Research Article
Hydrogeochemical Characteristics and Genesis of the Chazi Geothermal Field Area in Tibet
Table 1
Major constituents of the water samples in the study area.
| Field number | Geothermal display area | Sample type | Water temperature/°C | pH | ρB/(mg/L) | Hydrochemical type | Na+ | K+ | Ca2+ | Mg2+ | HCO3- | CO32- | Cl- | SO42- | TDS |
| DR28 | Lagejia spring | Hot spring | 85 | 8.3 | 386.2 | 35.1 | 2.9 | 0.0 | 449.2 | 106.9 | 158 | 89.9 | 1732 | HCO3-Na | DR32 | Semi spring | Hot spring | 89 | 8.7 | 790.5 | 125.5 | 0.7 | 0.0 | 0 | 571.3 | 722.8 | 10.1 | 4350 | Cl·CO3-Na | DR36 | Charongqurene spring | Hot spring | 65 | 7.1 | 564.7 | 58.2 | 53.3 | 6.7 | 807.5 | 0 | 262.9 | 436 | 2333.7 | HCO3·SO4- Na | DR37 | Dengle spring | Hot spring | 43 | 6.6 | 837.2 | 72.3 | 66.8 | 14.6 | 1201.1 | 0 | 919.3 | 37.5 | 3442.1 | Cl·HCO3-Na | DR40 | Pola spring | Hot spring | 30 | 6.6 | 107.1 | 5.1 | 8.5 | 0.2 | 99.8 | 0 | 90.5 | 43.6 | 421.4 | Cl ·HCO3-Na | DR42 | Qugu spring | Hot spring | 47 | 8.9 | 117.9 | 2.4 | 0.7 | <0.1 | 268.9 | 20.9 | 4.2 | 12.2 | 469.2 | HCO3-Na | DR44 | Seluo spring | Hot spring | 44 | 6.7 | 195.0 | 40.2 | 195.8 | 37.7 | 1105.2 | 0 | 226.6 | 2.9 | 1893.1 | HCO3·cl-ca·Na | DR45 | Cha spring | Hot spring | 48 | 7.1 | 476.4 | 26.6 | 70.9 | 9.2 | 1246.5 | 0 | 200.5 | 28.3 | 2242.3 | HCO3-Na | DR47 | Qugulongbu | Hot spring | 66 | 6.9 | 454.7 | 25.3 | 50.3 | 7.6 | 616.9 | 0 | 280.6 | 250.8 | 1903.5 | HCO3·cl-Na | DR48 | Shalei spring | Hot spring | 75 | 7.7 | 115.4 | 10.4 | 28.8 | 7 | 378.5 | 0 | 7.2 | 59.2 | 710.3 | HCO3-Na | XZDR9 | Tamaquzhen | Hot spring | 63 | 7.2 | 407.4 | 31.6 | 40 | 12.6 | 856.3 | 0 | 190.5 | 78.2 | 1919 | HCO3-Na | XZDR11 | Yinjianquzhen | Hot spring | 39 | 6.5 | 59.4 | 5.4 | 210 | 20.9 | 811.9 | 0 | 8.9 | 34.8 | 1113 | HCO3-Ca | XZDR15 | Gabudanni | Hot spring | 67 | 7.0 | 451.4 | 29.7 | 19.2 | <0.1 | 584.4 | 0 | 259.4 | 169.9 | 1922 | HCO3·Cl-Na | CKLSQ1 | Chazi Village | Hot spring | 87 | 7.8 | 481.9 | 39.1 | 12.8 | <0.1 | 654.9 | 87.1 | 165.1 | 121.9 | 1806.9 | HCO3-Na | CKLSQ2 | Chazi Village | Hot spring | 74 | 7.9 | 476.9 | 41.1 | 9.5 | <0.1 | 707.3 | 58.1 | 167.8 | 117.5 | 1844.1 | HCO3-Na | CQSH | Chazi Village | Chaqu River water | 7.5 | 7.5 | 13.1 | 1.4 | 40.9 | 6.6 | 115.9 | 0 | 1.41 | 47.3 | 279 | HCO3·SO4-Ca | CQXH | Chazi Village | Chaqu River water | 25.5 | 8.6 | 363.7 | 30.1 | 19.2 | 1.82 | 424.1 | 108.2 | 118.1 | 106.1 | 1386.1 | HCO3-Na | DLZBXH | Chazi Village | Dalong Zangbo River water | 6.5 | 8.3 | 8.1 | 2.5 | 44.5 | 4.9 | 78.4 | 1.1 | 3.1 | 75.3 | 233.2 | SO4·HCO3-Ca | J05 | Chazi Village | Well water | 4 | 7.5 | 5.7 | 2.3 | 25 | 2.1 | 78.7 | 0 | 2.7 | 16.6 | 115.6 | HCO3-Ca | DR28-1 | Lagejia spring | Hot spring | 85.5 | 9.1 | 365 | 41 | 7.2 | 1.9 | 261 | 234 | 165 | 132 | 1570 | CO3·Cl -HCO3 | DR28-2 | Lagejia spring | Hot spring | 78 | 8.4 | 388.9 | 35 | 0.6 | 0.2 | 590.6 | 36 | 112.1 | 102 | 1712 | HCO3-Na | DR28-3 | Lagejia spring | Hot spring | 85 | 8.7 | 350 | 39 | 0 | 0 | 447.2 | 100.8 | 151.7 | 77.8 | 1600 | HCO3-Na | DR32-1 | Semi spring | Hot spring | 86 | 8.7 | 700 | 104 | 3.4 | 4.2 | 490 | 306 | 674 | 65.8 | 4340 | Cl·CO3·HCO3-Na | DR42-1 | Qugu spring | Hot spring | 45 | 8.9 | 118 | 2.5 | 3.4 | 1.3 | 227 | 45.7 | 13.9 | 28.8 | 227 | HCO3·CO3·SO4·Cl-Na | DR44-1 | Seluo spring | Hot spring | 40 | 7.3 | 175 | 33.3 | 202 | 22.9 | 1040 | — | 157 | 74 | 1380 | HCO3·Cl-Ca·Na | DR45-1 | Cha spring | Hot spring | 44.5 | 7.3 | 443 | 26.5 | 73.8 | 12.5 | 1130 | — | 172 | 32.9 | 1560 | HCO3·Cl-Na·Ca | DR47-1 | Qugulongbu | Hot spring | 65.2 | 7 | 442.5 | 26.5 | 53.2 | 9.4 | 493 | — | 272 | 280 | 1600 | HCO3·Cl-Na·Ca | DR48-1 | Shalei spring | Hot spring | 76 | 7.5 | 125 | 12.5 | 34.3 | 8.3 | 38.1 | — | 9.6 | 26.8 | 510 | HCO3-Na·Ca | CKLSQ-1 | Chazi Village | Hot spring | 87 | 7.9 | 468 | 45 | 12 | 4.2 | 801 | — | 163 | 144 | 1560 | HCO3·Cl·SO4-Na |
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Note: DR28-1, DR28-2, DR28-3, DR32-1, DR42-1, DR44-1, DR45-1, DR47-1, DR48-1, and CKLSQ-1 are quoted from the report of Wei et al. [ 29]. |