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    Pressure-Retarded Osmosis Thermosyphon

    Source: Journal of Solar Energy Engineering:;2018:;volume( 140 ):;issue: 005::page 51006
    Author:
    Arias, Francisco J.
    ,
    de las Heras, Salvador
    DOI: 10.1115/1.4039893
    Publisher: The American Society of Mechanical Engineers (ASME)
    Abstract: The basis of a novel method for passive solar water heating homologous to the traditional thermosyphon but driven by salinity gradient induced by changes of salinity gradient induced by evaporation at the collector is outlined. Its purpose, likewise than a thermosyphon, is to simplify the transfer of liquid while avoiding the cost and complexity of a conventional pump. However, in this concept, the fluid motion is not obtained from the tendency of a less dense fluid to rise above a denser fluid (natural convection) but rather by taking advantage of the energy released during the spontaneous mixing of the low-concentration (evaporated fraction) solution and the high-concentration (no-evaporated fraction) solution, which have been previously separated into two streams in the evaporator module. Finally, the possibility of driving the thermal osmosis by the strong thermal dependence of the solubility featured by many solutions rather than evaporation is envisaged. One important point in favor of the proposed thermosyphon driven by thermo-osmosis is that makes possible downward heat and mass transfer, i.e., heat and mass transport from the top roofs (where solar collectors are generally placed) to the bottom (inside the homes), and then the use of expensive and voluminous tanks so characteristic of current thermosyphons driven by natural convection is no longer needed.
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      Pressure-Retarded Osmosis Thermosyphon

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4252877
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    contributor authorArias, Francisco J.
    contributor authorde las Heras, Salvador
    date accessioned2019-02-28T11:07:08Z
    date available2019-02-28T11:07:08Z
    date copyright5/29/2018 12:00:00 AM
    date issued2018
    identifier issn0199-6231
    identifier othersol_140_05_051006.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4252877
    description abstractThe basis of a novel method for passive solar water heating homologous to the traditional thermosyphon but driven by salinity gradient induced by changes of salinity gradient induced by evaporation at the collector is outlined. Its purpose, likewise than a thermosyphon, is to simplify the transfer of liquid while avoiding the cost and complexity of a conventional pump. However, in this concept, the fluid motion is not obtained from the tendency of a less dense fluid to rise above a denser fluid (natural convection) but rather by taking advantage of the energy released during the spontaneous mixing of the low-concentration (evaporated fraction) solution and the high-concentration (no-evaporated fraction) solution, which have been previously separated into two streams in the evaporator module. Finally, the possibility of driving the thermal osmosis by the strong thermal dependence of the solubility featured by many solutions rather than evaporation is envisaged. One important point in favor of the proposed thermosyphon driven by thermo-osmosis is that makes possible downward heat and mass transfer, i.e., heat and mass transport from the top roofs (where solar collectors are generally placed) to the bottom (inside the homes), and then the use of expensive and voluminous tanks so characteristic of current thermosyphons driven by natural convection is no longer needed.
    publisherThe American Society of Mechanical Engineers (ASME)
    titlePressure-Retarded Osmosis Thermosyphon
    typeJournal Paper
    journal volume140
    journal issue5
    journal titleJournal of Solar Energy Engineering
    identifier doi10.1115/1.4039893
    journal fristpage51006
    journal lastpage051006-4
    treeJournal of Solar Energy Engineering:;2018:;volume( 140 ):;issue: 005
    contenttypeFulltext
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    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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