Vertical Distribution of Biogenic Elements in Pore Waters of the Bering Sea.

Piston core samples of Bering Sea sediments were squeezed to obtain the interstitial fluids. Horizons sampled and reported are for 0, 2, 4, 8 and 16 m. These fluids were subsequently analyzed for alkalinity, ammonia, phosphate and silicate. Alkalinity and ammonia concentrations in the pore fluids in...

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Bibliographic Details
Main Author: Zaitseva,E D
Other Authors: GELLMAN RESEARCH ASSOCIATES JENKINTOWN PA
Format: Text
Language:English
Published: 1977
Subjects:
Physical and Dynamic Oceanography
*WATER CHEMISTRY
USSR
SPATIAL DISTRIBUTION
WATER
BIOCHEMISTRY
INTERSTITIAL
DEPTH
LONG RANGE(TIME)
NITROGEN
AMMONIA
SILICON
ORGANIC MATERIALS
TRANSLATIONS
OCEAN BOTTOM SAMPLING
DECOMPOSITION
SEA WATER
SEDIMENTS
PHOSPHATES
ALKALINITY
CORE SAMPLING
BERING SEA
CHEMICAL OCEANOGRAPHY
Interstitial water
Pore water
Bering Sea
Online Access:http://www.dtic.mil/docs/citations/ADA043289
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA043289
Description
Summary:Piston core samples of Bering Sea sediments were squeezed to obtain the interstitial fluids. Horizons sampled and reported are for 0, 2, 4, 8 and 16 m. These fluids were subsequently analyzed for alkalinity, ammonia, phosphate and silicate. Alkalinity and ammonia concentrations in the pore fluids increased uniformly with respect to depth. The ranges of concentration reported are 2.5 - 73.7 mg-equivalents/liter for alkalinity and 0.2 - 159 mg/liter for ammonia-nitrogen. Nitrogen was also determined in the surface horizon and found to vary between 0.04 and 0.29%. In some cases, phosphate also showed an increase in concentration with respect to depth but the range was only 0.2 - 7.5 PO4 mg/liter. Silicate values varied widely and no definable trends were noted. Concentrations of these biogenic elements in the pore fluids are attributed to the regeneration of biogenic material deposited in the sediments. Regeneration occurs in the uppermost layers for the most part and in some cases continues in deeper layers. Trans. from USSR Academy of Science Reports DAN SSSR v99 n2 1954, by Leo A. Barnard. Presented to Academician N. M. Strakhov, 13 Sep 54.

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