2. Aiming at the deficiencies of using Hoek-Brown strength criterion estimate the rock mass mechanical parameter in the practical application, the microstructure tensor is adopted to describe the parameters of the Hoek-Brown strength criterion, which can consider the anisotropism of slope rock mass.
The paper makes calculation and analysis of the water seepage flow of random cracked rock body and discusses,in particula,the influence of the anisotropism of osmotic coefficient on the mode of the seepege now of fissure water.
And the boundary integral equations for the torsion problem of an anisotropic bar with curvilinear cracks are also derived by using the isotropicalized boundary element method. Then the anisotropic problem can be solved on the base of the boundary element method of isotropic problem.
An anisotropic intermolecular potential of the HeNO complex has been obtained by utilizing the Huxley analytic function to fit the intermolecular energy data,which have been calculated at the theoretical level of the RCCSD(T)/aug-cc-pVTZ+bf.
The tearing mode instability and magnetic reconnection process in an anisotropic plasma ( P ⊥≠P ∥ , T ⊥≠T ∥ ) are numerically studied by a two dimensional three component time dependant compressible MHD simulation.
Radial shrinkage and swelling exceeded longitudinal shrinkage and swelling in all the rattan species, suggesting high anisotropism in movement.
Its reflection color is bluishgray to light-blue and it shows middle anisotropism and weak bireflectance.
The properties are name, chemical formula, color, bireflectance, anisotropism, internal reflection, reflectance at wavelengths of 470, 546, 589, and 650 nm, and polishing hardness and micro-indentation hardness.
Several common features of rotifers exhibit anisotropism (e.g.
Synthetic radtkeite shows strong optical anisotropism that is commonly masked by the abundant internal reflections.
Flow of an Anisotropic Dielectric Liquid in a Diverging Channel in a Strong Transverse Electric Field
Magnetic hydrodynamics of two-dimensional flows in a plasma with an anisotropic pressure
The hydrodynamic equations of Chew, Goldberger, and Low  are used to analyze certain types of two-dimensional flows of a plasma with an anisotropic pressure (the pressure along the magnetic field p∥ differs from the pressure across it p⊥).
In the present paper, we investigate numerically convection between two infinite coaxial cylinders with an anisotropic porous filling, using the equations of convection in the Darcy-Boussinesq approximation [1-3].
It is shown that when there are no gas phases and the liquid is incompressible the system of equations reduces to the general equations of the theory of elasticity of an anisotropic body with fictitious stress components.