Volume 80, Issue 6 pp. 2514-2524
Full Paper

In vivo bone 31P relaxation times and their implications on mineral quantification

Xia Zhao

Xia Zhao

Department of Radiology, Perelman School of Medicine, University of Pennsylvania, Philadelphia, Pennsylvania

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Hee Kwon Song

Hee Kwon Song

Department of Radiology, Perelman School of Medicine, University of Pennsylvania, Philadelphia, Pennsylvania

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Felix W. Wehrli

Corresponding Author

Felix W. Wehrli

Department of Radiology, Perelman School of Medicine, University of Pennsylvania, Philadelphia, Pennsylvania

Correspondence Felix W. Wehrli, Department of Radiology, Hospital of University of Pennsylvania, 1 Founders Building, 3400 Spruce Street, Philadelphia, PA 19104. Email: [email protected]Search for more papers by this author
First published: 09 May 2018
Citations: 8

Funding information: National Institutes of Health (NIH), Grant number R01-AR50068

Abstract

Purpose

The intersubject variations in bone phosphorus-31 (31P) T1 and urn:x-wiley:07403194:media:mrm27230:mrm27230-math-0001, as well as the implications on in vivo 31P MRI-based bone mineral quantification, were investigated at 3T field strength.

Methods

A technique that isolates the bone signal from the composite in vivo 31P spectrum was first evaluated via simulation and experiments ex vivo and subsequently applied to measure the T1 of bone 31P collectively with a spectroscopic saturation recovery sequence in a group of healthy subjects aged 26 to 76 years. urn:x-wiley:07403194:media:mrm27230:mrm27230-math-0002 was derived from the bone signal linewidth. The density of bone 31P was derived for all subjects from 31P zero TE images acquired in the same scan session using the measured relaxation times. Test–retest experiments were also performed to evaluate repeatability of this in vivo MRI-based bone mineral quantification protocol.

Results

The T1 obtained in vivo using the proposed spectral separation method combined with saturation recovery sequence is 38.4 ± 1.5 s for the subjects studied. Average 31P density found was 6.40 ± 0.58 mol/L (corresponding to 1072 ± 98 mg/cm3 mineral density), in good agreement with an earlier study in specimens from donors of similar age range. Neither the relaxation times (P = 0.18 for T1, P = 0.99 for urn:x-wiley:07403194:media:mrm27230:mrm27230-math-0003) nor 31P density (P = 0.55) were found to correlate with subject age. Average coefficients of variation for the repeat study were 1.5%, 2.6%, and 4.4% for bone 31P T1, urn:x-wiley:07403194:media:mrm27230:mrm27230-math-0004, and density, respectively.

Conclusion

Neither 31P T1 nor urn:x-wiley:07403194:media:mrm27230:mrm27230-math-0005 varies significantly in healthy adults across a 50-year age range, therefore obviating the need for subject-specific measurements.

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