Relevant bibliographies by topics / Biogeochemistry

Academic literature on the topic 'Biogeochemistry'

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Published: 4 June 2021
Last updated: 29 July 2024

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Journal articles on the topic "Biogeochemistry"

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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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Walbridge, Mark R. "Phosphorus Biogeochemistry." Ecology 81, no. 5 (May 2000): 1474–75. http://dx.doi.org/10.1890/0012-9658(2000)081[1474:pb]2.0.co;2.

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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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Brooks, Jim. "Environment Biogeochemistry." Geoderma 39, no. 2 (December 1986): 157–58. http://dx.doi.org/10.1016/0016-7061(86)90073-x.

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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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Burdige, David J. "Biogeochemistry of Estuaries." Eos, Transactions American Geophysical Union 88, no. 52 (December 25, 2007): 581. http://dx.doi.org/10.1029/2007eo520011.

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Oremland, R. S., and J. J. McCarthy. "Foreword: Methane Biogeochemistry." Global Biogeochemical Cycles 2, no. 4 (December 1988): ii. http://dx.doi.org/10.1029/gb002i004p000ii.

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Reeburgh, William S. "Oceanic Methane Biogeochemistry." Chemical Reviews 107, no. 2 (February 2007): 486–513. http://dx.doi.org/10.1021/cr050362v.

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Duursma, Egbert K. "Perspectives on Biogeochemistry." Marine Chemistry 37, no. 3-4 (April 1992): 286–88. http://dx.doi.org/10.1016/0304-4203(92)90084-n.

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Dissertations / Theses on the topic "Biogeochemistry"

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Mortimer, Robert J. G. "Biogeochemistry of iron." Thesis, University of Reading, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.262558.

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Guicharnaud, Rannveig A. "Biogeochemistry of Icelandic Andosols." Thesis, Available from the University of Aberdeen Library and Historic Collections Digital Resources. Online version available for University member only until July 1, 2014, 2009. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?application=DIGITOOL-3&owner=resourcediscovery&custom_att_2=simple_viewer&pid=53377.

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Guido-Garcia, Fabiola. "The biogeochemistry of iodine." Thesis, University of Manchester, 2016. https://www.research.manchester.ac.uk/portal/en/theses/the-biogeochemistry-of-iodine(031a6229-1a96-4068-9764-8291bafb0cad).html.

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Iodine-129 is a high-yield fission product of 235U and 239Pu; is produced in nuclear power plants and is therefore present in substantial quantities in radioactive wastes. In the environment, iodine exists as a range of species: iodate (IO3-), iodide (I-), elemental iodine (I2), HOI and organic species are the most common. The behaviour of iodine in the environment is linked to its speciation which can be affected by different factors such as pH, redox potential and enzymatic reduction. Previous research has shown that iodine speciation can determine its fate in the environment; however the mechanisms of redox cycling amongst the different species are not yet fully understood. This research project has focused on improving the understanding of the changes on speciation of iodine in sediment and mineral systems undergoing redox cycling reactions. The fate and changes in iodine speciation were studied under reducing and oxidising conditions, with all experiments conducted under circumneutral pH conditions. Overall the results showed that when microbial activity is promoted in a sediment system, iodate is reduced to iodide with the reduction occurring during manganese reduction. Further, when nitrate is present at high concentrations the reduction of iodate is retarded. A net release of native iodine from sediments was observed in all experiments conducted with sediments; confirming previous observations that sediment bound iodine is released from sediments under reducing conditions. Modest abiotic reduction of iodate was observed under manganese and iron reduction; and iodate reduction happened faster in a mixed system with iron and pure culture bacteria than solely by the pure culture alone or via abiotic reduction with Fe(II). When reduced experiments were exposed to air, concentrations of iodide decreased with no iodate ingrowth or losses in total iodine in solution. This suggested that iodide had been oxidised to intermediate species (I2, HOI) that were not detected, although this reaction has been described in past research. Finally, when no microbial activity is promoted, iodine remains as iodate which showed modest sorption onto sediment systems and Fe(III) oxide. Overall, these results highlight the important role that bacteria play in the reduction of iodate. This research also confirms that iodine speciation impacts on the fate of 129I throughout the environment, where it may be less mobile in an oxic environment than under reducing conditions. Moreover, some techniques of bioremediation (e.g. promoting metal reducing conditions) may cause the release of radioactive iodine to solution.
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Jones, Charles Nathaniel. "Floodplain Hydrology and Biogeochemistry." Diss., Virginia Tech, 2015. http://hdl.handle.net/10919/75169.

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River-floodplain connectivity is defined as the water mediated transfer of materials and energy between a river or stream and its adjacent floodplain. It is generally accepted that restoring and/or enhancing river-floodplain connectivity can reduce the downstream flux of reactive solutes such as nitrogen (N) and phosphorus (P) and thus improve downstream water quality. However, there is little scientific literature to guide ecological engineering efforts which optimize river-floodplain connectivity for solute retention. Therefore, the aim of my dissertation research was to examine feedbacks between inundation hydrology and floodplain biogeochemistry, with an emphasis on analyzing variation experienced along the river continuum and the cumulative effects of river-floodplain connectivity at the basin scale. This was completed through four independent investigations. Field sites ranged from the Atchafalaya River Basin, the largest river-floodplain system in the continental US, to the floodplain of a recently restored headwater stream in Appalachia. We also developed a method to examine river-floodplain connectivity across large- river networks and applied that methodology to US stream network. Largely, our results highlight the role floodwater residence time distributions play in floodplain biogeochemistry. In headwater streams, residence times restrict redox dependent processes (e.g. denitrification) and downstream flushing of reactive solutes is the dominant process. However, in large-river floodplains, redox dependent processes can become solute limited because of prolonged residence times and hydrologic isolation. In these floodplains, the dominant process is often autochthonous solute accumulation. Further, results from our modeling study suggest large-river floodplains have a greater impact on downstream water quality than floodplains associated with smaller streams, even when considering cumulative effects across the entire river network.
Ph. D.
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Dolor, Marvourneen Kimranee. "Investigation of Rhenium's biogeochemistry." College Park, Md. : University of Maryland, 2009. http://hdl.handle.net/1903/9260.

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Thesis (Ph. D.)--University of Maryland, College Park, 2009.
Thesis research directed by: Chemistry. Title from t.p. of PDF. Includes bibliographical references. Published by UMI Dissertation Services, Ann Arbor, Mich. Also available in paper.
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Tuit, Caroline Beth 1973. "The marine biogeochemistry of molybdenum." Thesis, Massachusetts Institute of Technology, 2003. http://hdl.handle.net/1721.1/58369.

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Thesis (Ph. D.)--Joint Program in Marine Geology and Geophysics (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric and Planetary Sciences, and the Woods Hole Oceanographic Institution), 2003.
Includes bibliographical references.
Prevailing wisdom holds that the vertical distribution of molybdenum (Mo) in the open ocean is conservative, despite Mo's important biological role and association with Mn oxides and anoxic sediments. Mo is used in both nitrogenase, the enzyme responsible for N2 fixation, and nitrate reductase, which catalyzes assimilatory and dissimilatory nitrate reduction. Laboratory culture work on two N2 fixing marine cyanobacteria, Trichodesmium and Crocosphaera, and a marine facultative denitrifier, Marinobacter hydrocarbanoclasticus, showed that Mo cell quotas in these organisms were positively correlated with Mo-containing enzyme activity. Mo concentrations in Crocosphaera dropped almost to blank levels when not fixing N2 suggesting daily synthesis and destruction of the entire nitrogenase enzyme and release of Mo. Trichodesmium cultures, however, retained a pool of cellular Mo even when not fixing N2. Colonies of Trichodesmium collected in the field have Mo:C tenfold higher than seen in culture, these Mo:C ratios were reflected in SPM samples from the same region. Fe:C ratios for Trichodesmium were between 12-160 pmol:mol in field and culured samples. The Fe:C ratio of Crocosphaera was established to be 15.8 =/+ 11.3 under N2 fixing conditions. Mo cellular concentrations in cultured organisms were too small to significantly influence dissolved Mo distributions, but may slightly affect Suspended Particulate Matter (SPM) distributions. Mean SPM Mo:C ratios were slightly elevated in regions of N2 fixation and denitrification.. A high precision (=/+ 0.5%) isotope dilution ICP-MS method for measuring Mo was developed to re-evaluate the marine distribution of Mo in the dissolved and particulate phase.
(cont.) Mn oxides were not found to significantly influence either the dissolved or SPM Mo distribution. Dissolved Mo profiles from the Sargasso and Arabian Sea were conservative. However, dissolved Mo profiles from the Eastern Tropical Pacific showed both depletion and enrichment of dissolved Mo possibly associated with interaction of Mo with coastal sediments. Dissolved Mo profiles in several California Borderland Basins showed 1-2 nM Mo depletions below sill depth. A more focused study of water column response to sediment fluxes using the high precision Mo analyses is necessary to determine whether these phenomena are related.
by Caroline Beth Tuit.
Ph.D.
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Williford, Kenneth Hart. "Biogeochemistry of the Triassic-Jurassic boundary /." Thesis, Connect to this title online; UW restricted, 2007. http://hdl.handle.net/1773/6708.

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Clark, James Richard. "Individual-based modelling of marine biogeochemistry." Thesis, University of East Anglia, 2010. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.539335.

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Moos, Simone Beatrice. "The marine biogeochemistry of chromium isotopes." Thesis, Massachusetts Institute of Technology, 2018. http://hdl.handle.net/1721.1/115788.

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Thesis: Ph. D., Joint Program in Oceanography/Applied Ocean Science and Engineering (Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), 2018.
Cataloged from PDF version of thesis.
Includes bibliographical references.
In the ocean, chromium (Cr) is a redox-sensitive trace metal. The reduction of Cr(VI) to Cr(III) occurs in oxygen deficient zones (ODZs), and Cr reduction in general has been identified as a significant Cr isotope fractionation mechanism. This thesis presents the first Cr isotope variations (653 Cr) in ODZs of the ocean and adds to the sparse Cr isotope data published for modern seawater. I developed a precise and accurate Cr isotope method for seawater samples. Seawater acidification converts total Cr to Cr(III) which is preconcentrated by Mg(OH) 2 coprecipitation. A three-column anion exchange chromatography scheme separates Cr from isobaric and polyatomic interferences present in the seawater and reagent matrixes. Isotope analysis is performed on a MC-ICP-MS IsoProbe. The addition of a 50Cr-54Cr double spike allows for accurate correction of procedural and instrumental Cr mass fractionations. The first Cr isotope ratio data for a full water column profile in the Pacific Ocean is presented. This station serves as a fully oxic counterpart to stations located within the ODZ of the Eastern Tropical North Pacific. At one station, Cr concentrations are lower and [delta]53Cr values are heavier within the ODZ. This is consistent with Cr reduction resulting in isotopically lighter, particle-reactive Cr(III), which is scavenged and exported from the water column. A strong correlation of [delta]53Cr and [delta]15 NNo3- at this station suggests that Cr reduction may be microbially mediated instead of simply being a product of thermodynamic equilibrium. Alternatively, Cr may be reduced by Fe(II). In the anoxic bottom waters of the Santa Barbara Basin a strong Cr reduction signal (lower [Cr], heavier [delta]53Cr) is observed, which may result from the same aforementioned Cr reduction mechanisms. A shift to the heaviest seawater Cr isotope signatures yet observed was detected in the oxic bottom waters of the shallow Arctic Chukchi shelf, while Cr concentrations decreased. This extreme isotope signal may result from Cr reduction by a reduced species (e.g. Fe(II)), which was released from the underlying anoxic shelf sediments. Cr in the Atlantic layer and in the bottom water of a central Arctic station appears to be shaped by a novel, unidentified process.
by Simone Beatrice Moos.
Ph. D.
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John, Seth G. "The marine biogeochemistry of zinc isotopes." Thesis, Massachusetts Institute of Technology, 2007. http://hdl.handle.net/1721.1/40968.

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Thesis (Ph. D.)--Joint Program in Chemical Oceanography (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), 2007.
Includes bibliographical references.
Zinc (Zn) stable isotopes can record information about important oceanographic processes. This thesis presents data on Zn isotopes in anthropogenic materials, hydrothermal fluids and minerals, cultured marine phytoplankton, natural plankton, and seawater. By measuring Zn isotopes in a diverse array of marine samples, we hope to understand how Zn isotopes are fractionated in the oceans and how Zn isotopes may be used as tracers of marine biogeochemical processes. Common forms of anthropogenic Zn had [delta]66Zn from +0.08 %o to +0.32 %o, a range similar to Zn ores and terrigenous materials. Larger variations were discovered in hydrothermal fluids and minerals, with hydrothermal fluids ranging in 666Zn from 0.02 %o to +0.93 %o, and chimney minerals ranging from -0.09 %o to +1.17 %o. Lower-temperature vent systems had higher [delta]666Zn values, suggesting that precipitation of isotopically light Zn sulfides drives much of the Zn isotope fractionation in hydrothermal systems. In cultured diatoms, a relationship was discovered between Zn transport by either high-affinity or low-affinity uptake pathways, and the magnitude of Zn isotope fractionation. We established isotope effects of [delta]66Zn = -0.2 %o for high-affinity uptake and [delta]66Zn = -0.8 %o for low-affinity uptake. This work is the first to describe the molecular basis for biological fractionation of transition metals. Biological fractionation of Zn isotopes under natural conditions was investigated by measuring Zn isotopes in plankton collected in the Peru Upwelling Region and around the world.
(cont.) Seawater dissolved Zn isotopes also reflect the chemical and biological cycling of Zn. The [delta]66Zn of deep seawater in the North Pacific and North Atlantic is about 0.5%0, and the dissolved [delta]66Zn gets lighter in the upper water column. This is unexpected based our observations of a biological preference for uptake of light Zn isotopes, and suggests that Zn transport to deep waters may occur by Zn adsorption to sinking particles rather than as primary biological Zn. The thesis, by presenting data on several important aspects of Zn isotope cycling in the oceans, lays the groundwork for further use of Zn isotopes as a marine biogeochemical tracer.
by Seth Greeley John.
Ph.D.
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Books on the topic "Biogeochemistry"

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H, Schlesinger William, ed. Biogeochemistry. Amsterdam: Elsevier, 2005.

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Fasham, Michael J. R., ed. Ocean Biogeochemistry. Berlin, Heidelberg: Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-642-55844-3.

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Cronan, Christopher S. Ecosystem Biogeochemistry. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-66444-6.

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Hayes, John M. Isotopic biogeochemistry. Bloomington, Ind: Indiana University Foundation, 1985.

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Warren, Howarth Robert, ed. Modern biogeochemistry. Dordrecht: Kluwer Academic Publishers, 2002.

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Mikhaĭlovich, Galimov Ėrik, ed. Pami͡a︡ti pervykh rossiĭskikh biokhimikov: Sbornik nauchnykh trudov. Moskva: "Nauka", 1994.

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Middelburg, Jack J. Marine Carbon Biogeochemistry. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-10822-9.

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Parmar, Nagina, and Ajay Singh, eds. Geomicrobiology and Biogeochemistry. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-41837-2.

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Degens, Egon T. Perspectives on Biogeochemistry. Berlin, Heidelberg: Springer Berlin Heidelberg, 1989. http://dx.doi.org/10.1007/978-3-642-48879-5.

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Reddy, Ramesh. Biogeochemistry of Wetlands. London: Taylor and Francis, 2008.

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Book chapters on the topic "Biogeochemistry"

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Mahowald, Natalie M. "Atmospheric Biogeochemistry biogeochemistry." In Encyclopedia of Sustainability Science and Technology, 606–22. New York, NY: Springer New York, 2012. http://dx.doi.org/10.1007/978-1-4419-0851-3_549.

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Smith, Walker O., Eileen E. Hofmann, and Anna Mosby. "Marine Biogeochemistry marine biogeochemistry." In Encyclopedia of Sustainability Science and Technology, 6372–86. New York, NY: Springer New York, 2012. http://dx.doi.org/10.1007/978-1-4419-0851-3_565.

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Hartnett, Hilairy Ellen. "Biogeochemistry." In Encyclopedia of Earth Sciences Series, 1–4. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-39193-9_169-1.

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Hartnett, Hilairy Ellen. "Biogeochemistry." In Encyclopedia of Earth Sciences Series, 107–11. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-39312-4_169.

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Schiebel, Ralf, and Christoph Hemleben. "Biogeochemistry." In Planktic Foraminifers in the Modern Ocean, 263–93. Berlin, Heidelberg: Springer Berlin Heidelberg, 2017. http://dx.doi.org/10.1007/978-3-662-50297-6_9.

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Zhao, Weilong, Zhijun Xu, and Nita Sahai. "Biogeochemistry." In Molecular Modeling of Geochemical Reactions, 311–39. Chichester, UK: John Wiley & Sons, Ltd, 2016. http://dx.doi.org/10.1002/9781118845226.ch9.

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Syvitski, James P. M., David C. Burrell, and Jens M. Skei. "Biogeochemistry." In Fjords, 241–70. New York, NY: Springer New York, 1987. http://dx.doi.org/10.1007/978-1-4612-4632-9_7.

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Sommer, Ulrich. "Biogeochemistry." In Freshwater and Marine Ecology, 335–72. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-42459-5_8.

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Sihi, Debjani, and Biswanath Dari. "Soil Biogeochemistry." In The Soils of India, 143–58. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-31082-0_8.

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Cronan, Christopher S. "Soil Biogeochemistry." In Ecosystem Biogeochemistry, 11–29. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-66444-6_2.

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Conference papers on the topic "Biogeochemistry"

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Shah Walter, Sunita. "Off-axis Hydrothermal Biogeochemistry." In Goldschmidt2023. France: European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.20522.

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Kappler, Andreas. "Iron Biogeochemistry in the Past, Present and Future - Endowed Biogeochemistry Lecture." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.8310.

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Dabsys, Edward, Joshua Beisel, Gretchen North, Allan N. Scott, and Christopher Oze. "BIOGEOCHEMISTRY OF PERCHLORATE IN MARTIAN REGOLITH." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-322966.

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Hannides, Angelos K., and Nicole Elko. "SAND BIOGEOCHEMISTRY IMPACTS OF BEACH NOURISHMENT ACTIVITIES." In 68th Annual GSA Southeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019se-327570.

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Chorover, Jon. "CRITICAL ZONE BIOGEOCHEMISTRY: LINKING STRUCTURE AND DYNAMICS." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-338314.

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Werne, J. "Keynote Lecture - Biogeochemistry of Sulfur: an Overview." In First EAGE/IFPEN Conference on Sulfur Risk Management in Exploration and Production. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201802776.

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Cañadas, Fuen, Dominic Papineau, and Graham Shields. "Biogeochemistry of late Ediacaran mineral-organic associations." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.6328.

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Ueno, Yuichiro, Toshiki Katsuta, Koudai Taguchi, Mayuko Nakagawa, Naohiro Yoshida, and Alexis Gilbert. "Application of fluorination method to isotopologue biogeochemistry." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.7358.

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Missen, Owen, Joël Brugger, Stuart Mills, Barbara Etschmann, Rahul Ram, and Jeremiah Shuster. "Tellurium Biogeochemistry in the World’s Richest Tellurium Hotspot." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1813.

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Bianchi, Thomas. "Key Geochemical Developments in the Origin of Biogeochemistry." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.3725.

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Reports on the topic "Biogeochemistry"

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Kersting, Annie B., and Mavrik Zavarin. Subsurface Biogeochemistry of Actinides. Office of Scientific and Technical Information (OSTI), June 2016. http://dx.doi.org/10.2172/1281679.

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Dunn, C. E. Biogeochemistry in Mineral Exploration. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132395.

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Li, Li. Deep Learning for Hydro-Biogeochemistry Processes. Office of Scientific and Technical Information (OSTI), March 2021. http://dx.doi.org/10.2172/1769693.

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Felmy, Andrew R., Eric J. Bylaska, David A. Dixon, Michel Dupuis, James W. Halley, R. Kawai, Kevin M. Rosso, et al. Computational Studies in Molecular Geochemistry and Biogeochemistry. Office of Scientific and Technical Information (OSTI), April 2006. http://dx.doi.org/10.2172/881689.

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Smith, Jeremy. Multi-Scale Modeling Framework for Mercury Biogeochemistry. Office of Scientific and Technical Information (OSTI), October 2020. http://dx.doi.org/10.2172/1671770.

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Wilkins, Michael, Audrey Sawyer, and Kenneth Williams. Seasonal controls on dynamic hyporheic zone redox biogeochemistry. Office of Scientific and Technical Information (OSTI), August 2016. http://dx.doi.org/10.2172/1506963.

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Denham, M., D. Kaplan, and C. Yeager. GROUNDWATER RADIOIODINE: PREVALENCE, BIOGEOCHEMISTRY, AND POTENTIAL REMEDIAL APPROACHES. Office of Scientific and Technical Information (OSTI), September 2009. http://dx.doi.org/10.2172/965394.

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Braswell, B. H. Jr. Global terrestrial biogeochemistry: Perturbations, interactions, and time scales. Office of Scientific and Technical Information (OSTI), December 1996. http://dx.doi.org/10.2172/527485.

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Jeffery, Nicole, Mathew Maltrud, Jonathan Wolfe, and Sean Mitchell. Arctic benthos biogeochemistry in E3SM: progress and applications. Office of Scientific and Technical Information (OSTI), September 2021. http://dx.doi.org/10.2172/1821333.

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Jeffery, Nicole. Ice-ocean interactions, marine biogeochemistry and the climate system. Office of Scientific and Technical Information (OSTI), May 2017. http://dx.doi.org/10.2172/1358151.

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