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Understanding the conformation of the profile of slopes up the physical-water parameters of the soil cover in a slope located on lithologies of Santa Maria Formation, in Santa Maria, RS
Authors: Ronaldo Facco, Mauro Kumpfer Werlang, Rafael Bilhan Freitas, Guilherme Cardoso Da Silva, Rodrigo Corrêa Pontes, Joel Albino Rabaiolli, Denise Cristina Borges e Rômulo Augusto Aragones Aita
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The strands are configured as one of the main elements of the landscape, when viewed in a short time, show up
with static appearance, however they are continually being worked by erosive or depositional processes. The main
objective is to contribute to the understanding of the profile conformation and shape of the slopes up the waterphysical parameters of soil cover on slopes situated on lithologies of Santa Maria Formation, in Santa Maria,
RS. According to the objectives of the work, it was used as a theoretical and methodological basis the proposal
structural analysis of soil cover, which allowed the understanding of the dynamics of soil cover and the relationship
with other landscape elements. After analysis of the results, there was obtained the following physical-hydric
behavior of horizons diagnoses of the soil profile, where it was identified the process of translocation of clay from
superficial diagnostic horizons A, AE, E and EB for subsurface BE and B, these being more durable, impermeable
horizons, contributing to turn convex the top of the slope. Already at the slope base, the concave shape is due to
regressive erosion of less resistant horizons and the organization thereof, commanded by surface and subsurface
water circulation.