Citation: | WANG Milei, DOU Yanguang, ZOU Liang, XUE Biying, HU Rui, YUE Baojing, XU Gang, LIN Xi, LI Linsen. HYDROCHEMICAL CHARACTERISTICS OF GROUNDWATER AND GENESIS OF MINERAL WATER AT LAOSHAN MOUNTAIN AND SURROUNDING AREAS, QINGDAO[J]. Marine Geology Frontiers, 2021, 37(9): 17-24. doi: 10.16028/j.1009-2722.2021.126 |
The Laoshan Mountain and its surrounding areas are rich in mineral water under the joint control of structural faults and weathering granite crust. In this paper, 14 hydrogeological wells are selected from the area surrounding the Laoshan Mountain for revealing the hydrogeological characteristics and concerned problems. The main hydrogeological problems are concentrated in the middle and lower reaches of rivers where human activities are frequent and active. Both industrial and agricultural pollution leads to the excess of nitrate in groundwater, in addition to saltwater intrusion occurred in the nearshore areas. A mineral water well located in the weathered crust of granite was discovered this time in the Lanseguigu District. The groundwater in the well belongs to the type of HCO3·SO4-Ca·Na. The contents of strontium (Sr) and metasilicic acid (H2SiO3) of the groundwater are 0.66 and 25.49 mg/L respectively, which are both higher than the standard content for drinking natural mineral water. The formation of the mineral water is closely related to the geological environment of the Laoshan area and mineral compositions of surrounding rocks. The strontium-metasilicic acid mineral water is formed by the dissolution of strontium and silica from granite into water by a long term water-rock interaction. This discovery is significant and may provide a new mineral water producing area in the Laoshan region of Qingdao.
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The map showing the locations of wells SW01-SW14 and mineral water factories
Distribution of hydrogeological problems in the main urban area of Qingdao and Lanseguigu District
Piper diagrams of groundwater samples
Comparison of chemical elements content of samples SW01-SW14 and drinking natural mineral water standard (GB 8537—2018)[2]
Comparison of chemical elements content of sample SW12 and drinking natural mineral water standard (GB 8537—2018)[2]