Náttúrufræðingurinn

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Náttúrufræðingurinn - 1981, Qupperneq 190

Náttúrufræðingurinn - 1981, Qupperneq 190
Bjömsson, Axel, Kristján Sœmundsson, Sigmundur Einarsson, Freyr Þórarinsson, Stefán Arnórs- son, Hrefna Krislmannsdóltir, Ásgrímur Guð- mundsson, Benedikt Steingrímsson & Þorsteinn Thorsleinsson. 1979. Hitaveita Akureyrar — Rannsókn jarðhita í Eyjafirði. Skýrsla Orkustofnunar, OS JHD 7827. Bjömsson, Sveinbjörn. 1969. Aætlun um rann- sókn háhitasvæða. Skýrsla Orkustofnun- ar, ágúst 1969. — 1980. Rannsóknir og undirbúningur virkjunar háhitasvæða. Arsskýrsla Rannsóknaráðs ríkisins 1978 og 1979. Einarsson, Trausti. 1937. Obereine Beziehung zwischen heissen Quellen und Gángen in der Islándischen Basaltformationen. Greinar I. 2.: 135—145. — 1942. Ober das Wesen der heissen Quel- len Islands. Rit XXVI. Thorannsson, Freyr. 1977. Om höggun Mið- norðurlands. Jarðfræðafélag Islands. Ráðstefna um íslenska jarðfræði 24. — 25. nóv. 1977. SUMMARY Exploration and exploitation of lowtemperature geothermal fields near Akureyri in Northern Iceland by Axel Björnsson Orkustofnun — Geothermal Division, Grensásvegur 9, Reykjavík, Iceland Otilization of natural hot water is of the utmost importance for the Icelandic eco- nomy. The total energy use for space heat- ing, obtained from geothermal water, is equivalent to 300.000 tons of fuel per year, which would otherwise have to be imported. This corresponds to savings of 1.5 tons of fuel per inhabitant per year. Geothermal utilization usually starts with economic evaluation of the proposed project followed by surface exploration of the geothermal fields, where geological, geochemical and geophysical methods are used. Thereafter exploration and produc- tion wells are drilled and tested in order to find the potential of the geothermal system. Akureyri is the largest town in Northern Iceland with about 12.000 inhabitants. Un- til 1976 most of the houses were heated with imported fuel. All attempts to find enough natural hot water for space heating in geothermal areas near the town had failed. During the oil crisis in 1973 hcating cost increased enormously and it became eco- nomically feasible to pipe hot water over longer distances. It was thcn decided to start again exploration of geothermal fields near Akureyri. New instruments and new explo- ration techniques had been developed and new drilling rigs had been bought which were capable of drilling much deeper than in the previous years. On the basis of geological mapping and extensive Schlum- berger resistivity measurements, performed in the summer of 1975, three geothermal fields in vicinity of Akureyri were selected for exploration drilling. The first well was drilled during the winter 1975—1976 in the Laugaland geothermal area about 13 km south of Akureyri. The drilling was success- ful and the well produced initially about 80 liters per second of 95°C hot water. After further exploration work e. g. geological, geophysical and chemical investigations, more drillholes were sunk in the area. About 180 liters persecond are now pumped from 6 wells which is enough for heating about 80% of all houses in Akureyri. Considerable effort is being put into further exploration and drilling of geothermal areas near Akureyri with the aim to find enough hot water for space heating of the whole town and for some industrial use in the future. 332
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