Abstract
It has been long recognised that some of the fundamental and engineering properties of soils exhibit a certain degree of anisotropy that eventually dictates their directional geoengineering behaviours. Consideration of the importance of the volume change behaviour of soils during shrinkage and a critical review of the literature suggests scopes for further research for the development of a better understanding of the anisotropy in volume change encountered during soil shrinkage. In this paper, anisotropy in volumetric shrinkage behaviour of soil is depicted with the theory of geometry factor and shrinkage strains. A systematic investigation and analysis on the evolution of geometry factors and shrinkage strains of several geomaterial samples during evaporative dewatering is reported herein. A theoretical framework for evaluating shrinkage geometry factors of a cylindrical soil specimen undergoing volume change during progressive moisture loss is described in this paper. Furthermore, based on experimental and literature data, shrinkage geometry factors of several specimens differing in terms of gradational properties, specimen size, evaporative boundary condition and pore fluid salinity are evaluated and discussed in detail in accordance with the theoretical framework. Linkages between shrinkage process, shrinkages strains and geometry factor are also analysed to underpin the usage of geometry factor and shrinkage strains to characterise anisotropy during soil shrinkage.
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Abbreviations
- α, β, n, m :
-
Parameters in the model by Kim et al. [19]
- εd/εv, RDS:
-
Relative diametrical strain
- ε d :
-
Diametrical strain
- Δd :
-
Change in specimen diameter
- Δh :
-
Change in specimen height
- ε l :
-
Longitudinal strain
- εl/εv, RLS:
-
Relative longitudinal strain
- ε v :
-
Volumetric strain
- A,p :
-
Parameters in the model by Sabnis et al. [43]
- d :
-
Specimen diameter at a given time
- d 0 :
-
Initial specimen diameter
- GMC:
-
Gravimetric moisture content
- h :
-
Specimen height at a given time
- h 0 :
-
Initial specimen height
- NMCOMC :
-
Normalised moisture content with respect to optimum moisture content
- POB:
-
Dredged mud sample from port of Brisbane reclamation site
- r s :
-
Static geometry factor
- \( r_{\text{s}}^{\prime } \) :
-
Representative static geometry factor
- r sd :
-
Static geometry factor corresponding to diametrical shrinkage
- r sl :
-
Static geometry factor corresponding to vertical shrinkage
- S s :
-
Shrinkage strain
- SLGE :
-
Shrinkage limit as defined in geotechnical engineering
- SSCC:
-
Soil shrinkage characteristic curve
- V :
-
Specimen volume at a given time
- V 0 :
-
Initial specimen volume
- w :
-
Gravimetric moisture content of the specimen at a given time
- w 0 :
-
Gravimetric moisture content of the specimen initially
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Acknowledgements
This work was funded by scholarship supports through ‘Australian Government Research Training Program Scholarship’ (Formerly ‘International Postgraduate Research Scholarship’), UQ Centennial Scholarship (The University of Queensland) and Top up scholarship (School of Civil Engineering, The University of Queensland) awarded to Mr. P.N. Mishra. The support through the Port of Brisbane/UQ research venture is gratefully acknowledged. We also thank the anonymous reviewers for their time and suggestions to improve the manuscript.
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Mishra, P.N., Zhang, Y., Bhuyan, M.H. et al. Anisotropy in volume change behaviour of soils during shrinkage. Acta Geotech. 15, 3399–3414 (2020). https://doi.org/10.1007/s11440-020-01015-6
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DOI: https://doi.org/10.1007/s11440-020-01015-6