Finite-difference time-domain analysis of ultrasound backscattering in cancellous bone

A. Hosokawa
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引用次数: 5

Abstract

Numerical analysis of ultrasound backscattering in cancellous bone was performed by using three-dimensional finite-difference time-domain (FDTD) simulations with numerical models reconstructed from microcomputed tomographic images of bovine bone. In the simulations, two cancellous bone models with different thicknesses were used. In each model, an artificial absorbing boundary was set at the back surface opposite to the front surface toward which an ultrasound pulse wave was transmitted from a concave transmitter/receiver in water. From the difference between the simulated waveforms for the two bone models, the reflected wave from the front surface could be canceled, and only the backscattered waves inside the bone could be extracted. For the ultrasound transmission parallel to the main orientation of the trabecular network, the backscattered waves from various bone depths were analyzed. The peak-to-peak amplitudes of the backscattered waves from the deep bone depths were moderately correlated with porosity [R2 = 0.43-0.54 (P <; 0.001)]. The backscattered waves from the deeper bone depth could be more clearly separated into the fast and slow waves, and the backscattered wave amplitude could be regarded as the slow wave amplitude.
松质骨超声后向散射的时域有限差分分析
采用三维时域有限差分(FDTD)方法对超声在松质骨中的后向散射进行了数值分析。在模拟中,使用了两种不同厚度的松质骨模型。在每个模型中,在与水下凹形发射器/接收器向前表面发射超声脉冲的前表面相对的后表面设置人工吸收边界。根据两种骨模型模拟波形的差异,可以消去来自前表面的反射波,只提取骨内部的后向散射波。对于平行于骨小梁网络主方向的超声传输,分析了不同骨深度的后向散射波。骨深部背散射波的峰对峰振幅与孔隙度呈中等相关性[R2 = 0.43-0.54 (P <;0.001)]。骨深越深的后向散射波越能清晰地分为快波和慢波,后向散射波振幅可视为慢波振幅。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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