abstract |
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Vertically oriented, continuous morphological structures like earthworm channels
significantly influence infiltration into soils. The initiation of flow in these
macropores and the water exchange (interaction) from macropores to the surrounding
soil matrix govern the flow and transport processes at field scale. This study explores
the factors affecting initiation and interaction of macropore flow and the interference
of both processes. Sprinkling experiments on different sites with a dye tracer in combination
with soil water content and matric potential measurements were carried out. The resultant dye
patterns, descriptions of the macropore network, and measured water fluxes have been used to
determine factors influencing initiation and interaction. Initiation of macropore flow started
either at the soil surface or from a saturated or partially saturated soil layer. The micro
topography at the surface and the macropore density directly control the inflow rate distribution
in macropores. Only a small percentage of macropores receive a considerable amount of water from
initiation at the surface. The inflow rates are almost equal for subsurface initiation. Macropore
density, macropore continuity, the size of macropores, soil hydraulic properties, and the water
content of the soil matrix determine interaction and losses to the bedrock. The results of this
study show that initiation and interaction considerably changes flow and transport processes in the
soil and thus the hydrological behaviour during rainfall events.
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