The thermal conductivity maps of the Flemish subsoil up to 100 meters, commissioned by the Department of Land and Soil Protection, Underground and Natural Resources, give the thermal conductivity of the Flemish subsurface to a depth of 100 m or up to the solid rock. This map of lines represents the average thermal conductivity of the Flemish subsurface up to 100 meters. The contours have an equidistance of 0.1 W/mK. Each jump therefore represents a difference in thermal conductivity of 0.1 W/mK.
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