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SM ISO690:2012 МОРАРУ, К.Е.. Условия формирования химического состава
подземных вод Молдовы
. In: Buletinul Institutului de Geologie şi Seismologie al AŞM, 2008, nr. 1, pp. 66-75. ISSN 1857-0046. |
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Buletinul Institutului de Geologie şi Seismologie al AŞM | |||||
Numărul 1 / 2008 / ISSN 1857-0046 | |||||
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Pag. 66-75 | |||||
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Hydrogeological cross-section of the Rep. of Moldova contains confined and unconfined
ground water. Unconfined aquifers are divided in leaching and continental saline water. Influence
of ascending deep water is minimized by geochemical evaporation barrier. Chemistry of confined
aquifer is under the influence of tectonic faults (water with high values of К , Mg2 , HCO3-, Cl-,
F -, pH, Ва, TDS and organic substances) and geochemistry of stable blocks (water have elevated
values of Са, Mg, SO4, Sr, Se). Helium (He) is a good tracer of open tectonic zones.
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