喀斯特地区泥石流物源量分析和敏感性评价——以贵州省威宁县二塘河流域为例
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王飞龙(1991-),男,汉族,河南周口人,硕士研究生,研究方向为环境地质、地质灾害、遥感应用。E-mail:584975674@qq.com

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P642.23

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Sediment Volume Analysis and Susceptibility Assessment of Debris Flow in Karst Area:A Case Study in Ertang River Basin of Weining County, Guizhou Province
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    摘要:

    选取典型喀斯特区域为研究区,根据数字高程模型(DEM)并结合遥感影像和野外实地调查,将研究区进行小流域的划分。针对喀斯特地区有其特定的环境和对地质灾害的特殊成灾机理,分析了土壤侵蚀对喀斯特地区泥石流灾害的贡献作用,并提出了研究区泥石流物源量的计算方法。从泥石流形成条件出发,基于流域单元,选取土壤侵蚀、侵蚀物源量、相对高差、纵坡降、沟壑密度、形成区平均坡度、沟道弯曲系数等7个评价因子,采用层次分析法确定各个评价指标的权重,对研究区二塘河流域17条泥石流沟做了敏感性评价。结果表明,评价结果能够反映研究区二塘河流域泥石流灾害的空间分布与区域活动特征,为小流域泥石流灾害的防治和土地合理利用提供了科学依据。

    Abstract:

    This paper choosen the typical Karst area as the study area, and divided the study area into small watersheds, which based on digitalelevation model (DEM) and remote sensing image and field investigation. Based on the specific environment and disaster mechanism of the geo -logical disaster in the Karst area, this paper analyzed the contribution of soil erosion to the debris flow disaster in the karst area , and put forwardthe calculating method of debris flow source of quantity. According to the formation conditions of debris flow and based on the watershed unit ,this paper choose seven evaluation factors such as the soil erosion, erosion of provenance, relative elevation, longitudinal slope, gully density,average slope of the formation area, channel bend coefficient, and used Analytic Hierarchy Process to determine the weight of each evaluationindex, and made the sensitivity evaluation of 17 debris flow in the Ertang River Basin of the study area. The evaluation results can reflect the spa -tial distribution and regional activity characteristics of debris flow disasters in Ertang River Basin , and provide a scientific basis for the preventionand control of debris flow hazards and rational land use in small watershed.

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  • 收稿日期:2017-04-15
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  • 在线发布日期: 2022-06-23
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