Influence of grain size distribution on the physical characteristics of cementing hydrate-bearing sediment

Nature gas hydrates (NGHs) are considered as an ideal substitute for traditional fossil fuel. The evaluation of the physical properties of hydrate-bearing sediment (HBS) is important to develop reasonable exploitation strategies and clarify the corresponding main controlling factors. In this study,...

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Autores principales: Peng Wu, Shenghua Yang, Xiangge Song, Xiang Sun, Yanghui Li
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Lenguaje:EN
Publicado: Elsevier 2021
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spelling oai:doaj.org-article:0d24261b26ab4cc9820835baac69eb4e2021-11-28T04:33:51ZInfluence of grain size distribution on the physical characteristics of cementing hydrate-bearing sediment2352-484710.1016/j.egyr.2021.07.014https://doaj.org/article/0d24261b26ab4cc9820835baac69eb4e2021-11-01T00:00:00Zhttp://www.sciencedirect.com/science/article/pii/S2352484721004789https://doaj.org/toc/2352-4847Nature gas hydrates (NGHs) are considered as an ideal substitute for traditional fossil fuel. The evaluation of the physical properties of hydrate-bearing sediment (HBS) is important to develop reasonable exploitation strategies and clarify the corresponding main controlling factors. In this study, to determine the influence of grain size distribution on the physical properties of HBSs, 24 hydrate-bearing models were reconstructed based on a novel pore-scale 3D morphological modeling algorithm. A series of pore system evaluations and permeability simulations were carried out by pore network modeling (PNM). Moreover, thermal and electrical simulations were carried out using the finite volume method (FVM). The results are as follows: (1) The smaller the grain size is, the smaller the radius of the pores and throats of HBSs will be, which makes it easier for the connectivity between pores and throats to deteriorate as the hydrate saturation increases. (2) With increasing hydrate saturation, the permeability of HBSs gradually decreases. According to the decline rate, it can be divided into two stages: in the first stage, it will decrease sharply, while in the second stage, it will decrease slowly. In general, the smaller the grain size is, the lower the permeability of HBSs will be. (3) The apparent thermal conductivity of HBSs will increase as the hydrate saturation increases. The smaller the grain size is, the higher the apparent thermal conductivity will be. (4) The smaller the grain size is, the lower the apparent electrical conductivity and the higher the resistivity index under the same hydrate saturation will be.Peng WuShenghua YangXiangge SongXiang SunYanghui LiElsevierarticleHydratePhysical characteristicGrain sizePore scaleElectrical engineering. Electronics. Nuclear engineeringTK1-9971ENEnergy Reports, Vol 7, Iss , Pp 8187-8197 (2021)
institution DOAJ
collection DOAJ
language EN
topic Hydrate
Physical characteristic
Grain size
Pore scale
Electrical engineering. Electronics. Nuclear engineering
TK1-9971
spellingShingle Hydrate
Physical characteristic
Grain size
Pore scale
Electrical engineering. Electronics. Nuclear engineering
TK1-9971
Peng Wu
Shenghua Yang
Xiangge Song
Xiang Sun
Yanghui Li
Influence of grain size distribution on the physical characteristics of cementing hydrate-bearing sediment
description Nature gas hydrates (NGHs) are considered as an ideal substitute for traditional fossil fuel. The evaluation of the physical properties of hydrate-bearing sediment (HBS) is important to develop reasonable exploitation strategies and clarify the corresponding main controlling factors. In this study, to determine the influence of grain size distribution on the physical properties of HBSs, 24 hydrate-bearing models were reconstructed based on a novel pore-scale 3D morphological modeling algorithm. A series of pore system evaluations and permeability simulations were carried out by pore network modeling (PNM). Moreover, thermal and electrical simulations were carried out using the finite volume method (FVM). The results are as follows: (1) The smaller the grain size is, the smaller the radius of the pores and throats of HBSs will be, which makes it easier for the connectivity between pores and throats to deteriorate as the hydrate saturation increases. (2) With increasing hydrate saturation, the permeability of HBSs gradually decreases. According to the decline rate, it can be divided into two stages: in the first stage, it will decrease sharply, while in the second stage, it will decrease slowly. In general, the smaller the grain size is, the lower the permeability of HBSs will be. (3) The apparent thermal conductivity of HBSs will increase as the hydrate saturation increases. The smaller the grain size is, the higher the apparent thermal conductivity will be. (4) The smaller the grain size is, the lower the apparent electrical conductivity and the higher the resistivity index under the same hydrate saturation will be.
format article
author Peng Wu
Shenghua Yang
Xiangge Song
Xiang Sun
Yanghui Li
author_facet Peng Wu
Shenghua Yang
Xiangge Song
Xiang Sun
Yanghui Li
author_sort Peng Wu
title Influence of grain size distribution on the physical characteristics of cementing hydrate-bearing sediment
title_short Influence of grain size distribution on the physical characteristics of cementing hydrate-bearing sediment
title_full Influence of grain size distribution on the physical characteristics of cementing hydrate-bearing sediment
title_fullStr Influence of grain size distribution on the physical characteristics of cementing hydrate-bearing sediment
title_full_unstemmed Influence of grain size distribution on the physical characteristics of cementing hydrate-bearing sediment
title_sort influence of grain size distribution on the physical characteristics of cementing hydrate-bearing sediment
publisher Elsevier
publishDate 2021
url https://doaj.org/article/0d24261b26ab4cc9820835baac69eb4e
work_keys_str_mv AT pengwu influenceofgrainsizedistributiononthephysicalcharacteristicsofcementinghydratebearingsediment
AT shenghuayang influenceofgrainsizedistributiononthephysicalcharacteristicsofcementinghydratebearingsediment
AT xianggesong influenceofgrainsizedistributiononthephysicalcharacteristicsofcementinghydratebearingsediment
AT xiangsun influenceofgrainsizedistributiononthephysicalcharacteristicsofcementinghydratebearingsediment
AT yanghuili influenceofgrainsizedistributiononthephysicalcharacteristicsofcementinghydratebearingsediment
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