Dye tracer and morphophysical properties to observe water flow in a Gleyic Luvisol

the understanding of the preferential water flow and solute transport is important with regard to losses of nutrients and pesticides that affect the quality of the groundwater or surface water resources. experiments using the brilliant blue dye tracer, a tension infiltrometer (ti) and a double square infiltrometer (di) were carried out in the experimental field site located around 15 km southeast of the city of rostock (north-eastern germany) on arable land in a pleistocene lowland landscape where corn (zea mays l.) and barley (hordeum spp.) had been cultivated. one day after dye the infiltration, a pit was dug and vertical profiles were prepared in the ti and di sites to assess the dye pathways in the subsoil of a gleyic luvisol. we wanted to examine if the mottled red and white (bleached) colour-pattern of the gleyic luvisol subsoil resulting from temporally stagnant water could be related to flow paths as visualized by dye tracing and if the soil colour could be related to other physical soil properties. biogenic soil structures were the main transport routes conducting water and solutes into great depth in short time. these pathways had lower bulk density and less cone resistance than the adjacent red or white (bleached) areas of the gleyic luvisol subsoil. the red areas were involved in transport because their water contents increased after as compared to before infiltration. however, the measured physical soil properties did not differ between white and red areas. we assume that red areas participate in transport at least by imbibing water from the adjacent biogenic flow paths.