Tasinkevych Yuriy, Podhajecki Jerzy, Falińska Katarzyna, Litniewski Jerzy
Institute of Fundamental Technological Research of the Polish Academy of Sciences, 5b Pawinskiego Str., 02-106 Warsaw, Poland.
Institute of Fundamental Technological Research of the Polish Academy of Sciences, 5b Pawinskiego Str., 02-106 Warsaw, Poland.
Ultrasonics. 2016 Feb;65:105-12. doi: 10.1016/j.ultras.2015.10.013. Epub 2015 Oct 24.
The paper presents a method that allows the thickness of a compact bone layer and longitudinal wave velocity in the bone to be determined simultaneously with the use of reflected waves, with particular emphasis on the case of layers when the propagation time through the layer is shorter than the time duration of the interrogating pulse. The proposed method estimates simultaneously the thickness of the cortical bone layer and acoustic wave velocity by fitting the temporal spectrum of the simulated reflected wave to the spectrum of the reflected wave measured experimentally. For the purpose of echo-simulations the model of "soft tissue - compact bone layer - cancellous bone" was developed. Next, the cost function was defined as the least square error between the measured and simulated temporal spectra. Minimization of the cost function allowed us to determine the values of the parameters of the cortical bone layer which best fitted the measurements. To solve the optimization problem a simulated annealing algorithm was used. The method was tested using acoustic data obtained at the frequency of 0.6 MHz and 1 MHz respectively for a custom designed bone mimicking phantom and a calf femur. For the cortical shell of the calf femur whose thickness varies from 2.1 mm to 2.4 mm and velocity of 2910 m/s, the relative errors of the thickness estimation ranged from 0.4% to 5.5%. The corresponding error of the acoustic wave velocity estimation in the layer was 3.1%. In the case of artificial bone the thickness of the cortical layer was equal to 1.05 and 1.2 mm and acoustic wave velocity was 2900 m/s. These parameters were determined with the errors ranging from 1.9% to 10.8% and from 3.9% to 4.5% respectively.
本文提出了一种方法,该方法能够利用反射波同时测定致密骨层的厚度和骨中的纵波速度,尤其着重于传播通过该层的时间短于探测脉冲持续时间的层的情况。所提出的方法通过将模拟反射波的时间谱与实验测量的反射波谱进行拟合,同时估计皮质骨层的厚度和声波速度。为了进行回波模拟,建立了“软组织 - 致密骨层 - 松质骨”模型。接下来,将代价函数定义为测量的和模拟的时间谱之间的最小二乘误差。代价函数的最小化使我们能够确定最符合测量结果的皮质骨层参数值。为了解决优化问题,使用了模拟退火算法。该方法分别使用在0.6 MHz和1 MHz频率下针对定制设计的仿骨模型和小牛股骨获得的声学数据进行了测试。对于厚度在2.1 mm至2.4 mm之间且速度为2910 m/s的小牛股骨皮质壳,厚度估计的相对误差范围为0.4%至5.5%。该层中声波速度估计的相应误差为3.1%。在人造骨的情况下,皮质层的厚度等于1.05和1.2 mm,声波速度为2900 m/s。这些参数的测定误差分别在1.9%至1.08%和3.9%至4.5%之间。