EGU26-7146, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-7146
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Analytical and Invertible Model for Transient Heat Transport in Layered Subsurface Media
Vishal Bashist1, Ratan Sarmah2, and Ickkshaanshu Sonkar3
Vishal Bashist et al.
  • 1Indian Institute of Technology, Ropar, Civil engineering, Rupnagar, India (vishal.23cez0005@iitrpr.ac.in)
  • 2Indian Institute of Technology, Ropar, Civil engineering, Rupnagar, India (ratan@iitrpr.ac.in )
  • 3Indian Institute of Technology, Ropar, Civil engineering, Rupnagar, India (ickkshaanshu@iitrpr.ac.in )

 Abstract

Accurate characterization of transient heat transport in layered subsurface media is fundamental to a wide range of environmental and hydrological applications, including groundwater recharge assessment, land-atmosphere interaction analysis, and climate signal detection in soils. This study presents a fully analytical solution for one-dimensional transient heat transfer in a two-layer soil system subjected to realistic, time-dependent surface temperature forcing associated with diurnal variations. The governing advection-conduction equation is solved using the Generalized Integral Transform Technique, which enables an exact treatment of interlayer thermal interactions while avoiding numerical inversion or interface-matching complexities. The resulting formulation yields a computationally efficient and stable solution that is well suited for both forward simulation and inverse analysis. The analytical solution is rigorously validated through comparison with high-resolution numerical simulations, demonstrating excellent agreement for both homogeneous and stratified soil configurations over a wide range of hydrothermal conditions. The inverse modeling capability of the framework is further demonstrated by coupling the analytical solution with a genetic algorithm to estimate vertical water flux from field-measured temperature data, highlighting its potential for non-invasive hydrological characterization. This work introduces a scalable, computationally efficient, and physically consistent framework for simulating and interpreting transient heat transport in layered subsurface systems. Owing to its generality, the proposed methodology is readily extendable to other diffusion-dominated transport processes, such as solute transport in stratified geological media, thereby enhancing its applicability across a broad range of geoscientific problems.

Keywords: Transient heat transport, Layered subsurface media, Analytical solution, Generalized Integral Transform Technique, Inverse modelling

How to cite: Bashist, V., Sarmah, R., and Sonkar, I.: Analytical and Invertible Model for Transient Heat Transport in Layered Subsurface Media, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-7146, https://doi.org/10.5194/egusphere-egu26-7146, 2026.

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