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WAVELET DE-NOISING OF TERRESTRIAL LASER SCANNER DATA FOR THE CHARACTERIZATION OF ROCK SURFACE ROUGHNESS

机译:小波脱模陆地激光扫描仪数据,用于岩石表面粗糙度的表征

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The application of terrestrial laser scanning to the study of rock surface roughness faces a major challenge: the inherent range imprecision makes the extraction of roughness parameters difficult. In practice, when roughness is in millimeter scale it is often lost in the range measurement noise. The parameters extracted from the data, therefore, reflect noise rather than the actual roughness of the surface. In this paper we investigate the role of wavelet de-noising methods in the reliable characterization of roughness using laser range data. The application of several wavelet decomposition and thresholding methods are demonstrated, and the performances of these methods in estimating roughness parameters are compared. As the main measure of roughness fractal dimension is derived from 1D profiles in different directions using the roughness length method. It is shown that wavelet de-noising in general leads to an improved estimation of the fractal dimension for the roughness profiles. The choice of the decomposition method is shown to have a minor effect on the de-noising results; however, the application of hard or soft thresholding mode does have a considerable influence on the estimated roughness measures. The presented results suggest that hard thresholding yields more accurate de-noised profiles for which the estimated roughness measures are more reliable.
机译:陆地激光扫描在岩石表面粗糙度研究中的应用面临重大挑战:固有范围不精确使得粗糙度参数的提取困难。在实践中,当粗糙度以毫米缩放时,它通常在范围测量噪声中丢失。因此,从数据中提取的参数反映了噪声而不是表面的实际粗糙度。在本文中,我们研究了小波去噪方法的作用,使用激光范围数据在粗糙度的可靠性表征中。对若干小波分解和阈值处理方法的应用进行了说明,并进行了估计粗糙度参数的这些方法的性能。由于粗糙度分形尺寸的主要措施是使用粗糙度长度法在不同方向上的1D型材。结果表明,通常的小波脱光导致粗糙度曲线的分形尺寸的改进估计。分解方法的选择显示对去噪结果产生微小的影响;然而,应用硬或软阈值模式的应用对估计的粗糙度措施具有相当大的影响。所提出的结果表明,硬阈值率为更精确的脱发曲线,估计的粗糙度测量更可靠。

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