Why do we study hydrates




















The intersection of the three-phase lines correspond to the quadruple point Q1 , where I-Lw-H-V coexist. Structure I Hydrate. Structure II Hydrate. A database study of 34 accurate organic crystal structures reveals that the most important factor determining a higher frequency of hydrates is the sum of the average donor and acceptor counts for the functional groups. We also examined a wide range of calculated molecular properties and found that increasing polar surface is correlated with increasing hydrate formation.

Infantes, L. To request permission to reproduce material from this article, please go to the Copyright Clearance Center request page. If you are an author contributing to an RSC publication, you do not need to request permission provided correct acknowledgement is given. If you are the author of this article, you do not need to request permission to reproduce figures and diagrams provided correct acknowledgement is given.

Read more about how to correctly acknowledge RSC content. Fetching data from CrossRef. Pokol, Z. Finta, M. You can use material from this article in other publications, without requesting further permission from the RSC, provided that the correct acknowledgement is given and it is not used for commercial purposes.

To request permission to reproduce material from this article in a commercial publication , please go to the Copyright Clearance Center request page. If you are an author contributing to an RSC publication, you do not need to request permission provided correct acknowledgement is given. If you are the author of this article, you do not need to request permission to reproduce figures and diagrams provided correct acknowledgement is given.

Read more about how to correctly acknowledge RSC content. Fetching data from CrossRef. This may take some time to load. Loading related content. Methane, the primary component of natural gas, is the most common of the gases that form gas hydrate. Because of that potential, the USGS and academic, government, and. Skip to main content. Search Search.

Apply Filter. Where are gas hydrates found? Gas hydrates are found in sub-oceanic sediments in the polar regions shallow water and in continental slope sediments deep water , where pressure and temperature conditions combine to make them stable. Map showing locations where gas hydrate has been Who studies gas hydrates?

Currently, groups of scientists in the U. The primary goals are What are gas hydrates? Gas hydrates are a crystalline solid formed of water and gas. It looks and acts much like ice, but it contains huge amounts of methane; it is known to occur on every continent; and it exists in huge quantities in marine sediments in a layer several hundred meters thick directly below the sea floor and in association with permafrost in the Arctic Filter Total Items: 4. Year Published: Assessment of undiscovered gas hydrate resources in the North Slope of Alaska, Using a geology-based assessment methodology, the U.

Collett, Timothy S. View Citation. Collett, T. Geological Survey Fact Sheet —, 4 p. Year Published: Gas hydrate in nature Gas hydrate is a naturally occurring, ice-like substance that forms when water and gas combine under high pressure and at moderate temperatures.

Ruppel, Carolyn D.



0コメント

  • 1000 / 1000