4.7 Article

A novel Kozeny-Carman-based permeability model for hydrate-bearing sediments

期刊

ENERGY
卷 234, 期 -, 页码 -

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.energy.2021.121203

关键词

Permeability; Hydrate-bearing sediment; Pore habit; Kozeny-Carman equation

资金

  1. National Key Research and Development Project [2018YFE0126400]
  2. National Natural Science Foundation of China [51708526]
  3. Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) [CUGGC09]

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The study proposed an innovative permeability-hydrate saturation model based on Poiseuille's law and the Kozeny-Carman equation, which was verified to have satisfactory performance in predicting the permeability of hydrate-bearing sediments. The normalized permeability decreases non-linearly as void ratio increases for a given hydrate saturation, with higher sensitivity at high hydrate saturation. The model can capture the main feature of permeability with hydrate saturation for coarse-grained hydrate-bearing sediments.
Permeability governs fluid flow in hydrate-bearing sediments (HBSs) and directly affects gas production efficiency. Reported models relating permeability to hydrate saturation are usually embedded with parameters whose physical meaning is not clear or difficult to determine. It limits their applicability in numerical simulations and practices. In this study, we proposed an innovative permeability-hydrate saturation model based on the Poiseuille's law and the Kozeny-Carman equation. The proposed model has single one parameter, the void ratio, which is physically sound and easily determined. This model was verified by experimental data and other existing models, and proved to have a satisfying performance in predicting the permeability of HBSs. The prediction results reached an asymptote in the range of k(meas)/2 <= k(predict) <= 2k(meas). For a given hydrate saturation, the normalized permeability decreases non-linearly as void ratio increases. The sensitivity of permeability of HBS to changes in void ratio is higher at high hydrate saturation. Overall, the proposed model can capture the main feature of permeability with hydrate saturation for coarse-grained HBS. The remaining uncertainty in this model underscores the important role of hydrate distribution, heterogeneity, anisotropy, and pore geometry of HBSs that are not characterized by the hydrate saturation and the void ratio. (C) 2021 Elsevier Ltd. All rights reserved.

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