In Situ Settling Behavior of Marine Snow

The settling velocities of undisturbed macroscopic aggregates known as marine snow were measured with SCUBA in surface waters off southern California and analyzed as a function of aggregate size, mass, and density. Sinking rates in the field varied exponentially with aggregate size and dry weight an...

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Bibliographic Details
Main Authors: Alldredge, Alice L., Gotschalk, Chris
Other Authors: CALIFORNIA UNIV SANTA BARBARA MARINE SCIENCE INST
Format: Text
Language:English
Published: 1988
Subjects:
Snow
Ice and Permafrost
*SNOW
*MARINE BIOLOGY
VOLUME
SIZES(DIMENSIONS)
CELLS
SHAPE
SPHERES
ELLIPSOIDS
PARTICLES
COEFFICIENTS
SURFACE WATERS
HETEROGENEITY
CALIFORNIA
BEHAVIOR
DRAG
REGULATIONS
SOUTH(DIRECTION)
POROUS MATERIALS
PHYTOPLANKTON
BUOYANCY
SINKING
REPRINTS
DENSITY
Ice
permafrost
Online Access:http://www.dtic.mil/docs/citations/ADA219077
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA219077
Description
Summary:The settling velocities of undisturbed macroscopic aggregates known as marine snow were measured with SCUBA in surface waters off southern California and analyzed as a function of aggregate size, mass, and density. Sinking rates in the field varied exponentially with aggregate size and dry weight and were consistently up to four times slower than rates measured in the laboratory. The excess densities of the 80 aggregates examined were calculated from volume and dry weight and ranged over four orders of magnitude with a median of .00014 grams/centimeters cubed. Aggregates of marine snow sank more slowly than predicted for either solid or porous spheres of equivalent volume and density, although their velocities were within the range expected for equivalent sinking prolate ellipsoids. No relationships between settling velocity and either excess density or particle shape were found. Drag coefficients of marine snow were also higher than predicted by theory for spheres of equivalent volume and density. These deviations from theoretical expectations may be partially explained by errors in the estimation of the excess densities of aggregates. Variability in the densities of the heterogeneous primary particles comprising marine snow (fecal pellets, clay- mineral particles, phytoplankton, molts, etc.) and the potential for buoyancy regulation by individual phytoplankton cells inhabiting aggregates make determination of excess density especially problematic. Keywords: Snow; Marine snow; Sinking rates; Reprints; Density; Marine biology. Published in Limnology Oceanography, v33 n3 p339-351 1988.

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