calculated from diffusive-advective mass-balances of pore water constituents. The limitations of the approach were tested with tracer experiments, which showed that diffusive-advective transport adequately described the flow of dissolved substances in peat columns. Incubation experiments quantified potential CO2, CH4, DOC, H2S and Fe 2+ production rates.
The vegetation assimilated most of the deposited nitrogen and sulfate when water table levels were high. Lowered water table levels resulted in seepage of sulfate to the water table, reduced the rates of photosynthesis, and increased the soil respiration rates. The potential for sulfate reduction was fairly large, despite small in situ sulfate concentrations, and the CO2 production could not be fully accounted for by known processes. Potential rates of sulfate reduction were large both in samples taken from the field site and from the controlled experiments. SO42- addition resulted partly in stimulation, partly in reduction of potential CH4 production rates suggesting that the relationship between sulfate reduction and methanogenesis is not exclusively competitive.
Changes of the water table level had in situ effects on CO2 and CH4 production rates not explainable by a distinction in aerobic/anaerobic conditions. Anaerobic in situ rates at greater depths were much lower when the water table was at the surface of the mesocosms than when it was at greater depths. This might have been due to in situ accumulation of CO2 and CH 4 in the deeper peat, which lowers the energy gain of anaerobic C mineralization. Flooding and draining of peat soil resulted in a delayed onset of CH 4 production, in increased anaerobic CO2 production and decreased CH4 production rates, and in the decoupling of gas exchange from production rates. These results document that fluctuations of environmental variables on short time scales have an impact on rates of C turnover in peat soils, and also limit the predictability of fluxes by statistical models.
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Dias, Isobelle A. "The environmental biogeochemistry of open ocean and partially enclosed marine systems." Thesis, University of Bristol, 1990. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.303738.

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Amasah, Reda. "Studies on the environmental microbiology and biogeochemistry of desert surface soils." Thesis, University of Sheffield, 2012. http://etheses.whiterose.ac.uk/2769/.

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Microorganisms play a key role in the functioning of the environment, particularly in relation to the biogeochemical cycles. Here, a study was made of the microbial activity of primitive desert surface soils in comparison with that exhibited by a fertile agricultural loam soil. The microbial transformations studied included nitrification, the hydrolysis of urea, the oxidation of elemental sulphur to sulphate and phosphate solubilisation; these processes were collectively used to study the biogeochemical activity of desert surface soils. Bacterial population densities in the desert surface soils, fertile loam soils and volcanic, cave rock samples were also determined. A variety of bacterial isolates from desert surface soils and cave rock samples have been identified using molecular identification techniques like DNA extraction, PCR amplification, determinations of 16S and 18S rRNA gene sequences. The isolation and characterization of extremophilic bacterial strains from a dormant volcano on the island of Reunion is reported, using molecular identification, morphological and physiological studies. As the area of the volcano, from which these bacteria were isolated, has not been recently active, it was considered of interest to determine if these bacteria grow, or merely survive, in a mesophilic environment. Nuclear magnetic resonance spectroscopy (NMR) was used to study the compatible solutes in these isolates when growing under high temperatures, low and high pH stresses and at various concentrations of NaCl. Finally, various environmental samples were tested in order to detect the presence of Mycoplasma using an EZ-PCR Mycoplasma Test Kit.
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Juice, Stephanie. "The Environmental Microbiome In A Changing World: Microbial Processes And Biogeochemistry." ScholarWorks @ UVM, 2020. https://scholarworks.uvm.edu/graddis/1181.

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Climate change can alter ecosystem processes and organismal phenology through both long-term, gradual changes and alteration of disturbance regimes. Because microbes mediate decomposition, and therefore the initial stages of nutrient cycling, soil biogeochemical responses to climate change will be driven by microbial responses to changes in temperature, precipitation, and pulsed climatic events. Improving projections of soil ecological and biogeochemical responses to climate change effects therefore requires greater knowledge of microbial contributions to decomposition. This dissertation examines soil microbial and biogeochemical responses to the long-term and punctuated effects of climate change, as well as improvement to decomposition models following addition of microbial parameters. First, through a climate change mesocosm experiment on two soils, I determined that biogeochemical losses due to warming and snow reduction vary across soil types. Additionally, the length of time with soil microbial activity during plant dormancy increased under warming, and in some cases decreased following snow reduction. Asynchrony length was positively related to carbon and nitrogen loss. Next, I examined soil enzyme activity, carbon and nitrogen biodegradability, and fungal abundance in response to ice storms, an extreme event projected to occur more frequently under climate change in the northeastern United States. Enzyme activity response to ice storm treatments varied by both target nutrient and, for nitrogen, soil horizon. Soil horizons often experienced opposite response of enzyme activity to ice storm treatments, and increasing ice storm frequency also altered the direction of the microbial response. Mid-levels of ice storm treatment additionally increased fungal hyphal abundance. Finally, I added explicit microbial parameters to a global decomposition model that previously incorporated climate and litter quality. The best mass loss model simply added microbial flows between litter quality pools, and addition of a microbial biomass and products pool also improved model performance compared to the traditional implicit microbial model. Collectively, these results illustrate the importance of soil characteristics to the biogeochemical and microbial response to both gradual climate change effects and extreme events. Furthermore, they show that large-scale decomposition models can be improved by adding microbial parameters. This information is relevant to the effects of climate change and microbial activity on biogeochemical cycles.
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Books on the topic "Environmental biogeochemistry"

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Biogeochemistry of the world's land. Moscow: Mir Publishers, 1994.

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Feng, Xionghan, Wei Li, Mengqiang Zhu, and Donald L. Sparks, eds. Advances in the Environmental Biogeochemistry of Manganese Oxides. Washington, DC: American Chemical Society, 2015. http://dx.doi.org/10.1021/bk-2015-1197.

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C, Adriano D., ed. Biogeochemistry of trace metals. Boca Raton: Lewis Publishers, 1992.

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Bedřich, Moldan, Černý Jiří V, International Council of Scientific Unions. Scientific Committee on Problems of the Environment., and United Nations Environment Programme, eds. Biogeochemistry of small catchments: A tool for environmental research. Chichester, West Sussex, England: Published on behalf of the Scientific Committee on Problems of the Environment (SCOPE) of the International Council of Scientific Unions (ICSU) and of the United Nations Environment Programme (UNEP) by Wiley, 1994.

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1956-, Hessen D. O., and Tranvik L. J. 1959-, eds. Aquatic humic substances: Ecology and biogeochemistry. Berlin: Springer, 1998.

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Elberling, Bo. Subsurface oxygen consumption: Environmental controls & impacts. [Copenhagen]: Kongelige Danske geografiske selskab, 2005.

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Reddy, K. R. Biogeochemistry of wetlands: Science and applications. Boca Raton: Taylor & Francis, 2008.

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Mannion, Antoinette M. Carbon: The link between environment, culture and technology. Reading, UK: Dept. of Geography, University of Reading, 2000.

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Wei liang jin shu sheng tai du li xue he sheng wu di qiu hua xue. Beijing: Ke xue chu ban she, 2011.

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Kelman, Wieder R., Novák Martin, Vile Melanie A, and BIOGEOMON, the International Symposium on Ecosystem Behavior (2002 : Reading, England), eds. Biogeochemical investigations of terrestrial, freshwater, and wetland ecosystems across the globe. Dordrecht, Netherlands ; Norwell, Mass: Kluwer Academic Publishers, 2004.

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Book chapters on the topic "Environmental biogeochemistry"

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Humborg, Christoph, Hans Estrup Andersen, Thorsten Blenckner, Mathias Gadegast, Reiner Giesler, Jens Hartmann, Gustaf Hugelius, et al. "Environmental Impacts—Freshwater Biogeochemistry." In Regional Climate Studies, 307–36. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-16006-1_17.

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Schneider, Bernd, Kari Eilola, Kaarina Lukkari, Bärbel Muller-Karulis, and Thomas Neumann. "Environmental Impacts—Marine Biogeochemistry." In Regional Climate Studies, 337–61. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-16006-1_18.

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Johnson, David Barrie. "The Biogeochemistry of Biomining." In Geomicrobiology: Molecular and Environmental Perspective, 401–26. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-9204-5_19.

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Bonnett, S. A. F., P. J. Maxfield, A. A. Hill, and M. D. F. Ellwood. "Biogeochemistry in the Scales." In Mathematical Advances Towards Sustainable Environmental Systems, 129–49. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-43901-3_7.

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Öberg, Gunilla M. "The Biogeochemistry of Chlorine in Soil." In The Handbook of Environmental Chemistry, 43–62. Berlin, Heidelberg: Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/b10447.

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Williams, David R. "Speciation of Chelating Agents and Principles for Global Environmental Management." In Biogeochemistry of Chelating Agents, 20–49. Washington, DC: American Chemical Society, 2005. http://dx.doi.org/10.1021/bk-2005-0910.ch002.

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Taillefert, Martial, and Tim F. Rozan. "Electrochemical Methods for the Environmental Analysis of Trace Elements Biogeochemistry." In Environmental Electrochemistry, 2–14. Washington, DC: American Chemical Society, 2002. http://dx.doi.org/10.1021/bk-2002-0811.ch001.

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Popov, Konstantin I., and Hans Wanner. "Stability Constants Data Sources: Critical Evaluation and Application for Environmental Speciation." In Biogeochemistry of Chelating Agents, 50–73. Washington, DC: American Chemical Society, 2005. http://dx.doi.org/10.1021/bk-2005-0910.ch003.

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Ammann, Adrian A. "Speciation of Aminopolycarboxylate and Aminophosphonate Metal Complexes by AEX ICP-MS in Environmental Water Samples." In Biogeochemistry of Chelating Agents, 108–20. Washington, DC: American Chemical Society, 2005. http://dx.doi.org/10.1021/bk-2005-0910.ch005.

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Djenbaev, B. M., and V. V. Ermakov. "Biogeochemistry Of Uranium And Selenium - Regional Problem Of Ecology." In Environmental Protection Against Radioactive Pollution, 125–26. Dordrecht: Springer Netherlands, 2003. http://dx.doi.org/10.1007/978-94-007-0975-1_24.

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Conference papers on the topic "Environmental biogeochemistry"

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Xiuhua Liu, Lin Li, and Zhi Wang. "Biogeochemistry characteristics of nitrogen in unsaturated soils of Jinghuiqu irrigation district." In 2011 International Symposium on Water Resource and Environmental Protection (ISWREP). IEEE, 2011. http://dx.doi.org/10.1109/iswrep.2011.5893170.

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Murphy, Collin, Byron A. Steinman, Kathryn Schreiner, David P. Pompeani, Seth Depasqual, Daniel J. Bain, and Bennett Hanson. "RECONSTRUCTION OF ARCHAIC COPPER MINING AND HOLOCENE ENVIRONMENTAL CONDITIONS ON ISLE ROYALE, MICHIGAN USING LAKE SEDIMENT BIOGEOCHEMISTRY." In 54th Annual GSA North-Central Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020nc-347993.

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Murphy, Collin, Byron A. Steinman, David P. Pompeani, Kathryn Schreiner, and Seth Depasqual. "RECONSTRUCTION OF ARCHAIC COPPER MINING AND HOLOCENE ENVIRONMENTAL CONDITIONS ON ISLE ROYALE, MICHIGAN USING LAKE SEDIMENT BIOGEOCHEMISTRY." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-339257.

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Onstott, T. C., D. P. Moser, Li-Hung Lin, J. Hall, K. Takai, D. L. Balkwill, J. K. Fredrickson, et al. "Microbiology and Biogeochemistry of Deep Hydrogeologic Environments of the Witwatersrand Basin, South Africa." In 7th SAGA Biennial Technical Meeting and Exhibition. European Association of Geoscientists & Engineers, 2001. http://dx.doi.org/10.3997/2214-4609-pdb.143.11.1.

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Reports on the topic "Environmental biogeochemistry"

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Ehrlich, H. L. Tenth international symposium on environmental biogeochemistry. Final technical report, December 15, 1990--December 14, 1991. Office of Scientific and Technical Information (OSTI), January 1992. http://dx.doi.org/10.2172/10160994.

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Newman, K. A., C. J. Ford, and J. T. Byrd. Final project report on arsenic biogeochemistry in the Clinch River and Watts Bar Reservoir: Volume 2, Quality assurance/quality control summary report for arsenic biogeochemistry in the Clinch River and Watts Bar Reservoir. Environmental Restoration Program. Office of Scientific and Technical Information (OSTI), April 1995. http://dx.doi.org/10.2172/67262.

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Dunn, C. E., and R. S. Angélica. Evaluation of biogeochemistry as a tool in mineral exploration and in monitoring environmental mercury dispersion in the Tapajós gold district, Amazonia, Brazil. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2000. http://dx.doi.org/10.4095/211400.

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