temperature and pressure in the svartsengi ... - Orkustofnun

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:r:I JHO-H$P - 2300 GG~ 83.08. 1023 Ab.SVARTSENGI 1983Cross section - F'" ~SG- #art"SG-8D ept h 204.1[m]500~ 219_6-+--237.1."'3 0 __SG-5 SG -6197. 0207.62172:223.8224.1227.5203.02296SG - 12150.0 .199.4220.57 50 -1239_724'7:0
f"i'T"':lJHO~HSP-2]OO GGL.:..L...J 83.08.1024 U.SVARTSENGI 1983Cross section- F5G-#Depth[m]5005G-8 SG-5 SG-6 SG-120~1--+---------~--------+---------1-----------!71.~204.'lIT.'1 203.0220.226 .4 221.3 291 ,,230I- 15. 8213 • UI.' U3.4 "'", ~ll .. 32262750234. ' 231.8 U55 219 4234.7 no.'""234. ' 234. ' Bro uu1000 234.' 2l5.5 2385 U5.312502H.9 235.5 238 8 U5. 3,234. '2l5~U81 U2 5235.0 UB8 Ut l235.0 U'O 22841500 235.0 1592.;235.0- -.; 2)92 00 •- •L0 •• 0 •2000 ..-" •1750.. •"U ••V> '"Fig.50 Cross-section F. Temperature distribution <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 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: time , but the change in temperatur
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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