Research Article
Geofluids Assessment of the Ayub and Shafa Hot Springs in Kopet-Dagh Zone (NE Iran): An Isotopic Geochemistry Approach
Table 1
Field parameters, major anion and cation compositions, and isotopic compositions of AP and SH hot spring and adjacent springs.
| Sample ID | Field parameter | Cations (mgL−1) | Anions (mgL−1) | Isotope ( VSMOW) | TDS (mgL−1) | EC (ms/cm) | PH | T (°C) | DO (% sat) | Eh (mv) | Ca+2 | Mg+ | Na+ | K+ | | | | Cl− | δ2H | δ18O |
| Sp. 1 | 247 | 499 | 8.0 | 25.0 | — | 82 | 104 | 33 | 67 | 3.1 | 16.0 | 184 | 130 | 8 | −62.6 | −9.0 | Sp. 2 | 443 | 953 | 8.1 | 18.0 | — | 112 | 147 | 49 | 109 | 3.7 | 0.0 | 284 | 336 | 35 | −61.8 | −8.5 | Sp. 3 | 307 | 626 | 7.6 | 16.9 | 146 | 141 | 110 | 28 | 84 | 3.6 | 24.0 | 150 | 234 | 46 | −58.8 | −8.3 | Sp. 4 | 372 | 782 | 7.1 | 14.0 | — | 173 | 70 | 250 | 3 | 0.0 | 28.0 | 176 | 36 | 6 | −66.2 | −9.4 | Sp. 5 | 146 | 334 | 7.7 | 16.9 | — | 195 | 89 | 41 | 94 | 3.4 | 64.0 | 110 | 343 | 49 | −70.5 | −9.9 | Sp. 6 | 218 | 444 | 7.7 | 12.1 | 204 | 184 | 60 | 48 | 34 | 1.8 | 80.0 | 160 | 85 | 9 | −65.6 | −9.3 | Sp. 7 | 296 | 604 | 7.5 | 17.2 | 137 | 173 | 71 | 52 | 59 | 3.4 | 60.0 | 170 | 172 | 21 | −66.4 | −9.1 | Sp. 8 | 550 | 1120 | 7.5 | 38.0 | 65 | −22 | 87 | 42 | 96 | 3.2 | 16.0 | 184 | 349 | 43 | −73.0 | −9.9 | Sp. 9 | 770 | 1559 | 7.1 | 21.0 | 55 | 104 | 188 | 84 | 170 | 29.6 | 8.0 | 286 | 707 | 166 | −71.8 | −9.9 | Sp. 10 | 469 | 957 | 7.3 | 36.0 | 19 | −72 | 67 | 40 | 75 | 2.1 | 4.0 | 190 | 263 | 37 | −73.1 | −10.2 | Sp. 11 | 454 | 930 | 8.3 | 16.0 | — | 58 | 280 | 346 | 9 | 17.4 | 56.0 | 256 | 423 | 52 | — | — | Sp. 12 | 404 | 825 | 8.1 | 25.0 | — | 131 | 81 | 52 | 99 | 2.7 | 24.0 | 196 | 392 | 38 | −65.3 | −8.8 | Sp. 13 | 780 | 1591 | 7.6 | 22.3 | 89 | 196 | 312 | 552 | 228 | 4.0 | 21.7 | 10 | 695 | 127 | — | — | Sp. 14 | 615 | 1256 | 7.3 | 16.4 | 45 | 112 | 230 | 440 | 224 | 0.0 | 21.7 | 10 | 366 | 32 | — | — | R. 1 | 285 | 581 | 8.4 | 22.7 | 134 | 150 | 53 | 43 | 52 | 1.4 | 72.0 | 110 | 142 | 31 | −72.1 | −10.1 | R. 2 | 251 | 511 | 8.3 | 26.4 | 129 | 134 | 172 | 130 | 128 | 64.0 | 26.1 | 5 | 145 | 42 | — | — | R. 3 | 966 | 1971 | 8.1 | 27.0 | 97 | 166 | 318 | 542 | 164 | 16.0 | 4.3 | 11 | 880 | 75 | — | — | R. 4 | 1280 | 2612 | 8.0 | 29.9 | 107 | 135 | 30 | 750 | 202 | 26.1 | 26.1 | 13 | 980 | 131 | — | — | R. 5 | 840 | 1714 | 8.3 | 25.5 | 159 | 129 | 360 | 360 | 184 | 21.7 | 4.3 | 11 | 640 | 99 | — | — | W. 1 | 349 | 713 | 7.4 | 16.4 | — | 101 | 190 | 330 | 244 | 8.7 | 26.1 | 6 | 280 | 44 | — | — | W. 2 | 462 | 978 | 7.1 | 18.6 | 92 | 101 | 200 | 190 | 240 | 13.0 | 21.7 | 8 | 445 | 48 | — | — |
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