Wave Propagation in Elastic Media
Wave Propagation in Elastic Media
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弹性介质中的波传播
DOI:
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发表时间:
1988
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影响因子:
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通讯作者:
Julian L. Davis
中科院分区:
文献类型:
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作者:
Julian L. Davis
In previous chapters we investigated the properties of waves propagating in water and in inviscid and viscous fluids. It was pointed out that the conservation law that distinguishes one medium from another is the energy equation. It is the conservation law that contains the appropriate equation of state or constitutive equation which defines the medium. For example, an adiabatic equation of state was used to define a fluid such as air and a different equation of state for water. The adiabatic condition cannot be used across a shock wave since we must allow for a jump in entropy, etc. It was further pointed out in previous chapters that the approach used in mathematically describing the conservation laws was the Euler representation. This representation is more useful in dealing with large particle motions of the fluid. It was also stated that the conservation laws contain the fundamental physics of a given situation in the sense that from these conservation equations, which are called the field equations, we can obtain the velocity, pressure fields, etc., which give the wave properties. Since the field equations were couched in the Eulerian coordinates, the various fields that were derived from their solutions were also expressed as functions of these Eulerian coordinates. In principle, we can map back into the Lagrangian coordinates and thereby obtain the particle trajectories.