Geothermal Probes

  • Stober I
  • Bucher K
N/ACitations
Citations of this article
6Readers
Mendeley users who have this article in their library.
Get full text

Abstract

The basic condition of near-surface geothermal energy utilization is the low temperature of the thermal reservoir. The temperature is typically lower than the working temperature of house heating. The heat transfer fluid in house heating systems requires a minimum temperature of about 20--30 {\textdegree}C, whereas ground temperatures are typically in the range of 5--15 {\textdegree}C. Therefore, in order to use the geothermal energy for the heating of buildings the transfer fluid temperature must be increased by means of a heat pump system. The highest reservoir temperatures are accessible to geothermal probes. Depending on the depth of the probe, drillhole heat exchangers may provide fluid temperatures of 10--12 {\textdegree}C depending on the local conditions (Central Europe). The temperature increase needed by the house heating system is then done by the heat pump. Most heat pumps are driven electrically. Electricity is expensive and produced with large losses from fossil energy resources in some countries.

Cite

CITATION STYLE

APA

Stober, I., & Bucher, K. (2013). Geothermal Probes. In Geothermal Energy (pp. 65–113). Springer Berlin Heidelberg. https://doi.org/10.1007/978-3-642-13352-7_6

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free