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Method for the production of carbon dioxide hydrates

Patent 5562891 Issued on October 8, 1996. Estimated Expiration Date: Icon_subject August 16, 2014. Estimated Expiration Date is calculated based on simple USPTO term provisions. It does not account for terminal disclaimers, term adjustments, failure to pay maintenance fees, or other factors which might affect the term of a patent.

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Method and system for throwing carbon dioxide into the deep sea
Patent #: 5293751
Issued on: 03/15/1994
Inventor: Asai

Method for the fixation of carbon dioxide, apparatus for fixing and disposing carbon dioxide, and apparatus for the treatment of carbon dioxide
Patent #: 5304356
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Inventor: Iijima, et al.

Method for the fixation of carbon dioxide
Patent #: 5364611
Issued on: 11/15/1994
Inventor: Iijima, et al.

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Inventors

Assignee

Application

No. 291593 filed on 08/16/1994

US Classes:

423/437.1, Carbon dioxide or carbonic acid62/53.1, Underground or underwater storage423/220, Carbon dioxide or hydrogen sulfide component588/250Geologic, marine, or extraterrestrial storage and containment (e.g., tectonic, volcanic, deep natural, manmade earth cavity, submarine placement sites, lunar, earth orbital, and solar placement, etc.)

Examiners

Primary: Straub, Gary P.
Assistant: Vanoy, Timothy C.

Attorney, Agent or Firm

Foreign Patent References

  • 0463663 EP 01/13/1992
  • 3-164419 JP. 07/13/1991
  • 4-11920 JP. 01/13/1992
  • 4-55681 JP 02/13/1992

International Classes

F17C 005/02
F25J 001/00
C01B 031/20

Abstract

A method is provided for producing CO2 hydrates. In the subject method, CO2 is first dissolved in water to produce a CO2 hydrate precursor. The CO2 hydrate precursor is then mixed with CO2 gas, resulting in hydrate production. Between the first and second steps, the CO2 hydrate precursor may optionally be cooled to at least 0° C. and/or CO2 hydrate nuclei may be introduced into the CO2 hydrate precursor. The method is carried out in a continuous hydrate production reactor. The subject method finds use in sequestering CO2 gas emissions in the form of hydrates, where the hydrates are deposited in high pressure, low temperature environments, such as in the ocean at depths greater than 1000 m or in subterranean fresh water aquifers.

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