Early-stage identification method of ice-water debris flow and application of early-stage identification method
An early identification and debris flow technology, applied to instruments, alarms, etc., can solve the problems of inability to effectively evaluate, prevent and warn of ice, cement and rock flows, in-depth research on terrain conditions, and inability to identify and correctly judge ice, cement and rock flows, etc., to achieve early identification The effect of reasonable judgment, accurate early recognition and judgment, and strong applicability
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Embodiment 1
[0029] The early identification method of ice and cement flow includes the following steps:
[0030] a. Through Google Earth or on-site measurement, determine the basic topographic data of ice and cement flow: the slope of the ditch bed in the formation area above the accumulation area below the glacier and snow accumulation area;
[0031] b. Measure the slope α of the gully bed of the glacier and the formation area below the snow accumulation area and above the snow accumulation area at different slope sections, and measure the channel slope with the channel length ≥ 10m as the standard;
[0032] c. Early identification of ice, cement and rock flows at different slopes through the slope α of the gully bed above the accumulation area below the glacier and snow-covered area:
[0033] When 14°<α<30°, it is identified as ice cement flow;
[0034] When α≤14° or α≥30°, it is identified as non-ice cement flow;
[0035]d. According to the early identification of ice cement rock flo...
Embodiment 2
[0038] The early identification method of ice and cement flow includes the following steps:
[0039] a. Through Google Earth or on-site measurement, determine the basic topographic data of ice and cement flow: the slope of the ditch bed in the formation area above the accumulation area below the glacier and snow accumulation area;
[0040] b. Measure the slope α of the gully bed of the glacier and the formation area below the snow accumulation area and above the snow accumulation area at different slope sections, and measure the channel slope with the channel length ≥ 10m as the standard;
[0041] c. Use the slope α of the gully bed above the accumulation area below the glacier and snow-covered area to identify the ice-cement rock flow at different slopes at an early stage:
[0042] When 14°<α<30°, it is identified as ice cement flow;
[0043] When α≤14° or α≥30°, it is identified as non-ice cement flow;
[0044] d. According to the early identification of ice cement rock fl...
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