Titill:
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A conceptual reservoir model and numerical simulation studies for the Miravalles geothermal field, Costa RicaA conceptual reservoir model and numerical simulation studies for the Miravalles geothermal field, Costa Rica |
Höfundur:
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Vallejos, Osvaldo E.
;
Jarðhitaskóli Háskóla Sameinuðu þjóðanna
|
URI:
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http://hdl.handle.net/10802/23312
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Útgefandi:
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United Nations University; Orkustofnun
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Útgáfa:
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1996 |
Ritröð:
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United Nations University., UNU Geothermal Training Programme, Iceland. Report ; 1996:18 |
Efnisorð:
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Jarðhiti; Jarðhitarannsóknir; Jarðhitanýting; Kosta Ríka
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ISSN:
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1670-7427 |
Tungumál:
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Enska
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Tengd vefsíðuslóð:
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http://www.os.is/gogn/unu-gtp-report/UNU-GTP-1996-18.pdf
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Tegund:
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Bók |
Gegnir ID:
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991010424449706886
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Athugasemdir:
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Myndefni: kort, línurit, töflur. |
Útdráttur:
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Commercial exploitation of the Miravalles geothermal field started in 1994 with eleven production wells and six reinjection wells. In this report a general description of the field is given. A conceptual model is defined, based on estimated formation temperatures and initial pressures in twenty-five wells. In the conceptual reservoir model a 260°C upflow zone is proposed in the north and an outflow zone in the south. The geothermal fluid moves laterally to the south at -100 to -300 m a.s.l. The wellfield is clearly bounded to the west by cold temperatures and low pressures. The character of the eastern boundary is unknown due to a lack of data in that region. Lumped modelling simulation suggests that the Miravalles field will behave as a closed reservoir system for the next years, resulting in rapid drawdown with time. This model may be pessimistic as only net production is considered in the study. A 3-D natural state model simulates reasonably well the temperature distribution in the wellfield, by using a large recharge rate of 180 kg/s of 270°C fluid and very low thermal conductivity of model boundaries. Further modelling studies must address critical questions such as future development of a two-phase reservoir zone, the destiny of reinjected fluids and the nature of the outflow zone south of the wellfield. |