Arctic Oil Biodegradation.

The abundance of microbial hydrocarbon oxidizers is reported from measurements in three widely distributed marine systems in the far north. Concomitant in situ organic substrate oxidation rates measured by (14)CO2 collection were 0.2 to 1.6 ng/l hr from an initial added concentration of 1.4 microgra...

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Bibliographic Details
Main Author: Button,D. K.
Other Authors: ALASKA UNIV COLLEGE INST OF MARINE SCIENCE
Format: Text
Language:English
Published: 1974
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA014096
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA014096
id ftdtic:ADA014096
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spelling ftdtic:ADA014096 2023-05-15T14:57:56+02:00 Arctic Oil Biodegradation. Button,D. K. ALASKA UNIV COLLEGE INST OF MARINE SCIENCE 1974-12 text/html http://www.dtic.mil/docs/citations/ADA014096 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA014096 en eng http://www.dtic.mil/docs/citations/ADA014096 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Microbiology Biological Oceanography *HYDROCARBONS *OIL SPILLS *ARCTIC REGIONS *BIODETERIORATION TEST METHODS METABOLISM CLAY CARBON DIOXIDE LABELED SUBSTANCES Carbon 14 DOT/5C Crude oil Text 1974 ftdtic 2016-02-20T10:07:50Z The abundance of microbial hydrocarbon oxidizers is reported from measurements in three widely distributed marine systems in the far north. Concomitant in situ organic substrate oxidation rates measured by (14)CO2 collection were 0.2 to 1.6 ng/l hr from an initial added concentration of 1.4 micrograms/l mixed amino acids and 2 to 50 ng/l hr from added dodecane solution. The solubility of dodecane in saline medium was determined and the predictability of high molecular weight alkane solubility confirmed. This true solution was used to show that a relatively high molecular weight hydrocarbon can be co-metabolized along with another substrate (arginine) from the dissolved phase. Dodecane derived CO2, arginine and glutamic acid were recovered from the 14C-dodecane, 12C-arginine medium after having been supplied to a continuous culture of a marine hydrocarbon oxidizing isolate. Clay sorption experiments were conducted which showed that the catalytic role of suspended sediments was negligible. No dodecane sorption by bentonite could be detected in a 20% saturated hydrocarbon solution. These and other data presented support the assumption that direct dissolved phase organic material metabolism is a normal ubiquitous marine process having characteristics compatible with submicrogram per liter steady state hydrocarbon concentrations. Text Arctic Defense Technical Information Center: DTIC Technical Reports database Arctic
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Microbiology
Biological Oceanography
*HYDROCARBONS
*OIL SPILLS
*ARCTIC REGIONS
*BIODETERIORATION
TEST METHODS
METABOLISM
CLAY
CARBON DIOXIDE
LABELED SUBSTANCES
Carbon 14
DOT/5C
Crude oil
spellingShingle Microbiology
Biological Oceanography
*HYDROCARBONS
*OIL SPILLS
*ARCTIC REGIONS
*BIODETERIORATION
TEST METHODS
METABOLISM
CLAY
CARBON DIOXIDE
LABELED SUBSTANCES
Carbon 14
DOT/5C
Crude oil
Button,D. K.
Arctic Oil Biodegradation.
topic_facet Microbiology
Biological Oceanography
*HYDROCARBONS
*OIL SPILLS
*ARCTIC REGIONS
*BIODETERIORATION
TEST METHODS
METABOLISM
CLAY
CARBON DIOXIDE
LABELED SUBSTANCES
Carbon 14
DOT/5C
Crude oil
description The abundance of microbial hydrocarbon oxidizers is reported from measurements in three widely distributed marine systems in the far north. Concomitant in situ organic substrate oxidation rates measured by (14)CO2 collection were 0.2 to 1.6 ng/l hr from an initial added concentration of 1.4 micrograms/l mixed amino acids and 2 to 50 ng/l hr from added dodecane solution. The solubility of dodecane in saline medium was determined and the predictability of high molecular weight alkane solubility confirmed. This true solution was used to show that a relatively high molecular weight hydrocarbon can be co-metabolized along with another substrate (arginine) from the dissolved phase. Dodecane derived CO2, arginine and glutamic acid were recovered from the 14C-dodecane, 12C-arginine medium after having been supplied to a continuous culture of a marine hydrocarbon oxidizing isolate. Clay sorption experiments were conducted which showed that the catalytic role of suspended sediments was negligible. No dodecane sorption by bentonite could be detected in a 20% saturated hydrocarbon solution. These and other data presented support the assumption that direct dissolved phase organic material metabolism is a normal ubiquitous marine process having characteristics compatible with submicrogram per liter steady state hydrocarbon concentrations.
author2 ALASKA UNIV COLLEGE INST OF MARINE SCIENCE
format Text
author Button,D. K.
author_facet Button,D. K.
author_sort Button,D. K.
title Arctic Oil Biodegradation.
title_short Arctic Oil Biodegradation.
title_full Arctic Oil Biodegradation.
title_fullStr Arctic Oil Biodegradation.
title_full_unstemmed Arctic Oil Biodegradation.
title_sort arctic oil biodegradation.
publishDate 1974
url http://www.dtic.mil/docs/citations/ADA014096
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA014096
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA014096
op_rights APPROVED FOR PUBLIC RELEASE
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