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recting for Center Frequency Variations in M ta Using the Partially Suppressed Water Sign Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D., M.D., Nan-Kuei Chen, Ph.D. Department of Radiology, Brigham and Women’s Hospital, Harvard Medical School, Boston MA is work was supported by NIH U41-RR019703, R21-CA11092, 5R25-CA08901 ISMRM Workshop on Data Processing for MR Spectroscopy and Imaging Warrenton, Virginia 11-13 November, 2006

Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

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Page 1: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

Correcting for Center Frequency Variations in MRSIData Using the Partially Suppressed Water Signal

Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D., M.D., Nan-Kuei Chen, Ph.D.

Department of Radiology, Brigham and Women’s Hospital,Harvard Medical School, Boston MA

This work was supported by NIH U41-RR019703, R21-CA11092, 5R25-CA089017.

ISMRM Workshop on Data Processing for MR Spectroscopy and ImagingWarrenton, Virginia 11-13 November, 2006

Page 2: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

• Several authors have reported methods using interleaved navigators to dynamically estimate the center frequency during a spectroscopic acquisition using a short acquisition without water suppression to correct spatial and spectral artifacts that would otherwise occur.

• Thiel et. al. Magn Reson Med. (2002)47:1077

Interleaved navigator during single voxel 1H-MRS acquisition

• Elbel and Maudsley. Magn Reson Med. (2005)53:465.

Interleaved navigator during 1H 3D-EPSI acquisition

• In preliminary work reported here, we explored using the raw phase-encoded data from a MRSI acquisition with partial water suppression to estimate the center frequency variations.

INTRODUCTION

Page 3: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

INTRODUCTION: Spatial Misregistration of MRSI Signal1

241 24

x

y

Reconstructed MRSI of a pre-selected rectangular voxel placed at the center of the field of view (shown in red) within a homogeneous phantom. The signal is largely localized to the pre-selected voxel but spatial misregistration is seen in both directions, x > y.

Page 4: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

INTRODUCTION: The Magnetic Field Drift

Center frequency variation with time estimated by interleaving MRSIs with and without PE.

Top: Plots from same magnet, separate acquisitions, without and with water suppression.Bottom: Plots from two 1.5T magnets acquired synchronously with water suppression.

Fre

quen

cy (

Hz)

Without suppression With suppression

Stable ωo Fluctuating ωo

Page 5: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

METHODS

Magnet: General Electric Signa 1.5T 12.0 hardware/software.

Localization: PRESS TR 1000/TE30 Rectangular voxel pre-selected in the axial plane of magnet isocenter

MRSI: 24 x 24 or 16 x 16 sequential phase encoding in x, y1 x 1 x 1 cm in-plane resolution

Navigators: Interleaved with MRSI with Gx = Gy = 0

Phantom: General Electric MRS brain phantom

NameName SymbolSymbol Conc.Conc.

Myo-inositolMyo-inositol mImI 7.5 mM7.5 mM

CholineCholine ChoCho 3.0 mM3.0 mM

CreatineCreatine CrCr 10.0 mM10.0 mM

GlutamateGlutamate GluGlu 12.5 mM12.5 mM

N-acetyl-L-aspartateN-acetyl-L-aspartate NAANAA 12.5 mM12.5 mM

LactateLactate LacLac 5.0 mM5.0 mM

Post-processing: MatLab, Power Mac

Page 6: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

METHODS: Interleaved MRSI and Navigators (Gx=Gy=0)

1 M

1

N

kx

ky

1 M

1

N

n=1

kx=N

t = TR

t = TR

t = TR

MR

SI

NA

VIG

AT

OR

SINTERLEAVED

m

2

3

2

n=N

3

t = 0

t = 2N×M×TR

n

kx=1

t = 2N×TR

n, kx

Page 7: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

METHODS: Uncorrected Data

ky

kxINTERLEAVED

MRSI

NAVIGATORS

y

x2D-FT

2D-FT

y

x

(Gx=Gy=0)

Page 8: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

METHODS: Uncorrected Data

ky

kxINTERLEAVED

MRSI

NAVIGATORS

2D-FT

2D-FT

y

x

y

x

(Gx=Gy=0)

Page 9: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

METHODS: Center Frequency Drift Estimation and CorrectionMethod Using Solvent Suppressed Navigators

t = 32 s

n, kx

ΔtΔωn

tiωe(t)ff nn

corrn

INTERLEAVED

samples used to estimate n(t)

t = 0

Page 10: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

METHODS: Center Frequency Drift Estimation and CorrectionUsing MRSI Data

t = 0

ky

kx

MRSI

INTERLEAVED

kx=2, ky=2

kx=9, ky=7

samples used to estimate n(t)

t = 32 s

1

161 16

Page 11: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

METHODS: Self Correction Using Unsuppressed Water

Shift parameter estimated from MRSIwhen values close to ‘true’ value (Hz)

Maximum signal level in orderof phase encoding steps

Shift parameter estimatedfrom navigators (Hz)

Uncorrected MRSI Self-corrected MRSI

kx=8, ky=1, 2, …, 16

Page 12: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

METHODS: Correction Strategies Using Interleaved Data

samples used to estimate n(t)

INTERLEAVED

NAVIGATORS MRSI

Self-Correction

NAVIGATORS MRSI

Navigated Correction

Page 13: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

METHODS: Correction Strategies Using MRSI Data

Reordered Correction Hybrid Correction

kx = 8, 9, and 10 reordered in data acquisition order to provide more equally distributed high SNR k-space data for estimating center frequency drift.

5

9

13

ky

kx

MRSI

5

9

13

kx

ky

MRSI1

In addition to reordering kx = 8, 9, and 10, Gx and Gy were set to 0 for kx = 1 to provide high SNR navigators every 16 TRs for estimating center frequency drift.

Page 14: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

Water

RESULTS: Comparison of Correction Strategies

No correction ReorderedWithout Correction

ReorderedWith Correction

HybridCorrection

NavigatedCorrection

Page 15: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

RESULTS: Comparison of Correction Strategies

No correction ReorderedWithout Correction

ReorderedWith Correction

HybridCorrection

NavigatedCorrection

NAA

Page 16: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

RESULTS: Comparison of Correction Strategies

No correction ReorderedWithout Correction

ReorderedWith Correction

HybridCorrection

NavigatedCorrection

NAA

Lac

NAACr

Cho

mIGlu

CrmI

Lac

NAACr

ChomI

Glu

CrmI

UncorrectedUncorrected Reordered correction

Page 17: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

FUTURE WORK: Additional Correction Strategies Using MRSI Data

Reordered Correction UsingAdditional Lines of kx

5

9

13

ky

kx

MRSI

5

9

13

ky

kx

MRSI11

Reordered Correction UsingCentral Portion of k-space

Error in the frequency shift parameter defined as the difference between the parameter estimated from the MRSI and the interleaved navigators. Low error is represented as white and high error as black.

Page 18: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

• We have demonstrated that it is possible to significantly reduce spatial artifact encountered in MRSI data resulting from fluctuations in the center frequency during MRSI data acquisition. These variations may be due to instrumentation, environmental or physiological factors

• In this work, the MRSI data itself was used to determine parameters used in the correction. This self-navigated correction approach is feasible when there is strong enough signal from water present in the raw data, either because residual water is intentionally left to provide a reference or because the data is acquired without solvent suppression.

• Future work will focus on improving the temporal resolution of the center frequency estimates by additional reordering of the high SNR points in k-space, validating the concept with multi-compartment phantoms, and evaluating the method using clinically relevant models.

SUMMARY

Page 19: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,

Spectrum from uncorrected MRSI data

Spectrum from corrected MRSI data

Lac

NAACr

Cho

mIGlu

CrmI

Lac

NAACr

ChomI

Glu

CrmI

Page 20: Correcting for Center Frequency Variations in MRSI Data Using the Partially Suppressed Water Signal Lawrence P Panych, Ph.D., Joseph R Roebuck, Ph.D.,