Method for judging outburst susceptibility of moraine lake without moraine embankment
A kind of easy-to-fire and glacial technology, applied in the direction of instruments, complex mathematical operations, data processing applications, etc., can solve the problems of difference in influence, failure to consider slope parameters, influence, etc., to improve accuracy, eliminate errors, and adaptability strong effect
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Embodiment 1
[0092] A method for judging the susceptibility of a moraine lake burst without a buried moraine embankment, comprising the following steps:
[0093] a. Determine whether the moraine lake is a moraine lake without buried moraine embankments;
[0094] b. Determine the basic parameters of the moraine lake without buried ice and moraine embankments through Google Earth, including the slope aspect of the parent glacier θ, the slope aspect of the dangerous ice body γ, the slope of the back water slope of the moraine embankment β, and the slope of the dangerous ice body at the back edge of the glacier lake α , the vertical height difference H between the center of mass of the dangerous ice body and the ice lake, the movement distance L between the center of mass of the dangerous ice body and the ice lake, the width of the transverse fissure W of the dangerous ice body, the distance L between the transverse fissure at the rearmost end of the dangerous ice body and the front end of the ...
Embodiment 2
[0140]A method for judging the susceptibility of a moraine lake burst without a buried moraine embankment, comprising the following steps:
[0141] a. Determine whether the moraine lake is a moraine lake without buried moraine embankments;
[0142] b. Determine the basic parameters of the moraine lake without buried ice and moraine embankments through Google Earth, including the slope aspect of the parent glacier θ, the slope aspect of the dangerous ice body γ, the slope of the back water slope of the moraine embankment β, and the slope of the dangerous ice body at the back edge of the glacier lake α , the vertical height difference H between the center of mass of the dangerous ice body and the ice lake, the movement distance L between the center of mass of the dangerous ice body and the ice lake, the width of the transverse fissure W of the dangerous ice body, the distance L between the transverse fissure at the rearmost end of the dangerous ice body and the front end of the d...
Embodiment 3
[0192] A method for judging the susceptibility of a moraine lake burst without buried moraine embankment, characterized in that it comprises the following steps:
[0193] a. Determine whether the moraine lake is a moraine lake without buried moraine embankments;
[0194] b. Determine the basic parameters of the moraine lake without buried ice and moraine embankments through Google Earth, including the slope aspect of the parent glacier θ, the slope aspect of the dangerous ice body γ, the slope of the back water slope of the moraine embankment β, and the slope of the dangerous ice body at the back edge of the glacier lake α , the vertical height difference H between the center of mass of the dangerous ice body and the ice lake, the movement distance L between the center of mass of the dangerous ice body and the ice lake, the width of the transverse fissure W of the dangerous ice body, the distance L between the transverse fissure at the rearmost end of the dangerous ice body and...
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