Abstract
Purpose
Inconsistent controlling factors of soil water content (SWC) spatial variation across regions and spatial scales have been acknowledged in previous studies. However, universal principles explaining these inconsistencies are still needed to be explored. The main aim of this study was to conclude the universal principles across regions and scales.
Materials and methods
In this study, based on the surface (< 10-cm soil depth) SWC dataset from Meng et al. (2021) (https://doi.org/10.5194/essd-13-3239-2021) and the relevant environmental variables (climate including temperature and precipitation, topography including elevation and slope, soil including sand and clay contents, and vegetation including normalized difference vegetation index or NDVI) in a 1500 km × 1500 km study region in China, we calculated the correlations between them, and identified the controlling factors of surface SWC in different subregions and at different spatial scales.
Results and discussion
Local factors like temperature, precipitation, and clay content that controling the vertical soil water replenishment and removal dominated the surface SWC spatial variation in this dry study region (mean SWC ≤ 0.10 m3 m−3). Nonlocal factors like topography (e.g., elevation and slope) and soil porosity (sand content) determining the lateral soil water redistribution had outweighed effects in the representative wet subregion. In addition, topography also exerted considerable effects on SWC in this study region due to its great spatial variability, especially when spatial scale < 800 km. As NDVI was complicatedly controlled by other environmental variables, its effect on SWC performed dramatic regional differentiation. In contrast, effect of slope on SWC was more associated with its spatial variability as it was independent from other environmental variables.
Conclusions
This study emphasized that the inconsistencies of controlling factors of SWC spatial variation can be comprehensively explained by different regimes in the dry and wet conditions, spatial variability of environmental variables and the interactions among different environmental variables. These findings can deepen our understanding of the controls on SWC spatial variation across regions and scales.
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Data availability
All data used for this study are publicly available. The SWC for 2005–2015 was accessed from https://zenodo.org/record/4738556. The elevation data was from http://data.tpdc.ac.cn/zh-hans/. The temperature and precipitation were accessed from https://doi.org/10.5281/zenodo.3185722 and https://doi.org/10.5281/zenodo.3114194, respectively. The soil sand and clay contents were from https://data.isric.org/. The NDVI data for 2005–2015 was from http://www.gscloud.cn/.
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Funding
This study was financially supported by the National Natural Science Foundation of China (42125103 and 42271061), the Youth Innovation Promotion Association, Chinese Academy of Sciences (2020317), and NIGLAS Foundation (E1SL002).
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Lai, X., Zhu, Q., Li, L. et al. Principles responsible for the inconsistent controlling factors of surface soil water content spatial variation across regions and scales. J Soils Sediments 23, 1877–1888 (2023). https://doi.org/10.1007/s11368-023-03427-9
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DOI: https://doi.org/10.1007/s11368-023-03427-9