论文信息 - Birch's Law: Why Is It So Good?

Birch's Law: Why Is It So Good?

Birch's law arises in the physics of solids as a linear approximation, in a certain range of density, of a power law. For a change of chemical composition within the same crystal structure, the velocity-density relation is constant with a slope of nearly -0.5 in the first-order approximation.

Dae H. Chung | D. H. Chung

[1] Naohiro Soga,et al. Some elastic constant data on minerals relevant to geophysics , 1968 .

[2] N. Christensen. Elastic properties of polycrystalline magnesium, iron, and manganese carbonates to 10 kilobars , 1972 .

[3] F. Birch. The velocity of compressional waves in rocks to 10 kilobars: 1. , 1960 .

[4] Chi‐yuen Wang,et al. Equation of state of periclase and some of its geophysical implications , 1969 .

[5] N. Christensen. Shear wave velocities in metamorphic rocks at pressures to 10 kilobars , 1966 .

[6] N. Christensen. Elasticity of ultrabasic rocks , 1966 .

[7] S. P. Marsh,et al. On the composition of the Earth's interior , 1964 .

[8] F. Birch,et al. Composition of the Earth's Mantle , 1937 .

[9] N. Christensen. Chemical changes associated with upper mantle structure , 1968 .

[10] A R Plummer,et al. Introduction to Solid State Physics , 1967 .