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Numerical analysis of fast and slow waves backscattered from various depths in cancellous bone

机译:松质骨中不同深度后向散射的快波和慢波的数值分析

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Ultrasound backscattering in cancellous bone was numerically investigated using finite-difference time-domain (FDTD) simulations. The cancellous bone models with various thicknesses were prepared, and artificial absorbing layers were set at the back surfaces. An ultrasound pulse wave was radiated toward the front surface and was transmitted in the direction parallel to the main trabecular orientation. The backscattered signal inside cancellous bone was isolated from the difference between two simulated waveforms obtained using the bone models with different thicknesses. In the simulated results of the incident and backscattered waveforms, the fast and slow waves, which could propagate mainly in the respective parts of the trabecular elements and the pore spaces, could be clearly observed. For each wave, the backscatter coefficient, which was defined as the amplitude ratio of the backscattered wave to the incident wave, was derived at various bone depths. At all bone depths, the backscatter coefficients of the fast wave were not correlated with porosity, but those of the slow wave were moderately correlated.
机译:使用有限差分时间域(FDTD)模拟,在数值研究中进行了超声波反向散射。制备具有各种厚度的松质骨模型,并在后表面设定人造吸收层。超声波脉冲波朝向前表面辐射,并在平行于主线前取向的方向上传递。消泡骨内的反向散射信号从使用具有不同厚度的骨模型获得的两个模拟波形之间的差异分离。在入射和反向散射的波形的模拟结果中,可以清楚地观察到主要在小梁元件和孔隙空间的各个部分中传播的快速和慢波。对于每个波,在各种骨深度中导出了被定义为反向散射波的幅度比的反向散射系数。在所有骨深处时,快波的反向散射系数与孔隙率没有相关,但是慢波的那些被中度相关。

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