Abstract
Geomaterials tend to be stratified due to the geological process, and their properties are often anisotropic. In this study, the quartet structure generation set (QSGS) method is adopted to reconstruct the mesoscale internal structure of anisotropic geomaterials. In addition, the fractal theory and several morphological parameters are employed to describe the structural features of anisotropic geomaterials. The effective thermal properties parallel and perpendicular to the layered structure are evaluated via the finite element method coupled with Monte Carlo simulations. A representative volume element of anisotropic geomaterials is determined by the homogenization method. The importance of morphological parameters is ranked by Pearson correlation coefficient. Results indicate that the porosity and arrangements of solid fabric have significant influences on thermal conductivity and its anisotropy. Prediction models for assessing the orthogonal thermal conductivities and anisotropic ratio are established, and their performances are benchmarked against the finite element analysis results. The results obtained from this work can provide a reference for the investigation of anisotropy of geomaterials properties and a link between effective thermal properties and features of the internal structure.
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Abbreviations
- A :
-
Area of each solid cluster
- a :
-
Major axis of an ellipse
- b :
-
Minor axis of an ellipse
- C :
-
Boundary length of a solid cluster
- C d :
-
Distribution probability of solid core
- D e :
-
Equivalent diameter of a solid cluster
- D f :
-
Fractal dimension
- D m :
-
Mass fractal dimension
- D s :
-
Surface fractal dimension
- d :
-
Length of a grid cell
- F max :
-
Maximum Feret diameter
- F min :
-
Minimum Feret diameter
- k :
-
Thermal conductivity
- k a :
-
Thermal conductivity of air
- k eff :
-
Effective thermal conductivity
- k s :
-
Thermal conductivity of solid
- k x :
-
Thermal conductivity along x-direction
- k y :
-
Thermal conductivity along y-direction
- k 0 :
-
Geometric mean value of ks and ka
- L m :
-
Length of an object at macroscale
- L :
-
Length of an object at mesoscale
- m :
-
Number of data points of each variable
- M(ε):
-
Measurement of a fractal subject in fractal theory
- N :
-
Shape function
- n :
-
Porosity
- P i :
-
Growth probability of solid along i-direction (i = 1, 2, 3, 4, 5, 6, 7, 8)
- q :
-
Heat flux density
- r k :
-
Anisotropy ratio of thermal conductivity
- T :
-
Temperature
- x i :
-
ith data points of variable x
- \(\overline{x}\) :
-
Mean values of variable x
- \(\overline{{x_{\max ,i} }}\) :
-
Average solid length along x-direction
- y i :
-
ith data points of variable y
- \(\overline{y}\) :
-
Mean values of variable y
- \(\overline{{y_{\max ,j} }}\) :
-
Average solid length along y-direction
- Y :
-
Ratio of P1 to P2
- Y 1 :
-
Average value of the aspect ratio of solid cluster
- Y 2 :
-
Anisotropy of solid cluster
- ε :
-
Length scale in fractal theory
- ρ :
-
Value of Pearson correlation coefficient
- Γ:
-
Boundary of simulated domain
- Ω:
-
Simulated domain
- FEM:
-
Finite element method
- LSM:
-
Least square method
- MCS:
-
Monte Carlo simulation
- PCC:
-
Pearson correlation coefficient
- QSGS:
-
Quartet structure generation set
- RMSE:
-
Root mean squared error
- RVE:
-
Representative volume element
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Acknowledgements
This research is supported by the National Natural Science Foundation of China (Grant Nos. 51879203; 52079099).
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Li, KQ., Miao, Z., Li, DQ. et al. Effect of mesoscale internal structure on effective thermal conductivity of anisotropic geomaterials. Acta Geotech. 17, 3553–3566 (2022). https://doi.org/10.1007/s11440-022-01458-z
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DOI: https://doi.org/10.1007/s11440-022-01458-z