Ultrashort echo time magnetization transfer (UTE-MT) imaging of cortical bone.
Ultrashort echo time magnetization transfer (UTE-MT) imaging of cortical bone.
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DOI:
10.1002/nbm.3316
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发表时间:
2015-07
影响因子:
2.9
通讯作者:
Du J
中科院分区:
文献类型:
--
作者:
Chang EY;Bae WC;Shao H;Biswas R;Li S;Chen J;Patil S;Healey R;D'Lima DD;Chung CB;Du J
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 TEs as low as 8 μs can detect signals from different water components in cortical bone. In this study we aim to evaluate two-dimensional (2D) UTE-MT imaging of cortical bone and its application in assessing cortical bone porosity as measured by 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, microcomputed tomography (μCT), and biomechanical testing. Off-resonance saturation ratios (OSR) 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 moderate 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. UTE-MT imaging of 122 human cortical bone samples: correlation between OSR (at 1.5 kHz) and μCT cortical porosity (A), Young’s modulus (B) and yield stress (C). OSR is negatively correlated with porosity, and positively correlated with Young’s modulus and yield stress.