Measurements of water-film thickness on cave walls and speleothems

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The water-film that coats cave walls and speleothems is a key player for the regulation of cave microclimate and the control of speleothem growth. In this paper, we demonstrate the capability of a confocal optical sensor to quantitatively measure on-site the rapid variations of water-film thickness when dripping, active condensation, or dryness occur on walls of various caves. Results obtained from a sample of four prehistoric caves and one stalagmite cave from Southwest France, indicate that the measurable thickness of water-films is generally in the 25-70 µm range for cave walls and reaches 200-300 µm on the horizontal plane of active speleothems. The high measurement frequency enables the monitoring of water-film dynamics for a few minutes, especially the tracking of thickness changes triggered by drop dripping and water flow. The optical sensor appears to be a promising tool for the conservation of prehistoric caves facing subsurface warming.

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