Soil moisture response to land use and topography across a semi-arid watershed: Implications for vegetation restoration on the Chinese Loess Plateau  被引量:1

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作  者:XIA Lu BI Ru-tian SONG Xiao-yu HU Wei LYU Chun-juan XI Xu LI Huai-you 

机构地区:[1]College of Resources and Environment,Shanxi Agricultural University,Taigu 030801,China [2]State Key Laboratory of Eco-hydraulics in Northwest Arid Region of China,Xi'an University of Technology,Xi'an 710048,China [3]The New Zealand Institute for Plant and Food Research Limited,Private Bag 4704,Christchurch 8140,New Zealand [4]School of Geography Science and Geomatics Engineering,Suzhou University of Science and Technology,Suzhou 215000,China [5]Xifeng Scientific Experiment Station of Soil and Water Conservation,Yellow River Conservancy Commission,Qingyang 745000,China

出  处:《Journal of Mountain Science》2022年第1期103-120,共18页山地科学学报(英文)

基  金:supported financially by the National Natural Science Foundation of China (41771259);the Shanxi Province Science Foundation for Youths (201901D211352);the Shanxi Incentive Foundation for Distinguished Doctorates (SXYBKY2019043);the Innovation Foundation of Science and Technology of Shanxi Agricultural University (2020BQ25)。

摘  要:Soil moisture is a limiting factor of ecosystem development in the semi-arid Loess Plateau. Characterizing the soil moisture response to its dominant controlling factors, such as land use and topography, and quantifying the soil-water carrying capacity for revegetation is of great significance for vegetation restoration in this region. In this study, soil moisture was monitored to a depth of 2 m in three land use types(native grassland, introduced grassland,and forestland), two landforms(hillslope and gully),and two slope aspects(sunny and shady) in the Nanxiaohegou watershed of the Loess Plateau,Northwest China. The MIKE SHE model was then applied to simulate the soil moisture dynamics under different conditions and determine the optimal plant coverage. Results showed that the average soil moisture was higher in native grassland than in introduced grassland and Platycladus orientalis forestland for a given topographic condition;however,a high soil moisture content was found in Robinia pseudoacacia forestland, with a value that was even higher than the native grassland of a sunny slope. The divergent results in the two forestlands were likely attributed to the differences in plant coverage. Gully regions and shady slopes usually had higher soil moisture, while lower soil moisture was usually distributed on the hillslope and sunny slope.Furthermore, the mean absolute relative error and Nash-Sutcliffe efficiency coefficient of the MIKE SHE model ranged between 2.8%–7.8% and 0.550–0.902,respectively, indicating that the model could effectively simulate the soil moisture dynamics. The optimal plant coverage was thus determined for hillslope P. orientalis by the model, corresponding to a leaf area index(LAI) value of 1.92. Therefore, for sustainable revegetation on the Loess Plateau,selecting suitable land use types(natural vegetation),controlling the planting density/LAI, and selecting proper planting locations(gully and shady slope regions) should be considered by local policy makers to avoid the over-consumptio

关 键 词:Soil moisture MIKE SHE Optimal plant coverage Land use TOPOGRAPHY 

分 类 号:S152.7[农业科学—土壤学]

 

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