This study uses seismological principles and techniques including waveform simulations and travel time calculations to reveal the nature of ultrasound wave propagation in long bones at small offsets (source-to-receiver distances) and times. Our experiments confirm the existence of reflected and converted body waves originating from wave interaction at the internal interfaces of a bone structure. We demonstrate that the bone ultrasound responses can be successfully simulated and properly interpreted based on a simple, horizontally layered approximation.
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Le et al. (2010) studied this question.
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