Traditional Culture Encyclopedia - Photography and portraiture - Remote sensing study on land subsidence in mining area
Remote sensing study on land subsidence in mining area
Study on dynamic expansion of surface subsidence area. The most effective remote sensing survey method is to use multi-temporal aerial remote sensing images of mining areas for superposition analysis. In a mine in Hebei Province, using multi-temporal and different kinds of aerial photography images, including panchromatic black-and-white photos, color infrared photos and multi-spectral images, these images were processed by computer to extract the expansion law of subsidence area. The processing flow is shown in Figure 3- 1 1.
Figure 3- Flow chart of image processing for dynamic expansion of surface subsidence in mining area +0 1
After the above processing, all the images are geometrically matched, and a band is extracted from each phase image and given different display colors to form a false color multi-phase matching image. The image clearly shows the shapes of subsidence areas in different periods. Therefore, combined with the geology and mining conditions of underground coal mining, the dynamic development law of subsidence area can be obtained.
Through the analysis of the surface subsidence area of this mine, it is concluded that the surface subsidence area will increase by 654.38+0.3 hm2 for every 6,543.8+0,000 tons of coal mined. The expansion direction of subsidence area is basically the same as that of underground mining, but the formation of subsidence area lags behind the formation of underground goaf, and the subsidence area will be stable after 1 ~ 2 years of coal mining.
The subsided waterlogged area appears dark gray-gray-black tone in black-and-white photos, but dark black in color infrared photos with clear boundaries. The depth of stagnant water shows different tones in color infrared photos. Through image analysis and field sampling, different types and depths of stagnant water can be delineated. This kind of accumulated water is usually divided into four types: deep water area, shallow water area, swamp area and seepage area. See Table 3-3 for the interpretation marks of color infrared aerial photographs.
Table 3-3 Classification and Interpretation Signs of Remote Sensing Images in a Coal Mine Subsidence and Water Accumulation Area in Hebei Province
The collapse boundary and shape of non-stagnant water subsidence area can also be extracted from color infrared photos. The extracted information and data can be converted into topographic maps or geographical maps to make thematic maps about the situation of subsidence areas, and the areas of various subsidence areas can also be calculated by computers or electronic orthogonal instruments. These maps and data are important basic data for formulating the treatment scheme of subsidence area. Figure 3- 12 is a remote sensing classification interpretation map of a coal mine subsidence area in Hebei Province, which uses the data of aerial remote sensing images and SPOT satellite images.
Figure 3- 12 Remote Sensing Classification Interpretation Map of Coal Mine Subsidence Area
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