Jökull


Jökull - 01.12.1961, Síða 50

Jökull - 01.12.1961, Síða 50
REFERENCES Barth, T. F. W.: Volcanic Geology, Hot Springs ancl Geysirs of Iceland. Carnegie Institution of Washington Publ. 587 (1950). Bodvarsson, G.: Geothermal Effects of the Pleistocene Glaciation in Iceland, Jökull, Vol. 7, (1957). Bodvarsson, G.: Physical Characteristics of Natur- al Heat Resources in Iceland. Conference on New Sources of Energy, Rome (1961). Published in Jökull, vol. 11. 1961. Bodvarsson, G. ancl Zoega, J.: Production, Di- stribution and Utilization of Natural Heat in Iceland. Conference on New Sources of Energy, Rome (1961). Jökull, vol. 11, 1961. Einarsson, T.: Ueber das Wesen der Heissen Quellen Islands. Societas Scientarium Is- landica, Reykjavík (1942). Krauskof, K. B.: Dissolution and Precipitation of Silica at Low Temperatures. Geochim. et Cosmochim. Acta Vol. 10, (1956). Tryggvason, E. and Báth, M.: Upper Crustal Structure of Iceland. (In press.). (1961). White, D. E., Brannock, W. W. and Murata, K. J.: Silica in hotspring waters. Geochim. et Cosmochimica Acta, Vol. 10, (1956). U. N. CONFERENCE ON NEW SOURCES OF ENERGY, ROME 1961: Production and Distribution of Natural Heat for Domestic and Industrial Heating in Iceland BY GUNNAR BODVARSSON and JOHANNES ZOÉGA SUMMARY. The present paper furnishes a brief review of some engineering and economic aspecls of the utilization of naiural heat for domestic and industrial heating in Iceland. At present, the total consumption of natural heat in the country corresponds to a saving in import of fuel oil of approximately 60,000 metric tons per year. The corresponding figure expected for 1970 is 160,000 metric tons per year, that is, about 800 kg per year ancl capita. The present procluclion cost of natural heat in three major thermal areas is ranging from 0.30 to 0.30 $/Gcal (one Gcal = 109 cal). The heat is in some areas available as high-tempera- ture water or low-pressure steam. Water at tem- perature of 130° C to 200° C is to be preferred as the medium for heat transport over more than a few kilometrers. The total cost of heat delivered by present systems amounts to approximately 4.00 $/Gcal. Various engineering cletails of the systems are discussed. Finally, a brief review is given of the present plans to supply the Reykjavík area with natural heat from the Krysuvik thermal area which is located some 30 km south of the city of Reykja- vík. This plan involves the building of a major supply system delivering approximately 300 Tcal/year of heat (one Tcal=1012 cal). About % of the heat delivered is intencled for industrial heating. I. INTRODUCTION. The utilization of natural heat was initiated in Iceland around 1925. The initial step con- sisted in the heating of a few houses and green- houses by means of natural hot water. A relative- ly rapicl development followed. As of now about 45,000 people in Iceland live in houses heated by natural heat. Moreover a large number of green-houses ancl swimming-pools are being provided with natural heat. Plans are now being workecl out for a consiclerable extension of the present systems. This paper is written for the purpose of giv- 48

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