Variability and spatial distribution of hydrodynamic properties in soil with preserved Caatinga

ABSTRACT The functions of soil water retention and hydraulic conductivity are indispensable for the characterization and modeling of the infiltration and water transfer processes in the vadose zone. In the case of the Brazilian semi-arid region, characterized by the scarcity of water resources, ther...

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Main Authors: José Martins de França Neto, Artur Paiva Coutinho, Simone Di Prima, Saulo de Tarso Marques Bezerra, Severino Martins dos Santos Neto, Ana Emília Carvalho de Gusmão da Cunha Rabelo, Aline Lima de Oliveira, Antonio Celso Dantas Antonino
Format: Article
Language:English
Published: Associação Brasileira de Recursos Hídricos 2021-08-01
Series:Revista Brasileira de Recursos Hídricos
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2318-03312021000100223&tlng=en
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author José Martins de França Neto
Artur Paiva Coutinho
Simone Di Prima
Saulo de Tarso Marques Bezerra
Severino Martins dos Santos Neto
Ana Emília Carvalho de Gusmão da Cunha Rabelo
Aline Lima de Oliveira
Antonio Celso Dantas Antonino
author_facet José Martins de França Neto
Artur Paiva Coutinho
Simone Di Prima
Saulo de Tarso Marques Bezerra
Severino Martins dos Santos Neto
Ana Emília Carvalho de Gusmão da Cunha Rabelo
Aline Lima de Oliveira
Antonio Celso Dantas Antonino
author_sort José Martins de França Neto
collection DOAJ
description ABSTRACT The functions of soil water retention and hydraulic conductivity are indispensable for the characterization and modeling of the infiltration and water transfer processes in the vadose zone. In the case of the Brazilian semi-arid region, characterized by the scarcity of water resources, there is a lack of information on the hydrodynamic properties of the soil. Also, these properties have numerous factors of variability, requiring the characterization of their magnitude and distribution in space. This research presents an analysis of the infiltration process and the hydrodynamic properties of the soil under native Caatinga forest, observing its spatial distribution. This vegetation is typical of the Brazilian semi-arid region. One developed a 48-point grid in an area of approximately 875 m2, and applied on it the Beerkan methodology. The analyzes were performed based on the application of the BEST-Slope algorithm and statistical measures of the position, dispersion, and adherence tests. The results showed medium to high variability indices for the hydrodynamic properties, with random spatial distribution, despite the verification of a homogeneous texture in the area. Thus, it was found that the soil structure was predominant in the processes of water infiltration.
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spelling doaj.art-bcae2a8837204e588f539fd2bd9e303c2022-12-22T04:13:12ZengAssociação Brasileira de Recursos HídricosRevista Brasileira de Recursos Hídricos2318-03312021-08-012610.1590/2318-0331.262120210058Variability and spatial distribution of hydrodynamic properties in soil with preserved CaatingaJosé Martins de França Netohttps://orcid.org/0000-0002-4094-6138Artur Paiva Coutinhohttps://orcid.org/0000-0002-0644-0037Simone Di Primahttps://orcid.org/0000-0002-5066-3430Saulo de Tarso Marques Bezerrahttps://orcid.org/0000-0002-5815-5908Severino Martins dos Santos Netohttps://orcid.org/0000-0003-2940-2129Ana Emília Carvalho de Gusmão da Cunha Rabelohttps://orcid.org/0000-0002-5928-0284Aline Lima de Oliveirahttps://orcid.org/0000-0002-4607-3825Antonio Celso Dantas Antoninohttps://orcid.org/0000-0002-4120-9404ABSTRACT The functions of soil water retention and hydraulic conductivity are indispensable for the characterization and modeling of the infiltration and water transfer processes in the vadose zone. In the case of the Brazilian semi-arid region, characterized by the scarcity of water resources, there is a lack of information on the hydrodynamic properties of the soil. Also, these properties have numerous factors of variability, requiring the characterization of their magnitude and distribution in space. This research presents an analysis of the infiltration process and the hydrodynamic properties of the soil under native Caatinga forest, observing its spatial distribution. This vegetation is typical of the Brazilian semi-arid region. One developed a 48-point grid in an area of approximately 875 m2, and applied on it the Beerkan methodology. The analyzes were performed based on the application of the BEST-Slope algorithm and statistical measures of the position, dispersion, and adherence tests. The results showed medium to high variability indices for the hydrodynamic properties, with random spatial distribution, despite the verification of a homogeneous texture in the area. Thus, it was found that the soil structure was predominant in the processes of water infiltration.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2318-03312021000100223&tlng=enVadose zoneBeerkanSoil water retention curveHydraulic conductivitySemi-arid
spellingShingle José Martins de França Neto
Artur Paiva Coutinho
Simone Di Prima
Saulo de Tarso Marques Bezerra
Severino Martins dos Santos Neto
Ana Emília Carvalho de Gusmão da Cunha Rabelo
Aline Lima de Oliveira
Antonio Celso Dantas Antonino
Variability and spatial distribution of hydrodynamic properties in soil with preserved Caatinga
Revista Brasileira de Recursos Hídricos
Vadose zone
Beerkan
Soil water retention curve
Hydraulic conductivity
Semi-arid
title Variability and spatial distribution of hydrodynamic properties in soil with preserved Caatinga
title_full Variability and spatial distribution of hydrodynamic properties in soil with preserved Caatinga
title_fullStr Variability and spatial distribution of hydrodynamic properties in soil with preserved Caatinga
title_full_unstemmed Variability and spatial distribution of hydrodynamic properties in soil with preserved Caatinga
title_short Variability and spatial distribution of hydrodynamic properties in soil with preserved Caatinga
title_sort variability and spatial distribution of hydrodynamic properties in soil with preserved caatinga
topic Vadose zone
Beerkan
Soil water retention curve
Hydraulic conductivity
Semi-arid
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2318-03312021000100223&tlng=en
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