39 / 2021-11-11 10:53:53
A semi-empirical model for water inflow into the tunnel in fractured-rock aquifers considering non-Darcian flow
Fractured rock,Water inflow,Tunnel,Non-Darcian flow,Semi-empirical equation
全文待审
洪斌 刘 / 中国地质大学(武汉)
佳庆 周 / 中国地质大学(武汉)
  Water inflow into the tunnel is usually estimated by assuming the flow in here follows the linear Darcy’s law. However, fluid flow in fractured-rock aquifers is prone to deviate from the Darcy’s law and arise to nonlinear flow phenomena due to significant inertial losses. Such a non-Darcian effect is seldom considered when evaluating water inflow into the tunnel in fractured-rock aquifers. In this study, we investigated the analytical method for predicting water inflow into the tunnel considering non-Darcian effect. A series of numerical simulations for water inflow into the tunnel were conducted with varying key parameters, in framework of non-Dacian flow characterized by the Forchheimer law. Based on these numerical results and an ingenious parameter integration method, a semi-empirical model was proposed to predict the water inflow into the tunnel involving with non-Darcian effect. The semi-empirical model has incorporated the classic theoretical formula for predicting water inflow and the Forchheimer equation for describing the non-Darcian flow. This model has a concise expression satisfying the dimensional consistency, and can be successfully reduced to the classic formula under Darcy flow regime. The validity of this semi-empirical model has been confirmed by the numerical results, showing a high fidelity for predicting water inflow into the tunnel. By means of this proposed model, the necessity of considering non-Darcian effect during calculating water inflow was finally proved in a large number of real engineering cases, including a karst tunnel project with detailed engineering geological data. The proposed model and the method used in this study can provide a guidance for accurately predicting water inflow into the tunnel under a complex non-Darcian flow regime.

 
重要日期
  • 会议日期

    11月26日

    2021

    11月28日

    2021

  • 11月23日 2021

    初稿截稿日期

  • 11月30日 2021

    报告提交截止日期

  • 11月30日 2021

    注册截止日期

主办单位
国家自然科学基金委员会地球科学学部
国际工程地质与环境协会(IAEG)
中国地质大学(武汉)
湖北省巴东县人民政府
承办单位
湖北三峡库区地质灾害国家野外科学观测研究站
湖北省巴东人民政府
中国地质大学(武汉)工程学院
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