Ólafur Flóvenz - The future of geothermal development in Iceland

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The future of geothermal development in Iceland A presentation by Ólafur G. Flóvenz at GGW conference in Reykjavík, 24.11.2016

Transcript of Ólafur Flóvenz - The future of geothermal development in Iceland

Page 1: Ólafur Flóvenz - The future of geothermal development in Iceland

The future of geothermal development in IcelandA presentation by Ólafur G. Flóvenz at GGW conference in Reykjavík, 24.11.2016

Page 2: Ólafur Flóvenz - The future of geothermal development in Iceland

Primary energy consumption in Iceland 1940-2015

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1940 1945 1950 1955 1960 1965 1970 1975 1980 1985 1990 1995 2000 2005 2010 2015

PJ

Hydro

Geothermal

Oil

Coal

Peat

Slide from Árni Ragnarsson, ÍSOR

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UGS – Unconventional Geothermal Systems

− To develop and use EGS technology at present reservoir depths − To address Superhot Geothermal Systems− To explore for high temperature systems inside the volcanic zone of Iceland but

outside the presently known high temperature system.

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Simplified geothermal map of Iceland

© Ólafur G. Flóvenz

The volcanic rift zone about 32000km2 and with average temperature gradient of about 100 °C/km

Protected High temperature fieldHarnessed high temperature field

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Sketch of a typical magmatic geothermal system

Downflow cooling

Low permeability rock

Heat source

Permeable fractures

250-350°C reservoir

Steam zone

High permeability zone, superheated or supercritical fluid

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Resistivity structure and natural seismicity

Outside the known H.T. fields

Superhot well into the magmatic intrusion

An EGS wellConventional well

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Example of Superhot Geothermal Systems: IDDP-1 in Krafla

Figure from G.Ó. Friðleifsson af HS OrkaPhoto: Elvar Eiríksson, ÍSOR

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Some lessons from IDDP-1

− The exploration method used to site the well did not have enough resolution to detect the magma body at 2 km depth

− The well design, selection of casing material and cementing methods need to be improved to avoid short lifetime of the well and its wellhead units.

− Chemical problems related to harsh chemistry of the steam has to be solved.

− At the top of the magma thin but highly permeable zone exists, most likely due to effective heat extraction and subsequent cooling of the rock.

− This observation fits perfectly with the experiment from extracting heat from the molten lava on the Vestmann Islands in the 1970ees.

400°C100°C0 m

60 m

From the ÍSOR database

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IDDP-2

Photo: Tobias B. Weisenberger, ÍSOR Figure from Egill Árni Guðnason, ÍSOR

Induced seismicity around IDDP-2

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Beautiful landscape to be protected

Photo from Ragna Karlsdóttir, ÍSOR

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Geological maps

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International co-operation

Geothermal plant in Indonesia Hot springs in New_Zealand

Photo: Ólafur G. Flóvenz

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Urgent future R&D topics:

− Development of exploration methods to estimate distribution of temperature and permeable fractures in the deeper part of geothermal reservoir in volcanic environment.

− Development of methods to estimate the mechanical properties of rock in superhot geothermal systems.

− Find the best methods to exploit and to stimulate superhot geothermal systems.− R&D to introduce and test new concepts in design of boreholes that sustain

superhot geothermal fluids. This includes studies of casing material and wellhead units, improved cementing methods, flexible casing couplings etc.

− R&D to solve chemical problems related to use of superhot fluid with harsh chemistry.

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Thank you