Cranny density parameters and porosity measured by elastic wave method in quasi-isotropic cranny rock masses

Hong-tu Wang , Jian-qing Jia , Xiao-hong Li , Xue-fu Xian , Guo-zhong Hu

Journal of Central South University ›› 2006, Vol. 13 ›› Issue (5) : 598 -602.

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Journal of Central South University ›› 2006, Vol. 13 ›› Issue (5) : 598 -602. DOI: 10.1007/s11771-006-0095-4
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Cranny density parameters and porosity measured by elastic wave method in quasi-isotropic cranny rock masses

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Abstract

According to the characteristic of elastic waves propagation in medium and the application of elastic waves method in rock mass engineering, the cranny mass with random crannies was regarded as quasi-isotropic cranny mass. In accordance with the rock rupture mechanics, principle of energy balance and Castiglano’s theorem, the relationship of effective dynamic parameters of elasticity (E, v, G) and cranny density parameters or porosity was put forward. On this basis, through the theory of elastic waves propagation in isotropic medium, the relationship between the elastic wave velocity and cranny density parameters and porosity was set up. The theoretical research results show that, in this kind of cranny rock masses, there is nonlinear relationships between the effective dynamic parameters of elasticity and wave velocities and the cranny density parameter or porosity; and with the increase of cranny density parameter or porosity of cranny rock masses, the effective dynamic modulus and the elastic wave velocities of cranny rock masses will decrease; and at the same time, when the cranny density parameter or porosity is very small, the effective dynamic modulus of elasticity and the elastic wave velocities change with the cranny density parameter, which can explain the sensitivity of effective elastic parameters and elastic wave velocities to cranny rock masses.

Keywords

quasi-isotropic cranny mass / wave velocities / effective dynamic parameter / cranny density parameter / porosity

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Hong-tu Wang, Jian-qing Jia, Xiao-hong Li, Xue-fu Xian, Guo-zhong Hu. Cranny density parameters and porosity measured by elastic wave method in quasi-isotropic cranny rock masses. Journal of Central South University, 2006, 13(5): 598-602 DOI:10.1007/s11771-006-0095-4

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References

[1]

HanDe-hua, NurA. Effects of porosity and clay constant on wave velocities in sandstones[J]. Geophysics, 1986, 51(11): 2093-2107

[2]

GaviglioP. Longitudinal waves propagation in a limestone: the relationships between velocities and density [J]. Rock Mech Rock Eng, 1989, 22(4): 290-299

[3]

LiJi-han. The effect of temperature on the elastic waves and sound emission[J]. Journal of Earthquake, 1986, 8(3): 242-245(in Chinese)

[4]

ShiGe, ShenWen-lue, YangDong-quan. The relationship of wave velocities with saturation and fluid distribution in pore space[J]. Chinese Journal of Geophysics, 2003, 46(1): 138-142 in Chinese)

[5]

LiuZhu-ping, WuXiao-wei, ChuZhe-han. The measure and research of rock sonic [J]. Journal of Earth Physics, 1994, 37(5): 659-666(in Chinese)

[6]

ShouPeiThe application of earthquake in engineering[M], 1982, Beijing, Geology Press(in Chinese)

[7]

GaoLong-sheng. The research of the elastic wave velocity under high-pressure of rocks from China mainland[J]. Journal of Earth Physics, 1975, 8(1): 26-38(in Chinese)

[8]

WuShao-wu. Apply the sonic to the stress of adjacent rock[J]. Earthquake, 1984, 4(6): 12-19(in Chinese)

[9]

LuoJin-tang. The effect of rock temperature on pressure wave velocity[J]. Journal of Rock and Soil Engineering, 1985, 7(5): 80-84(in Chinese)

[10]

ZimmermanR W, KingM SPropagation of acoustic waves through cranny rock[C]// Ashworth E. Research and Engineering Applications in Rock Masses, 1985, Netherlands, A. A. Balkema: 739-745

[11]

WillisJ R. A polarization approach to the scattering of elastic waves: I. scattering by a single inclusion[J]. J Mech Phys Solids, 1980, 28: 287-305

[12]

ShenLian-di, ShiGe. The effect in rock elastic wave velocity by saturability, frequency, type of fluid[J]. Journal of Earth Physics, 1992, 35(Suppl): 322-331(in Chinese)

[13]

IrwinG R. Analysis of stresses and strains near the ends of a cranny traversing a plate[J]. J Appl Mech, 1975, 24: 261-364

[14]

SihG CHandbook of stress intensity factors[M], 1973, Bethlehem, Lehigh University

[15]

HudsonJ A. Overall elastic properties of isotripic materials with arbitrary distribution of circular crannies[J]. Geophys J Int, 1990, 102: 465-469

[16]

WangHong-tu, XianXue-fu. The propagation characteristic of elastic waves in complicated stress situation[J]. Journal of Chongqing University, 1989, 12(4): 204-207(in Chinese)

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