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CO2 hydrate stability in oceanic sediments under brine conditions

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  • Qureshi, M Fahed
  • Khandelwal, Himanshu
  • Usadi, Adam
  • Barckholtz, Timothy A.
  • Mhadeshwar, Ashish B.
  • Linga, Praveen

Abstract

Carbon capture and storage (CCS) is a critical approach to reducing atmospheric carbon emissions. The United Nations [UN] Climate Change Conference COP26 Glasgow [2021] emphasized setting execution plans to reach the goal of a zero-carbon economy by 2050 as per the Paris Agreement [2015]. CO2 sequestration in deep-sea sediments in the form of clathrate hydrates is a promising technique as it provides a significant capacity for CO2 storage. Deep-sea sediments contain high salinity water, which will impair the CO2 storage capacity and hydrate stability. Therefore, it's essential to examine the effect of salinity on CO2 hydrate stability in simulated deep-sea sediments to foster real-time field application.

Suggested Citation

  • Qureshi, M Fahed & Khandelwal, Himanshu & Usadi, Adam & Barckholtz, Timothy A. & Mhadeshwar, Ashish B. & Linga, Praveen, 2022. "CO2 hydrate stability in oceanic sediments under brine conditions," Energy, Elsevier, vol. 256(C).
    • Handle: RePEc:eee:energy:v:256:y:2022:i:c:s0360544222015286
    DOI: 10.1016/j.energy.2022.124625
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