Paul de Heer1, Maurice B Bizino2, Hildo J Lamb2, and Andrew G Webb1
1CJ Gorter Center, Radiology, Leiden University Medical Center, Leiden, Netherlands, 2Radiology, Leiden University Medical Center, Leiden, Netherlands
Synopsis
Cardiac proton MR spectroscopy is a
challenging technique to perform in a reliable manner. In this study data
acquisition parameters are optimized in terms of signal-to-noise and
reproducibility. The optimal protocol was determined to be a PRESS localized
scan, local power optimization, pencil beam B0 shimming, a cardiac
trigger delay of 200 ms, MOIST water suppression and pencil beam navigator-based
respiratory compensation. With these parameters high intra- (r=1.000,
p<0.0001) and inter- (r=1.000, p=0.0004) session reproducibilities were
achieved. Bland-Altman analysis showed limits of agreement from -0.11 to 0.04 (intra)
and -0.15 to 0.9.Purpose
Cardiac proton MR spectroscopy is a
challenging technique to perform in a reliable manner(1). The aim of this study is to
optimize the reproducibility of cardiac measurements with respect to RF power
optimization, B0 shimming, the measurement point within cardiac cycle, the
method of respiratory motion correction and the choice of water suppression
technique. Finally, we use these optimized parameters to measure the intra- and inter-session
reproducibility in healthy volunteers.
Materials and
Methods
Data acquisition parameters were
optimized using forty-one healthy subjects (Table1).
1. Point
resolved spectroscopy (PRESS) spectra were acquired using a global- or local
power optimization. The global power optimization determines the optimal power
setting over a transverse slice while local power optimization uses a PRESS
sequence with a tip angle sweep of the two slice-selective refocussing pulses
to determine the optimal power setting locally. The SNR of the water signal was
calculated and compared for the two techniques using a Wilcoxon signed-rank
test;
2. PRESS
spectra were acquired using B0 shimming during free breathing and or within breath-holds.
The full-width-at-half-maximum (FWHM) of the water peak was determined and
compared using a Wilcoxon signed-rank test;
3. Eight
different measurement times were defined throughout the cardiac cycle and PRESS
(sixteen averages) spectra were acquired for each of the measurement times. The
standard deviation (SD) of the water signal amplitude for the averages was
calculated and plotted in a graph;
4. The water
signal amplitude SD was calculated from PRESS spectra (sixteen averages)
without respiratory compensation, with breath-holds and with navigator
triggering (2). The amplitude variation was
compared using Friedman`s ANOVA test and post-hoc Wilcoxon signed rank test;
5. The
residual water signal was measured for frequency selective excitation, chemical
shift selective (CHESS) and Multiply Optimized Insensitive Suppression Train (MOIST)
water suppression(3,4). The
residual water signal was compared using a Friedman`s ANOVA test and post-hoc
Wilcoxon signed rank test;
6. Intra- and
inter-session reproducibility was measured using a PRESS sequence (TE 35ms,
unsuppressed 6 averages, water suppressed 32 averages) with the aforementioned optimized
parameters. The myocardial triglyceride content (MTGC) was calculated for the
intra- and inter-sessions. The Spearman correlation coefficient was calculated
and Bland-Altman plots were constructed.
Results
1. The spectra
of thirteen of the fifteen subjects show a higher SNR using a local power
optimization compared to the global power optimization, while for the remaining
two subjects SNR did not differ. The mean SNR (±SD) of the water signal was 1787
(±787) using the global power optimization vs. 2173 (±626) for the local power
optimization (p=0.0002).
2. The average
linewidth without breathing compensation (±SD) was 19 Hz (±3.2) compared to 17 Hz
(±4.6) with breath-holds (p=0.15).
3. In figure 1 the SD of the water signal averages is plotted
against the cardiac trigger delay. For all subjects the SD was at its minimum
with a trigger delay around 200 ms, corresponding to the highest signal
stability in this region which was in line with a previous study(5). The optimal region was only
minimally affected by the heart rate of the subjects.
4. In figure 2
the amplitude variation for the three respiration compensation techniques is
shown. The mean amplitude variation was significantly lower for free-breathing
vs breath-holds (p=0.03) and for free-breathing vs navigator triggering
(p=0.03) as well as for breath-hold vs navigator triggering (p=0.02).
5. In figure 3 the residual water signal for water
suppression techniques are shown. The mean (±SD) residual water signal was 7.0%
(±4.8%), 1.1% (±0.9%) and 0.7% (±0.4%) for frequency selective excitation,
CHESS and MOIST water suppression respectively. The mean residual signal using
CHESS (p=0.01) or MOIST (p=0.01) water suppression was significantly
lower than using excitation water suppression.
6. The mean (±SD)
MTGC (in %) of the intra-sessions was 0.55 (±0.40) and 0.59 (±0.42)
and had good correlation (r=1.000, p<0.0001) with a mean difference of 0.04 with 95% limits of
agreement of -0.11 to 0.04 (fig 5A). The mean (±SD) MTGC (in %) of the inter-sessions was 0.60 (±0.42) and 0.63 (±0.45) with also good correlation (r=1.000,
p=0.0004) and a difference of 0.03 with 95% limits of agreement of -0.15 to 0.9
(fig 5B).
Conclusion
The optimal protocol to perform
cardiac MR spectroscopy was found to be a PRESS localized scan using a separate
suppressed and unsuppressed acquisition, local power optimization, pencil beam
B0 shimming, cardiac trigger delay of 200 ms, MOIST water
suppression and pencil beam navigator based respiratory compensation. When all
these parameters are used it is possible to get good intra-(r=1.000, p<0.0001) and inter-session (r=1.000, p=0.0004) correlation of MTGC and a reproducibility with small limits of agreement.
Acknowledgements
No acknowledgement found.References
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