Experimental Study on the Mechanical Properties of CH4 and CO2 Hydrate Remodeling Cores in Qilian Mountain

The CH4-CO2 replacement method has attracted global attention as a new promising method for methane hydrate exploitation. In the replacement process, the mechanical stabilities of CH4 and CO2 hydrate-bearing sediments have become problems requiring attention. In this paper, considering the hydrate c...

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Main Authors: Tingting Luo, Yanghui Li, Weiguo Liu, Xiang Sun, Shi Shen
Format: Article
Language:English
Published: MDPI AG 2017-12-01
Series:Energies
Subjects:
Online Access:https://www.mdpi.com/1996-1073/10/12/2078
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author Tingting Luo
Yanghui Li
Weiguo Liu
Xiang Sun
Shi Shen
author_facet Tingting Luo
Yanghui Li
Weiguo Liu
Xiang Sun
Shi Shen
author_sort Tingting Luo
collection DOAJ
description The CH4-CO2 replacement method has attracted global attention as a new promising method for methane hydrate exploitation. In the replacement process, the mechanical stabilities of CH4 and CO2 hydrate-bearing sediments have become problems requiring attention. In this paper, considering the hydrate characteristics and burial conditions of hydrate-bearing cores, sediments matrices were formed by a mixture of kaolin clay and quartz sand, and an experimental study was focused on the failure strength of CH4 and CO2 hydrate-bearing sediments under different conditions to verify the mechanical reliability of CH4-CO2 replacement in permafrost-associated natural gas deposits. A series of triaxial shear tests were conducted on the CH4 and CO2 hydrate-bearing sediments under temperatures of −20, −10, and −5 °C, confining pressures of 2.5, 3.75, 5, 7.5, and 10 MPa, and a strain rate of 1.0 mm/min. The results indicated that the failure strength of the CO2 hydrate-bearing sediments was higher than that of the CH4 hydrate-bearing sediments under different confining pressures and temperatures; the failure strength of the CH4 and CO2 hydrate-bearing sediments increased with an increase in confining pressure at a low confining pressure state. Besides that, the failure strength of all hydrate-bearing sediments decreased with an increase in temperature; all the failure strengths of the CO2 hydrate-bearing sediments were higher than those of the CH4 hydrate-bearing sediments in different sediment matrices. The experiments proved that the hydrate-bearing sediments would be more stable than that before CH4-CO2 replacement.
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spelling doaj.art-72b0fef49f8c4e7fba380546580b243e2022-12-22T02:57:14ZengMDPI AGEnergies1996-10732017-12-011012207810.3390/en10122078en10122078Experimental Study on the Mechanical Properties of CH4 and CO2 Hydrate Remodeling Cores in Qilian MountainTingting Luo0Yanghui Li1Weiguo Liu2Xiang Sun3Shi Shen4Key Laboratory of Ocean Energy Utilization and Energy Conservation of the Ministry of Education, Dalian University of Technology, Dalian 116024, ChinaKey Laboratory of Ocean Energy Utilization and Energy Conservation of the Ministry of Education, Dalian University of Technology, Dalian 116024, ChinaKey Laboratory of Ocean Energy Utilization and Energy Conservation of the Ministry of Education, Dalian University of Technology, Dalian 116024, ChinaKey Laboratory of Ocean Energy Utilization and Energy Conservation of the Ministry of Education, Dalian University of Technology, Dalian 116024, ChinaKey Laboratory of Ocean Energy Utilization and Energy Conservation of the Ministry of Education, Dalian University of Technology, Dalian 116024, ChinaThe CH4-CO2 replacement method has attracted global attention as a new promising method for methane hydrate exploitation. In the replacement process, the mechanical stabilities of CH4 and CO2 hydrate-bearing sediments have become problems requiring attention. In this paper, considering the hydrate characteristics and burial conditions of hydrate-bearing cores, sediments matrices were formed by a mixture of kaolin clay and quartz sand, and an experimental study was focused on the failure strength of CH4 and CO2 hydrate-bearing sediments under different conditions to verify the mechanical reliability of CH4-CO2 replacement in permafrost-associated natural gas deposits. A series of triaxial shear tests were conducted on the CH4 and CO2 hydrate-bearing sediments under temperatures of −20, −10, and −5 °C, confining pressures of 2.5, 3.75, 5, 7.5, and 10 MPa, and a strain rate of 1.0 mm/min. The results indicated that the failure strength of the CO2 hydrate-bearing sediments was higher than that of the CH4 hydrate-bearing sediments under different confining pressures and temperatures; the failure strength of the CH4 and CO2 hydrate-bearing sediments increased with an increase in confining pressure at a low confining pressure state. Besides that, the failure strength of all hydrate-bearing sediments decreased with an increase in temperature; all the failure strengths of the CO2 hydrate-bearing sediments were higher than those of the CH4 hydrate-bearing sediments in different sediment matrices. The experiments proved that the hydrate-bearing sediments would be more stable than that before CH4-CO2 replacement.https://www.mdpi.com/1996-1073/10/12/2078CH4-CO2 replacementhydrate-bearing sedimentsremodeling coresstress-strain curvesfailure strengthcohesion force
spellingShingle Tingting Luo
Yanghui Li
Weiguo Liu
Xiang Sun
Shi Shen
Experimental Study on the Mechanical Properties of CH4 and CO2 Hydrate Remodeling Cores in Qilian Mountain
Energies
CH4-CO2 replacement
hydrate-bearing sediments
remodeling cores
stress-strain curves
failure strength
cohesion force
title Experimental Study on the Mechanical Properties of CH4 and CO2 Hydrate Remodeling Cores in Qilian Mountain
title_full Experimental Study on the Mechanical Properties of CH4 and CO2 Hydrate Remodeling Cores in Qilian Mountain
title_fullStr Experimental Study on the Mechanical Properties of CH4 and CO2 Hydrate Remodeling Cores in Qilian Mountain
title_full_unstemmed Experimental Study on the Mechanical Properties of CH4 and CO2 Hydrate Remodeling Cores in Qilian Mountain
title_short Experimental Study on the Mechanical Properties of CH4 and CO2 Hydrate Remodeling Cores in Qilian Mountain
title_sort experimental study on the mechanical properties of ch4 and co2 hydrate remodeling cores in qilian mountain
topic CH4-CO2 replacement
hydrate-bearing sediments
remodeling cores
stress-strain curves
failure strength
cohesion force
url https://www.mdpi.com/1996-1073/10/12/2078
work_keys_str_mv AT tingtingluo experimentalstudyonthemechanicalpropertiesofch4andco2hydrateremodelingcoresinqilianmountain
AT yanghuili experimentalstudyonthemechanicalpropertiesofch4andco2hydrateremodelingcoresinqilianmountain
AT weiguoliu experimentalstudyonthemechanicalpropertiesofch4andco2hydrateremodelingcoresinqilianmountain
AT xiangsun experimentalstudyonthemechanicalpropertiesofch4andco2hydrateremodelingcoresinqilianmountain
AT shishen experimentalstudyonthemechanicalpropertiesofch4andco2hydrateremodelingcoresinqilianmountain