Nizhne-Shchapinsky thermal springs (Kamchatka) as an example of magnesium CO2-rich waters
The results of hydrochemical studies of Nizhne-Shapinsky (Kipely) CO2-rich thermal (39 °C) springs in 2021 are presented. The springs discharge within the Shchapina graben near active Kizimen volcano. Results include macro- and trace-component composition, isotopic composition of spring water, some...
Published in: | Bulletin of Kamchatka Regional Association «Educational-Scientific Center». Earth Sciences |
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Institute of Volcanology and Seismology FEB RAS
2023
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ftdoajarticles:oai:doaj.org/article:c848172cabd94d818bcf717e7aa94430 2024-01-28T10:06:55+01:00 Nizhne-Shchapinsky thermal springs (Kamchatka) as an example of magnesium CO2-rich waters N.A. Malik Yu.A. Taran I.Yu. Svirid A.R. Tskhovrebova 2023-12-01T00:00:00Z https://doi.org/10.31431/1816-5524-2023-4-60-48-66 https://doaj.org/article/c848172cabd94d818bcf717e7aa94430 RU rus Institute of Volcanology and Seismology FEB RAS http://www.kscnet.ru/journal/kraesc/article/view/779 https://doaj.org/toc/1816-5524 https://doaj.org/toc/1816-5532 1816-5524 1816-5532 doi:10.31431/1816-5524-2023-4-60-48-66 https://doaj.org/article/c848172cabd94d818bcf717e7aa94430 Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле, Vol 60, Iss 4, Pp 48-66 (2023) co2-rich thermal waters water-rock interaction shchapinsky graben kamchatka Geology QE1-996.5 article 2023 ftdoajarticles https://doi.org/10.31431/1816-5524-2023-4-60-48-66 2023-12-31T01:40:52Z The results of hydrochemical studies of Nizhne-Shapinsky (Kipely) CO2-rich thermal (39 °C) springs in 2021 are presented. The springs discharge within the Shchapina graben near active Kizimen volcano. Results include macro- and trace-component composition, isotopic composition of spring water, some gas components and dissolved strontium. The results are discussed using previously published and reported data, taking into account the geological and structural setting of the area, water-rock interactions, and simple thermochemical calculations to explain the rare, but typical for the chemical composition of some CO2-rich waters, predominance of magnesium over calcium. It is shown that waters of Nizhne-Shchapinsky springs are formed as a result of mixing of two components: deeper and more heated sodium chloride water and more superficial, less heated water of Mg-Ca-HCO3- composition, formed due to interaction with carbonate-bearing rocks and CO2 of magmatic origin. Article in Journal/Newspaper Kamchatka Directory of Open Access Journals: DOAJ Articles Shchapina ENVELOPE(159.492,159.492,55.439,55.439) Bulletin of Kamchatka Regional Association «Educational-Scientific Center». Earth Sciences 4(60) 48 66 |
institution |
Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
Russian |
topic |
co2-rich thermal waters water-rock interaction shchapinsky graben kamchatka Geology QE1-996.5 |
spellingShingle |
co2-rich thermal waters water-rock interaction shchapinsky graben kamchatka Geology QE1-996.5 N.A. Malik Yu.A. Taran I.Yu. Svirid A.R. Tskhovrebova Nizhne-Shchapinsky thermal springs (Kamchatka) as an example of magnesium CO2-rich waters |
topic_facet |
co2-rich thermal waters water-rock interaction shchapinsky graben kamchatka Geology QE1-996.5 |
description |
The results of hydrochemical studies of Nizhne-Shapinsky (Kipely) CO2-rich thermal (39 °C) springs in 2021 are presented. The springs discharge within the Shchapina graben near active Kizimen volcano. Results include macro- and trace-component composition, isotopic composition of spring water, some gas components and dissolved strontium. The results are discussed using previously published and reported data, taking into account the geological and structural setting of the area, water-rock interactions, and simple thermochemical calculations to explain the rare, but typical for the chemical composition of some CO2-rich waters, predominance of magnesium over calcium. It is shown that waters of Nizhne-Shchapinsky springs are formed as a result of mixing of two components: deeper and more heated sodium chloride water and more superficial, less heated water of Mg-Ca-HCO3- composition, formed due to interaction with carbonate-bearing rocks and CO2 of magmatic origin. |
format |
Article in Journal/Newspaper |
author |
N.A. Malik Yu.A. Taran I.Yu. Svirid A.R. Tskhovrebova |
author_facet |
N.A. Malik Yu.A. Taran I.Yu. Svirid A.R. Tskhovrebova |
author_sort |
N.A. Malik |
title |
Nizhne-Shchapinsky thermal springs (Kamchatka) as an example of magnesium CO2-rich waters |
title_short |
Nizhne-Shchapinsky thermal springs (Kamchatka) as an example of magnesium CO2-rich waters |
title_full |
Nizhne-Shchapinsky thermal springs (Kamchatka) as an example of magnesium CO2-rich waters |
title_fullStr |
Nizhne-Shchapinsky thermal springs (Kamchatka) as an example of magnesium CO2-rich waters |
title_full_unstemmed |
Nizhne-Shchapinsky thermal springs (Kamchatka) as an example of magnesium CO2-rich waters |
title_sort |
nizhne-shchapinsky thermal springs (kamchatka) as an example of magnesium co2-rich waters |
publisher |
Institute of Volcanology and Seismology FEB RAS |
publishDate |
2023 |
url |
https://doi.org/10.31431/1816-5524-2023-4-60-48-66 https://doaj.org/article/c848172cabd94d818bcf717e7aa94430 |
long_lat |
ENVELOPE(159.492,159.492,55.439,55.439) |
geographic |
Shchapina |
geographic_facet |
Shchapina |
genre |
Kamchatka |
genre_facet |
Kamchatka |
op_source |
Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле, Vol 60, Iss 4, Pp 48-66 (2023) |
op_relation |
http://www.kscnet.ru/journal/kraesc/article/view/779 https://doaj.org/toc/1816-5524 https://doaj.org/toc/1816-5532 1816-5524 1816-5532 doi:10.31431/1816-5524-2023-4-60-48-66 https://doaj.org/article/c848172cabd94d818bcf717e7aa94430 |
op_doi |
https://doi.org/10.31431/1816-5524-2023-4-60-48-66 |
container_title |
Bulletin of Kamchatka Regional Association «Educational-Scientific Center». Earth Sciences |
container_issue |
4(60) |
container_start_page |
48 |
op_container_end_page |
66 |
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1789334166107586560 |