Earth's field NMR in antarctica: A pulsed gradient spin echo NMR study of restricted diffusion in sea Ice
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[1] Nuclear spins in the Earth’s magnetic field , 1982 .
[2] E. Keller,et al. The Brine Content of Sea Ice Measured with a Nuclear Magnetic Resonance Spectrometer , 1966, Journal of Glaciology.
[3] R. Buckley,et al. Scattering and absorption of visible light by sea ice , 1987, Nature.
[4] M. Jeffries,et al. Structural characteristics of congelation and platelet ice and their role in the development of antarctic land-fast sea ice , 1993, Journal of Glaciology.
[5] Paul T. Callaghan,et al. An earth’s field nuclear magnetic resonance apparatus suitable for pulsed gradient spin echo measurements of self-diffusion under Antarctic conditions , 1997 .
[6] G. Planinšič,et al. Strong Nonuniform Magnetic Field for Self-Diffusion Measurement by NMR in the Earth′s Magnetic-Field , 1994 .
[7] J. E. Tanner,et al. Spin diffusion measurements : spin echoes in the presence of a time-dependent field gradient , 1965 .
[8] Guenther E. Frankenstein,et al. Equations for Determining the Brine Volume of Sea Ice from −0.5° to −22.9°C. , 1967, Journal of Glaciology.