Structure and Dynamics of Confined C-O-H Fluids Relevant to the Subsurface: Application of Magnetic Resonance, Neutron Scattering, and Molecular Dynamics Simulations

Geo-fluids consisting of C-O-H volatiles are the main mode of transport of mass and energy throughout the lithosphere and are commonly found confined in pores, grain boundaries and fractures. The confinement of these fluids by porous media at the length scales of a few nanometers gives rise to numer...

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Bibliographic Details
Main Authors: Siddharth S. Gautam, Salim Ok, David R. Cole
Format: Article
Language:English
Published: Frontiers Media S.A. 2017-06-01
Series:Frontiers in Earth Science
Subjects:
Online Access:http://journal.frontiersin.org/article/10.3389/feart.2017.00043/full