The aquatic particle number quandary

Optical surveys of aquatic particles and their particle size spectra have become important tools in studies of light propagation in water, classification of water masses, and the dynamics of trophic interactions affecting particle aggregation and flux. Here, we demonstrate that typical settings used...

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Main Authors: Alexander B. Bochdansky, Huanqing Huang, Maureen H. Conte
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-11-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2022.994515/full
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author Alexander B. Bochdansky
Huanqing Huang
Maureen H. Conte
author_facet Alexander B. Bochdansky
Huanqing Huang
Maureen H. Conte
author_sort Alexander B. Bochdansky
collection DOAJ
description Optical surveys of aquatic particles and their particle size spectra have become important tools in studies of light propagation in water, classification of water masses, and the dynamics of trophic interactions affecting particle aggregation and flux. Here, we demonstrate that typical settings used in image analysis vastly underestimate particle numbers due to the particle – gel continuum. Applying a wide range of threshold values to change the sensitivity of our detection system, we show that macrogels cannot be separated from more dense particles, and that a true particle number per volume cannot be ascertained; only relative numbers in relation to a defined threshold value can be reported. A quandary thus presents itself between choosing a detection threshold low enough to accurately record orders of magnitude more particles on one hand or selecting a higher threshold to yield better image quality of plankton on the other. By observing the dynamics of coagulation and dissolution steps unique to cation-bridged gels abundant in aquatic systems, we find naturally occurring gels, and microscopic particles attached to them, to cause the ill-defined particle numbers. In contrast, the slopes in particle number spectra remained largely unaffected by varying sensitivity settings of the image analysis. The inclusion of fainter particles that are not typically captured by imaging systems provides a window into the true microscale spatial heterogeneity at scales relevant to small plankton organisms and processes that are dependent on particle density such as surface-associated chemical reactions as well as particle coagulation and aggregation dynamics.
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spelling doaj.art-396c6caa7db54a32aa3aa09d58dfa07a2022-12-22T03:58:25ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452022-11-01910.3389/fmars.2022.994515994515The aquatic particle number quandaryAlexander B. Bochdansky0Huanqing Huang1Maureen H. Conte2Department of Ocean and Earth Sciences, Old Dominion University, Norfolk, VA, United StatesDepartment of Ocean and Earth Sciences, Old Dominion University, Norfolk, VA, United StatesBermuda Institute of Ocean Sciences, St. George's, BermudaOptical surveys of aquatic particles and their particle size spectra have become important tools in studies of light propagation in water, classification of water masses, and the dynamics of trophic interactions affecting particle aggregation and flux. Here, we demonstrate that typical settings used in image analysis vastly underestimate particle numbers due to the particle – gel continuum. Applying a wide range of threshold values to change the sensitivity of our detection system, we show that macrogels cannot be separated from more dense particles, and that a true particle number per volume cannot be ascertained; only relative numbers in relation to a defined threshold value can be reported. A quandary thus presents itself between choosing a detection threshold low enough to accurately record orders of magnitude more particles on one hand or selecting a higher threshold to yield better image quality of plankton on the other. By observing the dynamics of coagulation and dissolution steps unique to cation-bridged gels abundant in aquatic systems, we find naturally occurring gels, and microscopic particles attached to them, to cause the ill-defined particle numbers. In contrast, the slopes in particle number spectra remained largely unaffected by varying sensitivity settings of the image analysis. The inclusion of fainter particles that are not typically captured by imaging systems provides a window into the true microscale spatial heterogeneity at scales relevant to small plankton organisms and processes that are dependent on particle density such as surface-associated chemical reactions as well as particle coagulation and aggregation dynamics.https://www.frontiersin.org/articles/10.3389/fmars.2022.994515/fullparticlesmarine snowtransparent exopolymer particlesaquatic opticsimaginggels
spellingShingle Alexander B. Bochdansky
Huanqing Huang
Maureen H. Conte
The aquatic particle number quandary
Frontiers in Marine Science
particles
marine snow
transparent exopolymer particles
aquatic optics
imaging
gels
title The aquatic particle number quandary
title_full The aquatic particle number quandary
title_fullStr The aquatic particle number quandary
title_full_unstemmed The aquatic particle number quandary
title_short The aquatic particle number quandary
title_sort aquatic particle number quandary
topic particles
marine snow
transparent exopolymer particles
aquatic optics
imaging
gels
url https://www.frontiersin.org/articles/10.3389/fmars.2022.994515/full
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