Method for determining distributed explosive source triggering parameters
A technology of explosive seismic sources and excitation parameters, which is applied in the field of geophysical exploration, can solve the problems of restricting the application of distributed seismic sources and poor excitation effects, and achieve the effects of increasing frequency, broadening seismic wave frequency band, and increasing main frequency
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example 1
[0039] Example 1: Method for determining safe excitation parameters of three-layer soil medium structure:
[0040] Step 1: From the analysis of single-hole static penetration and geotechnical identification maps in the target area, it can be known (such as figure 2 ), there are two main types of soil within the range of 0-30m at this point: silt (and silt clay) and silt. The silt can be subdivided into three types: silt, silty clay, and silt and silty clay layer.
[0041] According to the static penetration test results, the rock and soil 30m thick from the ground are divided into three layers.
[0042] For the soil medium of the three layers, the density is detected by the ring knife method;
[0043] According to the arrival time of the seismic wave and the distance between the monitoring point and the charge package, the wave velocity of each layer can be obtained (the number of monitoring points = the number of layers);
[0044] use the formula Determine the modulus o...
example 2
[0061] Example 2: Determination method of safety excitation parameters of five-layer soil medium structure:
[0062] Step 1: According to the analysis of single-hole static sounding and rock-soil identification map in the target area, there are two main types of soil within the range of 0-30m at this point: silt (and silt clay) and silt. For silt, it can be subdivided into three types: silt, silty clay, and interbedded silt and silty clay.
[0063] According to the results of static penetration testing, the rock and soil 30m thick from the ground are divided into 5 layers.
[0064] For the soil medium of the 5 layers, the density is detected by the ring knife method;
[0065] According to the arrival time of the seismic wave and the distance between the monitoring point and the charge package, the wave velocity of each layer can be obtained (the number of monitoring points = the number of layers);
[0066] use the formula Determine the modulus of elasticity of the medium; ...
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