Research Article
Hydrogeochemical Characteristics and Formation of Low-Temperature Geothermal Waters in Mangbang-Longling Area of Western Yunnan, China
Table 2
Saturation indices of different minerals in geothermal waters.
| Sample | GS1 | GS2 | GS3 | GS4 | GS5 | GS6 | GS7 | GS8 | GS9 | GS10 | GS11 | GS12 | GS13 | GS14 |
| Anhydrite | −4.07 | −4.66 | −3.37 | −4.52 | −4.48 | −4.36 | −4.8 | −4.65 | −4.47 | −4.69 | −4.92 | −4.21 | −4.36 | −3.64 | Aragonite | −0.26 | −0.34 | −0.3 | −2.43 | −2.24 | −1.95 | −2.45 | −2.38 | −2.32 | −2.41 | 0.22 | −2.18 | −1.86 | −0.86 | Calcite | −0.12 | −0.19 | −0.16 | −2.29 | −2.1 | −1.81 | −2.31 | −2.24 | −2.18 | −2.27 | 0.36 | −2.04 | −1.72 | −0.72 | Chalcedony | 0.18 | 0.28 | 0.2 | 0.23 | 0.26 | 0.14 | 0.18 | 0.09 | 0.15 | 0.28 | 0.18 | 0.18 | 0.3 | 0.08 | Chrysotile | −5.78 | −6.25 | −5.94 | −15.59 | −14.3 | −12.51 | −15.68 | −15 | −12.57 | −15.55 | −7.23 | −12.69 | −15.7 | −8.58 | CO2 | −1.07 | −1.21 | −1.32 | −1.87 | −1.8 | −1.88 | −1.86 | −1.86 | −2.01 | −1.7 | −0.95 | −1.94 | −1.34 | −1.65 | Dolomite | 0.19 | −0.26 | −0.18 | −6.09 | −5.43 | −4.53 | −6.1 | −6.02 | −5.07 | −5.93 | 0.3 | −4.91 | −5.08 | −1.87 | Gypsum | −3.82 | −4.41 | −3.12 | −4.27 | −4.23 | −4.11 | −4.55 | −4.4 | −4.22 | −4.44 | −4.67 | −3.96 | −4.11 | −3.39 | Halite | −7.69 | −8.08 | −8.4 | −8.95 | −8.57 | −9.08 | −8.77 | −9.24 | −9.35 | −8.6 | −7.54 | −8.67 | −7.79 | −8.81 | Quartz | 0.59 | 0.69 | 0.62 | 0.64 | 0.68 | 0.55 | 0.6 | 0.5 | 0.57 | 0.69 | 0.59 | 0.59 | 0.71 | 0.5 | Sepiolite | −3.95 | −4.1 | −4.01 | −10.41 | −9.49 | −8.5 | −10.54 | −10.82 | −8.51 | −10.3 | −4.92 | −8.56 | −10.36 | −5.97 | SiO2 (a) | −0.64 | −0.55 | −0.62 | −0.59 | −0.56 | −0.68 | −0.64 | −0.74 | −0.67 | −0.55 | −0.64 | −0.65 | −0.52 | −0.74 | Talc | −1.66 | −1.93 | −1.76 | 11.37 | −10.01 | −8.46 | −11.54 | −11.92 | −8.49 | −11.23 | −3.11 | −8.57 | −11.34 | −4.65 |
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