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Temperature-induced deformational responses and microstructural alteration of sandstone

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dc.contributor.author MAHANTA, B
dc.contributor.author RANJITH, PG
dc.contributor.author VISHAL, V
dc.contributor.author SINGH, TN
dc.date.accessioned 2021-03-10T07:49:07Z
dc.date.available 2021-03-10T07:49:07Z
dc.date.issued 2020
dc.identifier.citation JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING 192 en_US
dc.identifier.issn 0920-4105
dc.identifier.issn 1873-4715
dc.identifier.uri https://doi.org/10.1016/j.petrol.2020.107239
dc.identifier.uri http://localhost:8080/xmlui/handle/100/28576
dc.description.abstract The high-temperature response of rock is quite useful for successful exploration and exploitation of various conventional as well as unconventional energy systems such as underground coal gasification, and geothermal energy, where the associated rocks are exposed to various temperature and pressure conditions. In this study, we have investigated the effect of temperature and thermal alteration of an Indian sandstone. An investigation using acoustic emission, digital image correlation through ARAMIS, micro-computed tomography (CT) techniques and thermogravimetric analysis was performed to study the mechanical responses of the sandstone with increasing temperatures. The results indicate that uniaxial compressive strength (UCS), tensile strength and elastic modulus of sandstone reduced significantly and aligned in an overall decreasing trend with increasing temperatures. The maximum and minimum UCS of sandstone were obtained at 400 degrees C and 700 degrees C, respectively. Acoustic emission (AE) responses of the sandstone indicated an early crack initiation and crack damage for high-temperature treated specimens. The deformation was further analysed using the ARAMIS digital image correlation technique, and strain levels were visually quantified that exhibited a widespread distribution of higher strain for thermally-treated specimens at 700 degrees C. Microstructural thermal damage and different pore-characteristics were studied using micro-CT techniques that provided valuable information about the connected and non-connected pores of the sandstone and their evolution with increasing temperatures. The outcomes suggest a heat-induced increment in porosity by nearly 40 percent upon heating the samples from 25 degrees C to 600 degrees C, which can be attributed due to the opening of new cracks that stimulated structural damage. en_US
dc.language.iso English en_US
dc.publisher ELSEVIER en_US
dc.subject SANDSTONE en_US
dc.subject THERMAL DAMAGE en_US
dc.subject ACOUSTIC EMISSION en_US
dc.subject MICROSTRUCTURE en_US
dc.subject MICRO-CT en_US
dc.subject MECHANICAL-PROPERTIES en_US
dc.subject FRACTURE-TOUGHNESS en_US
dc.subject THERMAL-PROPERTIES en_US
dc.subject ACOUSTIC-EMISSION en_US
dc.subject CRACK INITIATION en_US
dc.subject TENSILE-STRENGTH en_US
dc.subject GRANITIC-ROCKS en_US
dc.subject PERMEABILITY en_US
dc.subject BEHAVIOR en_US
dc.subject THRESHOLDS en_US
dc.title Temperature-induced deformational responses and microstructural alteration of sandstone en_US
dc.type Article en_US


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