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Abstract
We study the analytical modifications that take place on a gley-calcaric Fluvisol, FAO (1988) (1), which is classified, following Soil Taxonomy, as aquic, silty, fine, calcaric, thermic Xerofluvent, Soil Survey Staff (1990) (2). The used soil is located at the Vega de Granada, and is submited to an inundation riskwith residuary water proceding from one of the four water conduit which are present in thecity of Granada. A morphologic and analytical description of the studied soil is doing, as well thecharacteristics of the residuary water used for the irrigation; either an analytical pursuancerelated to the soil depth in the four zones form the selected piece of ground, before and aftersubmiting to the inundation risk.
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