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    DGT-based Measurement of Phosphorus in Sediment Microzones and Rhizospheres (Repost)

    Posted By: step778
    DGT-based Measurement of Phosphorus in Sediment Microzones and Rhizospheres (Repost)

    Shengrui Wang, Zhihao Wu, "DGT-based Measurement of Phosphorus in Sediment Microzones and Rhizospheres"
    English | 2016 | pages: 187 | ISBN: 9811007209 | PDF | 6,2 mb

    This book focuses on the development of DGT (diffusive gradients
    in thin films) and the related techniques for measuring and investigating the geochemical
    process and P transfer across the sediment/water or sediment/root interface in
    lakes. A series of DGT techniques such as new types of probes, test methods in sediment or the rhizosphere,
    DIFS (DGT induced fluxes in sediments and soils)
    model for kinetic P exchange, CID (computer imaging densitometry) for S(-II), and
    microchelex gel/LA-ICP-MS (laser
    ablation inductively coupled plasma mass spectrometry) have been developed.
    The corresponding chapters on the theory and
    methodology of DGT, the “internal P loading” or P transfer across sediment/root
    in two lakes, provide insights into the research method and conclusions, including
    the P release mechanism, the quantification of “internal P loading”, kinetic P
    exchange in DGT/sediment interface, Fe- or S(-II)-microniches at submillimeter
    scales in sediments for the prediction of P release, and DGT as a surrogate for the prediction of P uptake
    by roots.
    It also
    offers new perspectives in the fields of P analysis and P process in
    micro-interfaces in lakes using DGT techniques. The P remobilization from
    Fe-bound P, the coupled Fe-S(-II)-P geochemical reaction and algae biomass
    breakdown causing P release, are elucidated using DGT methods in sediment
    layers. DGT parameters and curves for time or distance
    derived from DIFS can be used to assess kinetic P
    release in the sediment microzone. CID and LA-ICP-MS methods deliver Fe- and
    S(-II) images at submillimeter scales, which can be used for the quantification
    of flux related to microniche peaks and the prediction of P release from
    Fe-microniche or Fe-S(-II)-P geochemical reactions. DGT measurements in-situ in
    rhizosphere or rhizonbox can
    give CE (effective
    concentration) and CDGT
    values for the prediction of P accumulated in plant tissues.
    This book provides a valuable reference resource for senior graduate
    students, lecturers and researchers in the fields of the geochemical process of
    eutrophic elements in lakes, lake eutrophication mechanism and environmental analysis.

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