Analysis of the data of hydrogeochemical monitoring of groundwater in the North Sivash artesian basin

The results of hydrogeochemical monitoring of the Sarmat-Meotis-Pontic sediments aquifer complex of the North Sivash artesian basin have been analyzed. The analysis based on a routine observations for 16 producing wells. The observations were made in the period from 2014 to 2017 years. A correlation...

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Main Authors: K. Ya. Bulakhova, S. M. Sudarikov
Format: Article
Language:Russian
Published: Sergo Ordzhonikidze Russian State University for Geological Prospecting 2019-06-01
Series:Известия высших учебных заведений: Геология и разведка
Subjects:
Online Access:https://geology.mgri-rggru.ru/jour/article/view/414
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spelling doaj-90ed3c17fc424a2f86bc8d25715a86732021-01-12T06:04:25ZrusSergo Ordzhonikidze Russian State University for Geological ProspectingИзвестия высших учебных заведений: Геология и разведка0016-77622618-87082019-06-0103647110.32454/0016-7762-2019-3-64-71376Analysis of the data of hydrogeochemical monitoring of groundwater in the North Sivash artesian basinK. Ya. Bulakhova0S. M. Sudarikov1Saint-Petersburg Mining University.Saint-Petersburg Mining University.The results of hydrogeochemical monitoring of the Sarmat-Meotis-Pontic sediments aquifer complex of the North Sivash artesian basin have been analyzed. The analysis based on a routine observations for 16 producing wells. The observations were made in the period from 2014 to 2017 years. A correlation and regression analysis has been made for definition of dependencies between changes in the concentrations of the normalized components. The results obtained allow us to evaluate the main factors of formation of the chemical composition of groundwater. At the present stage, metamorphosed waters are pulled up from the lower strata of the complex, that leads to an increase in the amount of mineralization. The formation of sulphate waters is primarily associated with the peculiarities of the geological structure, namely, the high gypsum content of quaternary deposits and the presence of hydraulic connection with the overlying aquifers. One of the reasons for the formation of sulphate waters is the anthropogenic impact associated with the close location of the acid accumulator containing sulfur tailing. The results obtained allow us to proceed to the next stage of the survey — the creation of a natural hydrogeological model of the research area and the carrying of the thermodynamic modeling.https://geology.mgri-rggru.ru/jour/article/view/414sarmatian-meotic-pontian aquifer complexnorth sivash artesian basincorrelation and regression analysisthe formation of groundwater
collection DOAJ
language Russian
format Article
sources DOAJ
author K. Ya. Bulakhova
S. M. Sudarikov
spellingShingle K. Ya. Bulakhova
S. M. Sudarikov
Analysis of the data of hydrogeochemical monitoring of groundwater in the North Sivash artesian basin
Известия высших учебных заведений: Геология и разведка
sarmatian-meotic-pontian aquifer complex
north sivash artesian basin
correlation and regression analysis
the formation of groundwater
author_facet K. Ya. Bulakhova
S. M. Sudarikov
author_sort K. Ya. Bulakhova
title Analysis of the data of hydrogeochemical monitoring of groundwater in the North Sivash artesian basin
title_short Analysis of the data of hydrogeochemical monitoring of groundwater in the North Sivash artesian basin
title_full Analysis of the data of hydrogeochemical monitoring of groundwater in the North Sivash artesian basin
title_fullStr Analysis of the data of hydrogeochemical monitoring of groundwater in the North Sivash artesian basin
title_full_unstemmed Analysis of the data of hydrogeochemical monitoring of groundwater in the North Sivash artesian basin
title_sort analysis of the data of hydrogeochemical monitoring of groundwater in the north sivash artesian basin
publisher Sergo Ordzhonikidze Russian State University for Geological Prospecting
series Известия высших учебных заведений: Геология и разведка
issn 0016-7762
2618-8708
publishDate 2019-06-01
description The results of hydrogeochemical monitoring of the Sarmat-Meotis-Pontic sediments aquifer complex of the North Sivash artesian basin have been analyzed. The analysis based on a routine observations for 16 producing wells. The observations were made in the period from 2014 to 2017 years. A correlation and regression analysis has been made for definition of dependencies between changes in the concentrations of the normalized components. The results obtained allow us to evaluate the main factors of formation of the chemical composition of groundwater. At the present stage, metamorphosed waters are pulled up from the lower strata of the complex, that leads to an increase in the amount of mineralization. The formation of sulphate waters is primarily associated with the peculiarities of the geological structure, namely, the high gypsum content of quaternary deposits and the presence of hydraulic connection with the overlying aquifers. One of the reasons for the formation of sulphate waters is the anthropogenic impact associated with the close location of the acid accumulator containing sulfur tailing. The results obtained allow us to proceed to the next stage of the survey — the creation of a natural hydrogeological model of the research area and the carrying of the thermodynamic modeling.
topic sarmatian-meotic-pontian aquifer complex
north sivash artesian basin
correlation and regression analysis
the formation of groundwater
url https://geology.mgri-rggru.ru/jour/article/view/414
work_keys_str_mv AT kyabulakhova analysisofthedataofhydrogeochemicalmonitoringofgroundwaterinthenorthsivashartesianbasin
AT smsudarikov analysisofthedataofhydrogeochemicalmonitoringofgroundwaterinthenorthsivashartesianbasin
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