Factors affecting soil moisture spatial variability for a humid forest hillslope. Issue 2 (21st November 2016)

• Record Type: Journal Article
• Authors: Gwak, Yongseok; Kim, Sanghyun
• Is Part Of: Hydrological processes. Volume 31:Issue 2(2017)
• Page Start: 431
• Page End: 445
• Publication Date: 2016-11-21
• Subjects: correlation analysis -- empirical orthogonal function -- forested hillslope -- soil moisture -- time domain reflectometry; Hydrology -- Periodicals; Hydrology -- Research -- Periodicals; Hydrologic models -- Periodicals; Hydrological forecasting -- Periodicals; 631.432
• DOI: 10.1002/hyp.11039
• Languages: English
• ISSNs: 0885-6087

Abstract

Abstract: Soil moisture is an important variable in explaining hydrological processes at hillslope scale. The distribution of soil moisture along a hillslope is related to the spatial distribution of the soil properties, the topography, the soil depth, and the vegetation. In order to investigate the factors affecting soil moisture, various environmental data were collected from a humid forest hillslope in this study. Several factors (the wetness index; the contributing area; the local slope; the soil depth; the composition of sand, silt, and clay; the scaling parameter; the hydraulic conductivity; the tree diameter at breast height; and the total weighted basal area) were evaluated for their effect on soil moisture and its distribution over the hillslope at depths of 10, 30, and 60 cm. Both linear correlation analysis and empirical orthogonal function analysis indicated that the soil texture was a dominant factor in soil moisture distribution. The impact of soil hydraulic conductivity was important for all soil moisture ranges at a depth of 30 cm, but those at 10 and 60 cm were limited to very wet and dry conditions, respectively. The relationships of the various factors with the spatial variability of soil moisture indicated the existence of a threshold soil moisture that is related to the composition of the soil and the factors related to the distribution of water in the study area.