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temperature and pressure in the svartsengi ... - Orkustofnun

temperature and pressure in the svartsengi ... - Orkustofnun

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3ABSTRACTThiS report ls a study of <strong>the</strong> distribution of an d changes<strong>in</strong> <strong>temperature</strong> <strong>and</strong> <strong>pressure</strong> <strong>in</strong> <strong>the</strong> high <strong>temperature</strong>geo<strong>the</strong>rmal field of Svartsengi. Use ls made of t h e variousmeasurements of <strong>the</strong> 12 <strong>in</strong>dividual wells at differentperiods <strong>and</strong> <strong>the</strong> cross-sections made from <strong>the</strong>s e measurementa. Consideration is given to <strong>the</strong> effect of drill<strong>in</strong>g,redrl111ng <strong>and</strong> re<strong>in</strong>jection on <strong>the</strong> t emperature profiles of<strong>the</strong> wells <strong>and</strong> <strong>the</strong> cross - sect 10ns <strong>and</strong> appropriate selectionsare made of reliable <strong>and</strong> repr esentative profiles of<strong>the</strong> many measurements. Bol11ng conditions of th e reservoir<strong>and</strong> evolution with time is studied. Some possibilitiesthat can cause <strong>the</strong> reservoir to be coo11ng down arepresented <strong>and</strong> discussed. They are boil<strong>in</strong>g effect s, lateralcold <strong>in</strong>flow, episoidal cold <strong>in</strong>flow <strong>and</strong> decr e ased lateral<strong>in</strong>flow of hot fl u ids.This study shows that <strong>the</strong>re is a sUbstantial cool<strong>in</strong>g <strong>and</strong><strong>pressure</strong> drawdown due to exploitation deep <strong>in</strong> <strong>the</strong>reservoir. It is found that <strong>temperature</strong> of <strong>the</strong> fluid isfairly stable dur<strong>in</strong>g exploitation. However, <strong>in</strong> <strong>the</strong> timebetween 1982 <strong>and</strong> 1983 significant t emperature changes areobserved In <strong>the</strong> reservoir. Th e reason for <strong>the</strong> cooli ng of<strong>the</strong> reservoir is found to be most li kely a recharge of cold<strong>in</strong>flow.

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