G
George J. Moridis
Researcher at Lawrence Berkeley National Laboratory
Publications - 307
Citations - 14455
George J. Moridis is an academic researcher from Lawrence Berkeley National Laboratory. The author has contributed to research in topics: Clathrate hydrate & Hydrate. The author has an hindex of 61, co-authored 285 publications receiving 12384 citations. Previous affiliations of George J. Moridis include Texas A&M University & National University of Singapore.
Papers
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Journal ArticleDOI
Numerical Analysis of Experiments on Thermally Induced Dissociation of Methane Hydrates in Porous Media
Zhenyuan Yin,George J. Moridis,George J. Moridis,George J. Moridis,Zheng Rong Chong,Hoon Kiang Tan,Praveen Linga +6 more
TL;DR: In this paper, the results of an experiment of methane hydrate dissociation by thermal stimulation in unconsolidated porous media heated through the vessel walls were analyzed by means of numerical simulation.
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The RealGas and RealGasH2O options of the TOUGH+ code for the simulation of coupled fluid and heat flow in tight/shale gas systems
TL;DR: Two new EOS additions to the TOUGH+ family of codes are developed, the RealGasH2O and RealGas, which allow the study of flow and transport of fluids and heat over a wide range of time frames and spatial scales not only in gas reservoirs, but also in problems of geologic storage of greenhouse gas mixtures, and of geothermal reservoirs with multi-component condensable and non-condensable gas mixture.
A domain decomposition approach for large-scale simulations of flow processes in hydrate-bearing geologic media
TL;DR: A domain decomposition approach for large-scale gas hydrate simulations with coarse-granularity parallel computation is developed and implemented into the TOUGH+HYDRATE code and has demonstrated excellent speedup and good scalability.
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Estimating the upper limit of gas production from Class 2 hydrate accumulations in the permafrost: 2. Alternative well designs and sensitivity analysis
TL;DR: In this paper, the authors evaluate two additional well designs for production from permafrost-associated (PA) hydrate deposits and determine that large volumes of gas can be produced at high rates (several MMSCFD) for long times using either well design.
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Contribution of oceanic gas hydrate dissociation to the formation of Arctic Ocean methane plumes
TL;DR: Reagan et al. as discussed by the authors investigated the contribution of Oceanic Gas Hydrate Dissociation to the formation of Arctic Ocean Methane Plumes and found that the contribution was positively correlated with the amount of oceanic gas hydrate dissociation.