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    Modeling of a Magma Energy Geothermal Open Cycle Power Plant

    Source: Journal of Energy Resources Technology:;1989:;volume( 111 ):;issue: 004::page 239
    Author:
    R. F. Boehm
    ,
    A. Ortega
    ,
    D. L. Berg
    DOI: 10.1115/1.3231430
    Publisher: The American Society of Mechanical Engineers (ASME)
    Abstract: We are currently investigating the engineering feasibility of drilling into an active magma body at a depth of roughly 5 km from the earth’s surface, establishing a downhole heat exchange region, and extracting thermal energy from the magma body by circulating fluid through this heat exchange region. In the present paper, we evaluate the overall thermodynamic performance of a conceptual magma energy system in which energy is added as heat to the fluid within the magma region and is converted to useful work in a power conversion cycle at the surface. Unusually high return temperatures and pressures may be available at the wellhead of such a circulating well. Investigated here is an open Rankine power system in which heated water from the magma well is circulated directly through a power conversion cycle. The downhole heat exchange region is established during the drilling process. As drilling proceeds into the magma, a solidified layer forms about the drilling tube due to heat exchange to the fluid. This solidified layer thermally fractures because of large temperature gradients between the cooled inner region and the heater outer region, thereby opening secondary flow paths. Two models of the downhole behavior have been used. In the simplest approach, denoted as the “infinite area model,” the water entering the pipe to return to the surface is assumed to be always at the temperature of the magma, independent of mass flow rate and other parameters. The other model is more detailed and the fractured heat exchange region is modeled as a cylindrical porous layer through which fluid flows vertically. The net power and other performance aspects for the systems are investigated in terms of various parameters, including the characteristics of the downhole heat transfer. It is concluded that the open Rankine cycle probably will not be appropriate for this application; however, the analysis provides the first insights into possible characteristics of this energy resource.
    keyword(s): Geothermal engineering , Modeling , Power stations , Cycles , Heat , Drilling , Fluids , Water , Temperature , Flow (Dynamics) , Energy conversion , Energy resources , Fracture (Process) , Fluid dynamics , Heat transfer , Temperature gradients , Rankine cycle , Power systems (Machinery) , Thermal energy AND Pipes ,
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      Modeling of a Magma Energy Geothermal Open Cycle Power Plant

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    http://yetl.yabesh.ir/yetl1/handle/yetl/105285
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    • Journal of Energy Resources Technology

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    contributor authorR. F. Boehm
    contributor authorA. Ortega
    contributor authorD. L. Berg
    date accessioned2017-05-08T23:29:47Z
    date available2017-05-08T23:29:47Z
    date copyrightDecember, 1989
    date issued1989
    identifier issn0195-0738
    identifier otherJERTD2-26430#239_1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/105285
    description abstractWe are currently investigating the engineering feasibility of drilling into an active magma body at a depth of roughly 5 km from the earth’s surface, establishing a downhole heat exchange region, and extracting thermal energy from the magma body by circulating fluid through this heat exchange region. In the present paper, we evaluate the overall thermodynamic performance of a conceptual magma energy system in which energy is added as heat to the fluid within the magma region and is converted to useful work in a power conversion cycle at the surface. Unusually high return temperatures and pressures may be available at the wellhead of such a circulating well. Investigated here is an open Rankine power system in which heated water from the magma well is circulated directly through a power conversion cycle. The downhole heat exchange region is established during the drilling process. As drilling proceeds into the magma, a solidified layer forms about the drilling tube due to heat exchange to the fluid. This solidified layer thermally fractures because of large temperature gradients between the cooled inner region and the heater outer region, thereby opening secondary flow paths. Two models of the downhole behavior have been used. In the simplest approach, denoted as the “infinite area model,” the water entering the pipe to return to the surface is assumed to be always at the temperature of the magma, independent of mass flow rate and other parameters. The other model is more detailed and the fractured heat exchange region is modeled as a cylindrical porous layer through which fluid flows vertically. The net power and other performance aspects for the systems are investigated in terms of various parameters, including the characteristics of the downhole heat transfer. It is concluded that the open Rankine cycle probably will not be appropriate for this application; however, the analysis provides the first insights into possible characteristics of this energy resource.
    publisherThe American Society of Mechanical Engineers (ASME)
    titleModeling of a Magma Energy Geothermal Open Cycle Power Plant
    typeJournal Paper
    journal volume111
    journal issue4
    journal titleJournal of Energy Resources Technology
    identifier doi10.1115/1.3231430
    journal fristpage239
    journal lastpage245
    identifier eissn1528-8994
    keywordsGeothermal engineering
    keywordsModeling
    keywordsPower stations
    keywordsCycles
    keywordsHeat
    keywordsDrilling
    keywordsFluids
    keywordsWater
    keywordsTemperature
    keywordsFlow (Dynamics)
    keywordsEnergy conversion
    keywordsEnergy resources
    keywordsFracture (Process)
    keywordsFluid dynamics
    keywordsHeat transfer
    keywordsTemperature gradients
    keywordsRankine cycle
    keywordsPower systems (Machinery)
    keywordsThermal energy AND Pipes
    treeJournal of Energy Resources Technology:;1989:;volume( 111 ):;issue: 004
    contenttypeFulltext
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