Method for evaluating ultrasonic attenuation coefficient of coal rock based on fractal dimension
A technology of attenuation coefficient and evaluation method, which is applied to the analysis of solids using sound waves/ultrasonic waves/infrasonic waves, material analysis and material analysis using sound waves/ultrasonic waves/infrasonic waves, and can solve problems such as difficulty in carrying out experiments and heavy workload, and achieve evaluation The effect of high accuracy, fast speed and less experimental data
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Embodiment 1
[0088] A method for evaluating coal rock ultrasonic attenuation coefficient based on fractal and fractal dimensions, comprising the following steps:
[0089] A. Drill standard coal rock samples, and group coal rock samples according to the number of cleats, cleat density, and cleat development angle;
[0090] B. Construct the two-dimensional numerical models of each group of coal samples, and calculate the box dimension of each two-dimensional numerical model to
[0091] and attenuation coefficient;
[0092] C. Construct a box dimension calculation model based on the development of coal and rock cleats;
[0093] D. Analyze the correlation between the attenuation coefficient of the two-dimensional numerical model of coal and rock and the box dimension, and build an evaluation model for the attenuation coefficient based on the box dimension.
Embodiment 2
[0095] Based on the principle of the above-mentioned embodiment, this embodiment discloses a specific implementation manner, and the coal rock sample is taken from a certain work area in Yunnan.
[0096] A. Drill standard coal and rock samples. The standard coal and rock samples drilled are cylindrical, without obvious block, with flat end faces, and both ends are perpendicular to the core axis.
[0097] According to the cleat angle and cleat distribution, the standard rock samples are divided into three groups. In this embodiment, six coal rock samples are drilled and divided into three groups A, B, and C, such as Figure 1 to Figure 6 As shown, the coal rock samples are respectively recorded as A1, A2, B1, B2, C1, and C2. Among them, the cleats of the two coal samples in group A are evenly distributed, the number of cleats is different, and the cleat angles are similar; the cleats of the two coal samples in group B are evenly distributed, the cleat densities are not equal, a...
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