Abstract:Clay translocation is among the most widespread processes in soils. It is generally identified by the presence of clay coatings at the macroscopic or microscopic scales. Nevertheless, several authors demonstrated that clay coatings have different origins, which renders the attribution of individual coatings to a particular process difficult. Therefore, their characterization at the microscopic scale is necessary. Modern synchrotron techniques allow mapping of the mineral composition of soil thin sections by X-… Show more
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