temperature and pressure in the svartsengi ... - Orkustofnun
temperature and pressure in the svartsengi ... - Orkustofnun temperature and pressure in the svartsengi ... - Orkustofnun
1 6~JHD-8 J - Z300 Hr.L'J:J 8 ~~0703 AAADepth[m)5009 11 7 8 4 5 6 12 :3 2100'-~----++---+4-~-+--~~~BI u"'"u'">-" t.J>,,'"!.J>....'" ::>"....z1000t 11 H1500\-rM ,'"~" .... -,,~;~"" ..... ,>,,'" ~:,'I;.... ''''-' /i:, ,I'-.!.--I!, ," :, " \' ,, -, -, '" ,~,
1 72.3 Resistivity studies of the fieldSurface hydrothermal manifestations are meager within theSvartsengi field and only scattered over about 4 squarekl1ometers. The resistivity surveys (Fig. 4) show thegeothermal area to be elongated NE - SW 1n the northern partbut ESE-WSW in the southern part (Georgsson, 1981), Acontinuous E- W striking low resistivity zone whichcoincides fairly closely wi th the Reykjanes seismic zonetha t has been interpreted as a plate boundary. Study ofcorrelation between resistivity salinity and temperatureseem to confirm that the low resistivity can only beexplained by anomalously high heat flow . This indicatesthat explol table geothermal energy may be found 1n theuppermost 1 - 2 km along the plate boundaries on theReykjanes Peninsula even far away from surface manifestations.2.~ TectoniC activity of the Reykjanes peninsulaOne can see the main zone of earthquakes and location ofquake epicenters on the area from Fig. 1. The tectonicactivity increases the permeability and thus creates somesort of a drainage system along the zone of earthquakes.Some geothermal areas like Svartsengi are situated wheresurface fissure swarms intersect the main zone of earthquakes.2.5 Hydrological characteristics of the geotherma l systemThe water percolates down from the infiltration area andflows along the permeable earthquake zone. On its way itwarms up and mixes with intrusive seawater. Where thesurface fissure swarms intersect the earthquake zone. thepermeability becomes great enough to allow free convection,thus forming a geothermal area.
- Page 1: TEMPERATURE ANDPRESSURE INTHE SVART
- Page 5 and 6: 5LIST OF CONTENTSPag eABSTRACT ....
- Page 7 and 8: 7Fig. 5 Conceptual flow model from
- Page 9 and 10: 9Fig.32 Svartsengi well SG-l0. Pres
- Page 11 and 12: 111 INTRODUCTION1.1 Scope of the re
- Page 13 and 14: 1 3to the former (Georgsson. 1981;
- Page 15: u JHD - BJ~2300 HF,83.05.0702 AAI>-
- Page 19 and 20: 1 9Fresh water is pumped from shall
- Page 21 and 22: ... T [IIKFII€9ISlOFoVI VII2.O
- Page 23 and 24: 2 3~ JHO-HSP - 2300 G9~ 83.091236 A
- Page 25 and 26: 25commissioned. Well SG - 7 was dri
- Page 27 and 28: 27~ J H D-HS~ - 9 0 00 Gl:iL.J::..J
- Page 29 and 30: 293.2 Temperature elementThe bourdo
- Page 31 and 32: SVARTSENG I ,WEL L SG-1SVAR TSENG I
- Page 33 and 34: 33temperature at the bottom of the
- Page 35 and 36: -".(!)'W (!)rJ)rJ)fa...J WrJ) 3-"
- Page 37 and 38: SVARTSENGIWELL SG-5SVARTSENGIWELL S
- Page 39 and 40: SVARTSENGIWELL SG-6SVARTSENGIWELL S
- Page 41 and 42: SVARTSENGI\JELL SG-7SVARTSENGIwELL
- Page 43 and 44: 430NNN~~•-••;;• •~0l•0
- Page 45 and 46: 45pressure profiles in Fig. 32. In
- Page 47 and 48: 47N,~• ~, •8 •"•a'i:i•L-N
- Page 49 and 50: ;-r-::I J HO - HS" - 2 300 Gq\//Ll:
- Page 51 and 52: EI]JHO-HSI> . 2300 GGI 83.08.1020 A
- Page 53 and 54: 53reservoir during 1976- 1981 Is fr
- Page 55 and 56: 55~ JHD-HSP-2300 GC!L...C.J 83.08.1
- Page 57 and 58: 575.1.~ Cross-section DIt is an E-W
- Page 59 and 60: 59rnJHO-HSI:>-Z300 GG.83 .08 .1010
- Page 61 and 62: I"jT'=I~ HD-H S P - 2 500 GC;L..t.J
- Page 63 and 64: time , but the change in temperatur
- Page 65 and 66: f"i'T"':lJHO~HSP-2]OO GGL.:..L...J
1 6~JHD-8 J - Z300 Hr.L'J:J 8 ~~0703 AAADepth[m)5009 11 7 8 4 5 6 12 :3 2100'-~----++---+4-~-+--~~~BI u"'"u'">-" t.J>,,'"!.J>....'" ::>"....z1000t 11 H1500\-rM ,'"~" .... -,,~;~"" ..... ,>,,'" ~:,'I;.... ''''-' /i:, ,I'-.!.--I!, ," :, " \' ,, -, -, '" ,~,
Change language