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Vertical Profiles of Soil Water Content as Influenced by Environmental Factors in a Small Catchment on the Hilly-Gully Loess Plateau

机译:黄土丘陵沟壑区小流域土壤水分垂直分布特征

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摘要

Characterization of soil water content (SWC) profiles at catchment scale has profound implications for understanding hydrological processes of the terrestrial water cycle, thereby contributing to sustainable water management and ecological restoration in arid and semi-arid regions. This study described the vertical profiles of SWC at the small catchment scale on the hilly and gully Loess Plateau in Northeast China, and evaluated the influences of selected environmental factors (land-use type, topography and landform) on average SWC within 300 cm depth. Soils were sampled from 101 points across a small catchment before and after the rainy season. Cluster analysis showed that soil profiles with high-level SWC in a stable trend (from top to bottom) were most commonly present in the catchment, especially in the gully related to terrace. Woodland soil profiles had low-level SWC with vertical variations in a descending or stable trend. Most abandoned farmland and grassland soil profiles had medium-level SWC with vertical variations in varying trends. No soil profiles had low-level SWC with vertical variations in an ascending trend. Multi-regression analysis showed that average SWC was significantly affected by land-use type in different soil layers (0–20, 20–160, and 160–300 cm), generally in descending order of terrace, abandoned farmland, grassland, and woodland. There was a significant negative correlation between average SWC and gradient along the whole profile (P<0.05). Landform significantly affected SWC in the surface soil layer (0–20 cm) before the rainy season but throughout the whole profile after the rainy season, with lower levels on the ridge than in the gully. Altitude only strongly affected SWC after the rainy season. The results indicated that land-use type, gradient, landform, and altitude should be considered in spatial SWC estimation and sustainable water management in these small catchments on the Loess Plateau as well as in other complex terrains with similar settings.
机译:在集水区尺度上表征土壤含水量(SWC)剖面对于理解陆地水循环的水文过程具有深远的意义,从而有助于干旱和半干旱地区的可持续水资源管理和生态恢复。这项研究描述了中国东北丘陵和黄土高原小流域尺度上西南沿海的垂直剖面,并评估了所选环境因素(土地利用类型,地形和地貌)对300厘米深度内平均西南沿海的影响。在雨季前后,从一个小流域的101个点取样土壤。聚类分析表明,高SWC处于稳定趋势(从上到下)的土壤剖面最常见于流域,特别是在与梯田有关的沟壑中。林地土壤剖面的SWC值较低,垂直变化呈下降趋势或稳定趋势。大部分废弃的农田和草地土壤剖面都具有中等水平的西南偏西,其垂直变化趋势不同。没有土壤剖面具有低水平的SWC,且垂直变化呈上升趋势。多元回归分析表明,不同土壤层(0–20、20–160和160–300 cm)的平均SWC受土地利用类型的影响很大,通常以梯田,废弃农田,草地和林地的降序排列。整个剖面上的平均SWC与梯度之间存在显着的负相关(P <0.05)。雨季之前,地貌对表土层(0–20 cm)的SWC产生了显着影响,但在雨季之后,整个地形都对SWC产生了影响,山脊上的水平低于沟壑。雨季之后,海拔高度仅严重影响西南海岸。结果表明,在黄土高原上这些小流域以及具有类似设置的其他复杂地形的空间SWC估算和可持续水资源管理中,应考虑土地利用类型,坡度,地形和海拔。

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