华南珠江三角洲地区地热水的地球化学及硼和锶的来源:水与岩石相互作用的影响

IF 3.4 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Journal of Geochemical Exploration Pub Date : 2024-05-02 DOI:10.1016/j.gexplo.2024.107492
Zhengan Wei , Shaopeng Huang , Chengshan Wang
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引用次数: 0

摘要

中国南方的珠江三角洲(PRD)地区拥有丰富的地热水资源。然而,由于缺乏基础地球化学研究,该地区地热资源的开发利用水平相对较低。为了了解珠三角地热系统的水岩相互作用过程,我们结合已报道的痕量元素(B、Sr和Br)和同位素(δ11B和87Sr/86Sr)以及常规示踪剂(主要元素),对地热水的地球化学进行了分析。Cl/Br 比率(从 31 到 639)证实了海洋盐度、沉淀和少量海绿石溶解的多源性。主要离子化学成分突出了离子交换、碳酸盐、硅酸盐和硫酸盐矿物溶解以及海水的影响。Cl/B 比率(61 至 22,583 )表明了与碳酸盐岩和长英岩的相互作用、海水的输入以及地下水的混合。硼同位素组成(δ11B)介于-9.22 和 +39.78 ‰之间。锶含量和 87Sr/86Sr 比值较为均匀,分别介于 0.06 至 32.26 毫克/升和 0.71239 至 0.72121 之间。硼和锶同位素特征表明,有三个过程促成了地热水的地球化学:1) 水/岩石相互作用,包括海洋碳酸盐岩、蒸发岩和花岗岩或/和片麻岩;2) 海水入侵;3) 浅层地下水混合。主要痕量元素化学和这些同位素系统学本身表明了流体起源或水岩相互作用过程方面的基本信息,但也提供了对中国南方珠三角地区地热系统更全面的了解。
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Geochemistry and sources of boron and strontium of geothermal waters from the Pearl River Delta region, South China: Implications for water-rock interactions

Pearl River Delta (PRD) region of South China is abundant of geothermal water resources. However, the development and utilization level of geothermal resources in this region is relatively low, due in part to the lack of fundamental geochemical research. To access water-rock interaction processes of the PRD geothermal system, we analyzed the geochemistry of geothermal waters by combining trace elements (B, Sr, and Br) and isotopes (δ11B and 87Sr/86Sr) with conventional tracers (major elements) that had been reported. The Cl/Br ratios (from 31 to 639) confirm the multi-source salinity of marine origin, precipitation, and a minor dissolution of halite. Major ions chemistry highlights the influence of ions exchange, the dissolution of carbonate, silicate, and sulphate minerals as well as the contribution of seawater. The Cl/B ratios (61 to 22,583) suggest interactions with carbonate rock and felsic rock, input of seawater, and groundwater mixing. Boron isotopic compositions (δ11B) range between −9.22 and +39.78 ‰. Sr contents and 87Sr/86Sr ratios are more homogeneous, falling between 0.06 and 32.26 mg/L and between 0.71239 and 0.72121, respectively. The B and Sr isotopic signatures show that three processes contribute to geochemistry of geothermal waters: 1) water/rock interaction involving marine carbonate rock, evaporite, and granitoid or/and gneiss, 2) seawater intrusion, and 3) shallow groundwater mixing. Major-trace element chemistry and these isotope systematics on their own indicates essential information on the aspects of fluid origin or water-rock interaction processes, and however provide a more comprehensive understanding of the geothermal system in the PRD region, South China.

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来源期刊
Journal of Geochemical Exploration
Journal of Geochemical Exploration 地学-地球化学与地球物理
CiteScore
7.40
自引率
7.70%
发文量
148
审稿时长
8.1 months
期刊介绍: Journal of Geochemical Exploration is mostly dedicated to publication of original studies in exploration and environmental geochemistry and related topics. Contributions considered of prevalent interest for the journal include researches based on the application of innovative methods to: define the genesis and the evolution of mineral deposits including transfer of elements in large-scale mineralized areas. analyze complex systems at the boundaries between bio-geochemistry, metal transport and mineral accumulation. evaluate effects of historical mining activities on the surface environment. trace pollutant sources and define their fate and transport models in the near-surface and surface environments involving solid, fluid and aerial matrices. assess and quantify natural and technogenic radioactivity in the environment. determine geochemical anomalies and set baseline reference values using compositional data analysis, multivariate statistics and geo-spatial analysis. assess the impacts of anthropogenic contamination on ecosystems and human health at local and regional scale to prioritize and classify risks through deterministic and stochastic approaches. Papers dedicated to the presentation of newly developed methods in analytical geochemistry to be applied in the field or in laboratory are also within the topics of interest for the journal.
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