Geothermics Report

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    Geothermics 49 (2014) 1

    Contents lists available atScienceDirect

    Geothermics

    j o u r n a l h o m e p a g e : w w w . e l s e v i e r . c o m / l o c a t e / g e o t h e r m i c s

    Preface

    Iceland Deep Drilling Project: The first well, IDDP-1, drilled into magma

    The Iceland Deep Drilling Project (IDDP) is a research anddevel-opment project, largely fundedby a consortium of Icelandic energycompanies,that is investigating the possibility of greatly increasingthe energy resources of Iceland by producing deep, high-enthalpy,supercritical geothermal fluids. If successful, it may be possibleto increase the power outputs of suitable geothermal wells byan order of magnitude, without increasing their environmentalfoot prints. This special issue of Geothermics brings together 15

    papers that report on (i) the concept of the IDDP, (ii) the first wellthat attempted to drill to 4.5km depth into the supercritical zonebelieved to exist in the Krafla volcanic caldera in NE Iceland, (iii)how the well was completed at only 2.1km depth after rhyolitemagmawas encountered at only 2.1km depth,(iv) the widerappli-cations of the IDDP concept to other parts of the world, and (v) theplans for drilling the next IDDP well in the Reykjanes geothermalfield, in SW Iceland.

    In one sense the first phase of the IDDP could be considered afailure as drilling planned for a depth of 4.5 km, had to be termi-nated at only 2.1km depth when >900C magma flowed into it.However this unexpected result proved to be a case of serendip-ity. The well was completed to produce from the >500 C contactzone of the intrusion. Subsequently during a two year-long flow

    test it became the worlds hottest producing geothermal well, witha well head temperature of more than 450 C, flowing dry super-heatedsteamat high pressures(40140 bar). However theflow testwas terminated when it was found that the wellhead mastervalveshad suffered mechanical failure under these extreme conditions.

    Currently the well is kept quenched by cold water injection whilenew master valves are being procured.

    While the future development of the shallow molten igneousintrusion at Krafla as an energy resource is being actively debated,the focus of the IDDP on supercritical geothermal systems isshifting attention to drilling a deep well on the Reykjanes Penin-

    sula in 20142015. This geothermal system, located where theMid-Atlantic Ridge comes on land, differs from other geothermalsystems in Iceland in that itshydrothermal fluid is modified seawa-ter. The proposed 45km deep well will explore for supercriticalconditions beneath the existing producing geothermal field, withthe aim of greatly enhancing its resource potential. At the sametime an extensive geophysical exploration program of the Reyk-

    janes Peninsula will be carried out by project IMAGE, an initiativefunded by the European Commission. Since its inception the IDDPindustrial consortium has been open to participation of interestedscientistsand the drilling program has providednumerous excitingadd-on science opportunities. At Krafla we were able to study thecoupling of the hydrothermal systemwith a magmatic heat source.At Reykjanes we will investigate the structure of a mid-ocean ridge

    and the roots of a hydrothermal system similar to those that arethe heat sources of black smoker hydrothermal vents.The guest editors of this special issue are grateful to the IDDP

    consortium of HS Orka Hf, Landsvirkjun, Orkuveita Reykjavkur,Orkustofnun, Statoil,andAlcoathat funded the engineeringaspectsof the program, andto theU.S. National ScienceFoundation andtheInternational Continental Scientific Drilling Program that togethermade the add-on science program of the IDDP possible.

    Guest Editor

    Wilfred A. EldersGuest Editor

    Gumundur . FrileifssonGuest Editor

    Bjarni PlssonE-mail address:[email protected]

    (W.A. Elders)

    Available online 19 September 2013

    0375-6505/$ see front matter 2013 Elsevier Ltd. All rights reserved.

    http://dx.doi.org/10.1016/j.geothermics.2013.08.012

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