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Warunki hydrogeochemiczne występowania wód siarczkowych w południowej części niecki miechowskiej

Bąk Ewelina, Bruczyńska Joanna, Lipiec Iwona

Przegląd Geologiczny

2021

Vol. 69, nr 10

687--696

The paper presents the characteristics of sulphide watersin the Busko-Zdrój, Solec-Zdrój and Kazimierza Wielka area. The chemical composition was determined on the basis of results of analyses of groundwater samples from the B-4b Aleksander, B-8b Michał, B-13 Anna, B-16a Wiesława, B-17 Ignacy, Busko C-1, Las Winiarski LW-1, Winiarski Forest LW-2, Cudzynowice GT-1, Solecki Shaft and Solec 2 Karol boreholes and the Gadawa (shaft), Szczerbaków (shaft) and Piestrzec springs. The following hydrochemical facies of sulphide waters were identified: Cl-Na, Cl-SO4-Na and SO4-Ca. Hydrogeochemical modelling allowed determining the saturation state of the solution relative to the mineral phases of the reservoir rocks.

Występowanie i możliwości zagospodarowania wód siarczkowych w rejonie Tarnobrzega

Felter A., Stożek J., Socha M., Sokołowski J.

Przegląd Geologiczny

2017

Vol. 65, nr 11/1

956--961

The long-term exploitation of sulphur deposits in the Tarnobrzeg region along with intense groundwater drainage caused a change of hydrodynamic and hydrogeochemical conditions. After the finishing of mining activities, the area has been reclamed, causing a return to near-natural conditions. Therefore, the geological and hydrogeological conditions are currently close to natural. This area is prospective for extraction of mineralized sulphide waters and their use in balneotherapy.

Charakterystyka hydrogeochemiczna wód siarczkowych rejonu Solca-Zdroju

Lipiec I., Wiktorowicz B.

Przegląd Geologiczny

2015

Vol. 63, nr 10/2

908--911

This paper shows characteristics of sulphurous waters from the Solec-Zdrój area. Evaluation of their chemistry was based on the results of analyses of groundwater sampled from boreholes in: Solec-Zdrój, Wełnin and Dobrowoda and from the springs: Senisławice, Gadawa, Szczerbaków and Piestrzec. The following hydrochemical facies of groundwater were identified: Ca‒SO4‒ HCO3 , S, Na‒Cl‒SO4 , S to Cl‒Na, S , with TDS in the range of 1.9‒47.0 g/dm3. Examined waters are also featured by considerable concentrations of iodine and fluorine. The research results proved that the geological setting is one of the most important factors defining the water chemistry variability. In general, the chemical composition of sulphide waters in this region is determined by the interactions between the groundwaters and rocks.