天津滨海新区深部地热流体水文地球化学特征
石晓今, 李嫄嫄, 黄贤龙

Hydrogeochemical characteristics of deep geothermal fluids in the Binhai New Area, Tianjin City
SHI Xiao-Jin, LI Yuan-Yuan, HUANG Xian-Long
表1 研究区地热流体主要组分含量
Table 1 The mail components of geothermal water in the study area
井号 热储层 K+ Na+ Ca2+ Mg2+ Cl- S O 4 2 - HC O 3 - SiO2 F- 矿化度 水化学类型
TG-34 Ed 7.4 1064 6.1 0.6 1169.8 8.2 781.1 49 5.21 2407.3 Cl·HCO3-Na
TG-33 Ed 4.9 593.3 9.7 0.8 402.4 235.9 555.3 42.5 7.08 3122.2 Cl·HCO3-Na
塘20-2 Ed 9.4 1190 8.4 0.9 1258.5 40.1 872.6 58.4 3.5 1692.1 Cl·HCO3-Na
ST-01 Ed 8.0 801.1 10.5 0.9 831.3 116.1 579.7 58.5 3.6 2406.1 Cl·HCO3-Na
ST-01B Ed 7.9 779.7 9.7 0.8 852.6 105.1 619.4 61 4 2436.2 Cl·HCO3-Na
BST-01 Jxw 79.9 201.4 36.4 6.8 85.1 200.8 414.9 94.5 8.23 1119.8 HCO3-Na
DG-53 Jxw 41.2 536.1 22.7 4.1 460.8 280.1 494.3 72 9.6 1915.5 Cl·HCO3-Na
DG-46 Jxw 72.5 642.8 38.1 7.9 581.4 343.9 454.6 83.8 10.4 2225 HCO3·Cl-Na
DG-45B Jxw 51.2 554.5 30.1 6.1 478.6 302.6 494.3 74.5 10.8 1991.9 Cl-Na