Granulometric fractions and physical-hydric behavior of sandy soils

Detalhes bibliográficos
Autor(a) principal: Santos, Nielton Gonçalo Nunes dos
Data de Publicação: 2019
Outros Autores: Olszevski, Nelci, Salviano, Alessandra Monteiro, Cunha, Tony Jarbas Ferreira, Giongo, Vanderlise, Pereira, Janielle Souza
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Agrarian (Dourados. Online)
Texto Completo: https://ojs.ufgd.edu.br/index.php/agrarian/article/view/7687
Resumo: Soils attributes such as granulometry and density determine the distribution of pore size and condition physical and differentiated hydraulic behavior. Thus, knowing the characteristics of the soils allow the use of more adequate management techniques that lead to the improvement of the performance of the use of this resource. The aim of this study was to evaluate the diameters of granulometric fractions and the physical-hydric behavior of sandy soils from semiarid region of Brazil. Trenches were excavated to collect, describe, and characterize the morphology of soil samples. The soil bulk density, particle density, granulometry, water retention curve, total porosity and pore size distribution were evaluated. The textural difference among soil studied is expressed with greater emphasis on the amount of macropores, high retention micropores and cryptopores. Fine and very fine sand are the most impacted granulometric fractions increasing macroporosity and reducing high tension microporosity and cryptoporosity. Luvisol with predominance of silt and clay fractions, presents a greater risk of densification and erosion, thus the use of lower irrigation levels is recommended. Acrisols and Luvisol, with predominance of fine and very fine sand fractions, present similar conditions of macroporosity and cryptopores with a low textural gradient. Acrisols and Luvisol do not present major problems regarding the reduction of hydraulic conductivity along the profile. Lower irrigation levels with higher application frequency are suggested due to the low water retention capacity and higher risk nutrients leaching.
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spelling Granulometric fractions and physical-hydric behavior of sandy soilsPhysical attributesMicroporosityPore size distributionWater dynamics.Soils attributes such as granulometry and density determine the distribution of pore size and condition physical and differentiated hydraulic behavior. Thus, knowing the characteristics of the soils allow the use of more adequate management techniques that lead to the improvement of the performance of the use of this resource. The aim of this study was to evaluate the diameters of granulometric fractions and the physical-hydric behavior of sandy soils from semiarid region of Brazil. Trenches were excavated to collect, describe, and characterize the morphology of soil samples. The soil bulk density, particle density, granulometry, water retention curve, total porosity and pore size distribution were evaluated. The textural difference among soil studied is expressed with greater emphasis on the amount of macropores, high retention micropores and cryptopores. Fine and very fine sand are the most impacted granulometric fractions increasing macroporosity and reducing high tension microporosity and cryptoporosity. Luvisol with predominance of silt and clay fractions, presents a greater risk of densification and erosion, thus the use of lower irrigation levels is recommended. Acrisols and Luvisol, with predominance of fine and very fine sand fractions, present similar conditions of macroporosity and cryptopores with a low textural gradient. Acrisols and Luvisol do not present major problems regarding the reduction of hydraulic conductivity along the profile. Lower irrigation levels with higher application frequency are suggested due to the low water retention capacity and higher risk nutrients leaching.Editora UFGD2019-10-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://ojs.ufgd.edu.br/index.php/agrarian/article/view/768710.30612/agrarian.v12i45.7687Agrarian; v. 12 n. 45 (2019); 318-327Agrarian Journal; Vol. 12 No. 45 (2019); 318-3271984-2538reponame:Agrarian (Dourados. Online)instname:Universidade Federal da Grande Dourados (UFGD)instacron:UFGDenghttps://ojs.ufgd.edu.br/index.php/agrarian/article/view/7687/5340Copyright (c) 2019 Agrarianinfo:eu-repo/semantics/openAccessSantos, Nielton Gonçalo Nunes dosOlszevski, NelciSalviano, Alessandra MonteiroCunha, Tony Jarbas FerreiraGiongo, VanderlisePereira, Janielle Souza2019-10-14T16:41:52Zoai:ojs.pkp.sfu.ca:article/7687Revistahttps://ojs.ufgd.edu.br/index.php/agrarianPUBhttps://ojs.ufgd.edu.br/index.php/agrarian/oairevistaagrarian@ufgd.edu.br||1984-25381984-252Xopendoar:http://ojs.ufgd.edu.br/index.php/agrarian/oaihttp://ojs.ufgd.edu.br/index.php/agrarian/oai2019-10-14T16:41:52Agrarian (Dourados. Online) - Universidade Federal da Grande Dourados (UFGD)false
dc.title.none.fl_str_mv Granulometric fractions and physical-hydric behavior of sandy soils
title Granulometric fractions and physical-hydric behavior of sandy soils
spellingShingle Granulometric fractions and physical-hydric behavior of sandy soils
Santos, Nielton Gonçalo Nunes dos
Physical attributes
Microporosity
Pore size distribution
Water dynamics.
title_short Granulometric fractions and physical-hydric behavior of sandy soils
title_full Granulometric fractions and physical-hydric behavior of sandy soils
title_fullStr Granulometric fractions and physical-hydric behavior of sandy soils
title_full_unstemmed Granulometric fractions and physical-hydric behavior of sandy soils
title_sort Granulometric fractions and physical-hydric behavior of sandy soils
author Santos, Nielton Gonçalo Nunes dos
author_facet Santos, Nielton Gonçalo Nunes dos
Olszevski, Nelci
Salviano, Alessandra Monteiro
Cunha, Tony Jarbas Ferreira
Giongo, Vanderlise
Pereira, Janielle Souza
author_role author
author2 Olszevski, Nelci
Salviano, Alessandra Monteiro
Cunha, Tony Jarbas Ferreira
Giongo, Vanderlise
Pereira, Janielle Souza
author2_role author
author
author
author
author
dc.contributor.author.fl_str_mv Santos, Nielton Gonçalo Nunes dos
Olszevski, Nelci
Salviano, Alessandra Monteiro
Cunha, Tony Jarbas Ferreira
Giongo, Vanderlise
Pereira, Janielle Souza
dc.subject.por.fl_str_mv Physical attributes
Microporosity
Pore size distribution
Water dynamics.
topic Physical attributes
Microporosity
Pore size distribution
Water dynamics.
description Soils attributes such as granulometry and density determine the distribution of pore size and condition physical and differentiated hydraulic behavior. Thus, knowing the characteristics of the soils allow the use of more adequate management techniques that lead to the improvement of the performance of the use of this resource. The aim of this study was to evaluate the diameters of granulometric fractions and the physical-hydric behavior of sandy soils from semiarid region of Brazil. Trenches were excavated to collect, describe, and characterize the morphology of soil samples. The soil bulk density, particle density, granulometry, water retention curve, total porosity and pore size distribution were evaluated. The textural difference among soil studied is expressed with greater emphasis on the amount of macropores, high retention micropores and cryptopores. Fine and very fine sand are the most impacted granulometric fractions increasing macroporosity and reducing high tension microporosity and cryptoporosity. Luvisol with predominance of silt and clay fractions, presents a greater risk of densification and erosion, thus the use of lower irrigation levels is recommended. Acrisols and Luvisol, with predominance of fine and very fine sand fractions, present similar conditions of macroporosity and cryptopores with a low textural gradient. Acrisols and Luvisol do not present major problems regarding the reduction of hydraulic conductivity along the profile. Lower irrigation levels with higher application frequency are suggested due to the low water retention capacity and higher risk nutrients leaching.
publishDate 2019
dc.date.none.fl_str_mv 2019-10-12
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv https://ojs.ufgd.edu.br/index.php/agrarian/article/view/7687
10.30612/agrarian.v12i45.7687
url https://ojs.ufgd.edu.br/index.php/agrarian/article/view/7687
identifier_str_mv 10.30612/agrarian.v12i45.7687
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv https://ojs.ufgd.edu.br/index.php/agrarian/article/view/7687/5340
dc.rights.driver.fl_str_mv Copyright (c) 2019 Agrarian
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Copyright (c) 2019 Agrarian
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Editora UFGD
publisher.none.fl_str_mv Editora UFGD
dc.source.none.fl_str_mv Agrarian; v. 12 n. 45 (2019); 318-327
Agrarian Journal; Vol. 12 No. 45 (2019); 318-327
1984-2538
reponame:Agrarian (Dourados. Online)
instname:Universidade Federal da Grande Dourados (UFGD)
instacron:UFGD
instname_str Universidade Federal da Grande Dourados (UFGD)
instacron_str UFGD
institution UFGD
reponame_str Agrarian (Dourados. Online)
collection Agrarian (Dourados. Online)
repository.name.fl_str_mv Agrarian (Dourados. Online) - Universidade Federal da Grande Dourados (UFGD)
repository.mail.fl_str_mv revistaagrarian@ufgd.edu.br||
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