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An integrated acoustic and electromagnetic wave-based technique to estimate subbottom sediment properties in a freshwater environment

机译:一种基于声波和电磁波的综合技术,可估算淡水环境中的底部沉积物特性

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An integrated acoustic and electromagnetic (EM) wave-based technique was developed to estimate sediment porosity and top-layer thickness in shallow freshwater environments. The integrated methodology reduces the limitation of each of the individual techniques and combines the data for a more robust inversion solution. The acoustic and EM-wave reflection coefficients are determined based on the ratios of reflected signal strengths from sediments and a reference aluminium plate. An iterative algorithm that uses reflection coefficients to optimize the sediment porosity was developed. Once the optimal sediment porosity is obtained, the acoustic and EM wave speeds and then the top-layer thickness were evaluated. In comparison with ground truth data, the measured and estimated sediment porosity and top-layer thickness show differences less than 8.6%. The new integrated method provides an efficient and accurate methodology to obtain sediment properties under different sediment conditions.
机译:开发了一种基于声波和电磁波(EM)的集成技术,以估算浅水浅层环境中的沉积物孔隙度和顶层厚度。集成的方法减少了每种单独技术的局限性,并将数据组合起来以提供更强大的反演解决方案。声反射和EM波反射系数是根据沉积物和参考铝板的反射信号强度之比确定的。提出了一种利用反射系数优化沉积物孔隙度的迭代算法。一旦获得最佳的沉积物孔隙度,就可以评估声波和EM波的速度,然后评估顶层的厚度。与地面真相数据相比,测得的和估算的沉积物孔隙度和顶层厚度的差异小于8.6%。新的集成方法提供了一种有效而准确的方法,可在不同的泥沙条件下获得泥沙特性。

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