Water saturation variation in a fire-heated limestone gallery monitored by ERT

Abstract

Summary Water migration within the rock mass during a fire has not yet been studied. Here, an innovative high resolution micro-ERT method is developed at a centimetric scale to measure this phenomenon. The method is two-step based: first, a correction of the electrode effect, and second, the correction of resistivity for rapid variations in temperature with high values. Water migration is successfully described within the wall of an underground limestone quarry with three phases: from fire ignition to 36 min, the surface dries to a 3-cm depth and a higher saturated layer forms deeper than 0.10 m; from 36 min to 46 min (fire supply stops), the rock dries out and water migrates from deeper parts of the rock wall, deeper than 20 cm, toward the surface; finally, after fire extinction, the water migrates through a readjustment phase until it returns to its initial state.