Technical Notes
Mar 2, 2022

Piecewise-Linear Model for Large-Strain Consolidation with Threshold Hydraulic Gradient

Publication: International Journal of Geomechanics
Volume 22, Issue 5

Abstract

Experimental studies found that water flow in clay might not obey Darcy’s law. In some fine-grained soils, the water flow could occur only when the threshold gradient was exceeded. This study investigates the effects of threshold gradient on the consolidation profile. The well-established model CNDF2 is employed with some modifications. Verification examples demonstrate the accuracy of the numerical simulation in this study. Compared with the existing solution in the literature, modeling results in this study are more reliable because the criterion of seepage is independent of the position of the seepage front. Parametric studies find that the excess pore-water pressure cannot be fully dissipated if there is a threshold gradient. A larger value of normalized threshold hydraulic gradient R will result in a larger value of residual excess pore-water pressure. A permeable bottom boundary can contribute to the dissipation of residual excess pore-water pressure. The final settlement will also be affected by the threshold hydraulic gradient. A larger value of R will lead to a smaller final settlement due to the residual excess pore-water pressure. The average degree of consolidation will not be affected by the threshold hydraulic gradient.

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Data Availability Statement

All data, models, or codes that support the findings of this study are available from the corresponding author upon reasonable request.
This research is supported by the National Key R&D Program of China (Grant No. 2016YFC0800200) and the National Natural Science Foundation of China (Grant Nos. 51878313 and 52078236), and the support is gratefully acknowledged.

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Go to International Journal of Geomechanics
International Journal of Geomechanics
Volume 22Issue 5May 2022

History

Received: Feb 1, 2021
Accepted: Dec 19, 2021
Published online: Mar 2, 2022
Published in print: May 1, 2022
Discussion open until: Aug 2, 2022

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Authors

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Ph.D. Candidate, Institute of Geotechnical and Underground Engineering, Huazhong Univ. of Science and Technology, Wuhan 430074, China. ORCID: https://orcid.org/0000-0003-0990-4084.
Professor, Institute of Geotechnical and Underground Engineering, Huazhong Univ. of Science and Technology, Wuhan 430074, China (corresponding author). ORCID: https://orcid.org/0000-0001-9679-4914. Email: [email protected]
X. D. Zhao
Former Research Student, Institute of Geotechnical and Underground Engineering, Huazhong Univ. of Science and Technology, Wuhan 430074, China.
Jia-Tai Lu
Research Student, Institute of Geotechnical and Underground Engineering, Huazhong Univ. of Science and Technology, Wuhan 430074, China.
Zhan-Fang Huang
Associate Professor, School of Construction Engineering, Shandong Univ. of Technology, Zibo 255000, China.

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Cited by

  • Fully Coupled Model for One-Dimensional Large-Strain Consolidation and Heat Conduction in Saturated Clay, Journal of Engineering Mechanics, 10.1061/JENMDT.EMENG-6852, 149, 4, (2023).
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  • General analytical solutions for one-dimensional large strain consolidation of soft soils under electro-osmosis–surcharge preloading, Soils and Foundations, 10.1016/j.sandf.2022.101211, 62, 5, (101211), (2022).

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