Reservoir diffusion properties of the Longmaxi shale in Shizhu area, Southern Sichuan basin, China

Diffusion ability is an important indicator of shale gas reservoir quality. In this paper, the diffusion coefficient of the Longmaxi Formation is measured via the free hydrocarbon concentration method, and the diffusion ability, influencing factors, and seepage flow are discussed. Results show that...

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Main Authors: Si Chen, Shangbin Chen, Uwamahoro Clementine, Yu Liu, Chu Zhang
Format: Article
Language:English
Published: SAGE Publishing 2018-09-01
Series:Energy Exploration & Exploitation
Online Access:https://doi.org/10.1177/0144598717751182
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spelling doaj-1204cbcadd3b47ae8f753626dda6ce212020-11-25T04:07:29ZengSAGE PublishingEnergy Exploration & Exploitation0144-59872048-40542018-09-013610.1177/0144598717751182Reservoir diffusion properties of the Longmaxi shale in Shizhu area, Southern Sichuan basin, ChinaSi ChenShangbin ChenUwamahoro ClementineYu LiuChu ZhangDiffusion ability is an important indicator of shale gas reservoir quality. In this paper, the diffusion coefficient of the Longmaxi Formation is measured via the free hydrocarbon concentration method, and the diffusion ability, influencing factors, and seepage flow are discussed. Results show that the diffusion coefficient of the Longmaxi Formation is between 1.23 × 10 −5 and 2.98 × 10 −5  cm 2  s −1 with an average value of 2.19 × 10 −5  cm 2  s −1 (confining pressure 3.0 MPa). The diffusion coefficient is calculated for various pressures using an empirical formula ( D  = 0.339 K 0.67 / M 0.5 ) and experimentally measured data. The estimated, temperature-corrected diffusion coefficient of the Longmaxi Formation is 3.94 × 10 −6 –7.24 × 10 −6  cm 2  s −1 with an average value of 5.28 × 10 −6  cm 2  s −1 for depths from 1000 to 3000 m (confining pressure 16.7–39.7 MPa). The diffusion coefficient increases with increasing depth of the reservoir due to the changes in pressure and temperature. Fitting parameters show that the porosity of the reservoir and clay minerals is positively correlated with the diffusion coefficient, and the diffusion coefficient is also related to factors such as total organic carbon and the maximum reflectance of vitrinite ( R o). The diffusion flow rate is 0.177–0.204 m 3  d −1 with an average of 0.182 m 3  d −1 . Linear seepage flow is 4.95 × 10 −4 –14.29 × 10 −4  m 3  d −1 with an average of 8.87 × 10 −4  m 3  d −1 , calculated from the diffusion coefficient and permeability per unit flow. These results indicate that the migration of shale gas in the deep region of the reservoir is mainly by diffusion. Therefore, diffusion is an important shale gas flow mechanism.https://doi.org/10.1177/0144598717751182
collection DOAJ
language English
format Article
sources DOAJ
author Si Chen
Shangbin Chen
Uwamahoro Clementine
Yu Liu
Chu Zhang
spellingShingle Si Chen
Shangbin Chen
Uwamahoro Clementine
Yu Liu
Chu Zhang
Reservoir diffusion properties of the Longmaxi shale in Shizhu area, Southern Sichuan basin, China
Energy Exploration & Exploitation
author_facet Si Chen
Shangbin Chen
Uwamahoro Clementine
Yu Liu
Chu Zhang
author_sort Si Chen
title Reservoir diffusion properties of the Longmaxi shale in Shizhu area, Southern Sichuan basin, China
title_short Reservoir diffusion properties of the Longmaxi shale in Shizhu area, Southern Sichuan basin, China
title_full Reservoir diffusion properties of the Longmaxi shale in Shizhu area, Southern Sichuan basin, China
title_fullStr Reservoir diffusion properties of the Longmaxi shale in Shizhu area, Southern Sichuan basin, China
title_full_unstemmed Reservoir diffusion properties of the Longmaxi shale in Shizhu area, Southern Sichuan basin, China
title_sort reservoir diffusion properties of the longmaxi shale in shizhu area, southern sichuan basin, china
publisher SAGE Publishing
series Energy Exploration & Exploitation
issn 0144-5987
2048-4054
publishDate 2018-09-01
description Diffusion ability is an important indicator of shale gas reservoir quality. In this paper, the diffusion coefficient of the Longmaxi Formation is measured via the free hydrocarbon concentration method, and the diffusion ability, influencing factors, and seepage flow are discussed. Results show that the diffusion coefficient of the Longmaxi Formation is between 1.23 × 10 −5 and 2.98 × 10 −5  cm 2  s −1 with an average value of 2.19 × 10 −5  cm 2  s −1 (confining pressure 3.0 MPa). The diffusion coefficient is calculated for various pressures using an empirical formula ( D  = 0.339 K 0.67 / M 0.5 ) and experimentally measured data. The estimated, temperature-corrected diffusion coefficient of the Longmaxi Formation is 3.94 × 10 −6 –7.24 × 10 −6  cm 2  s −1 with an average value of 5.28 × 10 −6  cm 2  s −1 for depths from 1000 to 3000 m (confining pressure 16.7–39.7 MPa). The diffusion coefficient increases with increasing depth of the reservoir due to the changes in pressure and temperature. Fitting parameters show that the porosity of the reservoir and clay minerals is positively correlated with the diffusion coefficient, and the diffusion coefficient is also related to factors such as total organic carbon and the maximum reflectance of vitrinite ( R o). The diffusion flow rate is 0.177–0.204 m 3  d −1 with an average of 0.182 m 3  d −1 . Linear seepage flow is 4.95 × 10 −4 –14.29 × 10 −4  m 3  d −1 with an average of 8.87 × 10 −4  m 3  d −1 , calculated from the diffusion coefficient and permeability per unit flow. These results indicate that the migration of shale gas in the deep region of the reservoir is mainly by diffusion. Therefore, diffusion is an important shale gas flow mechanism.
url https://doi.org/10.1177/0144598717751182
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