temperature and pressure in the svartsengi ... - Orkustofnun

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54rn.JHO.HS~.2300 GG83.08. 1013 Ail.SG - #0SG-12SVARTSENGI 1982 -Cross section - 8,SG-6SG-5Depth[m]14H190 4 17 .. 197.0203·°,09.6"0.0 203.0 219.2«,..500 199.4- 226/_ '1. '1.0229:~220.'233.4 227.:5'1.30234.2 230.0 I-750221.4 2. 3:5.:5 232.3-,,=>'>226. :5 '(, 237.0 236.9V1000, 232 .2 238.:5 237.81250232 .4 238.8 238 .:5228 .5 238 .8238.72. 29.6 238.8 NN233.4 239.0/ ~ '"234.3 N.,239,21500 /N0239. 2.- 0lli175020000 '"N.,Flg.~l Cross-sectlon B. Tem perature distribution <strong>in</strong> 1982.
55~ JHD-HSP-2300 GC!L...C.J 83.08.1014 AASG-#Depth[m]500SG-12SVARTSENGI 1983Cross section - BSG-6SG-5Or-----+----------------r------------+TemperatureDistribution(OC)213 .3 2302. 25 .3220---~~ __ __222.4352 35.42: 7.9750226.2219.4238 .1237.8221.9237.91000225.3236. 4235.5225,3236.4235..51250225.5222.3236 .1235.51500'":g'"1750 -"'228 .42. 2 8 .8/235.3235.4235.423!1 .0234.711'" C>'" -"'2000C> '"_Ill236 .1Flg.42 Cross- section B. Temperature distributi on <strong>in</strong> 1983·
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 and 16: u JHD - BJ~2300 HF,83.05.0702 AAI>-
Page 17 and 18: 1 72.3 Resistivity studies of the f
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: 53reservoir during 1976- 1981 Is fr
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
Page 67 and 68: 67r;r.:I~HO ·Hs~-noo GGL.:..J::J l
Page 69 and 70: 69["j'T'=l JHO·HS ~- 2.100 GGL.:..
Page 71 and 72: 7 1r,r::l JHO-HS P- 2 300 GG~ a3 .
Page 73 and 74: 73~ JHD·HSJ> · 2300 GOt..:J:.J 83
Page 75 and 76: 75rn JHD·HS~-2300GG83.09.1274 A"AS
Page 77 and 78: 777 CAUSES OF TEMPERATURE CHANGESEx
Page 79 and 80: 797.4 Decreased lateral inflow of h
Page 81 and 82: 818 CONCLUSIONS1. The Svartsengl re
Page 83 and 84: 83REFERENCESArnason, B .• 1976: G
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