Science – Society – Technology
From: The interplay of Malm carbonate permeability, gravity-driven groundwater flow, and paleoclimate – implications for the geothermal field and potential in the Molasse Basin (southern Germany), a foreland-basin play
Material property
Ice (< 0 °C)
Water (> 0 °C)
Density
918 kg m–3
999.8443 kg m–3
Heat capacity at constant pressure
2052 J kg–1 K–1
4219.4 J kg–1 K–1
Thermal conductivity
2.31 W m–1 K–1
0.562 W m–1 K–1