天然小沙样品粒度分布的免校准图像分析方法

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Vah Mélanie, Jarno Armelle, Marin François
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引用次数: 0

摘要

从床载或悬浮物迁移过程中采集的天然沙样可能太小,无法进行筛分。然而,将输运质量与沉积物尺寸联系起来对于校准沉积物输运模型至关重要。图像分析技术是一种既简单又廉价的替代方法。本研究提出了一个适用于天然沙粒和小砾石的一般规律,该规律从统计学角度将颗粒的伸长率与平整度联系起来,并在对颗粒形状和颗粒在筛网通道上的取向进行一些假设后,根据平板扫描仪提供的颗粒图像,给出最接近筛分技术的质量分布。所提出的模型基于椭圆形颗粒形状和颗粒优先穿过筛网对角线的假设。任何来自不同产地(河流、海洋和采石场)的同质或异质砂都可以直接进行分析,无需进一步校准。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Calibration-free image analysis method for grain-size distribution of small natural sand samples

Calibration-free image analysis method for grain-size distribution of small natural sand samples

Natural sand samples collected from bedload or suspension transport can be too small to be sieved. However, related transported mass to sediment size is crucial to calibrate sediment transport models. Image analysis technique can be an easy and cheap alternative. The present study proposes a general law valid for natural sand grains and small gravels that statistically relates elongation to flatness of particles and gives after some assumptions on grain shape and orientation of grains at the sieve mesh passage, the closest distribution of mass to sieving technique from images of grains given by a flatbed scanner. The proposed model is based on the hypothesis of an ellipsoidal grain shape and a preferential grain crossing aligned with the sieve diagonal. Any sand either homogeneous or heterogeneous from various origins (fluvial, marine and quarry) can be analysed directly without any further need for calibration.

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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
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