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- W1569377533 abstract "This chapter reviews some of the principal microbially driven chemical reactions within the sediment and considers the relationship between the mobility of some environmentally important radionuclides—namely, Cs, Tc, U, Np, and Pu. Microbial reactions control the chemical composition of the sedimentary environment during early diagenesis. These reactions involve the breakdown and hydrolysis of solid organic matter, the destruction or formation of inorganic compounds, and the chemical modification of pore-waters. Organic byproducts may, in turn, activate dormant microbial consortia elsewhere in the sediment profile, while inorganic byproducts may trigger important abiotic reactions between the solid and dissolved phases. In addition to the influence on the major elemental cycles, microbial activity can also greatly influence the fate and mobility of contaminants introduced into the sediments through anthropogenic activities. Microorganisms can also cause their direct immobilization by adsorbing contaminants to attached populations or promoting the indirect precipitation of authigenic phases that can either adsorb or co-precipitate the metals." @default.
- W1569377533 created "2016-06-24" @default.
- W1569377533 creator A5014203004 @default.
- W1569377533 creator A5036209910 @default.
- W1569377533 creator A5038478997 @default.
- W1569377533 creator A5077235831 @default.
- W1569377533 date "2002-01-01" @default.
- W1569377533 modified "2023-10-18" @default.
- W1569377533 title "Chapter 3 The role of microorganisms during sediment diagenesis: Implications for radionuclide mobility" @default.
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