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    Multiple Artificial Geothermal Cracks in a Hot Dry Rock Mass for Extraction of Heat

    Source: Journal of Energy Resources Technology:;1985:;volume( 107 ):;issue: 002::page 274
    Author:
    Y. Shibuya
    ,
    H. Sekine
    ,
    Y. Takahashi
    ,
    H. Abé
    DOI: 10.1115/1.3231189
    Publisher: The American Society of Mechanical Engineers (ASME)
    Abstract: Theoretical analysis is made for multiple geothermal cracks. A periodic array of two-dimensional cracks is considered as a model of the multiple geothermal cracks, and is anlayzed on the basis of the two-dimensional theory of quasi-static thermo-elasticity. The singular integral equations are derived from the boundary conditions, and they are solved by applying the combination of inversion formula and collocation method. Numerical results for the fluid temperature at an outlet, the rock mass temperature, the shape of the geothermal cracks and the stress distribution around the geothermal cracks are shown in graphs.
    keyword(s): Heat , Geothermal engineering , Fracture (Materials) , Rocks , Temperature , Fluids , Stress concentration , Boundary-value problems , Formulas , Integral equations , Shapes , Theoretical analysis AND Thermoelasticity ,
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      Multiple Artificial Geothermal Cracks in a Hot Dry Rock Mass for Extraction of Heat

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/99691
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    • Journal of Energy Resources Technology

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    contributor authorY. Shibuya
    contributor authorH. Sekine
    contributor authorY. Takahashi
    contributor authorH. Abé
    date accessioned2017-05-08T23:19:57Z
    date available2017-05-08T23:19:57Z
    date copyrightJune, 1985
    date issued1985
    identifier issn0195-0738
    identifier otherJERTD2-26404#274_1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/99691
    description abstractTheoretical analysis is made for multiple geothermal cracks. A periodic array of two-dimensional cracks is considered as a model of the multiple geothermal cracks, and is anlayzed on the basis of the two-dimensional theory of quasi-static thermo-elasticity. The singular integral equations are derived from the boundary conditions, and they are solved by applying the combination of inversion formula and collocation method. Numerical results for the fluid temperature at an outlet, the rock mass temperature, the shape of the geothermal cracks and the stress distribution around the geothermal cracks are shown in graphs.
    publisherThe American Society of Mechanical Engineers (ASME)
    titleMultiple Artificial Geothermal Cracks in a Hot Dry Rock Mass for Extraction of Heat
    typeJournal Paper
    journal volume107
    journal issue2
    journal titleJournal of Energy Resources Technology
    identifier doi10.1115/1.3231189
    journal fristpage274
    journal lastpage279
    identifier eissn1528-8994
    keywordsHeat
    keywordsGeothermal engineering
    keywordsFracture (Materials)
    keywordsRocks
    keywordsTemperature
    keywordsFluids
    keywordsStress concentration
    keywordsBoundary-value problems
    keywordsFormulas
    keywordsIntegral equations
    keywordsShapes
    keywordsTheoretical analysis AND Thermoelasticity
    treeJournal of Energy Resources Technology:;1985:;volume( 107 ):;issue: 002
    contenttypeFulltext
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