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temperature and pressure in the svartsengi ... - Orkustofnun

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665.2. 1 Distribution at 700 mThe <strong>temperature</strong> dIstribution <strong>in</strong> 1978,1982 <strong>and</strong> 1983 areshown In Figures 51. 52 <strong>and</strong> 53. In <strong>the</strong> beg<strong>in</strong>n<strong>in</strong>g ofproduction In 1978 for well SO-4 <strong>and</strong> In 1982 for wells8G - 7. 80 - 8 <strong>and</strong> SO - g, <strong>temperature</strong>s close to 240 0 C areobserved at this depth . In 1983 <strong>the</strong> highest <strong>temperature</strong>sat this level are approximately 235°C. The l evel at 700 mdepth is selected here to represent <strong>the</strong> top of <strong>the</strong>geo<strong>the</strong>rmal r eservoir <strong>in</strong> Svartsengi.5.2.2 Distribution at 1000 mThis level is considered to represent <strong>the</strong> mean level In <strong>the</strong>Svartsengi reservoir . Temperature distributions In 1978,1982 <strong>and</strong> 1983 are shown In Fig. 54, 55 <strong>and</strong> 56 . In <strong>the</strong><strong>in</strong>itial state (Fig. 54) t e mperatures of 240 0 C can beexpected <strong>in</strong> wells 8G-4 <strong>and</strong> SC - 5, <strong>and</strong> most probabl y also to<strong>the</strong> SW of <strong>the</strong>se wells. In 1982 <strong>the</strong> hottest part of <strong>the</strong>reservoir is <strong>in</strong> <strong>the</strong> south where 240°C is still recorded <strong>in</strong>wells SO-7, SO-8 <strong>and</strong> SO-11 (Fig. 55). One year later <strong>the</strong>hottest place <strong>in</strong> <strong>the</strong> reservoir is <strong>in</strong> <strong>the</strong> SE <strong>and</strong> <strong>the</strong><strong>temperature</strong> <strong>the</strong>re is approximately 235°C.5.2.3 Distribution at 1100 IDThis level was chosen <strong>in</strong> order to represent <strong>the</strong> deepestcommon level <strong>in</strong> <strong>the</strong> production <strong>in</strong>terval of <strong>the</strong> reservoir.Due to <strong>the</strong> different depths of <strong>the</strong> production wells. itwas necessary to select a level where all wells can berepresented. The <strong>temperature</strong> distributions at this levelfor <strong>the</strong> years 1978, 1982 <strong>and</strong> 1983 are shown <strong>in</strong> Fig. 57, 58<strong>and</strong> 59. The picture obta<strong>in</strong>ed is almost identical to <strong>the</strong>changes observed at 1000 ID depth. The hottest part of <strong>the</strong>reservoir <strong>in</strong> 1983 is <strong>the</strong> eastern part <strong>in</strong>clud<strong>in</strong>g wells SO-8,SO-5 <strong>and</strong> SO-6. From <strong>the</strong>se considerations <strong>and</strong> o<strong>the</strong>rs

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