Hydro-physical characterization of soils under the Restinga Forest

Authors

  • Miguel Cooper University of São Paulo; ESALQ – Dept. of Soil Science
  • Raquel Stucchi Boschi University of São Paulo; ESALQ – Dept. of Soil Science
  • Laura Fernanda Simões da Silva University of São Paulo; ESALQ – Dept. of Soil Science
  • Raul Shiso Toma Federal University of Ceará; CCA – Dept. of Soil Science
  • Pablo Vidal-Torrado University of São Paulo; ESALQ – Dept. of Soil Science

DOI:

https://doi.org/10.1590/1678-992x-2016-0103

Keywords:

Podzols, soil morphology, soil hydraulic properties

Abstract

Knowledge of the hydraulic properties of the soil is of crucial importance to an understanding of the interactions between vegetation, soil and water. There is little information available about the hydraulic properties of Podzol soils found in tropical regions. The aim of this study was to present the soil morphology and hydraulic properties of a toposequence situated in a permanent plot at the Ilha do Cardoso State Park (Cananéia, SP, Brazil). Ultradetailed soil maps were used to define a toposequence inside the permanent plot. Five profiles, representing the main types of soil, were opened along the toposequence, in which Podzols are dominant. The levels of bulk density, sand content, porosity and permeability in these soils were all high. Consequently, these soils have a high level of hydraulic conductivity with low water retention. This behavior undergoes an alteration in the Bh and Bs horizons due to the accumulation of organic and metallic compounds and a changing structure that modifies the pore distribution. Furthermore, the characterization of the hydro-physical functioning of soils in natural environments is an important source of encouragement to further investigative study of soil water dynamics and its relationship to the native vegetation.

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Published

2017-10-01

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How to Cite

Hydro-physical characterization of soils under the Restinga Forest. (2017). Scientia Agricola, 74(5), 393-400. https://doi.org/10.1590/1678-992x-2016-0103