(Table 3) Boron and chlorine in atmospheric moisture and rain water collected on the shore of the Golubaya Bay in 1970 ...
Boron and chlorine were determined in rain water and in atmospheric moisture condensed in a "Saratov" refrigerator. Ocean is the main source of boron on the earth surface. Boron evaporates from the ocean and enriches atmospheric precipitation: B/Cl ratio of ocean water (0.00024) increases...
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Online Access: | https://dx.doi.org/10.1594/pangaea.753312 https://doi.pangaea.de/10.1594/PANGAEA.753312 |
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ftdatacite:10.1594/pangaea.753312 2024-09-15T18:18:49+00:00 (Table 3) Boron and chlorine in atmospheric moisture and rain water collected on the shore of the Golubaya Bay in 1970 ... Bruevich, Semyon V Korzh, Vyacheslav D 1971 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.753312 https://doi.pangaea.de/10.1594/PANGAEA.753312 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Sample code/label Date Duration Wind direction description Wind speed, maximum Humidity, relative, minimum Sample volume Chlorine Chloride Boron Boron/Chlorine ratio Comment Rain water collector Titration Calculated ML19 Mikhail Lomonosov Archive of Ocean Data ARCOD dataset Supplementary Dataset Dataset 1971 ftdatacite https://doi.org/10.1594/pangaea.753312 2024-08-01T10:58:30Z Boron and chlorine were determined in rain water and in atmospheric moisture condensed in a "Saratov" refrigerator. Ocean is the main source of boron on the earth surface. Boron evaporates from the ocean and enriches atmospheric precipitation: B/Cl ratio of ocean water (0.00024) increases by factor of 10-15. Assuming that the average Cl content in global river runoff is 7.8 mg/l and boron content 0.013 mgl, B/Cl ratio in this runoff is 0.0017. The average B/Cl ratio in rain water of the Golubaya (Blue) Bay (Gelendzhik, Black Sea region) is 0.0026 and in condensates of atmospheric moisture during onshore and offshore winds in the same region it averages from 0.0029 to 0.0033. The maximum boron content in the condensates of this region during onshore winds was 0.032 mg/l and the minimum during offshore winds, 0.004 mg/l. /Cl ratio in sea water over the Atlantic Ocean and in the Gelendzhik area of the Black Sea varied within narrow range, mostly from 0.0025 to 0.0035. Similar B/Cl ratio (0.0024) was found for ... : Supplement to: Bruevich, Semyon V; Korzh, Vyacheslav D (1971): Boron exchange between the sea and the atmosphere. Oceanology, 11, 345-351 ... Dataset Mikhail Lomonosov DataCite |
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English |
topic |
Sample code/label Date Duration Wind direction description Wind speed, maximum Humidity, relative, minimum Sample volume Chlorine Chloride Boron Boron/Chlorine ratio Comment Rain water collector Titration Calculated ML19 Mikhail Lomonosov Archive of Ocean Data ARCOD |
spellingShingle |
Sample code/label Date Duration Wind direction description Wind speed, maximum Humidity, relative, minimum Sample volume Chlorine Chloride Boron Boron/Chlorine ratio Comment Rain water collector Titration Calculated ML19 Mikhail Lomonosov Archive of Ocean Data ARCOD Bruevich, Semyon V Korzh, Vyacheslav D (Table 3) Boron and chlorine in atmospheric moisture and rain water collected on the shore of the Golubaya Bay in 1970 ... |
topic_facet |
Sample code/label Date Duration Wind direction description Wind speed, maximum Humidity, relative, minimum Sample volume Chlorine Chloride Boron Boron/Chlorine ratio Comment Rain water collector Titration Calculated ML19 Mikhail Lomonosov Archive of Ocean Data ARCOD |
description |
Boron and chlorine were determined in rain water and in atmospheric moisture condensed in a "Saratov" refrigerator. Ocean is the main source of boron on the earth surface. Boron evaporates from the ocean and enriches atmospheric precipitation: B/Cl ratio of ocean water (0.00024) increases by factor of 10-15. Assuming that the average Cl content in global river runoff is 7.8 mg/l and boron content 0.013 mgl, B/Cl ratio in this runoff is 0.0017. The average B/Cl ratio in rain water of the Golubaya (Blue) Bay (Gelendzhik, Black Sea region) is 0.0026 and in condensates of atmospheric moisture during onshore and offshore winds in the same region it averages from 0.0029 to 0.0033. The maximum boron content in the condensates of this region during onshore winds was 0.032 mg/l and the minimum during offshore winds, 0.004 mg/l. /Cl ratio in sea water over the Atlantic Ocean and in the Gelendzhik area of the Black Sea varied within narrow range, mostly from 0.0025 to 0.0035. Similar B/Cl ratio (0.0024) was found for ... : Supplement to: Bruevich, Semyon V; Korzh, Vyacheslav D (1971): Boron exchange between the sea and the atmosphere. Oceanology, 11, 345-351 ... |
format |
Dataset |
author |
Bruevich, Semyon V Korzh, Vyacheslav D |
author_facet |
Bruevich, Semyon V Korzh, Vyacheslav D |
author_sort |
Bruevich, Semyon V |
title |
(Table 3) Boron and chlorine in atmospheric moisture and rain water collected on the shore of the Golubaya Bay in 1970 ... |
title_short |
(Table 3) Boron and chlorine in atmospheric moisture and rain water collected on the shore of the Golubaya Bay in 1970 ... |
title_full |
(Table 3) Boron and chlorine in atmospheric moisture and rain water collected on the shore of the Golubaya Bay in 1970 ... |
title_fullStr |
(Table 3) Boron and chlorine in atmospheric moisture and rain water collected on the shore of the Golubaya Bay in 1970 ... |
title_full_unstemmed |
(Table 3) Boron and chlorine in atmospheric moisture and rain water collected on the shore of the Golubaya Bay in 1970 ... |
title_sort |
(table 3) boron and chlorine in atmospheric moisture and rain water collected on the shore of the golubaya bay in 1970 ... |
publisher |
PANGAEA |
publishDate |
1971 |
url |
https://dx.doi.org/10.1594/pangaea.753312 https://doi.pangaea.de/10.1594/PANGAEA.753312 |
genre |
Mikhail Lomonosov |
genre_facet |
Mikhail Lomonosov |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.753312 |
_version_ |
1810456906979868672 |