怒江支流勐波罗河流域泥石流活动特征与危险性评价

    Activity characteristics and risk assessment of debris flow in Mengboluo River basin, a tributary of Nujiang River

    • 摘要: 勐波罗河为怒江左岸一级支流,其代表性特征为深切峡谷地貌、广布的沉积-变质软岩、断裂剪切破坏形成丰富物源等。选取勐波罗河右岸受灾严重的10条泥石流为研究对象,利用精细化调查成果和地理信息系统(Geographic Information System,GIS)分析技术,系统分析泥石流地形条件特征,精细划分物源类型和储量信息,开展泥石流流速、洪峰流量、一次固体物质总量等动力学特征参数研究。以沟谷流域作为单元,选取可启动物源量、山坡平均坡度、流域面积、沟道纵坡降、主沟长度、植被覆盖率和年均降雨量评价因子,完成了泥石流危险性评价。结果表明: ①受灾严重的10条泥石流沟物源总储量为140.49×104 m3,可启动物源量为38.96×104 m3,包括了崩滑堆积、沟床冲蚀、坡面侵蚀3大类物源,以沟床冲蚀类最为发育,可启动物源量达20.34×104 m3,通过物源类型现场分析,该流域右岸泥石流均属于稀性泥石流; ②区内暴雨洪峰流量整体较大,芦子园沟暴雨洪峰流量达到了108.92 m3/s,一次固体物质总量总体较大,芦子园沟一次固体物质总量达到了24.35×104 m3; ③危险性评价结果显示流域内有高危险泥石流6条、中危险泥石流3条、低危险泥石流1条,经野外验证,评价结果与现场情况高度吻合。研究成果可为怒江支流勐波罗河沿岸泥石流防治提供科学依据。

       

      Abstract: Mengboluo River is a first-level tributary on the left bank of Nujiang River. And it is representative in Nujiang River Basin due to its deep canyon landform, widespread sedimental -metamorphic soft rocks, and rich material sources formed by fault shear failure. Ten highly destructive debris flows on the right bank of Mengboluo River were selected as the study objects in this paper, and refined investigation results and Geographic Information System (GIS) analysis technology were adopted to systematically analyze topographic condition characteristics of the debris flows. Besides, provenance types and reserve information were finely classified. The research on dynamic characteristic parameters such as debris flow velocity, flood peak flow, and the total amount of primary solid matter was carried out. The authors took gully basin as the unit and selected the evaluation factors such as the dynamic reserve of material sources, the slope of the hillside, the basin area, the longitudinal slope of the gully, the length of the main gully, the vegetation coverage rate and the rainfall to complete the risk assessment of debris flow. The results showed that the total reserve of provenance in the 10 highly destructive debris flow gullies was 140.49×104 m3, and the amount of material sources that can be activated was 38.96×104 m3, including three major types of provenance, that is landslide accumulation, gully bed erosion, and slope surface erosion. Among them, gully bed erosion was the most developed, and the amount of provenance could be activated, reaching 20.34×104 m3. The debris flows on the right bank of this basin all belonged to rare debris flows, through on-site analysis of provenance types. The overall peak flow of the debris flow in the area was relatively large, and the peak flow of the debris flow in Luziyuan Valley reached 108.92 m3/s. The total amount of solid matter at one time was generally large, and the total amount of solid matter at one time in Luziyuan Valley reached 24.35×104 m3. The results of the risk assessment showed that there were 6 high-risk debris flows, 3 medium-risk debris flows and 1 low-risk debris flow in the basin. After field verification, the assessment results were highly consistent with the on-site conditions. The research results could provide scientific basis for the prevention and control of debris flows along Mengboluo River, a tributary of Nujiang River.

       

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