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Trace elements and sea salt aerosols over the sea areas around the Indian sub-continent

Khemani, LT and Momin, GA and Naik, MS and Prakasa Rao, PS and Kumar, R and Ramana Murty, BhV (1985) Trace elements and sea salt aerosols over the sea areas around the Indian sub-continent. Atmospheric Environment (1967), 19 (2). pp. 277-284.

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The nature and the characteristics of trace elements and sea salt aerosols in the ocean atmosphere around the Indian sub-continent was studied. For this purpose, concentrations of the total suspended particulates (TSP) as well as of its various chemical components together with their mass size distributions were measured on 11 days in May 1983. Over the sea regions around the sub-continent, sampling was done on board the research Vessel Gaveshani using a high volume air sampler and a multistage Andersen sampler. The concentrations of soil-origin elements (Al, Fe, Mn and Ca) were found to be at a maximum over the Arabian sea region suggesting the presence of dust particulates, transported from the Arabian peninsula. The near sea water ratio of CI/ Na was observed in giant size (> 2.5 μm dia) sea salt aerosols suggested that there was very little fractionation in these aerosols. The ratio value considerably decreased in the case of sub-μm sea salt particles. The chemical components originating from soil and from sea salt showed a unimodal distribution whereas those from anthropogenic sources showed a bimodal distribution.

Item Type: Article
Additional Information: Copyright of this article belongs to Elsevier
Uncontrolled Keywords: EARTH ATMOSPHERE - Trace Analysis; SEAWATER - Evaporation, INDIA CLIMATIC CHART; MARINE AEROSOLS SIZE DISTRIBUTION; SEA SALT FRACTIONATION, AEROSOLS, trace element, aerosol; air analysis; atmospheric dispersion; geographic distribution; nonhuman; priority journal; sea; theoretical study, aerosols; Arabian Sea; dust particulates
Subjects: Meteorology and Climatology
Depositing User: IITM Library
Date Deposited: 22 Apr 2015 10:05
Last Modified: 22 Apr 2015 10:05

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