Influence of physical attributes and pedotransfer function for predicting water retention in management systems

ABSTRACT The aims of this study were to evaluate the effects of the soil structural physical attributes on the water retention and to develop pedotransfer functions (PTFs) for the estimation of the soil water content (θ) at different matric potentials of a Dystrophic Red Latosol (Hapludox) under con...

Full description

Saved in:
Bibliographic Details
Main Authors: André C. Auler, Luiz F. Pires, Maria C. Pineda
Format: Article
Language:English
Published: Universidade Federal de Campina Grande
Series:Revista Brasileira de Engenharia Agrícola e Ambiental
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1415-43662017001100746&lng=en&tlng=en
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1850152945592565760
author André C. Auler
Luiz F. Pires
Maria C. Pineda
author_facet André C. Auler
Luiz F. Pires
Maria C. Pineda
author_sort André C. Auler
collection DOAJ
description ABSTRACT The aims of this study were to evaluate the effects of the soil structural physical attributes on the water retention and to develop pedotransfer functions (PTFs) for the estimation of the soil water content (θ) at different matric potentials of a Dystrophic Red Latosol (Hapludox) under conventional tillage (CT) and no-tillage (NT) soil management systems. The effects of long-term CT and NT (over 25 years) management on the soil bulk density (BD), total porosity (TP), macroporosity (Ma), microporosity (Mi) and water retention were investigated. The PTFs were developed to predict θ and used to evaluate the soil water retention curve only for the NT system. The NT system was characterized by smaller values of the soil BD and higher values of the soil TP and Mi than the CT system. The NT system exhibited a higher θ retained than the CT system for the pore-size interval of 0.2–30 μm. However, the CT system exhibited a large amount of water retention for pores smaller than 0.2 μm. The PTFs were utilized to estimate θ at matric potentials of -1, -3, -6, -10, -33, -100, -400, -800, and -1,500 kPa with adequate accuracy. The soil BD, Ma, Mi and sand content were the main variables considered to estimate θ for the different matric potentials evaluated.
format Article
id doaj-art-a9efef18bc3a4134a429b7db7c41f767
institution OA Journals
issn 1807-1929
language English
publisher Universidade Federal de Campina Grande
record_format Article
series Revista Brasileira de Engenharia Agrícola e Ambiental
spelling doaj-art-a9efef18bc3a4134a429b7db7c41f7672025-08-20T02:25:51ZengUniversidade Federal de Campina GrandeRevista Brasileira de Engenharia Agrícola e Ambiental1807-1929211174675110.1590/1807-1929/agriambi.v21n11p746-751S1415-43662017001100746Influence of physical attributes and pedotransfer function for predicting water retention in management systemsAndré C. AulerLuiz F. PiresMaria C. PinedaABSTRACT The aims of this study were to evaluate the effects of the soil structural physical attributes on the water retention and to develop pedotransfer functions (PTFs) for the estimation of the soil water content (θ) at different matric potentials of a Dystrophic Red Latosol (Hapludox) under conventional tillage (CT) and no-tillage (NT) soil management systems. The effects of long-term CT and NT (over 25 years) management on the soil bulk density (BD), total porosity (TP), macroporosity (Ma), microporosity (Mi) and water retention were investigated. The PTFs were developed to predict θ and used to evaluate the soil water retention curve only for the NT system. The NT system was characterized by smaller values of the soil BD and higher values of the soil TP and Mi than the CT system. The NT system exhibited a higher θ retained than the CT system for the pore-size interval of 0.2–30 μm. However, the CT system exhibited a large amount of water retention for pores smaller than 0.2 μm. The PTFs were utilized to estimate θ at matric potentials of -1, -3, -6, -10, -33, -100, -400, -800, and -1,500 kPa with adequate accuracy. The soil BD, Ma, Mi and sand content were the main variables considered to estimate θ for the different matric potentials evaluated.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1415-43662017001100746&lng=en&tlng=enno-tillageconventional tillagesoil porosity
spellingShingle André C. Auler
Luiz F. Pires
Maria C. Pineda
Influence of physical attributes and pedotransfer function for predicting water retention in management systems
Revista Brasileira de Engenharia Agrícola e Ambiental
no-tillage
conventional tillage
soil porosity
title Influence of physical attributes and pedotransfer function for predicting water retention in management systems
title_full Influence of physical attributes and pedotransfer function for predicting water retention in management systems
title_fullStr Influence of physical attributes and pedotransfer function for predicting water retention in management systems
title_full_unstemmed Influence of physical attributes and pedotransfer function for predicting water retention in management systems
title_short Influence of physical attributes and pedotransfer function for predicting water retention in management systems
title_sort influence of physical attributes and pedotransfer function for predicting water retention in management systems
topic no-tillage
conventional tillage
soil porosity
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1415-43662017001100746&lng=en&tlng=en
work_keys_str_mv AT andrecauler influenceofphysicalattributesandpedotransferfunctionforpredictingwaterretentioninmanagementsystems
AT luizfpires influenceofphysicalattributesandpedotransferfunctionforpredictingwaterretentioninmanagementsystems
AT mariacpineda influenceofphysicalattributesandpedotransferfunctionforpredictingwaterretentioninmanagementsystems