Preparation method of disturbed belt sample for reflecting stress state of primary rock
A technology of sample preparation and original rock stress, which is applied in the preparation of test samples, etc., can solve the problems of not considering the original rock stress state of rock or soil, cumbersome process, and great influence on test results, so as to achieve true data results Reliable, uniform density and moisture content, guaranteed uniformity effect
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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 project area.
[0065] Step A: Carry out on-site inv...
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