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                         4
                         Enhancing Geothermal Reservoirs
                         Thomas Schulte, G¨ unter Zimmermann, Francois Vuataz, Sandrine Portier, Torsten
                         Tischner, Ralf Junker, Reiner Jatho, and Ernst Huenges



                         4.1
                         Introduction

                         In many cases, drilling operations will not open up a geothermal reservoir under
                         such conditions that an extraction of geothermal energy is economically viable
                         without any further measures. Geothermal wells often have to be stimulated, in
                         order to increase well productivity. Different stimulation concepts have been applied
                         to enhance the productivity of geothermal wells. Formally, stimulation techniques
                         can be subdivided with respect to their radius of influence. Techniques to improve
                         the near-wellbore region up to a distance of few tens of meters are chemical
                         treatments, and thermal fracturing. The only approved stimulation method with
                         the potential to improve the far field, up to several hundreds of meters away from
                         the borehole is hydraulic fracturing.
                           The foundations, on which today’s enhanced geothermal systems (EGS) projects
                         are built were laid out in the early 1970s, when a hot dry rock (HDR) development
                         concept was worked out at Los Alamos National Lab, entailing drilling a well into
                         hot crystalline rock, using water under high pressure to create a large vertical
                         fracture by interaction with the in situ stress field, and finally to drill a second well
                         to access that fracture at some distance above the first wellbore. The Rosemanowes
                         experiment, performed by the Camborne School of mines, was set up in 1976,
                         aiming at testing at lower temperatures and at lower depth, and some of the ideas
                         that had emerged from earlier investigations, were experimented at Fenton Hill.
                         One of the main findings from these two pioneering endeavors was that deep
                         granites often are fractured and that potentially existing natural fracture systems
                         will determine the orientation and the propagation of the stimulation. Both projects
                         have been comprehensively presented by Armstead and Tester (1987), who also
                         give a broad overview of the state of stimulation technologies at the end of the
                         1980s.





                         Geothermal Energy Systems. Edited by Ernst Huenges
                         Copyright  2010 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim
                         ISBN: 978-3-527-40831-3
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