Skip to main content
Log in

Influence of Fine Content on the Soil–Water Characteristic Curve of Unsaturated Soils

  • Original Paper
  • Published:
Geotechnical and Geological Engineering Aims and scope Submit manuscript

Abstract

Unsaturated soils often exist as a mixture of coarse and fine particles in nature. However, the relationship between fine content and the soil–water characteristic curve (SWCC) is not sufficiently understood. In this paper, ten kinds of mixed soils with different percentages of fine contents were tested with the pressure-membrane apparatus, and the SWCC for each fine content was obtained. The results showed that when keeping the fine content between 10 and 60%, the water-holding capacity of the soil gradually decreased as the fine content increased. Otherwise, the water-holding capacity of the soil increased. With the same effect of matrix suction, the volumetric water content increased initially and then decreased with the increase of fine content. With the fine content within the range of 10–60%, a higher fine content resulted in a larger dehydration rate; otherwise, the dehydration rate of the soil decreased. In addition, a new fitting model was established for SWCC. The applicability of the new model was verified by combining new data with the existing experimental data and then discussing the physical meaning of each parameter in the model. Through the research in this paper, the quantitative relationship between fine content and SWCC was clarified, and a new SWCC model was established. The conclusions in this paper are helpful to understand the effect of the proportion of fine particles on the SWCC. The physical parameters of unsaturated soils which mixes fine and coarse particles, such as adsorption coefficient, permeability coefficient, and shear strength, could be obtained.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11

Similar content being viewed by others

References

  • Brooks RH (1964) Properties of porous media affecting fluid flow. Irrigation Draining Division ASCE 92(2):61–88

    Google Scholar 

  • Brooks RH, Corey AT (1964) Hydraulic properties of porous media. Hydrol Pap 3(1):352–366

    Google Scholar 

  • Chen YL, Huang D (2017) Influence of pore structure characteristics on soil–water characteristic curves under different stress states. Chin J Eng 39(1):147–154 (in Chinese)

    Google Scholar 

  • Dang FN, Liu HW, Wang X, Xue HB, Ma ZY (2015) Empirical formulas of permeability of clay based on effective pore ratio. Chin J Rock Mechan Eng 34(9):1909–1917 (in Chinese)

    Google Scholar 

  • Fredlund DG (2012) Unsaturated soil mechanics in engineering practice. Wiley, Hoboken, pp 286–321

    Book  Google Scholar 

  • Fredlund DG, Xing A (1994) Equations for the soil–water characteristic curve. Can Geotech J 31(4):521–532

    Article  Google Scholar 

  • Gardner WR (1958) Some steady-state solutions of the unsaturated moisture flow equation with application to evaporation from a water table. Soil Sci 85(4):228–232

    Article  Google Scholar 

  • Genuchten MTV (1980) A closed-form equation for predicting the hydraulic conductivity of unsaturated soils. Soil Sci Soc Am J 44(5):892–898

    Article  Google Scholar 

  • Kawai K, Kato S, Karube D, Rahardjo H, Toll DG, Leong EC (2000) The model of water retention curve considering effects of void ratio, unsaturated soils for Asia. In: Proceedings of the Asian conference on unsaturated soils, Unsat-Asia, Singapore, 18–19, May

  • Kong L, Sayem MHM, Tian H (2017) Influence of drying-wetting cycles on soil–water characteristic curve. Can Geotech J 55(2):208–216

    Article  Google Scholar 

  • Lim PC, Barbour SL, Fredlund DG (1998) The influence of degree of saturation on the coefficient of aqueous diffusion. Can Geotech J 35(5):811–827

    Article  Google Scholar 

  • Liu FY, Zhao Z, Zhou D, Zhao XG, Zhu L (2011) Effects of initial density and drying-wetting cycle on soil water characteristic curve of unsaturated loess. Rock Soil Mech 32:132–136 (in Chinese)

    Google Scholar 

  • Luo QX, Huang J, Chen Q (2014) Influence of vertical stress and dry density on soil–water characteristic curve of gravelly soil. Rock Soil Mech 35(3):729–734 (in Chinese)

    Google Scholar 

  • Luo XY, Liu WP, Fu MF (2016) Effects of gradation and vertical stress on soil–water characteristic curve in collapsing erosion area. J Southeast Univ 46(1):235–240 (in Chinese)

    Google Scholar 

  • Tan L, Wei C, Tian H, Wang H, Zhang Q, Invamp SP (2017) Experimental study on characteristics of pore water distribution and water-holding capacity of soil. J Eng Geol 25(1):73–79 (in Chinese)

    Google Scholar 

  • Vanapalli SK, Fredlund DG, Pufahl DE (1999) The influence of soil structure and stress history on the soil–water characteristics of a compacted till. Géotechnique 51(6):573–576

    Article  Google Scholar 

  • Wang DL, Luan MT, Yang Q (2009) Experimental study of SWCC of remolded unsaturated clay. Rock Soil Mech 30(3):751–756 (in Chinese)

    Google Scholar 

  • Xu YF, Sun DA (2001) Determination on of expansive soil strength using a fractal model. Fractals Complex Geom Patterns Scaling Nat Soc 9(1):51–60

    Google Scholar 

  • Zhang XD, Zhao CG, Cai GQ, Liu Y (2010) Research on influence of soil density on soil-water characteristic curve. Rock Soil Mech 31(5):1463–1468 (in Chinese)

    Google Scholar 

  • Zheng JL, Liu P (2006) A study on soil water characteristic curve of expansive soil. J Chang Commun Univ 22(4):1–5 (in Chinese)

    Google Scholar 

  • Zhou J, Yu JL (2005) Influences affecting the soil–water characteristic curve. J Zhejiang Univ Sci A (Appl Phys Eng) 6(8):797–804

    Article  Google Scholar 

Download references

Acknowledgements

The authors acknowledge financial support provided by The National Natural Science Foundation of China (No. 41807289) and Sichuan province fundamental scientific research (No. 18ZA0374).

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Xiangang Jiang.

Additional information

Publisher's Note

Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Jiang, X., Wu, L. & Wei, Y. Influence of Fine Content on the Soil–Water Characteristic Curve of Unsaturated Soils. Geotech Geol Eng 38, 1371–1378 (2020). https://doi.org/10.1007/s10706-019-01096-5

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s10706-019-01096-5

Keywords

Navigation