Knowledge Management System of Institue of Mechanics, CAS
| 一个考虑沉积物孔径分布特征的水合物相平衡模型 | |
| Alternative Title | A Phase Equilibrium Model for Gas Hydrates Considering Pore-Size Distribution of Sediments |
颜荣涛; 魏厚振; 吴二林; 王淑云 ; 韦昌富
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| Source Publication | 物理化学学报
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| 2011 | |
| Volume | 27Issue:2Pages:295-301 |
| ISSN | 1000-6818 |
| Abstract | 天然气水合物的相平衡条件一直是水合物相关研究的重点和难点.本文探讨了沉积物孔隙大小及其分布特征对水合物相平衡条件的影响机理,提出了有效孔隙半径的概念,并利用沉积物孔隙大小分布特征,假设孔径分布呈正态分布,建立了水合物饱和度和有效孔隙半径之间的定量关系;与传统的vander Waals-Plat-teeuw相平衡模型相结合,提出了一个考虑沉积物孔隙大小及其分布特征的相平衡模型.相对于传统模型,本模型所表达的相平衡条件不再是二维平面的p-T曲线,而是温度,压力以及水合物饱和度之间的三维定量关系.这一特征使得所建模型既能较为真实地反映水合物形成与分解机理,又能有效地考虑孔隙大小分布对水合物相平衡条件的影响.通过与实验数据对比,证明了所建模型的预测结果优于其他模型.本模型在温度和压力条件确定的情况下还可以预测沉积物中水合物的饱和度,因此,可用于地层中水合物储量计算 |
| Other Abstract | The phase equilibrium condition for gas hydrates has been an important and difficult subject in gas hydrate-related research.In this paper,the mechanism of the effect of pore-size distribution on the phase equilibrium is first explored and the concept of effective pore radius is proposed.Using information on the pore-size distribution of sediments,a relationship between hydrate saturation and effective pore radius is developed.Combined with the van der Waals-Platteeuw model,this relationship was then used to develop a new phase equilibrium model for gas hydrates in sediments,which can properly account for the effect of pore-size distribution.In contrast to the traditional models,this new model does not represent a curve on the p-T plane but instead addresses the relationship between the temperature,pressure,and hydrate saturation.Such a feature allows the new model to take into account the effect of pore-size distribution on the phase equilibrium while treating the formation and/or dissolution processes of gas hydrates in pores more realistically.The simulated results were compared with the experimental data available in literature showing that the new model gives better results compared with the other traditional models.Given the temperature and the pore pressure,the hydrate saturation can be determined using the proposed model.Therefore,the new model can be used to estimate the amount of hydrate resources in the field. |
| Keyword | 天然气水合物 相平衡 孔隙大小分布 水合物饱和度 |
| Subject Area | 力学 |
| URL | 查看原文 |
| Indexed By | CSCD |
| Language | 中文 |
| Funding Organization | 岩土力学与工程国家重点实验室资助课题(Z000801);中国科学院“百人计划”择优支持项目,中国科学院知识创新工程重要方向项目(KZCX2-YW-JS108)资助~~ |
| CSCD ID | CSCD:4134327 |
| Department | LMFS海洋土力学(LHO) |
| Citation statistics |
Cited Times:5[CSCD]
[CSCD Record]
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| Document Type | 期刊论文 |
| Identifier | http://dspace.imech.ac.cn/handle/311007/45061 |
| Collection | 水动力学与海洋工程重点实验室(2009-2011) |
| Corresponding Author | 颜荣涛 |
| Recommended Citation GB/T 7714 | 颜荣涛,魏厚振,吴二林,等. 一个考虑沉积物孔径分布特征的水合物相平衡模型[J]. 物理化学学报,2011,27,2,:295-301. |
| APA | 颜荣涛,魏厚振,吴二林,王淑云,&韦昌富.(2011).一个考虑沉积物孔径分布特征的水合物相平衡模型.物理化学学报,27(2),295-301. |
| MLA | 颜荣涛,et al."一个考虑沉积物孔径分布特征的水合物相平衡模型".物理化学学报 27.2(2011):295-301. |
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