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Assessment and correction of macroscopic field variations in 2D spoiled gradient-echo sequences
Martin Soellradl1, Andreas Lesch2, Johannes Strasser1
1Department of Neurology, Medical University of Graz, Graz, Austria.
Magnetic Resonance in Medicine
|December 24, 2019
Summary
This study presents a new model to correct dephasing in gradient-echo signals, improving accuracy for R2* and myelin water fraction mapping, especially with large flip angles.
Area of Science:
- Magnetic Resonance Imaging (MRI)
- Biophysics
Background:
- Gradient-echo (GRE) imaging is susceptible to dephasing artifacts caused by magnetic field variations.
- Accurate estimation of quantitative parameters like R2* and myelin water fraction (MWF) is crucial for various MRI applications.
- Large flip angles in GRE sequences can exacerbate dephasing effects, complicating quantitative analysis.
Purpose of the Study:
- To develop and validate a model for correcting dephasing effects in GRE signals.
- To account for arbitrary radiofrequency (RF) excitation pulses and large flip angles.
- To incorporate macroscopic field variations and their impact on signal magnitude and phase.
Main Methods:
- Numerical solution of Bloch equations to model dephasing across the slice profile.
- Inclusion of regional transmit RF field variations and slice profile scaling due to field gradients.
- Validation through simulations, phantom studies, and in vivo 3 Tesla MRI.
Main Results:
- The proposed model significantly reduces the influence of macroscopic field gradients on R2* and MWF estimations.
- Dephasing dependency on slice-selection gradient polarity was observed for flip angles ≥ 60°.
- Demonstrated improved accuracy and coverage for R2* and MWF mapping.
Conclusions:
- The developed model enhances the accuracy of R2* and MWF mapping, particularly when large flip angles are used.
- Accurate modeling requires considering phase variations along the slice profile and slice-selection gradient polarity.
- This approach is vital for robust quantitative MRI in the presence of field inhomogeneities.

