Bottled natural mineral waters from an andesitic aquifer in Slovenia are enriched in magnesium (1.1 g/l), sulphate (2.2 g/l) and dissolved inorganic carbon (204 g/l). We analysed major ions, trace elements, tritium activity, ¹⁴C, δ¹⁸O_H2O, δ²H_H2O, δ¹³C_DIC, gas composition and noble gases in six wells. In addition, ⁸⁷Sr/^/86Sr, δ³⁴S_SO4 and δ¹¹B were analysed here for the first time. Stable isotopes with δ¹⁸O = −11.97 to −10.30‰ and δ²H = −77.3 to −63.8 confirm meteoric origin. CO₂ degassing is evident at three wells, causing the oxygen shift of about −1.3‰. Tritium activity was detectable only in the shallowest well, where the freshwater component was dated to the 1960s. δ¹³C_DIC in five waters is −1.78 to + 1.33‰, typical of carbonate dissolution. Radiocarbon is low, 1.03–5.16 pMC. Chemical correction with bicarbonate concentration and δ¹³C correction methods gave best mean residence times, slightly longer than previously published. Sulphate has δ³⁴S 26.6–28.9‰ and δ¹⁸O 8.9–11.1‰ due to dissolution of evaporites in carbonate rocks. Boron at concentrations of 1.2–6.1 mg/l has two origins: δ¹¹B = 11.3–16.4‰ from hydrothermal alteration and δ¹¹B = 26.6–31.7‰ from carbonate dissolution. Strontium at concentrations of 0.5–22.0 mg/l has ⁸⁷Sr/^/86Sr, indicating three sources: 0.7106 for Miocene clastic rocks, 0.7082 for Triassic carbonates and 0.7070 for Lower Oligocene andesitic rocks. CO₂ represents the majority of the dissolved (> 98.84 vol%) and separated gas (> 95.23 vol%). Methane is only found in two wells with a max. of 0.30 vol%. All waters show excess helium and 16–97% of mantle-derived helium. Since all show subsurface degassing, the paleo-infiltration temperature could not be calculated.

来自斯洛文尼亚安山岩含水层的瓶装天然矿泉水富含镁 (1.1 g/l)、硫酸盐 (2.2 g/l) 和溶解的无机碳 (204 g/l)。对6口井进行了主量离子、微量元素、氚活度、¹⁴ C、δ ¹⁸ O _H2O、δ ² H _H2O、 δ ¹³ C _DIC 、气体成分和惰性气体分析。此外，这里首次分析了⁸⁷ Sr/ ^/86 Sr、δ ³⁴ S _SO4和δ ^{11 B。}稳定同位素δ ¹⁸ O = −11.97 至 −10.30‰ 和δ ² H = −77.3 至 −63.8 确认流星起源。CO ₂脱气在三个井中很明显，导致约-1.3‰的氧转移。仅在最浅的井中检测到氚活动，淡水成分可追溯到 1960 年代。五个水域的δ ¹³ C _{DIC为-1.78至+1.33‰，典型的碳酸盐溶解。}放射性碳很低，1.03–5.16 pMC。使用碳酸氢盐浓度和δ ¹³ C 校正方法进行的化学校正给出了最佳平均停留时间，比之前公布的时间稍长。硫酸盐具有δ ³⁴ S 26.6–28.9‰和δ ¹⁸O 8.9–11.1‰ 由于碳酸盐岩中蒸发岩的溶解。浓度为 1.2–6.1 mg/l 的硼有两个来源：δ ¹¹ B = 11.3–16.4‰ 来自热液蚀变，δ ¹¹ B = 26.6–31.7‰ 来自碳酸盐溶解。浓度为 0.5–22.0 mg/l 的锶有⁸⁷ Sr/ ^/86 Sr，表明三个来源：中新世碎屑岩 0.7106、三叠纪碳酸盐岩 0.7082 和下渐新世安山岩 0.7070。二氧化碳_{_}代表大部分溶解气体 (> 98.84 vol%) 和分离气体 (> 95.23 vol%)。甲烷仅在两个最大的井中发现。0.30 体积％。所有水域都显示出过量的氦气和 16-97% 的来自地幔的氦气。由于都显示地下脱气，因此无法计算古渗透温度。