Morpho-Physical and Chemical Characteristics of Mountain Soils in Central Leyte
Deejay Maranguit | Victor B. Asio
Abstract:
An important prerequisite to sustainable soil management is a good
understanding of soil morphological, physical and chemical characteristics.
Until now, very limited data are available on the characteristics of mountain
soils in the central part of Leyte Island. Thus, this study was conducted to
determine the morpho-physical and chemical characteristics of mountain soils
derived from andesite and shale in central Leyte, and to evaluate the effects of
parent material and topographic position on the properties of the soils.
Eight soil profiles representing the dominant parent materials and
topographic positions in the Abuyog-Mahaplag-Baybay portion of the central
mountain range of the island were examined. Results revealed that the soils
varied in their morphological, physical and chemical characteristics which to
some extent reflect the nature of their parent material and the slope positions
where they were formed. Soils derived from shale (Soil profiles 1, 2, 3 and 6)
developed into young (Fluventric Eutropepts) and well-developed (Typic
Hapludalfs) soils with generally moderate nutrient status. Soils derived from
andesite (Soil profiles 4, 5, 7 and 8) developed into young (Typic Dystropepts)
and well-developed (Typic Kandiudults) soils with generally low nutrient
status. Regardless of parent material, soils on summit slope position tended to
be better developed than soils on footslope and shoulder slope positions. The
study showed that the influence of parent material on soil development was
modified by the topographic position.
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