EROSIVE PROCESS CONTROL IN THE BRAZILIAN SEMIARID REGION

Authors

  • Júlio César Neves dos Santos Departament of Education, Instituto Federal do Triângulo Mineiro, Uberlândia, MG http://orcid.org/0000-0001-9466-5158
  • Eunice Maia de Andrade Agricultural Engineering Departament, Universidade Federal do Ceará, Fortaleza, CE http://orcid.org/0000-0002-9750-0364
  • Helba Araújo de Queiroz Palácio Departament of Education, Instituto Federal do Ceará, Iguatu, CE http://orcid.org/0000-0002-5105-4821
  • José Ribeiro de Araújo Neto Agricultural Engineering Departament, Universidade Federal do Ceará, Fortaleza, CE http://orcid.org/0000-0001-7118-1644
  • Jacques Carvalho Ribeiro Filho Departament of Environmental and Tecnological Sciences, Universidade Federal Rural do Semi-Árido, Mossoró, RN http://orcid.org/0000-0001-9544-009X

DOI:

https://doi.org/10.1590/1983-21252018v31n319rc

Keywords:

Hydrology. Water erosion. Sediment yield.

Abstract

The adoption of measures to prevent and control erosive processes requires information about the factors affecting the erosion and the sediment transport conditions. However, the sediment yield of a basin depends on the availability of eroded material and the sediment transport capacity. Thus, the objective of this study was to identify the factors that affect the sediment transport capacity at different spatial scales in an area with caatinga vegetation. The study was carried out in the Iguatu Experimental Basin, in the state of Ceará, Brazil, from 2009 to 2014, by monitoring two scale levels: watershed with 2.06 ha, and erosion plot with 20 m². The variables evaluated for the rainfall events were precipitation, intensity of rainfall, antecedent soil moisture, precipitation of the antecedent five days, consecutive dry days, peak flow, runoff depth, and sediment yield. During the study period, 263 rainfall events (>2 mm) and 86 events generating runoff were recorded. Three Principal Components (PC) were developed using the Principal Component Analysis, which explained more than 79% of the total variance. Variables connected to the kinetic energy capacity of the rainfall to disaggregate soil particles, the energy for sediment transport, and the soil water content were framed in the CP1, CP2, and CP3, respectively. In the evaluated scales, the sediment yield presented a high correlation with the runoff depth, which indicates limiting conditions for sediment yield by the mass flow energy.

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Published

28-05-2018

Issue

Section

Agricultural Engineering