Silty Mudstone Mechanical Properties under Freeze-Thaw Cycles
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Results reveal that under similar confining pressure, reducing temperature and increasing freeze-thaw cycles progressively amplify the degradation rate of P-wave velocity and specimen quality. Conversely, there is an exponential decline in elastic modulus values and peak stress. The internal friction angle and cohesion of silty mudstone also decrease exponentially with decreasing freezing temperature.
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Zhenning SHI创建时间：
2024-04-11
