Research of Water Phase Composition in Zeolites
Abstract The article presents the results of experimental studies of the content of unfrozen water in the zeolite of the Honguruu deposit of the Republic of Sakha (Yakutia). The initial moisture content ranged from 6,0 to 22,4 %. To determine the amount of unfrozen water, the method of continuous he...
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crioppubl:10.1088/1755-1315/666/4/042035 2024-06-02T08:13:47+00:00 Research of Water Phase Composition in Zeolites Kravtsova, O N Tappyrova, N I Ivanov, V A 2021 http://dx.doi.org/10.1088/1755-1315/666/4/042035 https://iopscience.iop.org/article/10.1088/1755-1315/666/4/042035 https://iopscience.iop.org/article/10.1088/1755-1315/666/4/042035/pdf unknown IOP Publishing http://creativecommons.org/licenses/by/3.0/ https://iopscience.iop.org/info/page/text-and-data-mining IOP Conference Series: Earth and Environmental Science volume 666, issue 4, page 042035 ISSN 1755-1307 1755-1315 journal-article 2021 crioppubl https://doi.org/10.1088/1755-1315/666/4/042035 2024-05-07T14:03:12Z Abstract The article presents the results of experimental studies of the content of unfrozen water in the zeolite of the Honguruu deposit of the Republic of Sakha (Yakutia). The initial moisture content ranged from 6,0 to 22,4 %. To determine the amount of unfrozen water, the method of continuous heating of the sample was used. For the studied samples, the content of unfrozen water in the temperature range from -15 to 0 °C does not depend on the initial humidity. In the range from -25 to -15 °C, jumps in the content of unfrozen water were found. Article in Journal/Newspaper Republic of Sakha Yakutia IOP Publishing Sakha IOP Conference Series: Earth and Environmental Science 666 4 042035 |
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Abstract The article presents the results of experimental studies of the content of unfrozen water in the zeolite of the Honguruu deposit of the Republic of Sakha (Yakutia). The initial moisture content ranged from 6,0 to 22,4 %. To determine the amount of unfrozen water, the method of continuous heating of the sample was used. For the studied samples, the content of unfrozen water in the temperature range from -15 to 0 °C does not depend on the initial humidity. In the range from -25 to -15 °C, jumps in the content of unfrozen water were found. |
format |
Article in Journal/Newspaper |
author |
Kravtsova, O N Tappyrova, N I Ivanov, V A |
spellingShingle |
Kravtsova, O N Tappyrova, N I Ivanov, V A Research of Water Phase Composition in Zeolites |
author_facet |
Kravtsova, O N Tappyrova, N I Ivanov, V A |
author_sort |
Kravtsova, O N |
title |
Research of Water Phase Composition in Zeolites |
title_short |
Research of Water Phase Composition in Zeolites |
title_full |
Research of Water Phase Composition in Zeolites |
title_fullStr |
Research of Water Phase Composition in Zeolites |
title_full_unstemmed |
Research of Water Phase Composition in Zeolites |
title_sort |
research of water phase composition in zeolites |
publisher |
IOP Publishing |
publishDate |
2021 |
url |
http://dx.doi.org/10.1088/1755-1315/666/4/042035 https://iopscience.iop.org/article/10.1088/1755-1315/666/4/042035 https://iopscience.iop.org/article/10.1088/1755-1315/666/4/042035/pdf |
geographic |
Sakha |
geographic_facet |
Sakha |
genre |
Republic of Sakha Yakutia |
genre_facet |
Republic of Sakha Yakutia |
op_source |
IOP Conference Series: Earth and Environmental Science volume 666, issue 4, page 042035 ISSN 1755-1307 1755-1315 |
op_rights |
http://creativecommons.org/licenses/by/3.0/ https://iopscience.iop.org/info/page/text-and-data-mining |
op_doi |
https://doi.org/10.1088/1755-1315/666/4/042035 |
container_title |
IOP Conference Series: Earth and Environmental Science |
container_volume |
666 |
container_issue |
4 |
container_start_page |
042035 |
_version_ |
1800737400881676288 |