Fig. 7From: Role of the capillary fringe on the dilatation of a low porosity limestone submitted to unidirectional freezingMain horizontal and vertical dilatation behavior according to freeze-thaw cycles and corresponding temperature of the surface and in depth at the level of the strain gage at a 1 cm, b 2 cm, c 4 cm, d 6 cm, e 8 cm, and f 10 cmBack to article page