Overview
- Authors:
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V. N. Zharkov
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Laboratory of Theoretical Physics, O. Yu. Shmidt Institute of Physics of Earth, Academy of Sciences of the USSR, Moscow, USSR
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V. A. Kalinin
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Laboratory of Theoretical Physics, O. Yu. Shmidt Institute of Physics of Earth, Academy of Sciences of the USSR, Moscow, USSR
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Table of contents (7 chapters)
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- V. N. Zharkov, V. A. Kalinin
Pages 1-19
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- V. N. Zharkov, V. A. Kalinin
Pages 20-31
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- V. N. Zharkov, V. A. Kalinin
Pages 32-85
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- V. N. Zharkov, V. A. Kalinin
Pages 86-105
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- V. N. Zharkov, V. A. Kalinin
Pages 106-177
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- V. N. Zharkov, V. A. Kalinin
Pages 178-206
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- V. N. Zharkov, V. A. Kalinin
Pages 207-235
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Back Matter
Pages 236-257
About this book
We started our work on theoretical methods in the phys ics of high pressures (in connec tion with geophysical applications) in 1956, and we immediately encountered many problems. Naturally, we searched the published Iiterature for solutions to these problems but whenever we failed to find a solution or when the solution did not satisfy us, we attempted to solve the problern ourselves. We realized that other investigators working in the physics of high pres sures would probably encounter the same problems and doubts. Therefore, we decided to write this book in order to save our colleagues time and effort. Apart from the descriptions of ex perimental methods, the book deals only with those problems which we encountered in our own work. Allproblems in high-pressure physics have, at present, only approximate solutions, which are very rough. Therefore, it is not surprising that different investigators approach the same problems in different ways. Our approach does not prejudge the issue and we are fully aware that there are other points of view. Our aim was always to solve a glven problern on a physical basis. For example, the concept of the Grüneisenparameter needs further develop ment but it is based on reliable physical ideas. On the other hand, Simon's equation for the melting curve has, in our opinion, no clear physical basis and is purely empirical. Equations of this type are useful in systematic presentation of the experimental material but they are un suitable for any major extrapolation.
