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本文用模型实验研究了声波在致密碳酸盐岩地层井中的传播特性。采用合金铭模拟致密碳酸盐岩地层，按10：1的比例制成缩小的模型井。模型并呈圆柱形，高0．4m，直径0．3m，中心并初在经0．02m。在井中充水时接收到一组全波列声波。实验观测到全波列中的折射纵波、折射横波、斯通利波的基本特征与理论分析一致，但实测的折射纵横波幅度比及它们的几何衰减与理论分析不符。我们认为引起这些差异的主要原因是理论分析没有考虑声源的指向性。
In this paper, the model experiment is used to study the propagation of acoustic waves in tight carbonate rock formations. Using alloy mounds to simulate tight carbonate formations, a reduced model well was made at a 10: 1 ratio. The model is cylindrical with a height of 0.4 m and a diameter of 0.3 m. The center is initially at 0.02 m. A full wave train of sound waves is received when the well is filled with water. The fundamental characteristics of the refracted, refracted and Stolley waves observed in the full-wave series are consistent with the theoretical analysis. However, the observed amplitude ratios of the refracted waves and their geometric decay are not consistent with the theoretical analysis. We think the main reason for these differences is that the theoretical analysis does not consider the directivity of the sound source.