Concentration of hydrogen sulfide in waters of the Black Sea in the layer of its coexistence with oxygen

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Main Authors: Novoselov, A A, Sovga, E E, Fashchuk, D Ya, Khomutov, S M, Sheremet'yeva, A I
Format: Dataset Open Access
Language:en
Published: PANGAEA 1987
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author Novoselov, A A
Sovga, E E
Fashchuk, D Ya
Khomutov, S M
Sheremet'yeva, A I
author_facet Novoselov, A A
Sovga, E E
Fashchuk, D Ya
Khomutov, S M
Sheremet'yeva, A I
collection Datos científicos de ciencias marinas y ambientales
contents About 100 parallel determinations of hydrogen sulfide by the volumetric and photometric methods were made in the layer of coexistence of oxygen with hydrogen sulfide (C layer). Thiosulfates were determined simultaneously. Regardless of locations of the stations, determinations by two methods coincided for the entire range of depths of occurrence of the C layer upper boundary. Within the C layer hydrogen sulfide readings obtained by these two independent methods agreed; thiosulfates were not found by direct measurements. Difference in the readings appears at the lower boundary of the C layer and below it, accompanied by appearance of thiosulfates. It is therefore concluded that it is correct to determine the upper boundary of the C layer by the iodometric method and to use concentration of hydrogen sulfide obtained by this method in the C layer to calculate rate of chemical oxidation of hydrogen sulfide in quasistationary processes.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_756616
institution PANGAEA
language en
publishDate 1987
publisher PANGAEA
record_format pangaea
spellingShingle Concentration of hydrogen sulfide in waters of the Black Sea in the layer of its coexistence with oxygen
Novoselov, A A
Sovga, E E
Fashchuk, D Ya
Khomutov, S M
Sheremet'yeva, A I
Archive of Ocean Data; ARCOD; Black Sea; DEPTH, water; Event label; Fluorometry; Hydrogen sulfide; Iodometric chemical method; Latitude of event; Longitude of event; ML44-N77; ML44-N80; ML44-N81; ML44-N85; ML44-N86; ML44-N87; ML44-N88; ML44-N91; ML44-N92; Oxygen; Thiosulfate; Water sample; WS
About 100 parallel determinations of hydrogen sulfide by the volumetric and photometric methods were made in the layer of coexistence of oxygen with hydrogen sulfide (C layer). Thiosulfates were determined simultaneously. Regardless of locations of the stations, determinations by two methods coincided for the entire range of depths of occurrence of the C layer upper boundary. Within the C layer hydrogen sulfide readings obtained by these two independent methods agreed; thiosulfates were not found by direct measurements. Difference in the readings appears at the lower boundary of the C layer and below it, accompanied by appearance of thiosulfates. It is therefore concluded that it is correct to determine the upper boundary of the C layer by the iodometric method and to use concentration of hydrogen sulfide obtained by this method in the C layer to calculate rate of chemical oxidation of hydrogen sulfide in quasistationary processes.
title Concentration of hydrogen sulfide in waters of the Black Sea in the layer of its coexistence with oxygen
topic Archive of Ocean Data; ARCOD; Black Sea; DEPTH, water; Event label; Fluorometry; Hydrogen sulfide; Iodometric chemical method; Latitude of event; Longitude of event; ML44-N77; ML44-N80; ML44-N81; ML44-N85; ML44-N86; ML44-N87; ML44-N88; ML44-N91; ML44-N92; Oxygen; Thiosulfate; Water sample; WS
url https://doi.org/10.1594/PANGAEA.756616