首页> 外文会议>Biennial ISEM Conference on Ecological Modelling for Global Change and Coupled Human and Natural System >The impacts of grassland vegetation degradation on soil hydrological and ecological effects in the source region of the Yellow River~A case study in Junmuchang region of Maqin country
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The impacts of grassland vegetation degradation on soil hydrological and ecological effects in the source region of the Yellow River~A case study in Junmuchang region of Maqin country

机译:草地植被降解对黄河源区土壤水文和生态效应的影响〜MAQIN国家君蒙昌地区案例研究

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As one of the special structure layers of grassland ecosystem, soil has significant hydrological and ecological effects. However, the soil interior hydrological and ecological effects will be affected by the grassland vegetation degradation. This research was carried out in the source region of the Yellow River, where grassland vegetation was in severe degradation, with the methods of choosing typical areas and quadrates to collect soil samples and doing experiments in laboratory. Some important results were obtained from this research which mainly contained four aspects as follows. (1) With the increasing of grassland degradation degrees, the capillary water holding capacity and saturated water content decreased in all soil layers as a whole. However, the capillary water holding capacity and saturated water content increased when the grassland degradation from middle degree to heavy degree in all soil layers. (2) With the increasing of grassland degradation degrees, the field water capacity first increased and then decreased in the 0~10cm layer and decreased in the means of "increasing-decreasing- increasing-decreasing" manners in the 10~20cm, but it gradually increased in the 20~30cm layers. (3) Soil saturated water content was mainly affected by the soil bulk density and total phosphorus, and the soil capillary water holding capacity was mainly affected by the soil bulk density, while the soil field water capacity was mainly affected by the total nitrogen. (4) Soil water retention was not a simple process of decreasing during the grassland degradation, but it was a changing process of differences. It was very important to protect the original grassland vegetation for the hydrological process in the river source regions and this research could provide the scientific basis for revealing the impacts of grassland vegetation degradation on soil hydrological and ecological effects in the region scale and displaying the effects of grassland vegetation degradation on river runoff forming and regulation.
机译:作为草原生态系统的特殊结构层之一,土壤具有显着的水文和生态效应。然而,土壤内部水文和生态效应将受草原植被降解的影响。该研究在黄河的源区进行,草地植被处于严重降解,具有选择典型区域和Quadrates以收集土壤样品并在实验室进行实验。从本研究中获得了一些重要成果,主要包含四个方面如下。 (1)随着草地降解程度的增加,整个土壤层的毛细管持有能力和饱和含水量下降。然而,当草地从中度降解到所有土层中的重度时,毛细管水持续容量和饱和含水量增加。 (2)随着草地降解程度的增加,田间水容量首先增加,然后在0〜10cm层中降低,并在10〜20cm中“增加 - 减少 - 递减减小”方式下降,但它逐渐增加20〜30cm层。 (3)土壤饱和含水量主要受土壤堆积密度和总磷的影响,土壤毛细管持有能力主要受土壤堆积密度的影响,而土壤田间水能主要受到总氮的影响。 (4)土壤水保留不是在草地降解过程中减少的简单过程,但它是一种不断变化的差异过程。保护原始草地植被用于河流源区的水文过程非常重要,这项研究可以为揭示草地植被降解对地区规模的土壤水文和生态效应的影响提供科学依据,并显示出效应草地植被降解河流径流成型和监管。

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