Isotopes of the Earths Hydrosphere

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Isotopes Of The Earths Hydrosphere

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Isotopes Of The Earths Hydrosphere

Amazon Renewed Refurbished products with a warranty. Future effort will be devoted into probing nature and reactivity of surface phases during coupled Fe oxidation and Cr reduction using both Fe and Cr isotopes. Microbial dissimilatory iron reduction produces ferrous iron, which is a very efficient reducing agent in the presence of mineral surfaces.

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It can reduce Cr VI , which is highly soluble, mobile and toxic, to insoluble Cr III that readily absorbes onto mineral surfaces and less toxic. A variety of Fe oxyhydroxide substrates including hematite, goethite, and poorly crystalline ferrihydrite will be examined to probe the nature and reactivity of surface phases formed during this coupled process using Fe isotope fractionations. As a second stage of this project, Cr isotope fractionations will be investigated, which system is largely underexplored compared with Fe isotope system.

Other project will examine the impact of microbial N utilization from rocks on chemical weathering. This project quantifies how and to what extent microorganisms affect chemical weathering rates when they utilize N-bearing rocks. Minerals comprising sedimentary rocks, such as feldspars and clays, contain ammonium as a substitute for potassium.

Traditional models of the N cycle emphasize nitrogen fixation from atmospheric N and uptake of N from soil organic matter but do not consider microbial utilization of N in rocks. This could have significant influence on chemical weathering rates and consequently the evolution of atmospheric CO 2. This could shed new light on the terrestrial N cycle.