Hazard assessment method of ice-water-debris flow and its application
A debris flow and risk technology, applied in data processing applications, material inspection products, instruments, etc., can solve problems such as the risk of hard-ice cement debris flow, in-depth research on unrecognized topographic conditions, etc., to achieve reasonable risk judgment, simple division method, Easy to execute effects
- Summary
- Abstract
- Description
- Claims
- Application Information
AI Technical Summary
Problems solved by technology
Method used
Image
Examples
Embodiment 1
[0033] The method for judging the danger of ice and cement flow includes the following steps:
[0034] a. Through Google Earth or on-site measurement, determine the basic topographical data of ice and cement flow: the area of glaciers and snow-covered areas A0, the slope of the ditch bed slope α and the width W of the ditch bed above the accumulation area below the glacier and snow-covered area;
[0035] b. Measure the slope α and width W of the gully bed in the glacier and the formation area below the snow accumulation area and above the snow accumulation area in different slope sections, and measure the gully slope with the gully length ≥ 10m as the standard;
[0036]c. From the relative area of glacier and snow area A=A0 / W 2 And the slope α of the gully bed above the accumulation area below the glacier and snow-covered area divides the danger levels of ice cement flow in different slope sections from high to low:
[0037] When A>500 and 14°<α<21°, the danger of ice cem...
Embodiment 2
[0044] The method for judging the risk of ice and cement rock flow includes the following steps:
[0045] a. Through Google Earth or on-site measurement, determine the basic topographical data of ice and cement flow: the area of glaciers and snow-covered areas A0, the slope of the ditch bed slope α and the width W of the ditch bed above the accumulation area below the glacier and snow-covered area;
[0046] b. Measure the slope α and width W of the gully bed in the glacier and the formation area below the snow accumulation area and above the snow accumulation area in different slope sections, and measure the gully slope with the gully length ≥ 10m as the standard;
[0047] c. From the relative area of glacier and snow area A=A0 / W 2 And the slope α of the gully bed above the accumulation area below the glacier and snow-covered area divides the danger levels of ice cement flow in different slope sections from high to low:
[0048] When A>500 and 14°<α<21°, the danger of ice...
Embodiment 3
[0057] The method for judging the risk of ice and cement rock flow includes the following steps:
[0058] a. Through Google Earth or on-site measurement, determine the basic topographical data of ice and cement flow: the area of glaciers and snow-covered areas A0, the slope of the ditch bed slope α and the width W of the ditch bed above the accumulation area below the glacier and snow-covered area;
[0059] b. Measure the slope α and width W of the gully bed in the glacier and the formation area below the snow accumulation area and above the snow accumulation area in different slope sections, and measure the gully slope with the gully length ≥ 10m as the standard;
[0060] c. From the relative area of glacier and snow area A=A0 / W 2 And the slope α of the gully bed above the accumulation area below the glacier and snow-covered area divides the danger levels of ice cement flow in different slope sections from high to low:
[0061] When A>500 and 14°<α<21°, the danger of ice...
PUM
Abstract
Description
Claims
Application Information
- R&D Engineer
- R&D Manager
- IP Professional
- Industry Leading Data Capabilities
- Powerful AI technology
- Patent DNA Extraction
Browse by: Latest US Patents, China's latest patents, Technical Efficacy Thesaurus, Application Domain, Technology Topic, Popular Technical Reports.
© 2024 PatSnap. All rights reserved.Legal|Privacy policy|Modern Slavery Act Transparency Statement|Sitemap|About US| Contact US: help@patsnap.com