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MRI Measurement of Hydrate Growth and an Application to Advanced CO 2 Sequestration Technology
Author(s) -
HIRAI SHUICHIRO,
TABE YUTAKA,
KUWANO KUNIHIRO,
OGAWA KUNIYASU,
OKAZAKI KEN
Publication year - 2000
Publication title -
annals of the new york academy of sciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.712
H-Index - 248
eISSN - 1749-6632
pISSN - 0077-8923
DOI - 10.1111/j.1749-6632.2000.tb06778.x
Subject(s) - dissolution , hydrate , clathrate hydrate , materials science , deep sea , atmosphere (unit) , ocean bottom , mineralogy , chemical engineering , chemistry , geology , oceanography , meteorology , physics , organic chemistry , seismology , engineering
A bstract : MRI measurements of hydrate thickness growth have been measured and this phenomenon applied to advanced CO 2 ocean dissolution technology. CO 2 droplets dissolve during the process of sinking from their release point into deep ocean, by forming fine hydrate particles inside CO 2 droplets before the droplets are released from a towed pipe on a moving ship. This results in a sufficiently long sequestration period from the atmosphere and further reduces biological impact. The increasing rate of hydrate film thickness in forming hydrate particles was measured by an ultrahigh‐pressure magnetic resonance imaging (MRI) technique.

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