Chemical characteristics of Central Indian Basin waters during the southern summer

Citation
Sn. De Sousa et al., Chemical characteristics of Central Indian Basin waters during the southern summer, DEEP-SEA II, 48(16), 2001, pp. 3343-3352
Citations number
12
Categorie Soggetti
Aquatic Sciences","Earth Sciences
Journal title
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY
ISSN journal
09670645 → ACNP
Volume
48
Issue
16
Year of publication
2001
Pages
3343 - 3352
Database
ISI
SICI code
0967-0645(2001)48:16<3343:CCOCIB>2.0.ZU;2-F
Abstract
Chemical properties of the water column were examined at the Indian Deep-se a Environment Experiment (INDEX) site in the Central Indian Basin (CIB), as a part of baseline studies prior to the benthic disturbance experiment for the environmental impact assessment of mining of polymetallic nodules. The study shows three equatorward moving water masses. (a) The Subsurface Sali nity Maximum in the depth range 125-200 m, characterized by high salinity ( 34.74-34.77 psu) and oxygen minimum associated with weak maxima in nutrient s. (b) The Deep Oxygen Maximum (234-245 muM) in the depth range 250-750 m, associated with minima in nutrients and relatively high pH. (c) The Salinit y Minimum Water (34.714-34.718 psu) corresponding to the Antarctic Intermed iate Water (AAIW) at depths 800-1200 m in the density (sigma (theta)) range 27.2-27.5. Progressive changes in these characteristics are attributed to mixing with waters above and below, and to oxidation of organic detritus en route. Among the three water masses, the oxygen maximum water shows the lo west changes in its properties, which may suggest that this water mass is m oving the fastest. (C) 2001 Elsevier Science Ltd. All rights reserved.