temperature and pressure in the svartsengi ... - Orkustofnun

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84Kjaran, S.P., Halldorsson G. K. , Thorhallsson, S . andEllasson J . , 1979: Reservoir engIneerIng aspects ofSvartsengl geothermal area. Geothermal ResourcesTransactions, 3, 337-339 .Kj a ran, S.P., Ellasson, J . and Halldorsson , G. K • • 1980:Svartsengl. Athugun a vinnslu jardhita . Orkustofnunreport OS800021/1980 , ROD10 - JH D17 .Mlchaelldes , E. E . • 1981: ThermodynamIc properties of geothermalf l uIds . Geot hermal Resources Counc i lTransactions , S . 361-364 .Stefansson . V. and Steingrimss on, B., 1981 : Geotherma lLogging, An introduction to techniques and i n t erpretation. Orkustofnun report OS800 17/JHD09,Reykjavik , 117 p .Thorhallsson, S.,19 79 : Combined generation of heat andelectricity from a geothermal brine a t Svartseng iin SW-Iceland . Geothermal Resources CouncilTransactions , 3, 733-736 .Vatnaskil, 1982 : Svartsengi . Vatnsbordslaekkun me d vinnslu .Report to Hltaveita Sudurnesja by Vatnaskil Ltd . •July 1982 .
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 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: 83REFERENCESArnason, B .• 1976: G
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