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A transferable method for the automated grain sizing of river gravels

机译:一种可转移的河砂砾自动粒度测定方法

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摘要

The spatial and temporal resolution of surface grain-size characterization is constrained by the limitations of traditional measurement techniques. In this paper we present an extremely rapid image-processing-based procedure for the measurement of exposed fluvial gravels and other coarse-grained sediments, defining the steps required to minimize the errors in the derived grain-size distribution. This procedure differs significantly from those used previously. It is based around a robust object-detection algorithm that produces excellent results on images exhibiting a wide range of sedimentary conditions, crucially, without any user intervention or site-specific parameterization. The procedure is tested using a data set comprising 39 images from three rivers with contrasting grain lithology, shape, roundness, and packing configuration and representing a very wide range of textures. It is shown to perform more consistently than the best existing automated method, achieving a precision equivalent to that obtainable by Wolman sampling, but taking between one sixth and one twentieth of the time. The error in area-by-number grain-size distribution percentiles is typically less than 0.05 ψ.
机译:表面粒度表征的时空分辨率受到传统测量技术的局限。在本文中,我们提出了一种非常快速的基于图像处理的程序,用于测量裸露的河床砾石和其他粗粒沉积物,定义了使导出的粒度分布误差最小化所需的步骤。此过程与以前使用的过程有很大不同。它基于强大的对象检测算法,该算法在显示各种沉积条件的图像上产生出色的结果,至关重要的是,无需任何用户干预或特定于地点的参数设置。使用包含来自三条河流的39张图像的数据集对该过程进行了测试,这些图像具有对比鲜明的颗粒岩性,形状,圆度和堆积构造,并表示非常广泛的纹理。它显示出比现有的最佳自动化方法更一致的性能,达到与Wolman采样所能达到的精度相当的精度,但所需的时间在六分之一至二十分之一之间。面积比晶粒尺寸分布百分位数的误差通常小于0.05ψ。

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