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  1. NTU Scholars
  2. 理學院
  3. 海洋研究所
Please use this identifier to cite or link to this item: https://scholars.lib.ntu.edu.tw/handle/123456789/364537
Title: Numerical modeling of gas hydrate emplacements in oceanic sediments
Authors: CHAR-SHINE LIU 
Keywords: Finite-elements; Gas hydrates; Methane solubility; Simulation
Issue Date: 2011
Journal Volume: 28
Journal Issue: 10
Start page/Pages: 1856-1869
Source: Marine and Petroleum Geology 
Abstract: 
We have implemented a 2-dimensional numerical model for simulating gas hydrate and free gas accumulation in marine sediments. The starting equations are those of the conservation of the transport of momentum, energy, and mass, as well as those of the thermodynamics of methane hydrate stability and methane solubility in the pore-fluid. These constitutive equations are then integrated into a finite element in space, finite-difference in time scheme. We are then able to examine the formation and distribution of methane hydrate and free gas in a simple geologic framework, with respect to the geothermal heat flow, fluid flow, the methane in-situ production and basal flux. Three simulations are performed, leading to the build up of hydrate emplacements largely linear through time. Models act primarily as free gas accumulators and are relatively inefficient with respect to hydrate emplacements: 26-33% of formed methane are converted to hydrate. Seepage of methane across the sea-floor is negligible for fluid flow below 2. 10-11 kg/m2/s. At 5.625 10-11 kg/m2/s however, 9.7% of the formed methane seeps out of the model. Moreover, along strike variation arising in the 2-dimensional model are outlined. In the absence of focused flow, the thermodynamics of hydrate accumulation are primarily one-dimensional. However, changes in free methane compressibility (density) and methane solubility (the intrinsic dissolved methane flux) subtlety impact on the formation of a free gas zone and the distribution of the hydrate emplacements in our 2-dimensional simulations. © 2011 Elsevier Ltd.
URI: http://www.scopus.com/inward/record.url?eid=2-s2.0-82455162567&partnerID=MN8TOARS
http://scholars.lib.ntu.edu.tw/handle/123456789/364537
DOI: 10.1016/j.marpetgeo.2011.03.011
SDG/Keyword: Dissolved methane; Finite difference; Finite Element; Focused-flow; Free gas; Geothermal heat flow; Hydrate accumulations; In-situ production; Marine sediments; Methane hydrates; Methane seep; Methane solubility; Numerical modeling; Numerical models; Oceanic sediments; Sea floor; Simulation; Anoxic sediments; Constitutive equations; Flow of fluids; Gases; Geothermal energy; Geothermal heating; Hydration; Methane; Numerical methods; Sedimentology; Solubility; Submarine geology; Thermodynamics; Transport properties; Gas hydrates; accumulation; compressibility; constitutive equation; emplacement; finite element method; gas hydrate; heat flow; marine sediment; mass transport; methane; momentum transfer; numerical model; seepage; solubility; thermodynamics; Calluna vulgaris
[SDGs]SDG14
Appears in Collections:海洋研究所

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