METHODS article
Front. Mar. Sci.
Sec. Ocean Observation
Volume 12 - 2025 | doi: 10.3389/fmars.2025.1539828
Optimizing an Image Analysis Protocol for Ocean Particles in Focused Shadowgraph Imaging Systems
Provisionally accepted- Department of Ocean and Earth Sciences, Old Dominion University, Norfolk, United States
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A variety of imaging systems are in use in oceanographic surveys, and the opto-mechanical configurations have become highly sophisticated. However, much less consideration has been given to the accurate reconstruction of imaging data. To improve reconstruction of particles captured by Focused Shadowgraph Imaging (FoSI), a system that excels at visualizing low-optical-density objects, we developed a novel object detection algorithm to process images with a resolution of ~ 12 m per pixel. Suggested improvements to conventional edge-detection methods are relatively simple and timeefficient, and more accurately render the sizes and shapes of small particles ranging from 24 to 500 m. In addition, we introduce a gradient of neutral density filters as a part of the protocol serving to calibrate recorded gray levels and thus determine the absolute values of detection thresholds. Set to intermediate detection threshold levels, particle numbers were highly correlated with beam attenuation (cp) measured independently. The utility of our method was underscored by its ability to remove imperfections (dirt, scratches and uneven illumination), and by capturing the transparent particle features such as found in gelatinous plankton, marine snow and a portion of the oceanic gel phase.
Keywords: Optical oceanography, Particle imaging, Shadowgraphy, binarization, Edge-detection, Gels, Particulate organic carbon, Schlieren
Received: 04 Dec 2024; Accepted: 11 Jun 2025.
Copyright: © 2025 Huang and Bochdansky. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
* Correspondence: Huanqing Huang, Department of Ocean and Earth Sciences, Old Dominion University, Norfolk, United States
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