Research Article
Research on the Hydrochemistry and Fault Control Mechanism of Geothermal Water in Northwestern Zhangzhou Basin
Table 4
Results of reservoir temperature of geothermal water samples in the study area (temperature in °C and concentration in mg/L).
| Sample ID | Emerging temperature | SiO2 | Quartz (no loss of steam) | Quartz (Verma and Santoyo) | Na/K (Fournier) | Na/K (Giggenbach) | Na/K (Verma and Santoyo) | K/Mg | Silica-enthalpy mixing model (C1) | Silica-enthalpy mixing model (C2) |
| TS-1 | 53 | 67.26 | 116.17 | 114.84-118.17 | 106.92 | 127.54 | 72.14-159.49 | 85.64 | 156.14 | 126 | TS-2 | 45.5 | 68.82 | 117.33 | 115.96-119.32 | 98.55 | 119.38 | 65.19-149.83 | 78.01 | 198.93 | 142 | TS-3 | 45 | 60.59 | 110.99 | 109.83-113.02 | 109.44 | 129.99 | 74.22-162.41 | 105.90 | 170.64 | 132 | TS-4 | 50.1 | 81.92 | 126.35 | 124.68-128.32 | 133.51 | 153.28 | 94.02-190.25 | 88.92 | 221.98 | 148 | TS-5 | 60.2 | 69.23 | 117.63 | 116.25-119.62 | 117.58 | 137.89 | 80.94-171.81 | 82.05 | 156.61 | 126 | TW-1 | 42.1 | 69.18 | 117.59 | 116.21-119.58 | 103.91 | 124.61 | 69.64-156.01 | 87.55 | 207.48 | 144 | TW-2 | 48.4 | 57.81 | 108.70 | 107.61-110.75 | 104.65 | 125.32 | 70.25-156.86 | 82.08 | 150.19 | 123 | TW-3 | 55.8 | 65.20 | 114.62 | 113.33-116.62 | 108.70 | 129.27 | 73.61-161.55 | 85.48 | 152.81 | 125 | TW-4 | 50.2 | 76.10 | 122.48 | 120.94-124.45 | 123.41 | 143.53 | 85.74-178.56 | 99.45 | 178.48 | 136 | TW-5 | 50 | 62.29 | 112.35 | 111.14-114.37 | 97.95 | 118.79 | 64.69-149.13 | 101.08 | 152.33 | 125 | TW-6 | 65 | 57.16 | 108.16 | 107.09-110.21 | 103.61 | 124.32 | 69.39-155.67 | 89.55 | 116.44 | 108 | TW-7 | 60 | 46.92 | 98.87 | 98.08-100.98 | 94.28 | 115.20 | 61.64-144.89 | 73.97 | 110.73 | 106 |
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