赣北与赣南地区典型中温温泉水文地球化学特征  

Hydrogeochemical characteristics of typical mid-temperature hot springs in northern and southern Jiangxi

作　　者：施兴华 白细民 孙占学[1] 刘金辉[2] 叶海龙 庞龙龙 关燕鹤 陈功新[2] SHI Xing-hua;BAI Xi-min;SUN Zhan-xue;LIU Jin-hui;YE Hai-long;PANG Long-long;GUAN Yan-he;CHEN Gong-xin(State Key Laboratory of Nuclear Resources and Environment,East China University of Technology,Nanchang 330013,China;School of Water Resources&Environmental Engineering,East China University of Technology,Nanchang 330013,China;Jiangxi Survey Design Research Institute Co.,Ltd.,Nanchang 330224,China;School of Geophysics and Measurement-control Technology,East China University of Technology,Nanchang 330013,China)

机构地区：[1]东华理工大学核资源与环境国家重点实验室,南昌330013 [2]东华理工大学水资源与环境工程学院,南昌330013 [3]江西省勘察设计研究院有限公司,南昌330224 [4]东华理工大学地球物理与测控技术学院,南昌330013

出　　处：《矿物岩石地球化学通报》2024年第3期521-532,共12页Bulletin of Mineralogy, Petrology and Geochemistry

基　　金：国家自然科学基金资助项目(41511130031);南昌市水文地质与优质地下水资源开发利用重点实验室基金资助项目(20232C22);江西省教育厅科技计划项目(GJJ2200771);东华理工大学博士科研基金资助项目(DHBK2019046);江西省重点研发计划“揭榜挂帅”项目(20223BBG74005)。

摘　　要：为践行“双碳”目标,助力中国地热资源的可持续开发利用,本文采用同位素手段和多矿物平衡模拟法,研究了赣北的白岭温泉与赣南的汤湖温泉和白石温泉的水化学特征。结果表明,白岭温泉(85℃)为弱碱性HCO_(3)-Na型硅-氟水,其总溶解固体(TDS)含量、H_(2)SiO_(3)含量和主要离子浓度均低于汤湖温泉(89℃,弱碱性HCO_(3)-Na型硅-氟水)和白石温泉(85℃,弱碱性SO_(4)-HCO_(3)-Na型硅-氟水)。三个温泉虽均来源于大气降水,但汤湖温泉和白石温泉水的地下滞留时间更长,而白岭温泉的循环深度更大。白岭温泉和汤湖温泉的水岩作用强烈,均存在明显的氧漂移现象,而白石温泉则发生水气同位素交换作用,导致热水的δ^(18)O值降低。长石、方解石、石膏、黄铁矿的溶解和H_(2)S的氧化为温泉中主要离子来源。白岭温泉、汤湖温泉和白石温泉的平均热储温度分别为125、135和149℃,属于中温地热资源,其补给高程分别为1455、1790和1050 m。In order to implement the″double carbon″goal and promote the sustainable development and utilization of China′s geothermal resources,the hydrochemical characteristics of Bailing Hot Spring in northern Jiangxi and Tanghu Hot Spring and Baishi Hot Spring in southern Jiangxi were studied by isotopic method and multi-mineral equilibrium simulation.The results showed that Bailing Hot Spring(85℃)is weak alkaline HCO_(3)-Na type silicon-fluorine water,and its TDS content,H_(2)SiO_(3)content and main ion concentration are lower than those of Tanghu Hot Spring(89℃,weak alkaline HCO_(3)-Na type silicon-fluorine water)and Baishi Hot Spring(85℃,weak alkaline SO_(4)-HCO_(3)-Na type silicon-fluorine water).Although the water of the three hot springs is derived from atmospheric precipitation,the underground retention time is longer in Tanghu Hot Spring and Baishi Hot Spring,while the circulation depth is greater in Bailing Hot Spring.Bailing Hot Spring and Tanghu Hot Spring have strong rock interaction and both show obvious Spring undergo water-gas isotope exchange,resulting in a decrease in δ^(18)O in hot water.Dissolution of feldspar,calcite,gypsum,pyrite and oxidation of H_(2)S provide the source of main ionic constituents in the hot springs.The average reservoir temperatures of Bailing Hot Spring,Tanghu Hot Spring and Baishi Hot Spring are 125,135 and 149℃,respectively,belonging to mid-temperature geothermal resources and the corresponding recharge elevations are 1455,1790 and 1050 m,respectively.

关 键 词：中温温泉 水化学特征 水-岩相互作用 同位素 

分 类 号：P641.3[天文地球—地质矿产勘探]