By measuring the velocity of the P wave and S wave on the three orthotropic different directions including parallel and vertical direction to the stratum of the compacted rock samples including slate
phyllite
mylonite and metasandstone
the two obvious anisotropy effects of P wave and S wave velocity are put forward. One is the conformity of the anisotropy of P wave and S wave velocity expressed by that the anisotropic indexes of S wave velocity would linearly increase as the P wave anisotropic indexes increase in a great degree
namely the anisotropy of S wave velocity is statistically proportional to that of P wave; the other effect is the variation between P wave and S wave velocity anisotropy
which is mainly expressed by that the anisotropic index of the P wave velocity is usually greater than S wave in the parallel and vertical directions to the stratum of the rock samples which means that the anisotropy of S wave velocity is inferior to that of P wave. Using numerical value test based on the wave velocity function of the transverse isotropic elastic medium
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微生物诱导碳酸钙沉淀-植被协同防护边坡抗侵蚀机制研究
Related Author
DU Zuo-long
HUANG Mao-song
LI Shu-cai
ZHANG Li
MA Xiu-yuan
XUE Yi-guo
WANG Zhe-chao
LI Yi-fan
Related Institution
Technology Center of China Construction Eighth Engineering Division
Key Laboratory of Geotechnical and Underground Engineering of Ministry of Education, Tongji University
Research Center of Geotechnical and Structural Engineering, Shandong University
Key Laboratory of Geological Hazards in Three Gorges Reservoir Area of Ministry of Education, China Three Gorges University
Dadu River Dagangshan Hydropower Development Co., Ltd., Ya’an