Soil water depletion depth by planted vegetation on the Loess Plateau
Soil water depletion depth by planted vegetation on the Loess Plateau
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DOI:
10.1007/s11430-009-0087-y
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发表时间:
2009-06
期刊:
影响因子:
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通讯作者:
Zhiqiang Wang;Baoyuan Liu;Gang Liu;Yong‐xiang Zhang
中科院分区:
文献类型:
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作者:
Zhiqiang Wang;Baoyuan Liu;Gang Liu;Yong‐xiang Zhang
Evapotranspiration of much planted vegetation exceeds precipitation, and this can deplete soil water and cause a deep dry layer in the soil profile, which is a serious obstacle to sustainable land use on the Loess Plateau, China. This study aimed to determine water depletion depth of planted grassland, shrub, and forest in a semiarid area on the Loess Plateau. Soil moisture of five vegetation types was measured to >20 m in depth. The vegetation types were crop, natural grasse, seven-year-old planted alfalfa (Medicago sativaL.), 23-year-old planted caragana (Caragana microphyllaLam.) shrub, and 23-year-old planted pine (Pinus tabulaeformisL) forest land. Through comparing moisture of planted alfalfa grass, caragana shrub, and pine forest to crop and natural grassland, the depth and amount of soil water consumed by grassland, caragana brush and pine forest was determined. The depth of soil water depleted by alfalfa, caragana brush, and pine forest reached 15.5, 22.4 and 21.5 m, respectively.