RELATIONSHIP BETWEEN PHYSICAL AND CHEMICAL PROPERTIES OF ENTISOLS-FLUVENTS AND EROSION IN THE SÃO FRANCISCO RIVER

Renisson Neponuceno Araújo Filho; Francisco Sandro Rodrigues Holanda; Moacyr  Cunha Filho; Victor Casimiro Piscoya; Jose de Oliveira Melo Neto; Danielle Vieira Guimarães

doi:10.1590/1983-21252021v34n218rc

Authors

Renisson Neponuceno Araújo Filho Department of Forest Engineering, Universidade Federal do Tocantins, Gurupi, TO, Brazil https://orcid.org/0000-0002-9747-1276
Francisco Sandro Rodrigues Holanda Department of Agronomical Engineering, Universidade Federal de Sergipe, São Cristovão, SE https://orcid.org/0000-0001-6812-6679
Moacyr Cunha Filho Department of Statistics and Informatics, Universidade Federal Rural de Pernambuco, Recife, SE https://orcid.org/0000-0002-3466-8143
Victor Casimiro Piscoya Department Rural Technology, Universidade Federal Rural de Pernambuco, Recife, SE https://orcid.org/0000-0003-1875-9771
Jose de Oliveira Melo Neto Department of Forest Engineering, Universidade Federal do Tocantins, Gurupi, TO, Brazil https://orcid.org/0000-0001-7451-204X
Danielle Vieira Guimarães Department of Soil Science, Universidade Federal de Lavras, Lavras, MG https://orcid.org/0000-0003-2312-5968

DOI:

https://doi.org/10.1590/1983-21252021v34n218rc

Keywords:

Lower São Francisco River. Environmental degradation. Soil stability.

Abstract

The intense anthropization in the lower São Francisco River and surrounding areas can lead to environmental degradation risks and, above all, makes the area more susceptible to soil erosion. This study aimed to identify and correlate the physical and chemical properties able to enhance erosive processes and slope instability in the watercourse margins of the lower São Francisco River, in Sergipe State, Brazil. To this end, disturbed and undisturbed samples of an Entisol-Fluvent soil were collected in the region, specifically in the city of Amparo de São Francisco. Physical (density, porosity, and texture) and chemical (pH, cation exchange capacity, base saturation, micro-, and macronutrients) analyses were performed. All physical properties and organic carbon contents were higher in the surface layers (Ap and AC) compared to the others. Organic carbon, phosphorus, and micronutrients had a negative correlation with soil density, showing higher contents and lower soil densities in the Ap and AC layers. The pedological characteristics of the evaluated soil layers are unable to provide soil resistance to water erosion.

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