Alberto Maria Gambelli, Federico Rossi, Giovanni Gigliotti
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引用次数: 0
Abstract
Carbon dioxide hydrates were formed and dissociated in a lab-scale apparatus, filled with demineralised water and porous sediments. Two different porous media were tested; the first consists of glass beads, commonly used to reproduce marine environments during lab-scale hydrate formation experiments. Natural basaltic sand, typical of the Icelandic margins, was chosen as second sediment. The role played by the two sediments, was analysed both during the hydrate formation and dissociation processes and the results were compared among each other. In particular, the pressure – temperature values measured during the dissociation phase, were compared with the phase boundary equilibrium conditions for pure carbon dioxide hydrates, carried out in absence of any porous sediment, collected from the scientific literature.
期刊介绍:
Heat Transfer Research (ISSN1064-2285) presents archived theoretical, applied, and experimental papers selected globally. Selected papers from technical conference proceedings and academic laboratory reports are also published. Papers are selected and reviewed by a group of expert associate editors, guided by a distinguished advisory board, and represent the best of current work in the field. Heat Transfer Research is published under an exclusive license to Begell House, Inc., in full compliance with the International Copyright Convention. Subjects covered in Heat Transfer Research encompass the entire field of heat transfer and relevant areas of fluid dynamics, including conduction, convection and radiation, phase change phenomena including boiling and solidification, heat exchanger design and testing, heat transfer in nuclear reactors, mass transfer, geothermal heat recovery, multi-scale heat transfer, heat and mass transfer in alternative energy systems, and thermophysical properties of materials.