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Thermo-osmosis effect in one dimensional half space consolidation

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Aktuelle Forschung in der Bodenmechanik 2013

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Zusammenfassung

In this paper, the thermo-poroelasticity theory fulfilling local thermal non-equilibrium condition (LTNE) is used to investigate the thermo-osmosis effect on one dimensional saturated poroelastic half space subjected to impact loadings. It has been reported in the literature that coupled flow known as thermo-osmosis by which flux is driven by temperature gradient, can significantly change the fluid flux in clay, argillaceous and many other porous materials whose permeability coefficients are very low. This study presents a mathematic model to investigate the coupled effect of thermo-osmosis in saturated porous medium. Analytical solutions of temperatures, pore pressure, stress, displacement and fluid flux are obtained by Laplace transform. Results for a typical clay are used to investigate the effect of thermo-osmosis. The effects of LTNE on temperatures, displacement and stress are also studied in this paper.

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Literaturverzeichnis

  1. Carnahan C L (1984). Thermodynamic coupling of heat and matter flows in near-field regions of nuclear waste repositiries. In: Scientific Basis for Nuclear Waste Management VII.:1023–1030

    Google Scholar 

  2. Srivastava R C, Avasthi P K (1975). Non-equilibrium thermodynamics of thermo-osmosis of water through kaolinite. J. Hydrol 24:111–120

    Article  Google Scholar 

  3. Hueckel T, Pellegrini R (1992). Effective stress and water pressure in saturated clays during heating-cooling cycles. Canadian Geotechnical Journal 29:1095–1120

    Article  Google Scholar 

  4. Letey J, Kemper W D (1969). Movement of water and salt through a clay-water system: experimental vertification of Onsager’s reciprocal relation. In: Soil Sci. Soc. Am. Proc 33:25–29

    Article  Google Scholar 

  5. McVay D (1984). Scientific Basis for Nuclear Waste Management VII. Elsevier Science Pub. Co, North-Holland

    Google Scholar 

  6. McTigue D (1990). Flow to a heated borehole in porous, thermoelastic rock: analysis. Water Resour. Res. 26:1763–1774

    Article  Google Scholar 

  7. Liu G B (2010). Mode of a spherical cavity’s thermo-elastodynamic response in a saturated porous medium for non-torsional loads. Computers and Geotechnics 37:381–390

    Article  Google Scholar 

  8. Small J C, Booker J R (1986). The behaviour of layered soil or rock containing a decaying heat source. Int. J. Numer Anal. Methods Geomech. 10:501–519

    Article  Google Scholar 

  9. Rajapakse, Senjuntichai(1985). Exact stiffness method for quasi-static of a multilayered poroelastic medium. International journal of solids and structures 32:1535–1553

    Google Scholar 

  10. Bai M, Abousleiman Y (1997). Thermoporoelastic coupling with application to consolidation. Int. J. Numer. Methods. Geomech. 21:121–132

    Google Scholar 

  11. Giroud A F(1998). Thermoelastic and thermoplastic response of a double-layer porous space containing a decaying heat source. Int. J. Numer Anal. Methods. Geomech. 22:133–149

    Article  Google Scholar 

  12. He L W, Jin Z H (2011). Effects of local thermal non-equilibrium on the pore pressure and thermal stresses around a spherical cavity in a porous medium. International journal of engineering science 49:240–252

    Article  Google Scholar 

  13. Nield D A (1998). Effect of local thermal nonequilibrium in steady convection processes in saturated porous media: Forced convection in a channel. Journal of porous media. 1:181–186

    Google Scholar 

  14. Nield D A, Bejan A (2006). Convection in porous media(3rd ed). Springer, Berlin

    Google Scholar 

  15. Durbin F (1974). Numerical inversion of laplace transformation: an efficient improvement to Durbin and Abate’s method. Comp. J. 17:371–376

    Article  Google Scholar 

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Author information

Authors and Affiliations

  1. Bochum, Deutschland

    Yang Yang & Tom Schanz

Authors
  1. Yang Yang
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  2. Tom Schanz
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Correspondence to Yang Yang .

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Editors and Affiliations

  1. Fakultät für Bau- und Umweltingenieurwissenschaften, Ruhr-Universität Bochum, Bochum, Germany

    Tom Schanz

  2. Fakultät Architektur und Bauingenieurwesen, TU Dortmund, Dortmund, Germany

    Achim Hettler

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Yang, Y., Schanz, T. (2014). Thermo-osmosis effect in one dimensional half space consolidation. In: Schanz, T., Hettler, A. (eds) Aktuelle Forschung in der Bodenmechanik 2013. Springer Vieweg, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-37542-2_6

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