华北克拉通北缘典型高锶花岗岩区域锶型矿泉水分布特征及成因
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P641.6

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河北省地矿局科研项目(454-0601-YBN-VKK1)


Study on Distribution Characteristics of Strontium Mineral Water in the Typical high-Sr granitearea in the northern margin of the North China Craton
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    摘要:

    华北克拉通北缘存在大量高锶花岗岩体,但其周边区域锶型矿泉水的赋存情况鲜有研究。本文首次以都山岩体作为典型高锶花岗岩,通过水文地质调查、水样采集、化验分析等方法,对其周边区域锶型矿泉水的分布和形成机理进行了分析。同时对寿王坟岩体、碾子峪岩体、小寺沟岩体、杨杖子岩体等四处高锶花岗岩体周边区域水体进行调查取样分析,以验证锶型矿泉水的分布规律。研究表明,都山岩体周边区域水体中均含锶元素,且距离岩体越近,水样中锶含量越高,最高达13.81 mg/L,远高于国内一般含锶矿泉水的锶含量,而外围长城系砂岩地层水样中锶含量最低。平面上,孔隙水中锶型矿泉水主要沿北东-南西向断裂带和南部挤压带分布;风化带网状基岩裂隙水和构造基岩裂隙水中锶型矿泉水沿北东-南西向断裂带分布;垂向上,孔隙水、风化带网状基岩裂隙水、构造基岩裂隙水中锶含量依次增加。区内高锶花岗岩为矿泉水形成提供了物源,地下水径流过程中地层中锶的不断溶出是形成高锶型矿泉水的内在机制,垂向三含水层可能存在水力联系,入渗过程中锶含量可能不断累积。深层构造基岩裂隙水水质、水量稳定,锶含量高,极具开发利用价值。其它四处高锶花岗岩体周边区域锶型矿泉水的分布与都山岩体区域呈现类似规律。该研究首次揭露高锶花岗岩区域锶型矿泉水的赋存规律,可为众多高锶花岗岩区域开发利用优质锶型矿泉水资源提供参考借鉴。

    Abstract:

    There are a lot of high-Sr granite in the north margin of north China craton, however, the occurrence of strontium type mineral water in the surrounding areas is rarely studied. In this paper, the distribution and formation mechanism of strontium mineral water in the surrounding area of Dushan rock mass which as a typical high-Sr granite were analyzed for the first time by hydrogeological survey, water sample collection and laboratory analysis. At the same time, the water bodies in the surrounding areas of four high strontium granite bodies such as Shouwangfen, Nian-ziyu, Xiao-sigou and Yangzhangzi rock mass were investigated and sampled to verify the distribution law of strontium type mineral water. The results show that Sr element is contained in all the water bodies around the Dushan rock mass, and the closer it is to the rock mass, the higher the strontium content in the water sample is, up to 13.81 mg/L, far higher than the other strontium-containing mineral water in China. but the strontium content of the water sample which in the sandstone of Ch is the lowest. In the horizontal, the Sr-type mineral water in the pore water is distributed mainly along both the NE-SW fault zone and the southern compression zone, whereas that in the fissure water and the tectonic bedrock fissure water is distributed only along the NE-SW fault zone. In the vertical, the Sr-type content increases with the sequence of the pore water, the weathering fissure water of network bedrock and the fissure water of tectonic bedrock. The high Sr granite of this area provides the source of Sr content for the formation of Sr-type mineral water. The continuous dissolution of Sr in stratum during the runoff of groundwater is the inherent mechanism. Hydraulic connection may exist in the three vertical aquifers and Sr content may accumulate during the infiltration process. The stable quality and quantity of the fissure water of deep tectonic bedrock suggest the great value for development and utilization. The distribution of strontium mineral water in the surrounding areas of the other four high strontium granitic rocks shows a similar pattern to that of the Dushan rock mass area. This study reveals the occurrence law of strontium mineral water in high-Sr granite region for the first time,and the results provide reference for the development and utilization of high quality strontium mineral water resources in many high-Sr granites.

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刘硕,马百衡,翟星,等. 华北克拉通北缘典型高锶花岗岩区域锶型矿泉水分布特征及成因[J]. 科学技术与工程, 2021, 21(5): 1721-1729.
Liu Shuo, Ma Baiheng, Zhai Xing, et al. Study on Distribution Characteristics of Strontium Mineral Water in the Typical high-Sr granitearea in the northern margin of the North China Craton[J]. Science Technology and Engineering,2021,21(5):1721-1729.

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  • 收稿日期:2020-05-14
  • 最后修改日期:2020-12-03
  • 录用日期:2020-07-26
  • 在线发布日期: 2021-03-18
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