Effects of lithology and land use on storm run‐off in east luxembourg

For a large part of the year, the forested catchments in the Keuper formation of east Luxembourg produce more direct run‐off on a storm basis than paired cultivated catchments. The occurrence of shrinkage cracks, their pronounced opening and closing, and the occurrence of natural pipes in the forested environment play a major role in explaining this phenomenon. The effect of land use on storm run‐off is studied in relation to that found for lithology in the same area.