Spatial Variability of Soil Characteristics along a Landscape Gradient in Bellanwila-Attidiya Area

Wetlands are comprised of unique components of soil, water and biodiversity which are interconnected. Although water and biodiversity components of wetlands are being somewhat investigated, a very few research have been carried out to investigate soil properties.This study focused on spatial variabi...

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Main Authors: S. Cooray, R.U.K. Piyadasa, D.Wickramasinghe
Format: Article
Language:English
Published: University of Sri Jayewardenepura 2012-05-01
Series:Journal of Tropical Forestry and Environment
Subjects:
GIS
Online Access:http://journals.sjp.ac.lk/index.php/JTFE/article/view/141/146
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spelling doaj-db2e31dc82654232ac2970f6abc1752c2020-11-24T21:56:47ZengUniversity of Sri JayewardenepuraJournal of Tropical Forestry and Environment2235-93622012-05-01216068Spatial Variability of Soil Characteristics along a Landscape Gradient in Bellanwila-Attidiya Area S. CoorayR.U.K. PiyadasaD.WickramasingheWetlands are comprised of unique components of soil, water and biodiversity which are interconnected. Although water and biodiversity components of wetlands are being somewhat investigated, a very few research have been carried out to investigate soil properties.This study focused on spatial variability of soil chemical and physical parameters in a land use gradient around the Bellanwila-Attidiya Sanctuary, This study was carried out for a period of 3 months and several random soil samples were obtained from all land use areas. Selected physical and chemical properties of soil were analyzed according to the Standard Methods and the GIS maps were developed using ArcView GIS 3.2. The results indicated that all chemical and physical parameters of soil varied across the land use gradient, except for temperature. According to the GIS maps there are apparent variations in distribution of soil properties. On the surface, the highest level of each parameter was found as follows: - NO3- – industrial area, PO4 3- - functioning paddy fields, SO4 2- - residential area, Cl- - residential area, Fe3+ - functioning paddy fields, moisture content - wetland, pH – industrial area, salinity- residential area, electrical conductivity – residential area. At a 1 m depth the pattern was different: NO3- – abandoned paddy fields, PO4 3- – functioning paddy fields, SO4 2- - wetland, Cl- - wetland, Fe3+ - residential area, moisture content - wetland, pH – industrial area, salinity - wetland, electrical conductivity - wetland. The findings clearly exhibit the increases in anthropogenic pressure have resulted in wide-scale alternation of soil properties, at least in the surface soil, across a land use gradient. Managing land use in the watershed of the wetland thus needs adequate attention to conserve this natural ecosystem.http://journals.sjp.ac.lk/index.php/JTFE/article/view/141/146soilphysical and chemical parameterswetlandGIS
collection DOAJ
language English
format Article
sources DOAJ
author S. Cooray
R.U.K. Piyadasa
D.Wickramasinghe
spellingShingle S. Cooray
R.U.K. Piyadasa
D.Wickramasinghe
Spatial Variability of Soil Characteristics along a Landscape Gradient in Bellanwila-Attidiya Area
Journal of Tropical Forestry and Environment
soil
physical and chemical parameters
wetland
GIS
author_facet S. Cooray
R.U.K. Piyadasa
D.Wickramasinghe
author_sort S. Cooray
title Spatial Variability of Soil Characteristics along a Landscape Gradient in Bellanwila-Attidiya Area
title_short Spatial Variability of Soil Characteristics along a Landscape Gradient in Bellanwila-Attidiya Area
title_full Spatial Variability of Soil Characteristics along a Landscape Gradient in Bellanwila-Attidiya Area
title_fullStr Spatial Variability of Soil Characteristics along a Landscape Gradient in Bellanwila-Attidiya Area
title_full_unstemmed Spatial Variability of Soil Characteristics along a Landscape Gradient in Bellanwila-Attidiya Area
title_sort spatial variability of soil characteristics along a landscape gradient in bellanwila-attidiya area
publisher University of Sri Jayewardenepura
series Journal of Tropical Forestry and Environment
issn 2235-9362
publishDate 2012-05-01
description Wetlands are comprised of unique components of soil, water and biodiversity which are interconnected. Although water and biodiversity components of wetlands are being somewhat investigated, a very few research have been carried out to investigate soil properties.This study focused on spatial variability of soil chemical and physical parameters in a land use gradient around the Bellanwila-Attidiya Sanctuary, This study was carried out for a period of 3 months and several random soil samples were obtained from all land use areas. Selected physical and chemical properties of soil were analyzed according to the Standard Methods and the GIS maps were developed using ArcView GIS 3.2. The results indicated that all chemical and physical parameters of soil varied across the land use gradient, except for temperature. According to the GIS maps there are apparent variations in distribution of soil properties. On the surface, the highest level of each parameter was found as follows: - NO3- – industrial area, PO4 3- - functioning paddy fields, SO4 2- - residential area, Cl- - residential area, Fe3+ - functioning paddy fields, moisture content - wetland, pH – industrial area, salinity- residential area, electrical conductivity – residential area. At a 1 m depth the pattern was different: NO3- – abandoned paddy fields, PO4 3- – functioning paddy fields, SO4 2- - wetland, Cl- - wetland, Fe3+ - residential area, moisture content - wetland, pH – industrial area, salinity - wetland, electrical conductivity - wetland. The findings clearly exhibit the increases in anthropogenic pressure have resulted in wide-scale alternation of soil properties, at least in the surface soil, across a land use gradient. Managing land use in the watershed of the wetland thus needs adequate attention to conserve this natural ecosystem.
topic soil
physical and chemical parameters
wetland
GIS
url http://journals.sjp.ac.lk/index.php/JTFE/article/view/141/146
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