Occurrence of thermal and mineralized waters as an opportunity for development of therapeutic resorts as the touristic attractions in Warsaw region

Izabella Gryszkiewicz, M. Socha
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Abstract

The thermal and mineralized waters in the subsurface of Sulejówek, Józefów, and Otwock towns of the Warsaw region have been analyzed. An initial assessment of the utilization of such waters based on deep boreholes and significance of these waters for development of the communities has been considered. The analysis shows that in the area of Sulejówek, Józefów and Otwock communes there are chloride and sodium waters in the aquifer of the Lower Cretaceous and the Jurassic of mineralization from about 10 to over 70 g/dm3, probably characterized by an increased content of specific components desirable in the case of waters used in balneotherapy – iodides (above 1 mg/dm3 in the lower cretaseous and lower jurassic) and divalent iron (over 10 mg/dm3 in the lower jurassic). The values of subsurface temperature in this area at a depth of 1000 m are about 35°C, at a depth of 2000 m the temperature exceeds 50°C. An optimist scenario includes a possibility of future development of touristic attractions in terms of therapeutic resorts in the Warsaw region.
温泉和矿化水的出现为华沙地区的旅游景点提供了发展疗养胜地的机会
对华沙地区Sulejówek、Józefów和Otwock镇地下的热水和矿水进行了分析。已经考虑了基于深钻孔对这种水的利用的初步评估以及这些水对社区发展的重要性。分析表明,在Sulejówek、Józefów和Otwock公社地区,下白垩统和成矿侏罗纪的含水层中含有氯化物和钠水,含量约为10至70 g/dm3以上,其特征可能是用于温泉治疗的水中所需的特定成分-碘化物(下白垩统和下侏罗纪超过1 mg/dm3)和二价铁(下侏罗纪超过10 mg/dm3)的含量增加。该地区1000m深地下温度约为35℃,2000m深地下温度超过50℃。乐观的情况包括在华沙地区的治疗胜地方面的旅游景点的未来发展的可能性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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