Modeling Heat Transfer through Permafrost Soil Subjected to Seasonal Freeze-Thaw
The present paper proposes an iterative implicit numerical method for simulating the thaw depth of permafrost soil. For this purpose, the enthalpy-porosity model was used for the phase change process, and the finite difference scheme FTCS (Forward Time Centered Space) was used for discretization. An...
Main Authors: | Alain Lubini Tshumuka, Abdelkader Krimi, Musandji Fuamba |
---|---|
Format: | Article |
Language: | English |
Published: |
MDPI AG
2022-10-01
|
Series: | Land |
Subjects: | |
Online Access: | https://www.mdpi.com/2073-445X/11/10/1770 |
Similar Items
-
A Conceptual Model to Quantify the Water Balance Components of a Watershed in a Continuous Permafrost Region
by: Alain Lubini Tshumuka, et al.
Published: (2023-12-01) -
Soil pore network response to freeze-thaw cycles in permafrost aggregates
by: Erin C. Rooney, et al.
Published: (2022-04-01) -
The Effect of Post-Fire Disturbances on a Seasonally Thawed Layer in the Permafrost Larch Forests of Central Siberia
by: Evgenii Ponomarev, et al.
Published: (2020-07-01) -
Cooling and wetting of soil decelerated ground freezing–thawing processes of the active layer in Xing'an permafrost regions in Northeast China
by: Bo-Quan Lu, et al.
Published: (2023-02-01) -
Linear disturbances on discontinuous permafrost: implications for thaw-induced changes to land cover and drainage patterns
by: Tyler J Williams, et al.
Published: (2013-01-01)