(Table 2) Composition of rain water collected over the Indian Ocean in 1967

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Autores principales: Bruevich, Semyon V, Korzh, Vyacheslav D
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 1969
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author Bruevich, Semyon V
Korzh, Vyacheslav D
author_facet Bruevich, Semyon V
Korzh, Vyacheslav D
collection Datos científicos de ciencias marinas y ambientales
contents Analytical data on the basic salt composition in evaporation products of sea (ocean) water and of rain water falling on the central area of the Indian Ocean are examined. Both hot and low-temperature (vacuum) distillation were used. When ocean water evaporates under calm conditions, sea salts in molecular-dispersed state, metamorphosed in the upper boundary layer, enter the atmosphere in addition to water vapor ("salt respiration of the ocean"). Concentration of these salts is about 0.5 mg per liter of water evaporated. Salts also enter the atmosphere from a foam-covered ocean surface as aerosols.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_753311
institution PANGAEA
language en
publishDate 1969
publisher PANGAEA
record_format pangaea
spellingShingle (Table 2) Composition of rain water collected over the Indian Ocean in 1967
Bruevich, Semyon V
Korzh, Vyacheslav D
Alkalinity, total; Alkalinity/chlorine ratio; Archive of Ocean Data; ARCOD; Br-K-68-1; Br-K-68-2; Br-K-68-3; Br-K-68-4; Bromide/Chlorine ratio; Bromine; Calcium; Calcium/Chlorine ratio; Calcium/Magnesium ratio; Calculated; Carbonate; Chlorine; Conductivity, electrical; Date/Time of event; Event label; Indian Ocean; Latitude of event; Longitude of event; Magnesium; Magnesium/Chlorine ratio; Potassium; Potassium/Chloride ratio; RAIN; Rain water collector; Sample volume; Sodium; Sodium/Chlorine ratio; Sodium/Potassium ratio; Sulfate; Sulfate/Chlorine ratio; Titration
Analytical data on the basic salt composition in evaporation products of sea (ocean) water and of rain water falling on the central area of the Indian Ocean are examined. Both hot and low-temperature (vacuum) distillation were used. When ocean water evaporates under calm conditions, sea salts in molecular-dispersed state, metamorphosed in the upper boundary layer, enter the atmosphere in addition to water vapor ("salt respiration of the ocean"). Concentration of these salts is about 0.5 mg per liter of water evaporated. Salts also enter the atmosphere from a foam-covered ocean surface as aerosols.
title (Table 2) Composition of rain water collected over the Indian Ocean in 1967
topic Alkalinity, total; Alkalinity/chlorine ratio; Archive of Ocean Data; ARCOD; Br-K-68-1; Br-K-68-2; Br-K-68-3; Br-K-68-4; Bromide/Chlorine ratio; Bromine; Calcium; Calcium/Chlorine ratio; Calcium/Magnesium ratio; Calculated; Carbonate; Chlorine; Conductivity, electrical; Date/Time of event; Event label; Indian Ocean; Latitude of event; Longitude of event; Magnesium; Magnesium/Chlorine ratio; Potassium; Potassium/Chloride ratio; RAIN; Rain water collector; Sample volume; Sodium; Sodium/Chlorine ratio; Sodium/Potassium ratio; Sulfate; Sulfate/Chlorine ratio; Titration
url https://doi.org/10.1594/PANGAEA.753311