- 积分
- 0
- 注册时间
- 2006-12-27
- 仿真币
-
- 最后登录
- 1970-1-1
|
发表于 2007-1-16 01:36:36
|
显示全部楼层
来自 美国
The initial modulus E_0 can be calculated through the formula E_0 = 2*G_0*(1+mu), where mu is the Poisson's ratio, the initial shear modulus G_0 can be determined by in-situ tests, laboratory tests, and empirical relations. In-situ tests include the cross-hole test, the seismic cone penetration test, and the surface wave test, etc. In laboratory, the resonant column test and bender element test are commonly used. In most tests, shear wave velocity needs to be measured to find the G_0 value by using the formula, G_0 = ρ * v_s, where ρ is the mass density and v_s is the measured shear wave velocity.
There are many empirical relations for determining the initial shear modulus. The general expression is given as G_0 = c_g * F(e) * p^n_g * pa^(1-n_g), where c_g and n_g are material constants, e is the void ratio reflecting the compactness of soil, F is a function of void ratio, p is the mean stress, and pa is the atmospheric pressure for normalization. The formula proposed by Hardin and Black (1968) is one of the widely used empirical relations given by G_0 = c_g * (e_g - e)^2/(1+e) * p^n_g * pa^(1-n_g), where e_g is also material constant.
sigma_3 is the minor principal principal stress. |
|