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Estimating soil erosion changes in the Wenchuan earthquake disaster area using geo-spatial information technology

机译:利用地理空间信息技术估算汶川地震灾区的土壤侵蚀变化

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摘要

The secondary disasters induced by the Wenchuan earthquake of May 12, 2008, such as landslides, collapsing rocks, debris flows, floods, etc., have changed the local natural landscape tremendously and caused heavy soil erosion in the earthquake-hit areas. Using thematic mapper images taken before the earthquake and airborne images taken after the earthquake, we extracted information about the destroyed landscape by utilizing remote sensing and geographical information system techniques. Then, taking into account multi-year precipitation, vegetation cover, soil type, land use, and elevation data, we evaluated the soil erosion area and intensity using the revised universal soil loss equation. Results indicate that the soil erosion in earthquake-hit areas was exacerbated, with the severe erosion area increasing by 279.2 km~(2), or 1.9percent of the total statistical area. Large amounts of soil and debris blocked streams and formed many barrier lakes over an area of more than 3.9 km~(2). It was evident from the spatial distribution of soil erosion areas that the intensity of soil erosion accelerated in the stream valley areas, especially in the valleys of the Min River and the Jian River.
机译:2008年5月12日汶川地震引发的继发性灾害,如滑坡,坍塌的岩石,泥石流,洪水等,极大地改变了当地的自然景观,并在受灾地区造成了严重的水土流失。使用地震前拍摄的专题制图仪图像和地震后拍摄的机载图像,我们利用遥感和地理信息系统技术提取了有关被破坏景观的信息。然后,考虑到多年降水,植被覆盖,土壤类型,土地利用和海拔数据,我们使用修正的通用土壤流失方程评估了土壤侵蚀面积和强度。结果表明,地震灾区土壤侵蚀加剧,重度侵蚀面积增加了279.2 km〜(2),占统计总面积的1.9%。大量的土壤和碎屑阻塞了河流,并在超过3.9 km〜(2)的区域内形成了许多屏障湖。从水土流失区域的空间分布可以明显看出,在流域,特别是the江和Jian江流域,水土流失的加剧。

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