Abstract:The Gilgai microrelief is characterized as a succession of alternating micromounds and depressions, in soils rich in expansive clays (2:1). Its genesis is related to successive cycles of wetting and drying, especially pronounced under conditions of imperfectly or poorly drained soils. There are still many gaps in the literature on the genesis, evolution and dynamics of the processes involved in areas with Gilgais in Brazil, so studies aimed at understanding their patterns of occurrence are necessary. Thus, the… Show more
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