Particle size distribution at Ocean Station Papa from nanometers to millimeters constrained with intercomparison of seven methods

Author:

Zhang Xiaodong1,Huot Yannick2,Gray Deric3,Sosik Heidi M.4,Siegel David5,Hu Lianbo67,Xiong Yuanheng16,Crockford E. Taylor4,Potvin Geneviève2,McDonnell Andrew8,Roesler Collin9

Affiliation:

1. 1Division of Marine Science, School of Ocean Science and Engineering, The University of Southern Mississippi, Stennis Space Center, MS, USA

2. 2Université de Sherbrooke, Sherbrooke, Quebec, Canada

3. 3Naval Research Laboratory, Washington, DC, USA

4. 4Woods Hole Oceanographic Institution, Woods Hole, MA, USA

5. 5Department of Geography, University of California Santa Barbara, Santa Barbara, CA, USA

6. 6Department of Earth System Science and Policy, University of North Dakota, Grand Forks, ND, USA

7. 7Ocean Remote Sensing Institute, Ocean University of China, Qingdao, Shandong, China

8. 8College of Fisheries and Ocean Sciences, University of Alaska Fairbanks, Fairbanks, AK, USA

9. 9Department of Earth and Oceanographic Science, Bowdoin University, Brunswick, ME, USA

Abstract

Particle size distribution (PSD) is a fundamental property that affects almost every aspect of the marine ecosystem, including ecological trophic interactions and transport of organic matter and trace elements. We measured PSDs using a suite of seven instruments in waters near Ocean Station Papa in the Northeast Pacific Ocean. These instruments and their sizing ranges are: Laser In-Situ Scattering and Transmissometer (LISST)-Volume Scattering Function meter (VSF) and Multispectral Volume Scattering Meter (MVSM), both sizing particles from 0.02 µm to 2000 µm; the LISST-100X, from 3 µm to 180 µm; the ViewSizer, from 0.3 µm to 2 µm; the Coulter Counter, from 2 µm to 40 µm; the Imaging Flow CytoBot (IFCB), from 5 µm to 100 μm; and the underwater vision profiler (UVP), from 100 µm to 2000 µm. Together, they cover an unprecedented size range spanning 5 orders of magnitude from 20 nm to 2 mm. The differences in size definition for the different instruments cause biases in comparing PSDs. The absolute differences in PSDs, after correcting for mean biases, were less than a factor of 3 among all the instruments, and within 50% among LISST-100X, LISST+MVSM, Coulter Counter and IFCB. We also found that particles of sizes <50 µm were not very porous; however, porosity must be considered for particles >50 µm. The merged PSDs, ranging from 0.02 µm to 2000 µm, showed little variation in the PSD slope in the upper 75 m of the water column even though the total number of particles decreased with depth. While submicrometer particles are numerically dominant, particles of sizes 1 µm to 100 µm account for 70–90% of the solid volume of particles. We expect that the results of this study will lead to improved estimates of mass and carbon flux in the study area.

Publisher

University of California Press

Subject

Atmospheric Science,Geology,Geotechnical Engineering and Engineering Geology,Ecology,Environmental Engineering,Oceanography

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