Hydro-physical characterization of soils under tropical semi-deciduous forest

The study of the hydro-physical behavior in soils using toposequences is of great importance for better understanding the soil, water and vegetation relationships. This study aims to assess the hydro-physical and morphological characterization of soil from a toposequence in Galia, state of São Paulo...

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Main Authors: Miguel Cooper, Jaqueline Dalla Rosa, João Carlos Medeiros, Thalita Campos de Oliveira, Raul Shiso Toma, Carlos Eduardo Pinto Juhász
Format: Article
Language:English
Published: Universidade de São Paulo 2012-04-01
Series:Scientia Agricola
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0103-90162012000200011
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spelling doaj-4703579decc24e67beee7a1bcb117ef82020-11-24T22:45:10ZengUniversidade de São PauloScientia Agricola0103-90161678-992X2012-04-0169215215910.1590/S0103-90162012000200011Hydro-physical characterization of soils under tropical semi-deciduous forestMiguel CooperJaqueline Dalla RosaJoão Carlos MedeirosThalita Campos de OliveiraRaul Shiso TomaCarlos Eduardo Pinto JuhászThe study of the hydro-physical behavior in soils using toposequences is of great importance for better understanding the soil, water and vegetation relationships. This study aims to assess the hydro-physical and morphological characterization of soil from a toposequence in Galia, state of São Paulo, Brazil). The plot covers an area of 10.24 ha (320 × 320 m), located in a semi-deciduous seasonal forest. Based on ultra-detailed soil and topographic maps of the area, a representative transect from the soil in the plot was chosen. Five profiles were opened for the morphological description of the soil horizons, and hydro-physical and micromorphological analyses were performed to characterize the soil. Arenic Haplustult, Arenic Haplustalf and Aquertic Haplustalf were the soil types observed in the plot. The superficial horizons had lower density and greater hydraulic conductivity, porosity and water retention in lower tensions than the deeper horizons. In the sub-superficial horizons, greater water retention at higher tensions and lower hydraulic conductivity were observed, due to structure type and greater clay content. The differences observed in the water retention curves between the sandy E and the clay B horizons were mainly due to the size distribution, shape and type of soil pores.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0103-90162012000200011UltisolAlfisolwater retentionsoil functioningimage analysis
collection DOAJ
language English
format Article
sources DOAJ
author Miguel Cooper
Jaqueline Dalla Rosa
João Carlos Medeiros
Thalita Campos de Oliveira
Raul Shiso Toma
Carlos Eduardo Pinto Juhász
spellingShingle Miguel Cooper
Jaqueline Dalla Rosa
João Carlos Medeiros
Thalita Campos de Oliveira
Raul Shiso Toma
Carlos Eduardo Pinto Juhász
Hydro-physical characterization of soils under tropical semi-deciduous forest
Scientia Agricola
Ultisol
Alfisol
water retention
soil functioning
image analysis
author_facet Miguel Cooper
Jaqueline Dalla Rosa
João Carlos Medeiros
Thalita Campos de Oliveira
Raul Shiso Toma
Carlos Eduardo Pinto Juhász
author_sort Miguel Cooper
title Hydro-physical characterization of soils under tropical semi-deciduous forest
title_short Hydro-physical characterization of soils under tropical semi-deciduous forest
title_full Hydro-physical characterization of soils under tropical semi-deciduous forest
title_fullStr Hydro-physical characterization of soils under tropical semi-deciduous forest
title_full_unstemmed Hydro-physical characterization of soils under tropical semi-deciduous forest
title_sort hydro-physical characterization of soils under tropical semi-deciduous forest
publisher Universidade de São Paulo
series Scientia Agricola
issn 0103-9016
1678-992X
publishDate 2012-04-01
description The study of the hydro-physical behavior in soils using toposequences is of great importance for better understanding the soil, water and vegetation relationships. This study aims to assess the hydro-physical and morphological characterization of soil from a toposequence in Galia, state of São Paulo, Brazil). The plot covers an area of 10.24 ha (320 × 320 m), located in a semi-deciduous seasonal forest. Based on ultra-detailed soil and topographic maps of the area, a representative transect from the soil in the plot was chosen. Five profiles were opened for the morphological description of the soil horizons, and hydro-physical and micromorphological analyses were performed to characterize the soil. Arenic Haplustult, Arenic Haplustalf and Aquertic Haplustalf were the soil types observed in the plot. The superficial horizons had lower density and greater hydraulic conductivity, porosity and water retention in lower tensions than the deeper horizons. In the sub-superficial horizons, greater water retention at higher tensions and lower hydraulic conductivity were observed, due to structure type and greater clay content. The differences observed in the water retention curves between the sandy E and the clay B horizons were mainly due to the size distribution, shape and type of soil pores.
topic Ultisol
Alfisol
water retention
soil functioning
image analysis
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0103-90162012000200011
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