4.7 Article

Laboratory Investigation Into the Formation and Dissociation Process of Gas Hydrate by Low-Field NMR Technique

Journal

JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
Volume 123, Issue 5, Pages 3339-3346

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2017JB014705

Keywords

Gas hydrate; low field NMR; T2 spectrum; formation and dissociation

Funding

  1. Fundamental Research Funds for the Central Universities [16CX05004A, 18CX06025A]
  2. National Natural Science Foundation of China [41404086, 41722403]
  3. Natural Science Foundation of Shandong Province, China [ZR2014DQ007]
  4. National Key Foundation for Exploring Scientific Instrument of China [2013YQ170463]
  5. National Science and Technology Major Project of China [2017ZX05039002]

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We monitored the gas hydrate through low-field nuclear magnetic resonance measurement. An observed decrease of the relaxation time (T-2) intensity corresponds to the formation process, whereas an increase of the intensity corresponds to the dissociation process. The right domain of the spectrum with T-2 larger than 10ms disappears gradually with the formation time, whereas the left domain with T-2 smaller than 1ms remains invariant, indicating the gas hydrate forms preferentially in larger pores. In addition, the right domain increases rapidly with the dissociation time, revealing that the gas hydrate preferentially decomposes in large pores. The spectrum distributions move toward the fast relaxation domain with the growth of gas hydrate, because the generated gas hydrate occupies the large pore and accelerate the relaxation rate. There is no obvious relationship between the gas hydrate saturation and the porosity, whereas the volume and preliminary dissociation ratio are strongly correlated with the porosity.

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