Convection Compensation in Gradient Enhanced Nuclear Magnetic Resonance Spectroscopy
✍ Scribed by Alexej Jerschow; Norbert Müller
- Publisher
- Elsevier Science
- Year
- 1998
- Tongue
- English
- Weight
- 151 KB
- Volume
- 132
- Category
- Article
- ISSN
- 1090-7807
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✦ Synopsis
Compensation of convection artifacts in gradient-enhanced nustronger than the effect of self-diffusion. In this article we clear magnetic resonance spectroscopy is introduced. Natural conpresent guidelines for the design of gradient sequences to vection caused by small temperature gradients over the sample avoid or compensate convection artifacts in gradient-envolume can lead to significant loss of magnetization in gradienthanced high-resolution NMR spectroscopy.
enhanced nuclear magnetic resonance spectroscopy, sometimes to
A gradient echo is obtained in an arbitrary pulse sequence its complete extinction or partial inversion. Even when the effect if the zeroth moment m 0 of the effective gradient G ଙ (t) is small, it still hampers a quantitative interpretation of spectra, vanishes (4): e.g., nuclear Overhauser effect buildup curves. By using modified pulse and gradient sequences it is possible to avoid the interference of convection, which is demonstrated by way of two examples:
[1] GOESY and GROESY. The principle of convection compensation is applicable to a wide variety of gradient-enhanced nuclear magnetic resonance experiments, in particular those where the interval The effective gradient may be written as between a defocusing and a refocusing pulsed field gradient is relatively long. ᭧ 1998 Academic Press G ଙ (t) Å p(t)rG(t),
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