Jeanloz

Low-pressure, Bl, phase and high-pressure, B2, phase data (Jeanloz and Ahrens, 1980). 

In order to relate the parameters of (4.5), the shock-wave equation of state, to the isentropie and isothermal finite strain equations of state (discussed in Section 4.3), it is useful to expand the shock velocity normalized by Cq into a series expansion (e.g., Ruoff, 1967 Jeanloz and Grover, 1988 Jeanloz, 1989). 

Moreover, upon comparing (4.32) with (4.14), it can be seen that (Jeanloz and Grover, 1988) the Birch-Murnaghan equation (4.32) with a2 = 0 describes the isentropic equation of state provided the linear shock-particle velocity relation (4.5) describes the Hugoniot. In combination, these require that... 

Bancroft et al. (1965), and in the case of CaO and the B1 to B2 transition discovered by Jeanloz and Ahrens (1979), complete reversion of the low-pressure phase occurs upon unloading. These latter transitions involve rearrangement of the lattice which can occur via its deformation rather than complete reconstruction. The volume change in the Si02 transition is much larger than in the case of CaO, as seen in Fig. 4.15. In contrast to the pressure-volume plane when plotted in the Ph-u, plane, the occurrence of these transitions is less striking in this representation (Fig. 4.14). 

Jeanloz, R. (1989), Shock Wave Equation of State and Finite Strain Theory, J. Geophys. Res 94, 5873-5886. 

Jeanloz, R., and Grover, R. (1988), Birch-Murnaghan and Us-Up Equations of State, in Proceedings of the American Physical Society Topical Conference on Shock Waves in Condensed Matter, Monterey, CA, 1987 (edited by Schmidt S.C. and N.C. Holmes), Plenum, New York, pp. 69-72. 

American Chemical Society Committee for Carbohydrate Nomenclature D. Horton (Chairman), L. Anderson, D.C. Baker, H.H. Baer, J.N. BeMiller, B. Bossenbroek, R. W. Jeanloz, K.L. Loening, W. A. Szarek, R.S. Tipson, W.J. Whelan, R.L. Whistler. 

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