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Variations of deep soil moisture under different vegetation types and influencing factors in a watershed of the Loess Plateau, China

机译:黄土高原流域不同植被类型下深层土壤水分的变化及其影响因素

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摘要

Soil moisture in deep soil layers is a relatively stable water resource for vegetation growth in the semi-arid Loess Plateau of China. Characterizing the variations in deep soil moisture and its influencing factors at a moderate watershed scale is important to ensure the sustainability of vegetation restoration efforts. In this study, we focus on analyzing the variations and factors that influence the deep soil moisture (DSM) in 80–500 cm soil layers based on a soil moisture survey of the Ansai watershed in Yan'an in Shanxi Province. Our results can be divided into four main findings. (1) At the watershed scale, higher variations in the DSM occurred at 120–140 and 480–500 cm in the vertical direction. At the comparable depths, the variation in the DSM under native vegetation was much lower than that in human-managed vegetation and introduced vegetation. (2) The DSM in native vegetation and human-managed vegetation was significantly higher than that in introduced vegetation, and different degrees of soil desiccation occurred under all the introduced vegetation types. Caragana korshinskii and black locust caused the most serious desiccation. (3) Taking the DSM conditions of native vegetation as a reference, the DSM in this watershed could be divided into three layers: (i) a rainfall transpiration layer (80–220 cm); (ii) a transition layer (220–400 cm); and (iii) a stable layer (400–500 cm). (4) The factors influencing DSM at the watershed scale varied with vegetation types. The main local controls of the DSM variations were the soil particle composition and mean annual rainfall; human agricultural management measures can alter the soil bulk density, which contributes to higher DSM in farmland and apple orchards. The plant growth conditions, planting density, and litter water holding capacity of introduced vegetation showed significant relationships with the DSM. The results of this study are of practical significance for vegetation restoration strategies, especially for the choice of vegetation types, planting zones, and proper human management measures.
机译:在半干旱黄土高原地区,深层土壤水分是植被生长的相对稳定的水资源。在适度的分水岭范围内表征深层土壤水分的变化及其影响因素对于确保植被恢复工作的可持续性很重要。在这项研究中,我们基于对山西延安安塞流域的土壤水分调查,重点分析影响80-500 cm土壤层深层土壤水分(DSM)的变化和因素。我们的结果可以分为四个主要发现。 (1)在分水岭尺度上,DSM在垂直方向的120–140和480–500 cm处出现较大的变化。在可比较的深度,天然植被下的DSM变化远低于人工管理的植被和引入的植被。 (2)原生植被和人为管理植被的DSM值明显高于引入植被,并且在所有引入植被类型下土壤干化程度都不同。柠条锦鸡儿和黑刺槐造成了最严重的干燥。 (3)以当地植被的DSM条件为参考,该流域的DSM可以分为三层:(i)降雨蒸腾层(80-220 cm); (ii)过渡层(220-400 cm); (iii)稳定层(400-500 cm)。 (4)流域尺度上影响帝斯曼的因素因植被类型而异。 DSM变化的主要局部控制是土壤颗粒组成和年平均降雨量。人类的农业管理措施可以改变土壤容重,从而导致农田和苹果园的DSM升高。引入植被的植物生长条件,种植密度和凋落物持水量与DSM呈显着关系。这项研究的结果对于植被恢复策略,特别是对植被类型,种植区域的选择和适当的人为管理措施的选择具有实际意义。

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