(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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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.753312 2023-05-15T17:12:46+02:00 (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 LATITUDE: 44.577000 * LONGITUDE: 37.979000 1971-11-10 text/tab-separated-values, 433 data points https://doi.pangaea.de/10.1594/PANGAEA.753312 https://doi.org/10.1594/PANGAEA.753312 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.753312 https://doi.org/10.1594/PANGAEA.753312 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow Supplement to: Bruevich, Semyon V; Korzh, Vyacheslav D (1971): Boron exchange between the sea and the atmosphere. Oceanology, 11, 345-351 Archive of Ocean Data ARCOD Boron Boron/Chlorine ratio Calculated Chloride Chlorine Comment Date Duration GB-SBIOAS Humidity relative minimum Mikhail Lomonosov ML19 RAIN Rain water collector Red Sea Sample code/label Sample volume Titration Wind direction description Wind speed maximum Dataset 1971 ftpangaea https://doi.org/10.1594/PANGAEA.753312 2023-01-20T08:51:34Z 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 atmospheric precipitation on the slope of the Terskei Ala-Tau near the Issyk-Kul Lake in 1969. Thus, although chemistries of boron and chlorine (in chlorides) are very different, the B/Cl ratio in the atmosphere is fairly constant. This can be taken as a confirmation of an assumption that salt composition of sea water passes into the atmosphere in molecularly dispersed state. Supposing that the ocean-atmosphere system is in equilibrium as regards to the boron budget, it can be assumed that the same amount of boron passes from the ocean into bottom sediments and from lithosphere rocks and soils into the hydrosphere. Dataset Mikhail Lomonosov PANGAEA - Data Publisher for Earth & Environmental Science Golubaya Bay ENVELOPE(9.750,9.750,-69.933,-69.933) ENVELOPE(37.979000,37.979000,44.577000,44.577000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Archive of Ocean Data ARCOD Boron Boron/Chlorine ratio Calculated Chloride Chlorine Comment Date Duration GB-SBIOAS Humidity relative minimum Mikhail Lomonosov ML19 RAIN Rain water collector Red Sea Sample code/label Sample volume Titration Wind direction description Wind speed maximum |
spellingShingle |
Archive of Ocean Data ARCOD Boron Boron/Chlorine ratio Calculated Chloride Chlorine Comment Date Duration GB-SBIOAS Humidity relative minimum Mikhail Lomonosov ML19 RAIN Rain water collector Red Sea Sample code/label Sample volume Titration Wind direction description Wind speed maximum 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 |
Archive of Ocean Data ARCOD Boron Boron/Chlorine ratio Calculated Chloride Chlorine Comment Date Duration GB-SBIOAS Humidity relative minimum Mikhail Lomonosov ML19 RAIN Rain water collector Red Sea Sample code/label Sample volume Titration Wind direction description Wind speed maximum |
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 atmospheric precipitation on the slope of the Terskei Ala-Tau near the Issyk-Kul Lake in 1969. Thus, although chemistries of boron and chlorine (in chlorides) are very different, the B/Cl ratio in the atmosphere is fairly constant. This can be taken as a confirmation of an assumption that salt composition of sea water passes into the atmosphere in molecularly dispersed state. Supposing that the ocean-atmosphere system is in equilibrium as regards to the boron budget, it can be assumed that the same amount of boron passes from the ocean into bottom sediments and from lithosphere rocks and soils into the hydrosphere. |
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://doi.pangaea.de/10.1594/PANGAEA.753312 https://doi.org/10.1594/PANGAEA.753312 |
op_coverage |
LATITUDE: 44.577000 * LONGITUDE: 37.979000 |
long_lat |
ENVELOPE(9.750,9.750,-69.933,-69.933) ENVELOPE(37.979000,37.979000,44.577000,44.577000) |
geographic |
Golubaya Bay |
geographic_facet |
Golubaya Bay |
genre |
Mikhail Lomonosov |
genre_facet |
Mikhail Lomonosov |
op_source |
P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow Supplement to: Bruevich, Semyon V; Korzh, Vyacheslav D (1971): Boron exchange between the sea and the atmosphere. Oceanology, 11, 345-351 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.753312 https://doi.org/10.1594/PANGAEA.753312 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.753312 |
_version_ |
1766069629964255232 |