Equilibrium of groundwater with carbonate minerals of the water-bearing rocks under anthropogenic impact (by the example of Kishinev, Moldova)
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TIMOSHENKOVA, A., PASECHNIK, Elena, TOKARENKO, O.. Equilibrium of groundwater with carbonate minerals of the water-bearing rocks under anthropogenic impact (by the example of Kishinev, Moldova). In: IOP Conference Series: Earth and Environmental Science: XVIII International Scientific Symposium in Honour of Academician M. A. Usov: Problems of Geology and Subsurface Development, Ed. 21, 7-11 aprilie 2014, Tomsk. Institute of Physics Publishing, 2014, Vol. 21, Issue 1 , p. 0. ISSN E-ISSN:1755-1315. DOI: https://doi.org/10.1088/1755-1315/21/1/012024
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IOP Conference Series: Earth and Environmental Science
Vol. 21, Issue 1 , 2014
Conferința "IOP Conference Series: Earth and Environmental Science"
21, Tomsk, Rusia, 7-11 aprilie 2014

Equilibrium of groundwater with carbonate minerals of the water-bearing rocks under anthropogenic impact (by the example of Kishinev, Moldova)

DOI:https://doi.org/10.1088/1755-1315/21/1/012024

Pag. 0-0

Timoshenkova A.1, Pasechnik Elena2, Tokarenko O.2
 
1 Institute of Geology and Seismology, ASM,
2 Tomsk Polytechnic University
 
 
Disponibil în IBN: 2 iunie 2023


Rezumat

The paper presents calculation results of equilibrium of groundwater in Kishenev with a variety of secondary carbonate minerals. It is shown that the groundwater-rock system is in equilibrium with some minerals, such as calcite, magnesite, dolomite, siderite, but at the same time is not in equilibrium with strontianite. It indicates that secondary mineral precipitation is possible. Specific nitrate chemical water type, which is rarely observed in nature and characterized by the presence of anthropogenic impact in this territory, in some cases is of higher saturation as compared to calcite, dolomite and magnesite due to the fact that nitrate ion content increases with the increase of calcium content.