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Experimental Investigation of Mechanical Properties of Black Shales after CO(2)-Water-Rock Interaction

The effects of CO(2)-water-rock interactions on the mechanical properties of shale are essential for estimating the possibility of sequestrating CO(2) in shale reservoirs. In this study, uniaxial compressive strength (UCS) tests together with an acoustic emission (AE) system and SEM and EDS analysis...

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Autores principales: Lyu, Qiao, Ranjith, Pathegama Gamage, Long, Xinping, Ji, Bin
Formato: Online Artículo Texto
Lenguaje:English
Publicado: MDPI 2016
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5509274/
https://www.ncbi.nlm.nih.gov/pubmed/28773784
http://dx.doi.org/10.3390/ma9080663
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author Lyu, Qiao
Ranjith, Pathegama Gamage
Long, Xinping
Ji, Bin
author_facet Lyu, Qiao
Ranjith, Pathegama Gamage
Long, Xinping
Ji, Bin
author_sort Lyu, Qiao
collection PubMed
description The effects of CO(2)-water-rock interactions on the mechanical properties of shale are essential for estimating the possibility of sequestrating CO(2) in shale reservoirs. In this study, uniaxial compressive strength (UCS) tests together with an acoustic emission (AE) system and SEM and EDS analysis were performed to investigate the mechanical properties and microstructural changes of black shales with different saturation times (10 days, 20 days and 30 days) in water dissoluted with gaseous/super-critical CO(2). According to the experimental results, the values of UCS, Young’s modulus and brittleness index decrease gradually with increasing saturation time in water with gaseous/super-critical CO(2). Compared to samples without saturation, 30-day saturation causes reductions of 56.43% in UCS and 54.21% in Young’s modulus for gaseous saturated samples, and 66.05% in UCS and 56.32% in Young’s modulus for super-critical saturated samples, respectively. The brittleness index also decreases drastically from 84.3% for samples without saturation to 50.9% for samples saturated in water with gaseous CO(2), to 47.9% for samples saturated in water with super-critical carbon dioxide (SC-CO(2)). SC-CO(2) causes a greater reduction of shale’s mechanical properties. The crack propagation results obtained from the AE system show that longer saturation time produces higher peak cumulative AE energy. SEM images show that many pores occur when shale samples are saturated in water with gaseous/super-critical CO(2). The EDS results show that CO(2)-water-rock interactions increase the percentages of C and Fe and decrease the percentages of Al and K on the surface of saturated samples when compared to samples without saturation.
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spelling pubmed-55092742017-07-28 Experimental Investigation of Mechanical Properties of Black Shales after CO(2)-Water-Rock Interaction Lyu, Qiao Ranjith, Pathegama Gamage Long, Xinping Ji, Bin Materials (Basel) Article The effects of CO(2)-water-rock interactions on the mechanical properties of shale are essential for estimating the possibility of sequestrating CO(2) in shale reservoirs. In this study, uniaxial compressive strength (UCS) tests together with an acoustic emission (AE) system and SEM and EDS analysis were performed to investigate the mechanical properties and microstructural changes of black shales with different saturation times (10 days, 20 days and 30 days) in water dissoluted with gaseous/super-critical CO(2). According to the experimental results, the values of UCS, Young’s modulus and brittleness index decrease gradually with increasing saturation time in water with gaseous/super-critical CO(2). Compared to samples without saturation, 30-day saturation causes reductions of 56.43% in UCS and 54.21% in Young’s modulus for gaseous saturated samples, and 66.05% in UCS and 56.32% in Young’s modulus for super-critical saturated samples, respectively. The brittleness index also decreases drastically from 84.3% for samples without saturation to 50.9% for samples saturated in water with gaseous CO(2), to 47.9% for samples saturated in water with super-critical carbon dioxide (SC-CO(2)). SC-CO(2) causes a greater reduction of shale’s mechanical properties. The crack propagation results obtained from the AE system show that longer saturation time produces higher peak cumulative AE energy. SEM images show that many pores occur when shale samples are saturated in water with gaseous/super-critical CO(2). The EDS results show that CO(2)-water-rock interactions increase the percentages of C and Fe and decrease the percentages of Al and K on the surface of saturated samples when compared to samples without saturation. MDPI 2016-08-06 /pmc/articles/PMC5509274/ /pubmed/28773784 http://dx.doi.org/10.3390/ma9080663 Text en © 2016 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC-BY) license (http://creativecommons.org/licenses/by/4.0/).
spellingShingle Article
Lyu, Qiao
Ranjith, Pathegama Gamage
Long, Xinping
Ji, Bin
Experimental Investigation of Mechanical Properties of Black Shales after CO(2)-Water-Rock Interaction
title Experimental Investigation of Mechanical Properties of Black Shales after CO(2)-Water-Rock Interaction
title_full Experimental Investigation of Mechanical Properties of Black Shales after CO(2)-Water-Rock Interaction
title_fullStr Experimental Investigation of Mechanical Properties of Black Shales after CO(2)-Water-Rock Interaction
title_full_unstemmed Experimental Investigation of Mechanical Properties of Black Shales after CO(2)-Water-Rock Interaction
title_short Experimental Investigation of Mechanical Properties of Black Shales after CO(2)-Water-Rock Interaction
title_sort experimental investigation of mechanical properties of black shales after co(2)-water-rock interaction
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5509274/
https://www.ncbi.nlm.nih.gov/pubmed/28773784
http://dx.doi.org/10.3390/ma9080663
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