Reactive Trace Metals as Indicators of Subduction and Ventilation Processes in the Ocean

The continuation of the Polar work originally proposed to the ONR in 1990 for this proposal had to be curtailed after the cancellation of the Barents Sea cruise in 1990 and after the P.I. was denied space on the trans-Polar expedition during the summer of 1991. Instead, after consultation with the O...

Full description

Bibliographic Details
Main Author: Measures, Chris
Other Authors: HAWAII UNIV AT MANOA HONOLULU
Format: Text
Language:English
Published: 1993
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA273585
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA273585
id ftdtic:ADA273585
record_format openpolar
spelling ftdtic:ADA273585 2023-05-15T15:38:36+02:00 Reactive Trace Metals as Indicators of Subduction and Ventilation Processes in the Ocean Measures, Chris HAWAII UNIV AT MANOA HONOLULU 1993-11-24 text/html http://www.dtic.mil/docs/citations/ADA273585 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA273585 en eng http://www.dtic.mil/docs/citations/ADA273585 Approved for public release; distribution is unlimited. Document partially illegible. DTIC AND NTIS Inorganic Chemistry Physical and Dynamic Oceanography Geology Geochemistry and Mineralogy Thermodynamics *METALS *VENTILATION *REACTIVITIES *OCEANS *EAST PACIFIC RISE *TRACE ELEMENTS WATER PROCESSING HEAT INDICATORS VENTS SHORES BARENTS SEA ALUMINUM SAMPLING FLUIDS PLUMES *SUBDUCTION *HYDROTHERMAL PLUMES Text 1993 ftdtic 2016-02-22T01:15:32Z The continuation of the Polar work originally proposed to the ONR in 1990 for this proposal had to be curtailed after the cancellation of the Barents Sea cruise in 1990 and after the P.I. was denied space on the trans-Polar expedition during the summer of 1991. Instead, after consultation with the ONR program manager the P.I. participated in a cruise designed to use trace elements to survey the hydrothermal plumes generated by sea-floor hydrothermal activity between 9 deg and 11 deg N on the East Pacific Rise. The P.I.'s participation in this cruise was designed to determine the magnitude and variability of dissolved Al enrichment the hydrothermal plumes which result from the mixing of hydrothermal vent fluids with the overlying sea water. Text Barents Sea Defense Technical Information Center: DTIC Technical Reports database Barents Sea Pacific
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Inorganic Chemistry
Physical and Dynamic Oceanography
Geology
Geochemistry and Mineralogy
Thermodynamics
*METALS
*VENTILATION
*REACTIVITIES
*OCEANS
*EAST PACIFIC RISE
*TRACE ELEMENTS
WATER
PROCESSING
HEAT
INDICATORS
VENTS
SHORES
BARENTS SEA
ALUMINUM
SAMPLING
FLUIDS
PLUMES
*SUBDUCTION
*HYDROTHERMAL PLUMES
spellingShingle Inorganic Chemistry
Physical and Dynamic Oceanography
Geology
Geochemistry and Mineralogy
Thermodynamics
*METALS
*VENTILATION
*REACTIVITIES
*OCEANS
*EAST PACIFIC RISE
*TRACE ELEMENTS
WATER
PROCESSING
HEAT
INDICATORS
VENTS
SHORES
BARENTS SEA
ALUMINUM
SAMPLING
FLUIDS
PLUMES
*SUBDUCTION
*HYDROTHERMAL PLUMES
Measures, Chris
Reactive Trace Metals as Indicators of Subduction and Ventilation Processes in the Ocean
topic_facet Inorganic Chemistry
Physical and Dynamic Oceanography
Geology
Geochemistry and Mineralogy
Thermodynamics
*METALS
*VENTILATION
*REACTIVITIES
*OCEANS
*EAST PACIFIC RISE
*TRACE ELEMENTS
WATER
PROCESSING
HEAT
INDICATORS
VENTS
SHORES
BARENTS SEA
ALUMINUM
SAMPLING
FLUIDS
PLUMES
*SUBDUCTION
*HYDROTHERMAL PLUMES
description The continuation of the Polar work originally proposed to the ONR in 1990 for this proposal had to be curtailed after the cancellation of the Barents Sea cruise in 1990 and after the P.I. was denied space on the trans-Polar expedition during the summer of 1991. Instead, after consultation with the ONR program manager the P.I. participated in a cruise designed to use trace elements to survey the hydrothermal plumes generated by sea-floor hydrothermal activity between 9 deg and 11 deg N on the East Pacific Rise. The P.I.'s participation in this cruise was designed to determine the magnitude and variability of dissolved Al enrichment the hydrothermal plumes which result from the mixing of hydrothermal vent fluids with the overlying sea water.
author2 HAWAII UNIV AT MANOA HONOLULU
format Text
author Measures, Chris
author_facet Measures, Chris
author_sort Measures, Chris
title Reactive Trace Metals as Indicators of Subduction and Ventilation Processes in the Ocean
title_short Reactive Trace Metals as Indicators of Subduction and Ventilation Processes in the Ocean
title_full Reactive Trace Metals as Indicators of Subduction and Ventilation Processes in the Ocean
title_fullStr Reactive Trace Metals as Indicators of Subduction and Ventilation Processes in the Ocean
title_full_unstemmed Reactive Trace Metals as Indicators of Subduction and Ventilation Processes in the Ocean
title_sort reactive trace metals as indicators of subduction and ventilation processes in the ocean
publishDate 1993
url http://www.dtic.mil/docs/citations/ADA273585
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA273585
geographic Barents Sea
Pacific
geographic_facet Barents Sea
Pacific
genre Barents Sea
genre_facet Barents Sea
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA273585
op_rights Approved for public release; distribution is unlimited. Document partially illegible.
_version_ 1766369721316278272