A Kalman filter-Hungarian algorithm with a postprocessor for tracking aeolian saltating particle in high-speed video

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL Earth Surface Processes and Landforms Pub Date : 2024-11-04 DOI:10.1002/esp.6014
Fanmin Mei, Hongji Zhou, Jin Su, Jinguang Chen
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Abstract

Saltating particle tracking (SPT) is an essential visualized channel to understand the dynamics of aeolian saltation at sand particle size scale, while the published SPTs could have low recall or accuracy rate and misestimate further saltation intensity. Hence, a Kalman filter-Hungarian algorithm with a postprocessor (KF-H-k) was proposed, where the Kalman filter was employed for predicting particle motion, and the Hungarian algorithm for optimizing global assignment, as well as the postprocessor with k-means cluster for correcting the erroneous recovered tracks by Kalman filter-Hungarian algorithm. The new SPT was validated in a digital high-speed video with various particle concentrations from a wind tunnel experiment. It demonstrated that compared with the previous SPTs, KF-H-k kept the highest and most stable accuracy (85% ~ 93%), the best spatial resolution, the moderate recall rate (50% ~ 70%) and time cost. The present work offers a new hybrid scheme for tracking sand particles accurately but alsodatasets for automatically identifying saltating tracks via machine learning models, very critical for insight into new hypothesis on sand ripple formation.

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一种带后处理器的卡尔曼滤波-匈牙利算法用于高速视频中风成跳跃粒子的跟踪
跳跃粒子跟踪(SPT)是了解沙粒尺度上风沙跃动动力学的重要可视化通道,但已有的SPT可能召回率或准确率较低,并对进一步的跳跃强度有错误估计。因此,提出了一种带有后处理器的卡尔曼滤波-匈牙利算法(KF-H-k),其中卡尔曼滤波器用于预测粒子运动,匈牙利算法用于优化全局分配,以及带有k-means聚类的后处理器用于校正卡尔曼滤波-匈牙利算法错误恢复的轨迹。新的SPT在风洞实验的不同颗粒浓度的数字高速视频中得到了验证。结果表明,与以往的spt相比,KF-H-k保持了最高和最稳定的正确率(85% ~ 93%)、最佳的空间分辨率、中等的查全率(50% ~ 70%)和时间成本。目前的工作提供了一种新的混合方案来准确地跟踪沙粒,同时也提供了通过机器学习模型自动识别跳跃轨迹的数据集,这对于深入了解沙纹形成的新假设非常重要。
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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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