Abstract

The experimental research program was developed in the Alto Paraopeba region, state of Minas Gerais, Southeastern Brazil. The main objective was to promote the geotechnical evaluation of soil samples from four cut slopes in residual soil profiles of highways and local secondary roads in order to assess the potential of the anthropic impact on the soil susceptibility to accelerated erosion processes. Soil samples were named: red residual soil (RRS); pink residual soil (PRS); yellow residual soil (YRS); and white residual soil (WRS). The methodology used consisted of geotechnical characterization tests, infiltration rate and modified mass loss by immersion tests performed on soil samples from these profiles, using the physical parameters and indirect assessment of erodibility proposed in 2000 by Bastos et al. The results of indirect assessment of erodibility, which were derived from tests based on the MCT methodology, highlighted the different susceptibility of the investigated soils to hydric erosion. The parameters proposed by the referred authors were complementary to conventional criteria for an adequate classification of tropical soils into their respective classes of erodibility. Among the tested soil samples, the highest erodibility was associated with the YRS and PRS, respectively, in the natural and pre-moistened conditions, as well as it was not detected erodibility in the RRS and WRS.

Highlights

  • The erosion term comes from the Latin erode-erodere meaning to corrode, with several definitions in the literature

  • Given the context described previously, this study investigated, via geotechnical laboratory tests, the susceptibility to accelerated erosion of cuts in residual soil profiles in some highways and local secondary roads of the city of Ouro Branco, Alto Paraopeba, state of Minas Gerais, southeastern Brazil

  • Soil samples studied are from four cut slopes of roads in residual soil profiles typical of the region of the Alto Paraopeba in the state of Minas Gerais

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Summary

Introduction

The erosion term comes from the Latin erode-erodere meaning to corrode, with several definitions in the literature. Erosion is a term that represents a series of actions, including the loosening, dragging and deposition of soil particles caused by erosive agents such as ice, wind, gravity and water. When erosion is a natural process, it is considered a geological agent that changes terrestrial landscapes, in a slow mechanism measured by geological time. Human interference modifies this natural process and usually accelerates its action and increases its intensity. When human action is characterized as promoting and intensifying the processes of water erosion, the Maringá, v. 331-337, Oct.-Dec., 2015 term used is accelerated hydric erosion (BASTOS et al, 2000) When human action is characterized as promoting and intensifying the processes of water erosion, the Maringá, v. 37, n. 4, p. 331-337, Oct.-Dec., 2015 term used is accelerated hydric erosion (BASTOS et al, 2000)

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