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植被斑块性对黄土高原废弃农田地下水分分布的影响。

Effect of vegetation patchiness on the subsurface water distribution in abandoned farmland of the Loess Plateau, China.

机构信息

School of Geography and Tourism, Shaanxi Normal University, Shaanxi, Xi'an 710119, China.

School of Geography and Tourism, Shaanxi Normal University, Shaanxi, Xi'an 710119, China.

出版信息

Sci Total Environ. 2020 Dec 1;746:141416. doi: 10.1016/j.scitotenv.2020.141416. Epub 2020 Jul 31.

Abstract

Patchiness of grassland results in important effects on ecohydrological processes in arid and semiarid areas; however, the influences on subsurface water flow and soil water distribution remain poorly understood, particularly during vegetation succession on slopes. This study examined these effects by comparing the water flow behaviors and preferential infiltration between vegetation patches (VP) and interspace patches (IP) in three sites at different states of vegetation succession (grass, subshrub and shrub) in abandoned farmland of the Loess Plateau, China. Dye tracer infiltration showed that patchiness of vegetation increased spatial variations of soil water and preferential infiltration by increasing the densities of fine root length and fine root volume in the soil profile. Moreover, the more abundant and intricate roots following a lateral direction beneath VP likely contributed to lateral flow and infiltration variability. However, differences between VP and IP were not significant because considerable living fine roots and decayed roots of IP also provided preferential flow pathways. Our finding indicated that IP could compete with VP for access to soil water resources, which potentially increased hillslope-scale infiltration and reduced surface runoff and erosion risk. Under the different states of vegetation succession, subshrub patches showed significantly greater preferential infiltration volume (28.53 mm) and contribution of preferential infiltration to total infiltration (60.58%) than grass and shrub patches. Vegetation patch size made positive effects on improving preferential flow and water movement. Greater preferential flow in subshrub patches played a positive role in soil water storage and replenishment. Therefore, natural restoration of a slope area with small heterogeneity in preferential flow can be successfully applied in the Loess Plateau, particularly during the subshrub succession state.

摘要

草地的斑块性对干旱半干旱地区的生态水文过程有重要影响;然而,其对地下水流和土壤水分分布的影响仍知之甚少,特别是在坡面植被演替过程中。本研究通过对比中国黄土高原废弃农田三个处于不同植被演替阶段(草地、亚灌丛和灌丛)的三个样点中植被斑块(VP)和间隔斑块(IP)的水流行为和优先入渗,来研究这些影响。示踪剂染色入渗试验表明,植被斑块性通过增加土壤剖面中细根长度和细根体积的密度,增加了土壤水分的空间变异性和优先入渗。此外,VP 下方沿侧向方向更丰富、更复杂的根系可能有助于侧向流动和渗透的变化。但是,VP 和 IP 之间的差异并不显著,因为 IP 中大量有生活力的细根和腐烂的根也提供了优先流路径。本研究结果表明,IP 可能与 VP 竞争土壤水资源,这可能增加坡面尺度的入渗,降低地表径流和侵蚀风险。在不同的植被演替阶段,亚灌丛斑块表现出显著更大的优先入渗体积(28.53 毫米)和优先入渗对总入渗的贡献(60.58%),而草地和灌丛斑块则较小。植被斑块大小对改善优先流和水分运移有积极影响。亚灌丛斑块中更大的优先流对土壤水分储存和补给起到了积极作用。因此,在黄土高原,特别是在亚灌丛演替阶段,对具有较小优先流非均质性的坡面区域进行自然恢复是可行的。

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