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Journal of Arid Land
Journal of Arid Land  2019, Vol. 11 Issue (1): 123-134    DOI: 10.1007/s40333-018-0123-x     CSTR: 32276.14.s40333-018-0123-x
Orginal Article     
Spatial variability of soil water content and related factors across the Hexi Corridor of China
Xiangdong LI1,2, Ming'an SHAO1,2,3,*(), Chunlei ZHAO3, Xiaoxu JIA2,3
1 State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling 712100, China
2 College of Natural Resources and Environment, University of Chinese Academy of Sciences, Beijing 100190, China
3 Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
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Abstract  

Soil water content (SWC) is a key factor limiting ecosystem sustainability in arid and semi-arid areas of the Hexi Corridor of China, which is characterized by an ecological environment that is vulnerable to climate change. However, there is a knowledge gap regarding the large-scale spatial distribution of SWC in this region. The specific objectives of this study were to determine the spatial distribution patterns of SWC across the Hexi Corridor and identify the factors responsible for spatial variation of SWC at a regional scale. This study collected and analyzed SWC in the 0-100 cm soil profile from 109 field sampling sites (farmland, grassland and forestland) across the Hexi Corridor in 2017. We selected 17 factors, including land use, topography (latitude, longitude, elevation, slope gradient, and slope aspect), soil properties (soil clay content, soil silt content, soil bulk density, saturated hydraulic conductivity, field capacity, and soil organic carbon content), climate factors (mean annual precipitation, potential evaporation, and aridity index), plant characteristic (vegetation coverage) and planting pattern (irrigation or rain-fed), as possible environmental variables to analyze their effects on SWC. The results showed that SWC was 0.083 (±0.067) g/g in the 0-100 cm soil profile and decreased in the order of farmland, grassland and forestland. The SWC in the upper soil layers (0-20, 20-40 and 40-60 cm) had obvious difference when the mean annual precipitation differed by 200 mm. The SWC decreased from southeast to northwest following the same pattern as precipitation, and had a moderate to strong spatial dependence in a large effective range (75-378 km). The SWC showed a similar distribution and had no significant difference between soil layers in the 0-100 cm soil profile. The principal component analysis showed that the mean annual precipitation, geographical position (longitude and latitude) and soil properties (soil bulk density and soil clay content) were the main factors dominating the variance of environmental variables. A stepwise linear regression equation showed that plant characteristic (vegetation coverage) and soil properties (soil organic carbon content, field capacity and soil clay content) were the optimal factors to predict the variation of SWC. Soil clay content could be better to explain the SWC variation in the deeper soil layers compared with the other factors.

Key words： soil water content      spatial variability      geostatistical analysis      soil clay content      Hexi Corridor     
Received: 06 March 2018      Published: 10 February 2019
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Xiangdong LI
Ming'an SHAO
Chunlei ZHAO
Xiaoxu JIA
Cite this article:

Xiangdong LI, Ming'an SHAO, Chunlei ZHAO, Xiaoxu JIA. Spatial variability of soil water content and related factors across the Hexi Corridor of China. Journal of Arid Land, 2019, 11(1): 123-134.

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http://jal.xjegi.com/10.1007/s40333-018-0123-x     OR     http://jal.xjegi.com/Y2019/V11/I1/123

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