A preparation method of a dislocation zone sample reflecting the stress state of the original rock
A technology of sample preparation and original rock stress, applied in the preparation of test samples, etc., can solve the problems of not considering the original rock stress state of rock or soil, the process is cumbersome, and the test results are greatly affected, and the data results are true. Reliable, uniform density and moisture content, guaranteed uniformity
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[0064] The area of the Baihetan Hydropower Station site generally develops an interlayer dislocation zone with poor mechanical properties that is rare in other projects. The interlayer stagger zone C2 of the underground powerhouse on the left bank tends to the upper reaches of the right bank on the whole. The thickness of C2 basaltic tuff is 100cm, and the thickness is 20-30cm. It has poor properties, is easy to soften when exposed to water, has low strength, and will produce plastic deformation and shear deformation. It is the main weak interlayer in the factory area on the left bank. C3, C4, C5 and other interlayer dislocation belts are distributed near the underground powerhouse on the right bank, which are exposed in different parts such as the roof arch of the factory building, and a large-scale roof arch collapse is likely to occur. The undisturbed samples of this test were taken from the horizontal boreholes in the engineering area.
[0065] Step A: Carry out on-site...
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