Microscopic distribution of fluid in Sulige tight sandstone gas reservoir and its influencing factors
The Lower Shihezi Formation in the eastern part of Sulige gas field has high water content, where the exploitation of tight sandstone gas reservoir is considerably affected by the characteristics of fluid occurrence. Specifically, this study analyzed the porosity, permeability, lithology, pore throa...
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Emergency Management Press
2023-12-01
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Series: | 矿业科学学报 |
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Online Access: | http://kykxxb.cumtb.edu.cn/en/article/doi/10.19606/j.cnki.jmst.2023.06.002 |
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author | Zhang Hanpeng Ren Dazhong Zhang Rongjun Qu Le Li Tian Li Qihui |
author_facet | Zhang Hanpeng Ren Dazhong Zhang Rongjun Qu Le Li Tian Li Qihui |
author_sort | Zhang Hanpeng |
collection | DOAJ |
description | The Lower Shihezi Formation in the eastern part of Sulige gas field has high water content, where the exploitation of tight sandstone gas reservoir is considerably affected by the characteristics of fluid occurrence. Specifically, this study analyzed the porosity, permeability, lithology, pore throat heterogeneity and connectivity and their effects on fluid occurrenceby rock and ore identification, porosity and permeability analysis and NMR centrifugation. Results show that: ①the tight sandstone reservoir in the study area shows poor pore flow capacity, and bound water saturation. The flow capacity is closely related to the gas flow pressure difference (centrifugal force). ②Intercalations play a key role in controlling flow capacity. Abundant kaolinite content indicates that the reservoir has better connectivity, larger pore size and stronger overall pore water flow capacity. Illite has a strong water-holding capacity, which could easily cause capillary obstruction and limited flow capacity. ③The gas flow pressure difference (centrifugal force)is exponentially related to the pore diameter of reservoir pore water flow. ④The critical pore throat radius of the effective reservoir space is 0.089μm, and the mobile water saturation is 23.95% in Xiashihezi Formation in the eastern part of Sulige gas field. |
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institution | Directory Open Access Journal |
issn | 2096-2193 |
language | English |
last_indexed | 2024-03-11T10:55:54Z |
publishDate | 2023-12-01 |
publisher | Emergency Management Press |
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series | 矿业科学学报 |
spelling | doaj.art-166c17d6d140498d8e755241fce98c192023-11-13T08:03:05ZengEmergency Management Press矿业科学学报2096-21932023-12-018674475710.19606/j.cnki.jmst.2023.06.002kykxxb-8-6-744Microscopic distribution of fluid in Sulige tight sandstone gas reservoir and its influencing factorsZhang Hanpeng0Ren Dazhong1Zhang Rongjun2Qu Le3Li Tian4Li Qihui5Shaanxi Key Laboratory of Advanced Stimulation Technology for Oil & Gas Reservoirs, Xi'an Shiyou University, Xi'an Shaanxi 710065, ChinaShaanxi Key Laboratory of Advanced Stimulation Technology for Oil & Gas Reservoirs, Xi'an Shiyou University, Xi'an Shaanxi 710065, ChinaXi'an Key Laboratory of Tight Oil (Shale Oil)Development, Xi'an Shiyou University, Xi'an Shaanxi 710065, ChinaXi'an Key Laboratory of Tight Oil (Shale Oil)Development, Xi'an Shiyou University, Xi'an Shaanxi 710065, ChinaShaanxi Key Laboratory of Advanced Stimulation Technology for Oil & Gas Reservoirs, Xi'an Shiyou University, Xi'an Shaanxi 710065, ChinaShaanxi Key Laboratory of Advanced Stimulation Technology for Oil & Gas Reservoirs, Xi'an Shiyou University, Xi'an Shaanxi 710065, ChinaThe Lower Shihezi Formation in the eastern part of Sulige gas field has high water content, where the exploitation of tight sandstone gas reservoir is considerably affected by the characteristics of fluid occurrence. Specifically, this study analyzed the porosity, permeability, lithology, pore throat heterogeneity and connectivity and their effects on fluid occurrenceby rock and ore identification, porosity and permeability analysis and NMR centrifugation. Results show that: ①the tight sandstone reservoir in the study area shows poor pore flow capacity, and bound water saturation. The flow capacity is closely related to the gas flow pressure difference (centrifugal force). ②Intercalations play a key role in controlling flow capacity. Abundant kaolinite content indicates that the reservoir has better connectivity, larger pore size and stronger overall pore water flow capacity. Illite has a strong water-holding capacity, which could easily cause capillary obstruction and limited flow capacity. ③The gas flow pressure difference (centrifugal force)is exponentially related to the pore diameter of reservoir pore water flow. ④The critical pore throat radius of the effective reservoir space is 0.089μm, and the mobile water saturation is 23.95% in Xiashihezi Formation in the eastern part of Sulige gas field.http://kykxxb.cumtb.edu.cn/en/article/doi/10.19606/j.cnki.jmst.2023.06.002tight sandstone gas reservoirnuclear magnetic resonanceinfiltration absorptionthe movable fluid pore fluid distribution |
spellingShingle | Zhang Hanpeng Ren Dazhong Zhang Rongjun Qu Le Li Tian Li Qihui Microscopic distribution of fluid in Sulige tight sandstone gas reservoir and its influencing factors 矿业科学学报 tight sandstone gas reservoir nuclear magnetic resonance infiltration absorption the movable fluid pore fluid distribution |
title | Microscopic distribution of fluid in Sulige tight sandstone gas reservoir and its influencing factors |
title_full | Microscopic distribution of fluid in Sulige tight sandstone gas reservoir and its influencing factors |
title_fullStr | Microscopic distribution of fluid in Sulige tight sandstone gas reservoir and its influencing factors |
title_full_unstemmed | Microscopic distribution of fluid in Sulige tight sandstone gas reservoir and its influencing factors |
title_short | Microscopic distribution of fluid in Sulige tight sandstone gas reservoir and its influencing factors |
title_sort | microscopic distribution of fluid in sulige tight sandstone gas reservoir and its influencing factors |
topic | tight sandstone gas reservoir nuclear magnetic resonance infiltration absorption the movable fluid pore fluid distribution |
url | http://kykxxb.cumtb.edu.cn/en/article/doi/10.19606/j.cnki.jmst.2023.06.002 |
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