This site requires Cookies enabled in your browser for login.
Updating ...
WaterNet Home
WaterNet
for
pour le
Canada
Menu
WaterNet
Home
GWFO
Home
Master
List
Data
Centre
Collections
X
Defaults
Select All
Websites
X
Global Water Futures Observatories (GWFO) Global Water Futures (GWF) Global Institute for Water Security (GIWS) International Network of Alpine Research Catchment Hydrology
Legacy Research Programs
X
Changing Cold Regions Network (CCRN) Drought Research Initiative (DRI) International Network of Alpine Research Catchment Hydrology (Legacy Site) Improving Processes & Parameterization for Prediction in Cold Regions Hydrology (IP3) The Mackenzie Global Energy and Water Cycle Experiment (GEWEX) Study (MAGS)
Legacy sites
Map
Utilities
X
Account Settings Metadata Editor Record List Alias List Editor
Data Centre
Data Type Editor
. . .
X
Clear
Select All
Advanced Search
Go to Top⇡
Related items loading ...
Fetching Chart ...
Publication Additional Information Download
Authorship
Zhao, L., D.M. Gray and D.H. Male
Title
Numerical analysis of simultaneous heat and water transfer during infiltration into frozen ground
Year
1997
Publication Outlet
J. Hydrology, 200, 345-363
DOI
https://doi.org/10.1016/S0022-1694%2897%2900028-0
Citation
Zhao, L., D.M. Gray and D.H. Male, (1997). Numerical analysis of simultaneous heat and water transfer during infiltration into frozen ground. J. Hydrology, 200, 345-363.
Abstract
This paper concerns heat transfer and water infiltration into a homogeneous, unsaturated, frozen soil. A numerical analysis of the processes, which is based on the local volume averaging formulation of transport phenomena in porous media, is described. Simultaneous heat and mass transfers with phase changes are considered. The results of the simulations provide an insight into the mechanics of the infiltration process. They suggest that infiltration involves primarily two flow regimes, a transient regime and a quasi-steady-state regime. Once the quasi-steady-state regime is reached, the energy needed to increase soil temperature at depth is supplied by latent heat released from freezing of water in the upper layers of soil. The effects of surface saturation, initial soil saturation and initial soil temperature on infiltration are examined.
Program Affiliations
GWF: Global Water Futures
Publication Stage
N/A
Additional Information
Year 1997 confirmed!!.
Download Links
https://doi.org/10.1016/S0022-1694%2897%2900028-0
© 2026 - WaterNet Version 2026-06-15
Global Water Futures Observatories
Powered by
G W F Net
T-2023-01-20-g1nsZg1Bl1F0m6lktuROvItQ Publication 1.0