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GeoPLASMA-CE aims to foster the share of shallow geothermal use in heating and cooling strategies in central Europe. Geothermal methods are a locally available, endogenous heat source not affected by emissions, which is a present and future key technology in order to reduce emissions hazardous to climate and air quality. The project intends to create a web-based interface between geoscientific experts and public as well as private stakeholders to make the existing know-how about resources and risks associated to geothermal use accessible for territorial energy planning and management strategies in Central Europe.
What is shallow geothermal energy?
Shallow geothermal energy (also: near surface geothermal energy) is the heat available or rather stored in the ground. It is available everywhere and anytime, regardless of daytime or season. In central Europe, the temperature in a depth of 20 metres amounts to a constant temperature of roundabout 10 °C. Every 100 metres deeper the temperature increases by 3 K. It can be used for cooling and heating purposes (deep geothermal energy also for electricity production). The heat of the ground is usually extracted in closed loop systems, rarer in open loop systems. Geothermal energy is renewable, ecologically friendly and space-saving at the surface.
Closed loop systems
Closed loop systems use pipes made of polyethylene for heating and cooling. They can be installed vertically down to several hundred meters (tube systems) or horizontally meandering in depths of 1,0 to 1,5 meters (collectors). There are also more compact collectors combining vertical and horizontal energy extraction. Furthermore, foundation piles of buildings are also used for geothermal installations. Several tubes, piles or collectors can be combined to install higher capacity systems.
All closed systems use brine (a mixture of water and a refrigerant like gylcol or ethanol) which continuously circulates in the pipes. Below the surface this fluid absorbs heat from the ground and flows back to the top. A heat exchanger transfers the fluid’s heat to the heat pump and its refrigerant fluid. Compression raises the temperature of the refrigerant fluid in the heat pump from around 10 up to 60 °C. After passing the heat exchanger the brine returns to the ground and a new cycle begins. For cooling in summer, the process is reversed: the heat is extracted from the building and carried back to the ground. This can be done in a very economical way as a free cooling process.
Open loop systems
The process of open loop systems is very similar to closed loop systems, but it uses groundwater directly as heat source. No additional water or fluids are needed. In an extraction well ground water is pumped to the surface, where it transfers its energy via heat exchangers to the heat pump. Afterwards the water is reinjected to the groundwater horizons using an injection well.
The 6th Polish Geothermal Congress took place on 23-25th October, 2018 in Zakopane. The Congress gathered over 180 participants. The Congress was also attended by GeoPLASMA-CE experts, from the Polish Geological Institute - National Research Institute and AGH University of Science and Technology.
3.- 5. 10.2018
GeoPLASMA-CE has been presented at 5th Slovenian geological Congress held in Velenje, Slovenia. The congress has successfully fostered dialogue between more than 200 scientists and professional geologists on the one hand, and end users of results on the other hand.
more then 20 Associated Partners from 8 EU countries
Web-based portal for decision support and information systems based on 3D data models
Web based expert platform for transfer of knowledge and connecting stakeholders of shallow geothermal use in Central Europe
The portal is under construction and already publicly available via https://portal.geoplasma-ce.eu.
Integrative management strategies for the use of shallow geothermal methods in the selected pilot areas
Harmonized strategies for planning, mapping, management and monitoring of shallow geothermal use based on joint transnational standards
GeoPLASMA-CE in Vienna (Austria) focuses on the challenges of geothermal use of groundwater in the city districts 21 and 22. The pilot area covers parts of the groundwater body Marchfeld, which already host many shallow geothermal applications. Growing numbers of single installations will influence each other and prevent a sustainable use of groundwater for heating and cooling.
What is our plan to overcome this challenge? Find out here...
The objective of the project activities in Ljubljana pilot area (Slovenia) is to quantify spatial distribution of shallow geothermal potential for utilisation with ground source heat pumps and integrate this information into development and management strategies of the city with a goal to meet environmental objectives set in the Ljubljana city Sustainable Energy Action Plan 2010 - 2020.
What is our plan to achieve this? Find out here…
Krakow city pilot project area (Poland) occupies an area of approx 326,9 km2 and covers the area within the administrative border. Krakow is the second largest and one of the oldest cities in Poland with population of 762,448 (as on 30th of June 2016), comprised ca. 2% of the population of Poland and 23% of the Lesser Poland Voivodeship respectively. Krakow is situated by the Vistula (polish Wisła) River. The city stretches from the North to the South approx. 18 km, whereas from the West to the East approx. 31 km. Point of the highest elevation within the city limits to 383 m above sea level.
Find out more here...
Pilot area Bratislava (Slovakia, Austria) includes Bratislava city and the transboundary part of Austria in the vicinity, including town Hainburg with the total evaluated area of 603 km2 (Slovak part - 367 km2 and Austrian part 236 km2). From geological point of view pilot area is diverse including hard rocks (granites, limestones, dolomites) and non-consolidated sediments (gravels, sands, calys). Estimated population in the pilot area is around 450,000 inhabitants (434,000 in Slovakia and 16,000 in Austria) including urban and rural areas resulting in different population density and different energy needs. The energy market, regulation, support and consumer behaviour is different in both countries and so having its own specifics that will be evaluated within the project. At the end this will lead to proper further recommendations delivered to policy makers and stakeholders.
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The transboundary Wałbrzych / Broumov pilot area (Poland, Czechia) covers 1,245 km2 in the Sudety Mts and is characterized by very complex geological structure comprising several units made of metamorphic, volcanic and sedimentary rocks. This mountainous area with around 240,000 inhabitants, once a coal mining industrial district, is today focusing on tourism based on local landscape attractions and clean air. These conditions imply to enhance utilization of ground source heat pumps as energy sources in the investigated area.
Find out more here…
The Vogtland / W – Bohemia pilot area (Germany, Czechia) is a transboundary area located in the SW Saxon part of the Vogtland region and extends to the most western part of Bohemia. The pilot area is especially suitable for using geothermal energy, since the Eger valley corresponds to a lithospheric uplift which causes geothermal gradients twice as high as in the surrounding regions. The deeply circulating water in this tectonically active region forms thermal and mineral springs. The usage of this balneal water is in conflict with the geothermal usage, such that a detailed study of land-use conflicts is necessary, when a strategy of geothermal energy supply is established. The central part of the pilot area close to state border consists of a mountain range. In its foothills, many small towns and villages are located on the both sides of the border. The infrastructural development of this region can significantly benefit from the usage of shallow geothermal energy.
Find out more here…
You are invited to take a look and download the following project deliverables:
3D Modelling workshop in Prague (D.T3.3.1)
e-Newsletter No. 2 (D.C.2.2)
GeoPLASMA-CE Data structure (D.T2.3.1)
Synopsis of conflict mapping (D.T2.2.3)
Synopsis of geological 3D modelling methods (D.T2.2.1)
Promotional leaflet in English language (D.C.2.1)
e-Newsletter No. 1 (D.C.2.2)
1 july 2016
30 june 2019
Borehole heat exchangers – current state, barriers and development in Poland, May 2018
EUropa in Wien, May 2018
4. meeting of the European GeoModelling Community, March 2018
26. Meeting of the German Association for Hydrogeology at Ruhr-Universität Bochum, March 2018
Workshop “New horizons in geological and geo‑environmental monitoring”, March 2018
GeoTHERM expo & congress in Offenburg, March 2018
Meeting with stakeholders of the Wałbrzych pilot area, November 2017
Knowledge exchange workshop in Salzburg, November 2017
Climathon 2017 in Krakow, October 2017
Renexpo® Poland fair and VI. PORT PC congress, October 2017
Summary Conference of GeoHeatPol project, October 2017
Networking of Geothermal4PL and GeoPLASMA-CE in Checiny, October 2017
Knowledge exchange workshop in Munich, September 2017
National stakeholders's event in Ljubljana, August 2017
Important visit from Brussels, June 2017
GeoPLASMA-CE at Geothermal Technology Workshop in Brussels, June 2017
GeoPLASMA-CE lecture at TU Bergakademie Freiberg, June 2017
geoENERGIE Tag 2017 in Freiberg, May 2017
Mapping and Assessment Workshop at the DGK in Essen, December 2016
International conference on heat pumps ZEO 2016 in Ljubljana, November 2016
The GeoPLASMA-CE Polish kick-off workshop, November 2016
5th Polish Geothermal Congress, October 2016
Kick-Off Meeting at the European Geothermal Conference in Strasbourg, September 2016