Today again Lovrenc Pavlin and Markus Oismüller were operating the groundwater sampling at the groundwater wells from the deep boreholes in the HOAL catchment. In an interval of 2 months this sampling is taking place in the HOAL at the 8 deep wells in the catchment. The samples are analysed for chemical parameters and their isotopic signature.
The temporal soil net is currently prepared and checked for the next installation in the HOAL fields. As soon as the farmers will be finished with the tillage of their land the 11 temporal soil net stations will in addition with the 20 permanent stations measure the soil moisture in the HOAL in 4 different depths with a resolution of 30 minutes.
Recently the homepage of the European network of hydrological observatories - short 'ENOHA' was launched. The aims of ENOHA are to create a network of well-instrumented and monitored hydrological observatories and to ensure a close cooperation between several European research institutions.
The linked catchments are the TERENO catchments in Germany, the HOBE catchment in Denmark, and the HOAL catchment in Austria. Data series of key hydrological fluxes and states in high quality based on a common data policy from these catchments will be provided within this project.
For more information visit https://www.enoha.eu/.
Recently Lovrenc Pavlin, new doctoral student from Slovenia in our DK programme, was operating a sampling from the groundwater wells from the deep boreholes in the HOAL catchment.
In total at 6 wells samples have been taken which will be analysed for chemical parameters but also for stable isotopes and age dating.
Nives Balenovic, doctoral student from Croatia working in a cooperation project from IKT Petzenkirchen, BOKU Vienna and CTU Prague, started recently her PhD about 'Kinetic energy of rainfall as driving force of soil detachment and transport' (also known as splash erosion).
She is doing her field experiments in the HOAL catchment, where she installed so called splash cups for analysing the kinetic energy of rainfall. Due to the installations in the HOAL she can also take use of the data of the climate station and the present weather sensor, which is measuring raindrop and rainfall characteristics (size, velocity, distribution and intensity).
If heavy rainfall occurs it hits the soil in the soil cups and erodes the soil. The eroded soil is collected in the outer bucket and quantitative determined. Also the surface changes of the soil cups and the soil loss in the cups are analysed via photogrammetry.