Skip to main content
U.S. flag

An official website of the United States government

Groundwater flow with energy transport and water-ice phase change: Numerical simulations, benchmarks, and application to freezing in peat bogs

January 1, 2007

In northern peatlands, subsurface ice formation is an important process that can control heat transport, groundwater flow, and biological activity. Temperature was measured over one and a half years in a vertical profile in the Red Lake Bog, Minnesota. To successfully simulate the transport of heat within the peat profile, the U.S. Geological Survey's SUTRA computer code was modified. The modified code simulates fully saturated, coupled porewater-energy transport, with freezing and melting porewater, and includes proportional heat capacity and thermal conductivity of water and ice, decreasing matrix permeability due to ice formation, and latent heat. The model is verified by correctly simulating the Lunardini analytical solution for ice formation in a porous medium with a mixed ice-water zone. The modified SUTRA model correctly simulates the temperature and ice distributions in the peat bog. Two possible benchmark problems for groundwater and energy transport with ice formation and melting are proposed that may be used by other researchers for code comparison.

Citation Information

Publication Year 2007
Title Groundwater flow with energy transport and water-ice phase change: Numerical simulations, benchmarks, and application to freezing in peat bogs
DOI 10.1016/j.advwatres.2006.08.008
Authors J.M. McKenzie, Clifford I. Voss, D. I. Siegel
Publication Type Article
Publication Subtype Journal Article
Series Title Advances in Water Resources
Series Number
Index ID 70030134
Record Source USGS Publications Warehouse
USGS Organization Toxic Substances Hydrology Program

Related Content