Related Experiment Video
Updated: Dec 20, 2025

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
Published on: June 8, 2015
Evaporation versus imbibition in a porous medium
Charlotte Van Engeland1, Benoît Haut2, Laurent Spreutels3
1TIPs (Transfers, Interfaces and Processes), Université libre de Bruxelles, Brussels, Belgium; Chemical Engineering Department, Polytechnique Montréal, Montréal, Canada.
This study presents a general analytical solution for liquid front dynamics in porous media, considering capillary imbibition, gravity, and evaporation. The liquid front
Area of Science:
- Fluid dynamics
- Porous media physics
- Interfacial phenomena
Background:
- Controlling liquid movement in porous materials is vital for applications like groundwater flow, oil recovery, and material processing.
- Existing models often simplify or neglect the interplay between capillary forces, gravity, and evaporation.
- A comprehensive understanding of these combined effects is needed for accurate prediction and control.
Purpose of the Study:
- To derive a general analytical solution for flat liquid front dynamics in porous media.
- To investigate the influence of capillary imbibition, gravity, and evaporation on liquid front movement.
- To classify and analyze the different types of liquid front dynamics based on key dimensionless numbers.
Main Methods:
- Derivation of a general analytical solution incorporating capillary, gravitational, and evaporative forces.
- Introduction and analysis of two dimensionless numbers: gravity-capillary number (G) and evaporation-capillary number (E).
- Comprehensive analysis of liquid front dynamics as a function of G and E, including limiting cases.
Main Results:
- The liquid front dynamics are governed by the gravity-capillary number (G) and evaporation-capillary number (E).
- Seven distinct types of liquid front dynamics, categorized into three main behaviors, were identified.
- Simplified expressions for the general solution were derived for each limiting case.
Conclusions:
- The derived analytical solution provides a unified framework for understanding liquid front dynamics in porous media.
- The study reveals a rich variety of dynamic behaviors influenced by fluid properties, porous medium characteristics, and environmental conditions.
- Estimated G and E values highlight common regimes and dynamics encountered in practical applications, aiding in prediction and control.
Related Concept Videos
Porosity and Absorption of Aggregate
When all pores in an aggregate are filled with water, the aggregate is considered saturated and surface-dry. If left in dry air, water will evaporate until the...
Theories of Dissolution: Diffusion Layer Model
This process starts with a thin layer, saturated with the drug, forming at the interface between the solid and liquid. The solute then diffuses from this layer into the main solution. The Noyes-Whitney equation suggests that the rate of dissolution relies on the diffusion...
Vapor Pressure
Volatilization
Phase Transitions: Vaporization and Condensation
Vaporization

