Deep and bottom water characteristics in the Owen Fracture Zone, Western Arabian Sea
DRS at CSIR-National Institute of Oceanography
View Archive InfoField | Value | |
Title |
Deep and bottom water characteristics in the Owen Fracture Zone, Western Arabian Sea
|
|
Creator |
Naqvi, S.W.A.
Kureishy, T.W. |
|
Subject |
Oceanography and Limnology
particulate organic matter oxidation nutrients (mineral) benthic boundary layer deep-water masses bottom water submarine features fracture zones ISW, Arabian Sea |
|
Description |
Hydro chemical studies at a station (10 degrees 34.l'N,56 degrees 31,7'E) in the Owen Fracture zone reveal an active movement of bottom water as approx 75 m thick, cold, low-salinity layer. Silicate profile exhibits a broad maximum coinciding with a salinity maximum at about 3 km depth in conformity with earlier results. Within the benthic layer, an increase in AOU is observed associated with minor increases in nutrients, presumably due to the oxidation of particulate organic matter sinking from the surface layer
|
|
Date |
1995-06-15T10:01:21Z
2017-09-29T13:48:18Z 1995-06-15T10:01:21Z 2017-09-29T13:48:18Z 1986 |
|
Type |
Journal Article
|
|
Identifier |
Indian Journal of Marine Sciences, vol.15; 1986; 48-49
0379-5136 http://drs.nio.org/drs/handle/2264/6175 |
|
Language |
en
|
|
Relation |
Indian J Mar Sci
SCI |
|
Publisher |
CSIR-NISCAIR
|
|