CHEMICAL AND PHYSICAL DATA, CHINCOTEAGUE BAY AREA, JULY 1943 TO JUNE 1953

A study was made of the possible causes for decline of oyster production and of means for restoring productivity. Water samples were taken at numerous stations (designated by the latitude and longitude to the nearest 0.1 min) with a Forest bottle of 1-1 capacity. Top and bottom samples were taken wh...

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Main Authors: MCGARY, JAMES W., SEILING, FRED N.
Other Authors: JOHNS HOPKINS UNIV BALTIMORE MD CHESAPEAKE BAY INST
Format: Text
Language:English
Published: 1953
Subjects:
Online Access:http://www.dtic.mil/docs/citations/AD0019914
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0019914
id ftdtic:AD0019914
record_format openpolar
spelling ftdtic:AD0019914 2023-05-15T17:32:18+02:00 CHEMICAL AND PHYSICAL DATA, CHINCOTEAGUE BAY AREA, JULY 1943 TO JUNE 1953 MCGARY, JAMES W. SEILING, FRED N. JOHNS HOPKINS UNIV BALTIMORE MD CHESAPEAKE BAY INST 1953-07 text/html http://www.dtic.mil/docs/citations/AD0019914 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0019914 en eng http://www.dtic.mil/docs/citations/AD0019914 Approved for public release; distribution is unlimited. Document partially illegible. DTIC AND NTIS Physical and Dynamic Oceanography *CHEMICAL OCEANOGRAPHY PRODUCTION WATER INSHORE AREAS METEOROLOGICAL DATA OXYGEN SAMPLING PRODUCTIVITY FILTERS SALINITY SURFACE TEMPERATURE NORTH ATLANTIC OCEAN BOTTOM HEIGHT BOTTLES WAVES DISSOLVING FORESTS PHOTOMETERS LATITUDE LONGITUDE TURBIDITY OYSTERS CHINCOTEAGUE BAY Text 1953 ftdtic 2016-02-22T08:11:23Z A study was made of the possible causes for decline of oyster production and of means for restoring productivity. Water samples were taken at numerous stations (designated by the latitude and longitude to the nearest 0.1 min) with a Forest bottle of 1-1 capacity. Top and bottom samples were taken when depth was greater than 2.5 ft. The analyses induced determinations of surface temperature, salinity, and dissolved oxygen content. The degree of turbidity was obtained by measuring the extent of transmission (at lambda of 425, 525, and 650 mmicrons), with a Fisher filter photometer, through a 5-cm cell containing the sample. Wave heights, meteorological data, and current observations were also made. Text North Atlantic Defense Technical Information Center: DTIC Technical Reports database Lambda ENVELOPE(-62.983,-62.983,-64.300,-64.300)
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Physical and Dynamic Oceanography
*CHEMICAL OCEANOGRAPHY
PRODUCTION
WATER
INSHORE AREAS
METEOROLOGICAL DATA
OXYGEN
SAMPLING
PRODUCTIVITY
FILTERS
SALINITY
SURFACE TEMPERATURE
NORTH ATLANTIC OCEAN
BOTTOM
HEIGHT
BOTTLES
WAVES
DISSOLVING
FORESTS
PHOTOMETERS
LATITUDE
LONGITUDE
TURBIDITY
OYSTERS
CHINCOTEAGUE BAY
spellingShingle Physical and Dynamic Oceanography
*CHEMICAL OCEANOGRAPHY
PRODUCTION
WATER
INSHORE AREAS
METEOROLOGICAL DATA
OXYGEN
SAMPLING
PRODUCTIVITY
FILTERS
SALINITY
SURFACE TEMPERATURE
NORTH ATLANTIC OCEAN
BOTTOM
HEIGHT
BOTTLES
WAVES
DISSOLVING
FORESTS
PHOTOMETERS
LATITUDE
LONGITUDE
TURBIDITY
OYSTERS
CHINCOTEAGUE BAY
MCGARY, JAMES W.
SEILING, FRED N.
CHEMICAL AND PHYSICAL DATA, CHINCOTEAGUE BAY AREA, JULY 1943 TO JUNE 1953
topic_facet Physical and Dynamic Oceanography
*CHEMICAL OCEANOGRAPHY
PRODUCTION
WATER
INSHORE AREAS
METEOROLOGICAL DATA
OXYGEN
SAMPLING
PRODUCTIVITY
FILTERS
SALINITY
SURFACE TEMPERATURE
NORTH ATLANTIC OCEAN
BOTTOM
HEIGHT
BOTTLES
WAVES
DISSOLVING
FORESTS
PHOTOMETERS
LATITUDE
LONGITUDE
TURBIDITY
OYSTERS
CHINCOTEAGUE BAY
description A study was made of the possible causes for decline of oyster production and of means for restoring productivity. Water samples were taken at numerous stations (designated by the latitude and longitude to the nearest 0.1 min) with a Forest bottle of 1-1 capacity. Top and bottom samples were taken when depth was greater than 2.5 ft. The analyses induced determinations of surface temperature, salinity, and dissolved oxygen content. The degree of turbidity was obtained by measuring the extent of transmission (at lambda of 425, 525, and 650 mmicrons), with a Fisher filter photometer, through a 5-cm cell containing the sample. Wave heights, meteorological data, and current observations were also made.
author2 JOHNS HOPKINS UNIV BALTIMORE MD CHESAPEAKE BAY INST
format Text
author MCGARY, JAMES W.
SEILING, FRED N.
author_facet MCGARY, JAMES W.
SEILING, FRED N.
author_sort MCGARY, JAMES W.
title CHEMICAL AND PHYSICAL DATA, CHINCOTEAGUE BAY AREA, JULY 1943 TO JUNE 1953
title_short CHEMICAL AND PHYSICAL DATA, CHINCOTEAGUE BAY AREA, JULY 1943 TO JUNE 1953
title_full CHEMICAL AND PHYSICAL DATA, CHINCOTEAGUE BAY AREA, JULY 1943 TO JUNE 1953
title_fullStr CHEMICAL AND PHYSICAL DATA, CHINCOTEAGUE BAY AREA, JULY 1943 TO JUNE 1953
title_full_unstemmed CHEMICAL AND PHYSICAL DATA, CHINCOTEAGUE BAY AREA, JULY 1943 TO JUNE 1953
title_sort chemical and physical data, chincoteague bay area, july 1943 to june 1953
publishDate 1953
url http://www.dtic.mil/docs/citations/AD0019914
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0019914
long_lat ENVELOPE(-62.983,-62.983,-64.300,-64.300)
geographic Lambda
geographic_facet Lambda
genre North Atlantic
genre_facet North Atlantic
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0019914
op_rights Approved for public release; distribution is unlimited. Document partially illegible.
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