Birch-Murnaghan equation of state: Difference between revisions

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m (Added some internal links + slight tidy.)
(Changed a minus for a plus in the equation.)
 
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:<math> p=\frac{3B_0}{2}\left[\left(\frac{V_0}{V}\right)^{7/3}-\left(\frac{V_0}{V}\right)^{5/3}\right] </math>
:<math> p=\frac{3B_0}{2}\left[\left(\frac{V_0}{V}\right)^{7/3}-\left(\frac{V_0}{V}\right)^{5/3}\right] </math>


Where <math>B_0</math> is the isothermal (or calibration) [[Compressibility |bulk modulus]].  However, since this form is not dependent on the bulk modulus derivative, <math>B_0'</math>, it is rarely used and either the first order or third order form are used.  The third order shows increased accuracy over the Murnaghan equation of state and has a relatively simple analytical form:
Where <math>B_0</math> is the isothermal (or calibration) [[Compressibility |bulk modulus]].  However, since this form is not dependent on the bulk modulus derivative, <math>B_0'</math>, it is rarely used and either the first order or third order form are used.  The third order shows increased accuracy over the Murnaghan equation of state and has a relatively simple analytical form (Eq. 4.42 in <ref>[http://dx.doi.org/10.2277/052166392X Jean-Paul Poirier "Introduction to the Physics of the Earth's Interior", Cambridge University Press, 2nd Edition (2000)] ISBN 9780521663922</ref>):


:<math> p=\frac{3B_0}{2}\left[\left(\frac{V_0}{V}\right)^{7/3}-\left(\frac{V_0}{V}\right)^{5/3}\right]\left[1-\frac{3}{4}\left(B_0'-4\right)\left(\left(\frac{V_0}{V}\right)^{2/3}-1\right)\right]</math>
:<math> p=\frac{3B_0}{2}\left[\left(\frac{V_0}{V}\right)^{7/3}-\left(\frac{V_0}{V}\right)^{5/3}\right]\left[1+\frac{3}{4}\left(B_0'-4\right)\left(\left(\frac{V_0}{V}\right)^{2/3}-1\right)\right]</math>


==References==
==References==
<references/>
<references/>
[[category: equations of state]]
[[category: equations of state]]

Latest revision as of 16:10, 3 November 2011

An extension, or rather a generalization, of the Murnaghan equation of state was presented by Albert F. Birch in 1947. [1] It has become known as the Birch-Murnaghan equation of state. The generalization followed from the identification that the strain energy could be approximated as a Taylor series based on the finite strain in the crystal. Common orders include first, second and third, where the first order approximation reduces to the Murnaghan equation of state.

Since finite strain is represented as:

The internal energy, , for the strain is defined as a Taylor expansion:

The pressure, then is the derivative of this equation:

The second order form is thus:

Where is the isothermal (or calibration) bulk modulus. However, since this form is not dependent on the bulk modulus derivative, , it is rarely used and either the first order or third order form are used. The third order shows increased accuracy over the Murnaghan equation of state and has a relatively simple analytical form (Eq. 4.42 in [2]):

References[edit]