Modeling Cesium Partitioning in the Rhizosphere: A Focus on the Role of Root Exudates.
Авторы: Siegel R., Alshawabkeh A., Palmer C.
2003 г.
Soil and Sedim.
A conceptual model is being developed for the prediction of cesium partitioning between bound, aqueous, and phytoextracted phases in the rhizosphere. The model categorizes the processes that impact cesium partitioning into six submodels: geochemistry, physical factors, root density, microorganisms, nutrients, and root exudates. A seventh submodel (Cs fate) describes Cs movement between the three phases. Functional relationships and parametric values within and between the submodels are developed based on literature, field characterization, and laboratory experiments. Sensitivity analyses were first conducted to evaluate the effects of root exudates on Cs partitioning. The model was also used to test the sensitivity of root density, microbial population, potassium requirement and concentration, and moisture content on the concentration of root exudates and consequently on Cs partitioning. An increase in the concentration of root exudates results in a greater decrease in the bound concentration and greater increase in the aqueous and phytoextracted concentrations. In general, the other parameters affect Cs partitioning according to how they affect the fate of root exudates. However, the comprehensive nature of the system renders a complex overall effect on Cs partitioning. In summary, the model provides a framework for better understanding the complex interaction of processes that control Cs fate in the rhizosphere.
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