Volume 9 Issue 3
Jul.  2016
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Eduardo E. Alonso, Núria M. Pinyol. 2016: Numerical analysis of rapid drawdown: Applications in real cases. Water Science and Engineering, 9(3): 175-182. doi: 10.1016/j.wse.2016.11.003
Citation: Eduardo E. Alonso, Núria M. Pinyol. 2016: Numerical analysis of rapid drawdown: Applications in real cases. Water Science and Engineering, 9(3): 175-182. doi: 10.1016/j.wse.2016.11.003

Numerical analysis of rapid drawdown: Applications in real cases

doi: 10.1016/j.wse.2016.11.003
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  • Corresponding author: Eduardo E. Alonso
  • Received Date: 2015-09-02
  • Rev Recd Date: 2016-06-12
  • In this paper, the rapid drawdown scenario is analyzed by means of numerical examples as well as modeling of real cases with in situ measurements. The aim of the study is to evaluate different approaches available for calculating pore water pressure distributions during and after a drawdown. To do that, a single slope subjected to a drawdown is first analyzed under different calculation alternatives, and numerical results are discussed. Simple methods, such as the undrained analysis and pure flow analysis, implicitly assuming a rigid soil skeleton, lead to significant errors in pore water pressure distributions when compared with the coupled flow-deformation analysis. In the second case study, a similar analysis is performed for the upstream slope of the Glen Shira Dam, Scotland, and numerical results are compared with field measurements during a controlled drawdown. Field records indicate that classical undrained calculations are conservative but unrealistic. Then, a recent case of a major landslide triggered by a rapid drawdown in a reservoir is interpreted. A key aspect of the case is the correct characterization of permeability of a representative soil profile. This is achieved by combining laboratory test results and a back analysis of pore water pressure time records during a period of reservoir water level fluctuations. The results highlight the difficulty of predicting whether the pore water pressure is overestimated or underestimated when using simplified approaches, and it is concluded that predicting the pore water pressure distribution in a slope after rapid drawdown requires a coupled flow-deformation analysis in saturated and unsaturated porous media.

     

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