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Experimental Study of Mixed Gas Hydrates from Gas Feed Containing CH 4 , CO 2 and N 2 : Phase Equilibrium in the Presence of Excess Water and Gas Exchange

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  • Ludovic Nicolas Legoix

    (GEOMAR, Helmholtz Centre for Ocean Research Kiel, Wischhofstr. 1-3, D-24148 Kiel, Germany
    Institut Français de Recherche pour l’Exploitation de la Mer (IFREMER), Centre de Bretagne, Département Ressources Physiques et Ecosystèmes de Fond de Mer, Unité des Géosciences Marines, 29280 Plouzané, France)

  • Livio Ruffine

    (Institut Français de Recherche pour l’Exploitation de la Mer (IFREMER), Centre de Bretagne, Département Ressources Physiques et Ecosystèmes de Fond de Mer, Unité des Géosciences Marines, 29280 Plouzané, France)

  • Christian Deusner

    (GEOMAR, Helmholtz Centre for Ocean Research Kiel, Wischhofstr. 1-3, D-24148 Kiel, Germany)

  • Matthias Haeckel

    (GEOMAR, Helmholtz Centre for Ocean Research Kiel, Wischhofstr. 1-3, D-24148 Kiel, Germany)

Abstract

This article presents gas hydrate experimental measurements for mixtures containing methane (CH 4 ), carbon dioxide (CO 2 ) and nitrogen (N 2 ) with the aim to better understand the impact of water (H 2 O) on the phase equilibrium. Some of these phase equilibrium experiments were carried out with a very high water-to-gas ratio that shifts the gas hydrate dissociation points to higher pressures. This is due to the significantly different solubilities of the different guest molecules in liquid H 2 O. A second experiment focused on CH 4 -CO 2 exchange between the hydrate and the vapor phases at moderate pressures. The results show a high retention of CO 2 in the gas hydrate phase with small pressure variations within the first hours. However, for our system containing 10.2 g of H 2 O full conversion of the CH 4 hydrate grains to CO 2 hydrate is estimated to require 40 days. This delay is attributed to the shrinking core effect, where initially an outer layer of CO 2 -rich hydrate is formed that effectively slows down the further gas exchange between the vapor phase and the inner core of the CH 4 -rich hydrate grain.

Suggested Citation

  • Ludovic Nicolas Legoix & Livio Ruffine & Christian Deusner & Matthias Haeckel, 2018. "Experimental Study of Mixed Gas Hydrates from Gas Feed Containing CH 4 , CO 2 and N 2 : Phase Equilibrium in the Presence of Excess Water and Gas Exchange," Energies, MDPI, vol. 11(8), pages 1-12, July.
  • Handle: RePEc:gam:jeners:v:11:y:2018:i:8:p:1984-:d:160916
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    References listed on IDEAS

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    1. E. Dendy Sloan, 2003. "Fundamental principles and applications of natural gas hydrates," Nature, Nature, vol. 426(6964), pages 353-359, November.
    2. Hailong Lu & Yu-taek Seo & Jong-won Lee & Igor Moudrakovski & John A. Ripmeester & N. Ross Chapman & Richard B. Coffin & Graeme Gardner & John Pohlman, 2007. "Complex gas hydrate from the Cascadia margin," Nature, Nature, vol. 445(7125), pages 303-306, January.
    3. Ludovic Nicolas Legoix & Livio Ruffine & Jean-Pierre Donval & Matthias Haeckel, 2017. "Phase Equilibria of the CH 4 -CO 2 Binary and the CH 4 -CO 2 -H 2 O Ternary Mixtures in the Presence of a CO 2 -Rich Liquid Phase," Energies, MDPI, vol. 10(12), pages 1-11, December.
    4. Christian Deusner & Nikolaus Bigalke & Elke Kossel & Matthias Haeckel, 2012. "Methane Production from Gas Hydrate Deposits through Injection of Supercritical CO 2," Energies, MDPI, vol. 5(7), pages 1-29, June.
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