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渗透系数各向异性对地下水封洞室涌水量影响的数值模拟分析
Effect analysis of hydraulic conductivity anisotropy on hydraulic discharge of groundwater sealed caverns using numerical simulation method
【Author】 Zhou Pengpeng~1,Li Guomin~1,Shi Jingxi~2,Shi Gongyu~2,Wu Runjian~1 (1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China; 2.Beijing Feiyan Petrochemical Enviromental Protection Technology Development CO.,LTD,Beijing 102500,China)
【机构】 中国科学院地质与地球物理研究所; 北京飞燕石化环保科技发展有限公司;
【摘要】 为了分析洞室涌水量,本文运用数值模拟技术建立了研究区地下水的三维数值模型。在模型中综合考虑了基岩裂隙含水介质渗透系数(K)的各向异性,应用水均衡计算分析了不同K_v/K_h比值条件对洞室涌水量的影响。结果表明:随着K_v/K_h比值增加,洞室涌水量也相应有所增加;K_v/K_h比值的变化对洞室涌水量的变化趋势影响不明显;不同K_v/K_h比值条件下,初期涌水量平均增加速率较为一致,而后随着时间的推移,增加速率出现分异,K_v/K_h比值越大,涌水量增加速率越小;运营期K_v/K_h比值的增加对涌水量的影响较施工期明显。
【Abstract】 To analyse the hydraulic discharge of groundwater sealed caverns,the study area as a three-dimensional groundwater flow model using numerical simulation method is created.In the model,the hydraulic conductivity anisotropy of fissure aquifer medium is comprehensively considered and the influence of different K_v/K_h ratios to the hydraulic discharge of the caverns through analyzing water equilibrium is analyzed.The results reveals that the hydraulic discharge of the caverns increases with the increase of the K_v/K_h ratio;the variation of the K_v /K_h ratio has little effect to the trend of the hydraulic discharge;under different K_v/K_h ratio conditions,the average increase rate of hydraulic discharge in early time is more consistent.Then,the increase rate of different K_v/K_h ratio conditions becomes different.The larger the K_v/K_h ratio is,the smaller the average increase rate of hydraulic discharge is.The influence of K_v/K_h ratio increasing in operation period is more obvious than that in excavating period.
- 【会议录名称】 中国科学院地质与地球物理研究所第11届(2011年度)学术年会论文集(中)
- 【会议名称】中国科学院地质与地球物理研究所第11届(2011年度)学术年会
- 【会议时间】2012-01-05
- 【会议地点】中国北京
- 【分类号】P641
- 【主办单位】中国科学院地质与地球物理研究所