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The influence of litter crusts on soil properties and hydrological processes in a sandy ecosystem

机译:沙地生态系统中凋落物结皮对土壤特性和水文过程的影响

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摘要

Litter crusts are integral components of the water budget in terrestrial ecosystems, especially in arid areas. This innovative study is designed to quantify the ecohydrological effectiveness of litter crusts in desert ecosystems. We focus on the positive effects of litter crusts on soil water holding capacity and water interception capacity compared with biocrusts. Litter crusts significantly increased soil organic matter compared to biocrusts and bare lands, by 2.4 times and 3.8 times, respectively. Higher organic matter content resulted in increased soil porosity and decreased soil bulk density. Meanwhile, soil organic matter can help to maintain maximum infiltration rates. Litter crusts significantly increased the water infiltration rate under high water supply. Our results suggested that litter crusts significantly improve soil properties, thereby influencing hydrological processes. Litter crusts play an important role in improving hydrological effectiveness and provide a microhabitat conducive to vegetation restoration in dry sandy ecosystems.
机译:地壳是陆地生态系统中水预算不可或缺的组成部分,尤其是在干旱地区。这项创新的研究旨在量化沙漠生态系统中垃圾c的生态水文有效性。与生物结皮相比,我们重点研究了结皮对土壤持水量和截水能力的积极影响。与生物地壳和裸地相比,凋零的地壳显着增加了土壤有机质,分别增加了2.4倍和3.8倍。较高的有机质含量导致土壤孔隙度增加和土壤容重降低。同时,土壤有机质可以帮助维持最大的渗透率。在高供水条件下,小结皮明显增加了水的渗透率。我们的研究结果表明,凋落物结皮可显着改善土壤性质,从而影响水文过程。凋落的结皮在提高水文有效性方面起着重要作用,并提供了有利于干旱沙质生态系统植被恢复的微生境。

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