Influence of Initial Conditions on Unsaturated Groundwater Flow Models

  • Authors

    • Aizat Mohd Taib
    • Mohd Raihan Taha
    • Dayang Zulaika Abang Hasbollah
    2019-01-30
    https://doi.org/10.14419/ijet.v8i1.2.24868
  • rainfall, groundwater flow, unsaturated soils,
  • Slope failure in unsaturated soils is common in tropical countries due to the seasonal pattern of abundant rainfall preceding a period of prolonged drying. Much research has been undertaken to understand the behaviour of unsaturated slopes and reduce the number of catastrophic failures. The initial conditions are important factors in numerical modelling of the groundwater flow yet rarely considered in detail in the literature. This paper presents a parametric study of the initial conditions at a slope in Bukit Timah, Singapore. The intensity and duration of rainfall are varied to assess the effect on the pore-water pressure in the slope. The generated pore-water pressure profile is compared with field measurements and previous numerical studies. It is discovered that a low rainfall, with an intensity of 1x10-7 m/s over a period of 62 days, results in initial pore-water pressure which is consistent with data recorded at the field. Unlike the duration, changes in the rainfall intensity are shown to have a significant effect on the pore-water pressure in the slope. This study, therefore, demonstrates the importance of determining appropriate initial conditions in unsaturated groundwater flow analysis.

     

     


     
  • References

    1. [1] Toll DG (2001), Rainfall-induced landslides in Singapore. Geotechnical Engineering, 149(4), 211-216.

      [2] Tsaparas I, Rahardjo H, Toll DG, and Leong EC (2002), Controlling parameters for rainfall-induced landslides. Computers and Geotechnics, 29(1), 1-27.

      [3] Oh S and Lu N (2015), Slope stability analysis under unsaturated conditions: Case studies of rainfall-induced failure of cut slopes. Engineering Geology, 184, 96-103.

      [4] Zhang LL, Fredlund DG, Fredlund MD, and Wilson GW (2014), Modeling the unsaturated soil zone in slope stability analysis. Canadian Geotechnical Journal, 51(12), 1384-1398.

      [5] Zhang LL, Fredlund DG, Zhang LM, and Tang WH (2004), Numerical study of soil conditions under which matric suction can be maintained. Canadian Geotechnical Journal, 41(4), 569-582.

      [6] Van Genuchten MT (1980), A closed-form equation for predicting the hydraulic conductivity of unsaturated soils. Soil Science Society of America Journal, 44(5), 892-898.

      [7] Fredlund DG & Xing A (1994), Equations for the soil-water characteristic curve. Canadian Geotechnical Journal, 31(3), 521-532.

      [8] Leong EC & Rahardjo H (1997), Review of soil-water characteristic curve equations. Journal of geotechnical and geoenvironmental engineering, 123(12), 1106-1117.

      [9] Leong EC and Rahardjo H, 1997. Permeability functions for unsaturated soils. Journal of Geotechnical and Geoenvironmental Engineering, 123(12), 1118-1126.

      [10] Childs EC & Collis-George N, "The permeability of porous materials", Proceedings of the Royal Society of London. Series A, Mathematical and Physical Sciences, (1950), 201(1066), 392-405.

      [11] Marshall TJ (1958), A relation between permeability and size distribution of pores. Journal of Soil Science, 9(1), 1-8.

      [12] Galavi V, Groundwater flow, fully coupled flow deformation and undrained analyses in PLAXIS 2D and 3D. 2010, Plaxis BV.

      [13] Plaxis, Scientific manual. 2012.

      [14] Plaxis, Material models manual. 2012.

      [15] Rahardjo H, Santoso VA, Leong EC, Ng YS, and Hua CJ (2011), Numerical analyses and monitoring performance of residual soil slopes. Soils and foundations, 51(3), 471-482.

      [16] GeoSlope IL, SEEP/W user's guide for finite element seepage analysis, (2004), GEO-SLOPE International Ltd, Calgary, Alta.

      [17] Kristo C, Rahardjo H, and Satyanaga A (2017), Effect of variations in rainfall intensity on slope stability in Singapore. International Soil and Water Conservation Research, 5(4), 258-264.

      [18] Jeong S, Kim J, and Lee K, Effect of clay content on well-graded sands due to infiltration. Vol. 102. 2008. 74-81.

      [19] Ng CW, Wang B, and Tung YK (2001), Three-dimensional numerical investigations of groundwater responses in an unsaturated slope subjected to various rainfall patterns. Canadian Geotechnical Journal, 38(5), 1049-1062.

  • Downloads

  • How to Cite

    Mohd Taib, A., Raihan Taha, M., & Zulaika Abang Hasbollah, D. (2019). Influence of Initial Conditions on Unsaturated Groundwater Flow Models. International Journal of Engineering & Technology, 8(1.2), 34-40. https://doi.org/10.14419/ijet.v8i1.2.24868