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Ultrashort echo time magnetization transfer (UTE-MT) imaging of cortical bone

  • Author(s): Chang, EY
  • Chang, EY
  • Bae, WC
  • Shao, H
  • Biswas, R
  • Li, S
  • Chen, J
  • Chen, J
  • Patil, S
  • Healey, R
  • D'Lima, DD
  • Chung, CB
  • Chung, CB
  • Du, J
  • et al.

Published Web Location

https://doi.org/10.1002/nbm.3316Creative Commons Attribution 4.0 International Public License
Abstract

© 2015 John Wiley & Sons, Ltd. Magnetization transfer (MT) imaging is one way to indirectly assess pools of protons with fast transverse relaxation. However, conventional MT imaging sequences are not applicable to short T2 tissues such as cortical bone. Ultrashort echo time (UTE) sequences with TE values as low as 8μs can detect signals from different water components in cortical bone. In this study we aim to evaluate two-dimensional UTE-MT imaging of cortical bone and its application in assessing cortical bone porosity as measured by micro-computed tomography (μCT) and biomechanical properties. In total, 38 human cadaveric distal femur and proximal tibia bones were sectioned to produce 122 rectangular pieces of cortical bone for quantitative UTE-MT MR imaging, μCT, and biomechanical testing. Off-resonance saturation ratios (OSRs) with a series of MT pulse frequency offsets (Δf) were calculated and compared with porosity assessed with μCT, as well as elastic (modulus, yield stress, and strain) and failure (ultimate stress, failure strain, and energy) properties, using Pearson correlation and linear regression. A moderately strong negative correlation was observed between OSR and μCT porosity (R2=0.46-0.51), while a moderate positive correlation was observed between OSR and yield stress (R2=0.25-0.30) and failure stress (R2=0.31-0.35), and a weak positive correlation (R2=0.09-0.12) between OSR and Young's modulus at all off-resonance saturation frequencies. OSR determined with the UTE-MT sequence provides quantitative information on cortical bone and is sensitive to μCT porosity and biomechanical function.

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