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在固体物理模拟测试系统上，用自制的纵、横波换能器观测了简单的层状三维固体模型的透射和反射波场，得到了几种振型的地震记录剖面。通过分析记录剖面上各种波的同相轴发现，在固体物理模拟实验中，不但能很好地记录到各种报型的主振动波场，还能接收到换能器杂振动引起的波场。这种波场既取决于换能器本身的性能，也受耦合条件的影响，而且与偏振和测试方式有关，从而加剧了固体介质中波场的复杂性。文章充分利用高性能纵、横渡换能器，着重定性地分析了各种剖面中杂振动波场的传播机理，为固体物理模型实验提供了纵、横波波场的基本特征。在国内首次给出了多种振型的固体地震模拟记录剖面。
In the solid state physical simulation test system, the transmission and reflection wave fields of a simple layered three-dimensional solid model are observed by using homemade longitudinal and transverse wave transducers, and several types of seismic record sections are obtained. Through the analysis of the records of various waves on the profile of the phase axis found in the solid state physical simulation experiments, not only can be well documented various types of reports of the main vibration wave field, but also receive the vibration caused by the transducer vibration field . This wavefield depends on both the performance of the transducer itself and the coupling conditions, but also on the polarization and test methods, exacerbating the complexity of the wavefield in a solid medium. This paper makes full use of high-performance longitudinal and transversal transducers, and qualitatively analyzes the propagation mechanism of the miscellaneous vibration wave fields in various sections, which provides the fundamental characteristics of the longitudinal and transverse wavefields for solid-state physical model experiments. For the first time in China, a variety of mode shapes of solid seismic analog recording profiles are given.