首页> 外文会议>International Soil Conservation Organization Conference vol.2; 20020526-31; Beijing(CN) >Vegetation Destruction and Restoration Effects on Soil Erosion Process on the Loess Plateau
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Vegetation Destruction and Restoration Effects on Soil Erosion Process on the Loess Plateau

机译:黄土高原地区植被破坏与恢复对土壤侵蚀过程的影响

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Vegetation destruction or natural vegetation restoration greatly affects soil erosion process and eco-environmental change. Studies on soil erosion on the Loess Plateau have been focused on soil erosion process and erosion control at severe soil erosion regions where vegetation was completely destroyed. However, there are few available data to quantify effects of vegetation destruction or natural vegetation restoration on soil erosion process. The Ziwuling area on the Loess Plateau, where original vegetation destruction by human activities about 130 years ago, the secondary vegetation restoration during the past about 130 years, and deforestation again, provides an experimental area to quantify effects of vegetation change on soil erosion and eco-environment. The objective of this paper was to use data from field investigation and runoff plot observation to quantify effects of vegetation change on soil erosion. The results showed that before the secondary vegetation restoration, i.e., about 130 years ago, soil erosion conditions in the Ziwuling region were similar to present loessial hilly-gully region of Yan'an-Ansai-Zhidan zone. After the secondary vegetation restoration, soil erosion was very slight, impacts of rainfall and topographical condition on soil erosion were not well obvious, and vegetation effect on soil erosion was predominated. Ephemeral gully erosion at hillslopes and gully erosion at gully slopes or valley ceased, and sediment deposition occurred in ephemeral gully and gully channels during process of the secondary vegetation restoration. Meanwhile, valley erosion and gravitative erosion was almost controlled by vegetation. The soil-erosion was changed from man-made accelerated erosion to natural erosion under ecological balance. Once the secondary forest land was converted to cropland, soil erosion greatly increased, soil erosion rate from a newly deforested land reached 10,000 t/(km~2 · yr) to 24,000 t/(km~2 · yr), which was 787 to 1682 times greater, as compared to woodland. These results show that man-made accelerated erosion play in a cardinal role in the regions where vegetation was completely destroyed by human activities. These finding will help to improve the understanding relationship between vegetation change and soil erosion, and to provide powerful data to make strategies for rehabilitating better eco-environment in the northwestern region of China.
机译:植被破坏或自然植被恢复极大地影响了土壤侵蚀过程和生态环境的变化。黄土高原地区的土壤侵蚀研究主要集中在植被被完全破坏的严重土壤侵蚀地区的土壤侵蚀过程和侵蚀控制。但是,几乎没有可用的数据来量化植被破坏或自然植被恢复对土壤侵蚀过程的影响。黄土高原的子午岭地区,约130年前人类活动破坏了原始植被,近130年来又进行了次生植被恢复,再度砍伐森林,这为量化植被变化对土壤侵蚀和生态的影响提供了实验区域。 -环境。本文的目的是利用野外调查和径流图观测数据来量化植被变化对土壤侵蚀的影响。结果表明,在次生植被恢复之前,即大约130年前,子午岭地区的土壤侵蚀状况与目前的延安—安塞—芝丹地区的黄土丘陵沟壑区相似。次生植被恢复后,水土流失很小,降雨和地形条件对水土流失的影响并不明显,植被对水土流失的影响最为明显。在次生植被恢复过程中,山坡上的临时沟壑侵蚀和沟壑或山谷沟壑的侵蚀停止了,在短暂的沟壑和沟渠中发生了沉积物沉积。同时,谷地侵蚀和重力侵蚀几乎受植被控制。在生态平衡下,土壤侵蚀从人为的加速侵蚀转变为自然侵蚀。次生林地转变为耕地后,土壤侵蚀大大增加,新毁林地的土壤侵蚀率达到10,000 t /(km〜2·yr)至24,000 t /(km〜2·yr),即787至是林地的1682倍。这些结果表明,人为加速侵蚀在植被被人类活动完全破坏的地区起着重要作用。这些发现将有助于增进对植被变化与水土流失之间关系的理解,并提供有力的数据来制定策略,以恢复中国西北地区更好的生态环境。

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