$Differential characterization of stress sensitivity and its main control mechanism in deep pore-fracture clastic reservoirs$
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Differential characterization of stress sensitivity and its main control mechanism in deep pore-fracture clastic reservoirs

Abstract Stress sensitivity in reservoirs is critical during the exploitation of oil and gas fields. As a deep clastic reservoir under strong tectonic compression, the Ahe Formation in the northern tectonic zone of the Kuqa depression exhibited strong stress sensitivity effect. However, the conventi...

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Autores principales:	Denglin Han, Huachao Wang, Chenchen Wang, Wenfang Yuan, Juan Zhang, Wei Lin, Rongrong Hu
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2021
Materias:	Medicine R Science Q
Acceso en línea:	https://doaj.org/article/227091b4219447169f08b3e0b7d9bcd9
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spelling	oai:doaj.org-article:227091b4219447169f08b3e0b7d9bcd92021-12-02T14:25:32ZDifferential characterization of stress sensitivity and its main control mechanism in deep pore-fracture clastic reservoirs10.1038/s41598-021-86444-32045-2322https://doaj.org/article/227091b4219447169f08b3e0b7d9bcd92021-04-01T00:00:00Zhttps://doi.org/10.1038/s41598-021-86444-3https://doaj.org/toc/2045-2322Abstract Stress sensitivity in reservoirs is critical during the exploitation of oil and gas fields. As a deep clastic reservoir under strong tectonic compression, the Ahe Formation in the northern tectonic zone of the Kuqa depression exhibited strong stress sensitivity effect. However, the conventional evaluation method by using permeability damage rate as a constraint restricts the mechanistic understanding of the strong stress sensitivity effect. In this study, morphology of stress sensitivity test curve, coupled with rate change of permeability and extent of irreversible damage in actual sample measurement through micro-CT in-situ scanning, is used to characterize differentially. The strong stress sensitivity effects of the studied intervals can be divided into three types: (1) rapid change in permeability–weak irreversible damage, (2) moderate change in permeability–strong irreversible damage and (3) moderate change in permeability–moderate irreversible damage. The strong stress sensitivity is caused by the micro-pores and micro-fractures, which are widely developed in the studied reservoir. The mechanisms caused by the two types of pore are different. The stress sensitivity effects in micro-fracture-rich reservoirs are characterized by rapid change in permeability and weak irreversible damage. Meanwhile, the stress sensitivity effects in micro-pore-rich reservoirs are manifested as moderate change in permeability and strong irreversible damage. The study shows that the differences in the content of micro-pores and micro-fractures and their reverse mechanisms of stress sensitivity co-create different types of stress sensitivity within the samples. Accordingly, the differences of the stress sensitivity type in macroscopic samples are caused by the competition between the microscopic differences of pore types.Denglin HanHuachao WangChenchen WangWenfang YuanJuan ZhangWei LinRongrong HuNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 11, Iss 1, Pp 1-12 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	Medicine R Science Q
spellingShingle	Medicine R Science Q Denglin Han Huachao Wang Chenchen Wang Wenfang Yuan Juan Zhang Wei Lin Rongrong Hu Differential characterization of stress sensitivity and its main control mechanism in deep pore-fracture clastic reservoirs
description	Abstract Stress sensitivity in reservoirs is critical during the exploitation of oil and gas fields. As a deep clastic reservoir under strong tectonic compression, the Ahe Formation in the northern tectonic zone of the Kuqa depression exhibited strong stress sensitivity effect. However, the conventional evaluation method by using permeability damage rate as a constraint restricts the mechanistic understanding of the strong stress sensitivity effect. In this study, morphology of stress sensitivity test curve, coupled with rate change of permeability and extent of irreversible damage in actual sample measurement through micro-CT in-situ scanning, is used to characterize differentially. The strong stress sensitivity effects of the studied intervals can be divided into three types: (1) rapid change in permeability–weak irreversible damage, (2) moderate change in permeability–strong irreversible damage and (3) moderate change in permeability–moderate irreversible damage. The strong stress sensitivity is caused by the micro-pores and micro-fractures, which are widely developed in the studied reservoir. The mechanisms caused by the two types of pore are different. The stress sensitivity effects in micro-fracture-rich reservoirs are characterized by rapid change in permeability and weak irreversible damage. Meanwhile, the stress sensitivity effects in micro-pore-rich reservoirs are manifested as moderate change in permeability and strong irreversible damage. The study shows that the differences in the content of micro-pores and micro-fractures and their reverse mechanisms of stress sensitivity co-create different types of stress sensitivity within the samples. Accordingly, the differences of the stress sensitivity type in macroscopic samples are caused by the competition between the microscopic differences of pore types.
format	article
author	Denglin Han Huachao Wang Chenchen Wang Wenfang Yuan Juan Zhang Wei Lin Rongrong Hu
author_facet	Denglin Han Huachao Wang Chenchen Wang Wenfang Yuan Juan Zhang Wei Lin Rongrong Hu
author_sort	Denglin Han
title	Differential characterization of stress sensitivity and its main control mechanism in deep pore-fracture clastic reservoirs
title_short	Differential characterization of stress sensitivity and its main control mechanism in deep pore-fracture clastic reservoirs
title_full	Differential characterization of stress sensitivity and its main control mechanism in deep pore-fracture clastic reservoirs
title_fullStr	Differential characterization of stress sensitivity and its main control mechanism in deep pore-fracture clastic reservoirs
title_full_unstemmed	Differential characterization of stress sensitivity and its main control mechanism in deep pore-fracture clastic reservoirs
title_sort	differential characterization of stress sensitivity and its main control mechanism in deep pore-fracture clastic reservoirs
publisher	Nature Portfolio
publishDate	2021
url	https://doaj.org/article/227091b4219447169f08b3e0b7d9bcd9
work_keys_str_mv	AT denglinhan differentialcharacterizationofstresssensitivityanditsmaincontrolmechanismindeepporefractureclasticreservoirs AT huachaowang differentialcharacterizationofstresssensitivityanditsmaincontrolmechanismindeepporefractureclasticreservoirs AT chenchenwang differentialcharacterizationofstresssensitivityanditsmaincontrolmechanismindeepporefractureclasticreservoirs AT wenfangyuan differentialcharacterizationofstresssensitivityanditsmaincontrolmechanismindeepporefractureclasticreservoirs AT juanzhang differentialcharacterizationofstresssensitivityanditsmaincontrolmechanismindeepporefractureclasticreservoirs AT weilin differentialcharacterizationofstresssensitivityanditsmaincontrolmechanismindeepporefractureclasticreservoirs AT rongronghu differentialcharacterizationofstresssensitivityanditsmaincontrolmechanismindeepporefractureclasticreservoirs
_version_	1718391357423222784

Differential characterization of stress sensitivity and its main control mechanism in deep pore-fracture clastic reservoirs

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