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    Volume 45 Issue 11
    Nov.  2020
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    Article Navigation >  Earth Science  > 2020  >  45(11): 4236-4253
    Sun Houyun, Wei Xiaofeng, Sun Xiaoming, Jia Fengchao, Li Duojie, He Zexin, Li Jian, 2020. Formation Mechanism and Geological Construction Constraints of Metasilicate Mineral Water in Yudaokou, Hannuoba Basalt Area. Earth Science, 45(11): 4236-4253. doi: 10.3799/dqkx.2020.011
    Citation: Sun Houyun, Wei Xiaofeng, Sun Xiaoming, Jia Fengchao, Li Duojie, He Zexin, Li Jian, 2020. Formation Mechanism and Geological Construction Constraints of Metasilicate Mineral Water in Yudaokou, Hannuoba Basalt Area. Earth Science, 45(11): 4236-4253. doi: 10.3799/dqkx.2020.011
    shu

    Formation Mechanism and Geological Construction Constraints of Metasilicate Mineral Water in Yudaokou, Hannuoba Basalt Area

    doi: 10.3799/dqkx.2020.011
    • 1.

      School of Water Resources and Environment, China University of Geosciences, Beijing 100083, China

    • 2.

      Beijing Institute of Geology for Mineral Resources, Beijing 100012, China

    • 3.

      Tianjin Center, China Geological Survey, Tianjin 300170, China

    • Received Date: 2020-01-24
    • Publish Date: 2020-11-15
      Abstract
    • Metasilicate mineral groundwater is widely distributed in basaltic area of Bashang area in North Hebei Province. It is of great significance to ascertain the formation mechanism and water-rock interaction process for the rational development and utilization of mineral water and the water conservation function of Beijing-Tianjin-Hebei region. Hydrochemical components statistical analysis, chemical weathering process of basaltic, mineral equilibrium phase of water-rock interaction process, δD, δ18O, δ13C isotopes and radioisotope dating by 14C were used to identify the geological construction constraints and ascertain the formation mechanism of metasilicate mineral groundwater. The results show that the mineral groundwater of study area is characterized by low mineralization while the main hydrochemical types of groundwater are HCO3- Ca·Mg and HCO3- Na·Ca. The outcropping mechanism of mineral water can be divided into two types:deep cyclic leaching of tectonic faults and stratified enrichment of recharge type. The age of groundwater in the upper paleoweathering crust is about 4 050 a, and the dissolved inorganic carbon of groundwater comes from the mixing of soil CO2 and mantle CO2. Metasilicic acid in groundwater originates from the weathering and hydrolysis of plagioclase, pyroxene and forsterite in basaltic. Hydrogeochemical response of rock weathering is controlled by rock mineral leaching and affected by hydrochemical parameters cation exchange. The formation and distribution of metasilicate mineral water are restricted by the basalt geological construction, and controlled by weathering mechanism of rocks and hydrogeochemical conditions.

       

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