Land-use change effect on the hydro-dynamic characteristics of soil in the Brazilian semi-arid region
The search for better living conditions has led the residents of the Brazilian semi-arid region to plant forage crops, leading to a gradual decrease in the native vegetation (Caatinga) of this region. The effects caused by the replacement of Caatinga with palm, for example, have been little studied,...
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Instituto de Pesquisas Ambientais em Bacias Hidrográficas (IPABHi)
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doaj-aef34974c7ed487399e5f16812c34dbc2020-11-25T02:04:33ZengInstituto de Pesquisas Ambientais em Bacias Hidrográficas (IPABHi)Revista Ambiente & Água1980-993X2020-04-0115211410.4136/ambi-agua.2368Land-use change effect on the hydro-dynamic characteristics of soil in the Brazilian semi-arid regionWillames Albuquerque Soares0https://orcid.org/0000-0003-3268-7241Simone Rosa da Silva1https://orcid.org/0000-0001-7138-7546José Romualdo de Sousa Lima2https://orcid.org/0000-0003-2983-4650Departamento de Física de Materiais. Escola Politécnica de Pernambuco. Universidade de Pernambuco (UPE), Rua Benfica, n° 455, CEP: 50720-001, Recife, PE, Brazil Departamento de Engenharia Civil. Escola Politécnica de Pernambuco. Universidade de Pernambuco (UPE), Rua Benfica, n° 455, CEP: 50720-001, Recife, PE, Brazil. Unidade Acadêmica de Garanhuns. Universidade Federal Rural de Pernambuco (UFRPE), Avenida Bom Pastor, s/n, CEP: 55292-278, Garanhuns, PE, Brazil. The search for better living conditions has led the residents of the Brazilian semi-arid region to plant forage crops, leading to a gradual decrease in the native vegetation (Caatinga) of this region. The effects caused by the replacement of Caatinga with palm, for example, have been little studied, especially with regard to the physical and hydraulic properties of the soil. The objective of this study was to compare the physical-hydraulic characteristics of a litholic neosol in two areas having different vegetation cover: one area cultivated with forage palm (O. ficus-indica) and the other covered by native Caatinga. Differences in soil structure, especially in porosity, between the natural and cultivated soils were observed to control the hydrodynamic processes, resulting in changes in water retention curves and hydraulic conductivity. Natural soil presents low values of hydraulic conductivity when compared to those of cultivated soil. This increase is probably due to soil management required for forage palm cultivation. The natural soil structure, characterized by relatively low saturated hydraulic conductivity values, presents an infiltrability that favors surface runoff. Human activities in the study area have promoted changes in the soil’s physical attributes, decreasing density and increasing porosity. Consequently, there is an increase in water infiltration into the soil and a reduction of runoff in cultivated areas, confirming results obtained in previous studies.https://www.scielo.br/scielo.php?script=sci_arttext&pid=S1980-993X2020000200300&lng=en&nrm=iso&tlng=enforage palminfiltrationweibull distribution |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Willames Albuquerque Soares Simone Rosa da Silva José Romualdo de Sousa Lima |
spellingShingle |
Willames Albuquerque Soares Simone Rosa da Silva José Romualdo de Sousa Lima Land-use change effect on the hydro-dynamic characteristics of soil in the Brazilian semi-arid region Revista Ambiente & Água forage palm infiltration weibull distribution |
author_facet |
Willames Albuquerque Soares Simone Rosa da Silva José Romualdo de Sousa Lima |
author_sort |
Willames Albuquerque Soares |
title |
Land-use change effect on the hydro-dynamic characteristics of soil in the Brazilian semi-arid region |
title_short |
Land-use change effect on the hydro-dynamic characteristics of soil in the Brazilian semi-arid region |
title_full |
Land-use change effect on the hydro-dynamic characteristics of soil in the Brazilian semi-arid region |
title_fullStr |
Land-use change effect on the hydro-dynamic characteristics of soil in the Brazilian semi-arid region |
title_full_unstemmed |
Land-use change effect on the hydro-dynamic characteristics of soil in the Brazilian semi-arid region |
title_sort |
land-use change effect on the hydro-dynamic characteristics of soil in the brazilian semi-arid region |
publisher |
Instituto de Pesquisas Ambientais em Bacias Hidrográficas (IPABHi) |
series |
Revista Ambiente & Água |
issn |
1980-993X |
publishDate |
2020-04-01 |
description |
The search for better living conditions has led the residents of the Brazilian semi-arid region to plant forage crops, leading to a gradual decrease in the native vegetation (Caatinga) of this region. The effects caused by the replacement of Caatinga with palm, for example, have been little studied, especially with regard to the physical and hydraulic properties of the soil. The objective of this study was to compare the physical-hydraulic characteristics of a litholic neosol in two areas having different vegetation cover: one area cultivated with forage palm (O. ficus-indica) and the other covered by native Caatinga. Differences in soil structure, especially in porosity, between the natural and cultivated soils were observed to control the hydrodynamic processes, resulting in changes in water retention curves and hydraulic conductivity. Natural soil presents low values of hydraulic conductivity when compared to those of cultivated soil. This increase is probably due to soil management required for forage palm cultivation. The natural soil structure, characterized by relatively low saturated hydraulic conductivity values, presents an infiltrability that favors surface runoff. Human activities in the study area have promoted changes in the soil’s physical attributes, decreasing density and increasing porosity. Consequently, there is an increase in water infiltration into the soil and a reduction of runoff in cultivated areas, confirming results obtained in previous studies. |
topic |
forage palm infiltration weibull distribution |
url |
https://www.scielo.br/scielo.php?script=sci_arttext&pid=S1980-993X2020000200300&lng=en&nrm=iso&tlng=en |
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