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    Storage of Heated Water in Underground Openings

    Source: Journal of Geotechnical Engineering:;1989:;Volume ( 115 ):;issue: 005
    Author:
    Yoshinori Inada
    ,
    Raymond L. Sterling
    DOI: 10.1061/(ASCE)0733-9410(1989)115:5(597)
    Publisher: American Society of Civil Engineers
    Abstract: A study is carried out of the anticipated effects on the rock surrounding a storage cavern due to the storage of water at elevated temperatures. Properties of granite and andesite at temperatures between 15 ° C and 100 ° C determined in laboratory experiments are then measured. The rock properties are compressive strength, tensile strength, tangential Young's modulus, Poisson's ratio, coefficient of thermal expansion, and thermal diffusivity. Results are determined for rock specimens prepared in both a dry and a wet condition. In general, the rock properties are adversely affected by moisture and by an increase in temperature. The effect of an increase in temperature is more significant in the wet‐rock specimens. The experimental rock properties determined were used in a numerical analysis to determine the effect of the storage of heated water at a temperature of 100 ° C in a 10‐m‐diameter circular underground opening at a depth of 100 m below the ground surface. For the conditions analyzed, the results indicated that rock surrounding the opening would not be overstressed.
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      Storage of Heated Water in Underground Openings

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    contributor authorYoshinori Inada
    contributor authorRaymond L. Sterling
    date accessioned2017-05-08T20:35:21Z
    date available2017-05-08T20:35:21Z
    date copyrightMay 1989
    date issued1989
    identifier other%28asce%290733-9410%281989%29115%3A5%28597%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/20456
    description abstractA study is carried out of the anticipated effects on the rock surrounding a storage cavern due to the storage of water at elevated temperatures. Properties of granite and andesite at temperatures between 15 ° C and 100 ° C determined in laboratory experiments are then measured. The rock properties are compressive strength, tensile strength, tangential Young's modulus, Poisson's ratio, coefficient of thermal expansion, and thermal diffusivity. Results are determined for rock specimens prepared in both a dry and a wet condition. In general, the rock properties are adversely affected by moisture and by an increase in temperature. The effect of an increase in temperature is more significant in the wet‐rock specimens. The experimental rock properties determined were used in a numerical analysis to determine the effect of the storage of heated water at a temperature of 100 ° C in a 10‐m‐diameter circular underground opening at a depth of 100 m below the ground surface. For the conditions analyzed, the results indicated that rock surrounding the opening would not be overstressed.
    publisherAmerican Society of Civil Engineers
    titleStorage of Heated Water in Underground Openings
    typeJournal Paper
    journal volume115
    journal issue5
    journal titleJournal of Geotechnical Engineering
    identifier doi10.1061/(ASCE)0733-9410(1989)115:5(597)
    treeJournal of Geotechnical Engineering:;1989:;Volume ( 115 ):;issue: 005
    contenttypeFulltext
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