Validation of the percolation‐based effective‐medium approximation model to estimate soil thermal conductivity DOI
Andres Patrignani, Behzad Ghanbarian, G. J. Kluitenberg

et al.

Soil Science Society of America Journal, Journal Year: 2023, Volume and Issue: 87(6), P. 1275 - 1284

Published: Aug. 8, 2023

Abstract Soil thermal conductivity (λ) has broad applications in soil science, hydrology, and engineering. In this study, we applied the percolation‐based effective‐medium approximation (P‐EMA) to estimate saturation dependence of () using data from 38 undisturbed samples collected across state Kansas. The P‐EMA model four parameters including a scaling exponent ( t s ), critical water content (θ c conductivities at oven‐dry (λ dry ) full sat conditions. To curve, values λ were measured properties analyzer θ estimated as function clay content. Thermal was also Johansen model. By comparison with observations, resulted root mean square error (RMSE) ranging 0.029 0.158 W m −1 K , whereas had an RMSE 0.021 0.173 . Our results demonstrate that comparable accuracy widely used saturation‐dependent soils minimal input parameters. Future studies should focus on better understanding physical meaning improve our ability percolation principles.

Language: Английский

Generalized model for predicting the thermal conductivity of fine-grained soils DOI
Huayang Lei,

Yu Bo,

Lei Wang

et al.

Geothermics, Journal Year: 2023, Volume and Issue: 113, P. 102752 - 102752

Published: May 29, 2023

Language: Английский

Citations

6

Experimental study and three-dimensional visualization model on the thermal conductivity of unsaturated frozen soil based on nuclear magnetic resonance DOI
Zhifeng Ren, Haiqiang Jiang, Jiankun Liu

et al.

Acta Geotechnica, Journal Year: 2023, Volume and Issue: 19(6), P. 3925 - 3938

Published: Oct. 26, 2023

Language: Английский

Citations

6

Experimental Study and Simulation of Thermal Conductivity of Saturated Frozen Soil DOI
Zhifeng Ren, Enliang Wang, Jiankun Liu

et al.

Journal of Thermal Science and Engineering Applications, Journal Year: 2023, Volume and Issue: 15(11)

Published: July 18, 2023

Abstract The aim of this study was to enhance the accuracy predicting temperature field frozen soil and reduce workload thermal parameter testing. To achieve this, we employed a three-phase model comprising soil, water, ice. unfrozen water content in at varying temperatures determined using nuclear magnetic resonance spectroscopy (NMR), while conductivity measured by characteristic analyzer. A matlab software-based random then established imported into COMSOL simulation software. repeatability reproducibility were verified proportions pore ice determine degree accuracy.The results demonstrated that maintained dynamic equilibrium relationship with temperature, which influenced soil. consistent those obtained from instrument measurements trends respect temperature. average PBIAS value between calculated values 0.0139, indicating theoretical feasibility. Comparison experimental data confirmed effectiveness our approach, providing novel concept simple method for engineering areas experience seasonal freezing.

Language: Английский

Citations

4

Assessment of thermal conductivity prediction models for compacted bentonite-based backfill material DOI
Pawan Kishor Sah, Shiv Shankar Kumar

International Journal of Environmental Science and Technology, Journal Year: 2024, Volume and Issue: 22(6), P. 4571 - 4582

Published: Aug. 22, 2024

Language: Английский

Citations

1

Validation of the percolation‐based effective‐medium approximation model to estimate soil thermal conductivity DOI
Andres Patrignani, Behzad Ghanbarian, G. J. Kluitenberg

et al.

Soil Science Society of America Journal, Journal Year: 2023, Volume and Issue: 87(6), P. 1275 - 1284

Published: Aug. 8, 2023

Abstract Soil thermal conductivity (λ) has broad applications in soil science, hydrology, and engineering. In this study, we applied the percolation‐based effective‐medium approximation (P‐EMA) to estimate saturation dependence of () using data from 38 undisturbed samples collected across state Kansas. The P‐EMA model four parameters including a scaling exponent ( t s ), critical water content (θ c conductivities at oven‐dry (λ dry ) full sat conditions. To curve, values λ were measured properties analyzer θ estimated as function clay content. Thermal was also Johansen model. By comparison with observations, resulted root mean square error (RMSE) ranging 0.029 0.158 W m −1 K , whereas had an RMSE 0.021 0.173 . Our results demonstrate that comparable accuracy widely used saturation‐dependent soils minimal input parameters. Future studies should focus on better understanding physical meaning improve our ability percolation principles.

Language: Английский

Citations

2