Preseismic Groundwater Ion Content Variations: Observational Data in Flowing Wells of the Kamchatka Peninsula and Conceptual Model

Repeated manifestations of hydrogeochemical anomalies in groundwater ion content variations before local strong earthquakes were recorded in three flowing wells of the Petropavlovsk-Kamchatsky test site. A model of changes in chemical composition of groundwater is considered using observational data...

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Published in:Minerals
Main Authors: Galina Kopylova, Svetlana Boldina
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/min11070731
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spelling ftmdpi:oai:mdpi.com:/2075-163X/11/7/731/ 2023-08-20T04:07:39+02:00 Preseismic Groundwater Ion Content Variations: Observational Data in Flowing Wells of the Kamchatka Peninsula and Conceptual Model Galina Kopylova Svetlana Boldina agris 2021-07-06 application/pdf https://doi.org/10.3390/min11070731 EN eng Multidisciplinary Digital Publishing Institute Mineral Geochemistry and Geochronology https://dx.doi.org/10.3390/min11070731 https://creativecommons.org/licenses/by/4.0/ Minerals; Volume 11; Issue 7; Pages: 731 flowing well groundwater chemistry earthquake magnitude precursor Kamchatka Peninsula conceptual model Text 2021 ftmdpi https://doi.org/10.3390/min11070731 2023-08-01T02:07:35Z Repeated manifestations of hydrogeochemical anomalies in groundwater ion content variations before local strong earthquakes were recorded in three flowing wells of the Petropavlovsk-Kamchatsky test site. A model of changes in chemical composition of groundwater is considered using observational data and modeling of two waters mixing with contrasting composition in a zone of increased permeability in aquifer. Hydrodynamic parameters of the model—relaxation time of water pressure impulses and the time of mixed water movement in aquifer and wellbore—can vary from days to hundreds of days in individual wells. These parameters determine the duration and morphological features of anomaly in mixed water from a well. Using observational data from self-flowing well M-1, an assessment was made of chemical composition and mineralization of two mixing waters and their ratio in mixed water under background conditions and during the preparation of earthquake on 2 March 1992, Mw = 6.9. Text Kamchatka Kamchatka Peninsula MDPI Open Access Publishing Kamchatka Peninsula ENVELOPE(160.000,160.000,56.000,56.000) Petropavlovsk ENVELOPE(158.626,158.626,53.067,53.067) Petropavlovsk-Kamchatsky ENVELOPE(158.651,158.651,53.044,53.044) Minerals 11 7 731
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic flowing well
groundwater chemistry
earthquake
magnitude
precursor
Kamchatka Peninsula
conceptual model
spellingShingle flowing well
groundwater chemistry
earthquake
magnitude
precursor
Kamchatka Peninsula
conceptual model
Galina Kopylova
Svetlana Boldina
Preseismic Groundwater Ion Content Variations: Observational Data in Flowing Wells of the Kamchatka Peninsula and Conceptual Model
topic_facet flowing well
groundwater chemistry
earthquake
magnitude
precursor
Kamchatka Peninsula
conceptual model
description Repeated manifestations of hydrogeochemical anomalies in groundwater ion content variations before local strong earthquakes were recorded in three flowing wells of the Petropavlovsk-Kamchatsky test site. A model of changes in chemical composition of groundwater is considered using observational data and modeling of two waters mixing with contrasting composition in a zone of increased permeability in aquifer. Hydrodynamic parameters of the model—relaxation time of water pressure impulses and the time of mixed water movement in aquifer and wellbore—can vary from days to hundreds of days in individual wells. These parameters determine the duration and morphological features of anomaly in mixed water from a well. Using observational data from self-flowing well M-1, an assessment was made of chemical composition and mineralization of two mixing waters and their ratio in mixed water under background conditions and during the preparation of earthquake on 2 March 1992, Mw = 6.9.
format Text
author Galina Kopylova
Svetlana Boldina
author_facet Galina Kopylova
Svetlana Boldina
author_sort Galina Kopylova
title Preseismic Groundwater Ion Content Variations: Observational Data in Flowing Wells of the Kamchatka Peninsula and Conceptual Model
title_short Preseismic Groundwater Ion Content Variations: Observational Data in Flowing Wells of the Kamchatka Peninsula and Conceptual Model
title_full Preseismic Groundwater Ion Content Variations: Observational Data in Flowing Wells of the Kamchatka Peninsula and Conceptual Model
title_fullStr Preseismic Groundwater Ion Content Variations: Observational Data in Flowing Wells of the Kamchatka Peninsula and Conceptual Model
title_full_unstemmed Preseismic Groundwater Ion Content Variations: Observational Data in Flowing Wells of the Kamchatka Peninsula and Conceptual Model
title_sort preseismic groundwater ion content variations: observational data in flowing wells of the kamchatka peninsula and conceptual model
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/min11070731
op_coverage agris
long_lat ENVELOPE(160.000,160.000,56.000,56.000)
ENVELOPE(158.626,158.626,53.067,53.067)
ENVELOPE(158.651,158.651,53.044,53.044)
geographic Kamchatka Peninsula
Petropavlovsk
Petropavlovsk-Kamchatsky
geographic_facet Kamchatka Peninsula
Petropavlovsk
Petropavlovsk-Kamchatsky
genre Kamchatka
Kamchatka Peninsula
genre_facet Kamchatka
Kamchatka Peninsula
op_source Minerals; Volume 11; Issue 7; Pages: 731
op_relation Mineral Geochemistry and Geochronology
https://dx.doi.org/10.3390/min11070731
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/min11070731
container_title Minerals
container_volume 11
container_issue 7
container_start_page 731
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