Abstract:Research purposes: Water inrush is a major engineering hazard in karst water-rich tunnels, and its research is of great practical significance. Based on a total of 7 surface water samples and 35 groundwater samples, collected from Xiangyang Tunnel for hydrochemical analysis, this study takes Xiangyang Tunnel as an example to investigate the mechanism of water inrush in deep and long tunnels in karst mountainous areas in Southwest China and provides a scientific basis for the prevention and control of water inrush in karst tunnels along this route. Research conclusions: (1) The hydrochemical types of water samples in the tunnel area are mainly HCO3-Ca, with weak alkaline and low mineralization. The chemical properties of surface water and groundwater are similar, and the hydraulic connection is close. (2) The hydrochemical composition is mainly affected by the weathering and dissolution of silicate and carbonate rocks, as well as cation exchange. (3) The Ca2+ and Mg2+ in groundwater and surface water mainly come from the dissolution of calcite and dolomite in limestone dolomite, and the weathering of feldspar minerals in clastic sandstone. (4) Na+ comes from atmospheric precipitation and the weathering of silicates. (5) Carbonate minerals plays a dominant role in rock weathering and dissolution. (6) The research results can provide reference for the design of tunnel lines in karst areas.
裴建国,梁茂珍,陈阵. 西南岩溶石山地区岩溶地下水系统划分及其主要特征值统计[J]. 中国岩溶, 2008(1): 6-10.Pei Jianguo, Liang Maozhen, Chen Zhen.Classification of Karst Groundwater System and Statistics of the Main Characteristic Values in Southwest China Karst Mountain[J].Carsologica Sinica, 2008(1):6-10.
[2]
吴华英,李腾芳,程瑞瑞,等. 我国岩溶地下水受污染的原因与污染特征[J]. 中国矿业, 2021(S1): 101-104.Wu Huaying, Li Tengfang, Cheng Ruirui, etc. Causes and Characteristics of the Pollution of Karst Groundwater in China[J].China Mining Magazine, 2021(S1): 101-104.
[3]
林云,娄亚南,武亚遵,等. 华蓥山隧道隧址区水文地球化学特征及涌水来源识别[J]. 水资源与水工程学报,2017(5): 43-48.Lin Yun,Lou Yanan,Wu Yazun,etc. Hydrogeochemical Characteristics and Identification of Water Source in Huayingshan Tunnel District[J].Journal of Water Resources and Water Engineering, 2017(5): 43-48.
[4]
Li H, Kagami H.Groundwater Level and Chemistry Changes Resulting From Tunnel Construction Near Matsumoto City, Japan[J].Environmental Geology, 1997(1-2):76-84.
[5]
陈鹏. 贵州省董当隧道岩溶区水文地质特征研究[J].资源信息与工程,2022(2):23-25.Chen Peng.The Hydrogeological Features of Dongdang Tunnel Karst Zone, Guizhou Province[J]. Resource Information and Engineering, 2022(2): 23-25.
[6]
Arthur M Piper.A Graphic Procedure in the Geochemical Interpretation of Water‐analyses[J]. Eos, Transactions American Geophysical Union, 1944(6): 914-928.
[7]
袁兴成, 张云辉, 王鹰, 等.鲜水河断裂带地热水化学特征及结垢趋势分析[J]. 沉积与特提斯地质, 2023(2): 357-372.Yuan Xingcheng, Zhang Yunhui, Wang Ying, etc. Geothermal Water Chemical Characteristics and Scaling Analysis of Xianshuihe Fault Zone[J]. Sedimentary Geology and Tethyan Geology,2023(2):357-372.
[8]
杨艳林,靖晶,齐信,等.赣州北部丘陵山区浅层地下水化学特征及成因分析[J].中国地质调查,2023(6): 60-68.Yang Yanlin, Jing Jing, Qi Xin, etc. Hydrochemical Characteristics and Formation Mechanism of Shallow Groundwater in the Northern Hilly Region of Ganzhou[J]. Geological Survey of China, 2023(6): 60-68.