We are looking for a doctoral candidate (project assistant, pre-doc) for research work in the project "Hydrology Weinviertel".

Read more

On May 28, 2025, the Institute of Hydraulic Engineering and Water Resources Management organized a field day for 72 master's students at the…

Read more

Hydrological parameters have been recorded in the HOAL - the Hydrological Open-Air Laboratory - since the end of the Second World War. Since 2010,…

Read more

Since the old erosion measurement weir at monitoring site E1 had become somewhat outdated, it was high time to install a new one.
On March 18, 2025, a…

Read more

The Rich Diversity of Water Flow Paths Makes the HOAL an Ideal Laboratory

A wide range of runoff generation mechanisms occurs in the HOAL which makes it a genuine laboratory where hypotheses of flow and transport can be tested, either by controlled experiments or by contrasting sub-regions of different characteristics. This diversity also ensures that the HOAL is representative of a range of catchments around the world.

Due to shallow, low permeable soils, the concave part of the catchment was tile drained in the 1950s in an effort to reduce water logging. Two tile drain systems do not dry out during the year while two are ephemeral.

There are two clearly visible springs that directly discharge into the stream draining the HOAL. The water from one of them originates from a fractured siltstone aquifer with distinct hydrologic and chemical characteristics while another spring has more shallow water contributions.

In the south-eastern part of the catchment is a small wetland close to the stream which permanently seeps into the stream. The wetland is fed by springs at its upper part and usually responds very quickly to all types of rainfall due to its high saturation state.

During high intensity thunderstorms in summer and spring, infiltration excess overland flow tends to occur with a very substantial, fast contribution from the tile drainage system.

During major storms, saturation overland flow occurs across the fields (mainly in the depression areas) which enters the stream at three locations. In winter rain-on-snow runoff may occur as saturation overland flow during large events which causes gully erosion.

The main runoff generation mechanism in winter is through lateral subsurface pathways (shallow subsurface preferential flowpaths, drainage pipes). Even minor events will lead to a significant increase of stream flow due to high soil moisture during the winter. After freezing periods, when the soil is still frozen, infiltration excess overland flow may occur.