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Cofunded by the European Union

Institution/Coordinating Institution : 
LTER-Austria - Gesellschaft für ökologische Langzeitforschung
Country : 
Austria
Current Status : 
Active
Location : 
Petzenkirchen Austria
RI Type : 
Distributed RI (Central Hub and interlinked National Nodes RI)
Level of Access : 
Other
(Austrian RI database)
Cost of Access : 
Other
(Please contact the responsible person.)
Water4All Keywords : 
Ecosystem services
Domains and thematic area : 
Ecosystems
(ydrological catchment with a variety of sensors for the monitoring of water budget, climate and material flows: - runnoff measurement at 13 stations (surface water, drainage, springs) - measuring barrage (water level, water quality, microbiology)...)

The Petzenkirchen HOAL (Hydrology Open Air Laboratory) catchment is situated in the western part of Lower Austria (48°9' N, 15°9' E). The catchment area at the outlet (termed MW) is 66 ha. The elevation of the catchment ranges from 268 to 323ma.s.l. with a mean slope of 8 %. At present, 87% of the catchment area is arable land, 5% is used as pasture, 6% is forested and 2% is paved. The crops are mainly winter wheat and maize. The climate can be characterised as humid with a mean annual temperature of 9.5°C and a mean annual precipitation of 823mm/yr from 1990 to 2014. Precipitation tends to be higher in summer than in winter. Crop evapotranspiration (ETc) estimated by the FAO (1998) method using local climate data and crop growth information for this period was 471mm/yr. Annual evapotranspiration estimated by the water balance ranged from 435 to 841 with a mean of 628mm/yr (1990–2014) (assuming deep percolation is negligible). The natural surface water outlet of the catchment is known as the Seitengraben stream. Mean annual flow from the catchment in this stream is 4.1 L/s (or 195mm/yr) (1990–2014). Mean flows tend to peak in the spring. The largest flood events on record occurred in 1949 and 2002 with estimated peak discharges of 2.800 and 2.000 L/s, respectively. The highest discharge in recent times occurred in summer 2013 with 660 L/s. The subsurface consists of Tertiary sediments of the Molasse zone and fractured siltstone. The dominant soil types are Cambisols and Planosols with medium to poor infiltration capacities. Gleysols occur close to the stream.

Research Infrastructures

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The Water4All Partnership - Water Security for the Planet - is a funding programme for scientific research in freshwater. It aims to tackle water challenges to face climate change, help to achieve the United Nations’ Sustainable Development Goals and boost the EU’s competitiveness and growth.

It is co-funded by the European Union within the frame of the Horizon Europe programme (a key funding programme for research and innovation). The Partnership duration is for seven years from 2022.

The Water4All objective is to enable water security at a large scale and in the long term. Its goal is also to tackle water issues in a holistic frame. 

All forms of life on earth need water. All human activities operate with this resource. Water is part of our everyday life. It is also integrated within urban and countryside landscapes. It is one of the most valuable elements we share with plants and animals.

These simple facts must be kept in mind to understand the Water4All ambition.

This resource is weakened in many places due to climate changes, and human habits. We know that we can improve the way we use water. Everyone has a role to play and especially the scientific research community.

Scientific research is the heart of the Partnership as It is a powerful tool to improve knowledge on preserving, restoring, and managing this essential resource. 

International cooperation is also needed as water has no borders on Earth and runs from one country to another.

Water4All brings together a broad and cohesive group of 90 partners from 33 countries in the European Union and beyond. This consortium gathers partners from the whole water Research, Development and Innovation (RDI) chain.