Rising damp is the moisture that comes from subsoil water and is transmitted upwards through the pores of building materials, thanks to the physical property of capillarity.
Humidity by capillarity is maximum at ground level and decreases with height; can be seen on both the exterior and interior walls of a building, normally leaving white dust on the surface, which corresponds to the salts of the building materials that the water has dissolved in its ascension.
This type of humidity mainly appears in low floors at the bottom of walls, both inside and outside, between floor tiles, and in basement walls.In the world, more than 75% of buildings have rising damp, resulting in a progressive deterioration of the walls and soils with serious consequences for health and the economy.