Introduction, Definitions

Terrestrial-heat offers a natural longtherm Usage, independent of climate, daytime and season for heat- and electricity-Production. Different temperatures and depths gives a huge amount of possibilities for its usage.

Terrestrial energy is the warmth, stored underneath the Earth surface. The warmth originates from the decay of natural Rodioisotope in the rock of the earth's crust as well as from the heat exchange with the deeper interior of the earth. The use of the terrestrial heat is called Geotherm.

In most regions of the earth the temperature in a Depth of 500 m is about 25-30° C and in 1000 m Depth already about 35-45° C. There are also regions, in which under appropriate geological conditions (thinned earth's crust, volcanism, convection of fluids) in this depth temperatures of 100° C, 200° C or even more can be achieved!

Terrestrial heat is an almost inexhaustible energy source. Due to this fact the Geotherm gained a strongly significance in the past years and is an extraordinary hope for the future power supply. The value of the Geotherm in relation to future energy policy scenarios increases clearly.

 

Advantages of the Terrestrial Energy

Geotherm is a emission-free and locally usable energy source. By its dual function as a source and reservoir for low-temperature heating and cooling systems, it is characterised in particular.

The terrestrial heat increases independence of foreign energy and offers the advantage of most different forms for application. Terrestrial heat can be used variously. In the international rank list Switzerland takes a leading position with the use of the terrestrial energy in the form of low-temperature warmth. Heat production with terrestrial heat probes, geostructures, Tunnelwather etc. could already be realized by numerous installations. Meanwhile steps has been made, to produce electricity with deep lying geothermal energy.

 

Regularities of the temperatures in the underground

The temperature fluctuations during the day are noticeable still in a depth of around 50 cm. Seasonal differences can be found even in 10 - 20 Meter depth. Below that the earth temperature – without considerable groundwater circulation – is extraordinarily constant.

Schätzung des Temperaturverlaufs im Untergrund bei Bedingungen im Schweizer Mittelland. Grafik S. Cattin, CREGE

 

Estimation of the temperature gradient in the underground of central Switzerland


According to a proven rule, the temperature in about 10 meters of depth is 1 degree higher in the annual average, compared to the average air temperature over the ground. Thus in central Switzerland the ground temperature in this depth is about 11 to 12 °C. Among that begins the range of assignable geothermal gradients, uninfluenced by the surface - also the range with constant rise in temperature with increasing depth.  

 

Heating and Cooling

Gebäude geheizt und gekühlt durch ein ErdwärmesondenfeldThe technologies to the use of the terrestrial heat were so far predominantly developed and used to supplying heating energy: Warmth for apartment and office buildings, for greenhouses, lane keeping at a moderate temperature and for various production processes.Meanwhile it was realized that the underground can be used as a reservoir during summer time and thus also can be used for the more and more interesting aspects of room-cooling.
With terrestrial heat probes and geo structures, as well as with air-filled earthregisters, buildings can be air-conditioned, without having to use energy-intensive air-conditioners. If both types of use - heating and cooling - are taken in consideration, the geothermal solution becomes still more efficiently and economically interesting. Besides the application potential is very large.