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Tourism potential of the mineral waters of sub-Carpathian area of Dambovita and Prahova rivers (Romania)

机译：Dambovita河和Prahova河（罗马尼亚）的喀尔巴阡亚地区矿泉水的旅游业潜力

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摘要

Sub-Carpathian sector located between Dambovita and Prahova rivers is composed of Mio-Pliocene formations, with a wide variety of sedimentary rocks wich influence and conditions on the position and characteristics of groundwater. Lithological constitution characterized by an alternation of permeable horizons (conglomerates, sandstones, gravels, sands) with impermeable horizons (clay and marl) with inhomogeneous thickness and the presence of faults, hydrocarbon resources and salt pits, have important influences to the distribution, reservoir conditions and chemical characteristics of groundwater. Mineral waters are characterized by a variable content of mineral and organic substances, falling within the category of chloride, sodium, bromine, iodine, sulphate and sulphide: chlorosodics waters, extended on the line Jintea - Baicoi - Floresti -Moreni - Gura Ocnitei - Razvad; sulphurous waters which is developing between Vulcana and Pucioasa; iodo-bromine mineral waters with a wide spread, due to oil structures. Some other mineral waters are such as wells of Vulcana, Varfuri, Moreni, Gura Ocnitei, Urseiu, Barbuleju. Because of curative mineral water capacity of the geographic area analyzed, they could be used to treat various diseases but also are not sufficiently valued for tourism, so only Pucioasa may be regarded as representative in this regard.
机译：位于Dambovita河和Prahova河之间的亚喀尔巴阡山脉部分由Mio-上新世地层组成，沉积岩种类繁多，对地下水的位置和特征具有影响和条件。岩石构造的特征是渗透性层位（砾岩，砂岩，砾石，沙子）与不渗透层位（粘土和泥灰岩）的厚度不均匀，并且断层，油气资源和盐坑的存在对分布，储层条件具有重要影响和地下水的化学特性。矿泉水的特征是矿物质和有机物质的含量可变，属于氯化物，钠，溴，碘，硫酸盐和硫化物的类别：含氯的水，沿线延伸Jintea-Baicoi-Floresti -Moreni-Gura Ocnitei-Razvad ;在Vulcana和Pucioasa之间发展的亚硫酸水；由于石油结构，碘溴矿泉水分布广泛。其他一些矿泉水包括Vulcana，Varfuri，Moreni，Gura Ocnitei，Urseiu，Barbuleju的水井。由于所分析地理区域的治愈性矿泉水容量，它们可以被用来治疗各种疾病，但在旅游业中却没有足够的价值，因此在这方面，只有Pucioasa可以被视为代表。

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