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磁共振成像评估的皮质骨孔隙率与显微CT孔隙率高度相关。

Magnetic resonance imaging assessed cortical porosity is highly correlated with μCT porosity.

作者信息

Bae Won C, Patil Shantanu, Biswas Reni, Li Shihong, Chang Eric Y, Statum Sheronda, D'Lima Darryl D, Chung Christine B, Du Jiang

机构信息

Department of Radiology, University of California, San Diego, CA, USA; Department of Radiology, VA San Diego Healthcare System, La Jolla, CA, USA.

Shiley Center for Orthopaedic Research & Education, Scripps Clinic, La Jolla, CA, USA.

出版信息

Bone. 2014 Sep;66:56-61. doi: 10.1016/j.bone.2014.06.004. Epub 2014 Jun 11.

Abstract

Cortical bone is typically regarded as "MR invisible" with conventional clinical magnetic resonance imaging (MRI) pulse sequences. However, recent studies have demonstrated that free water in the microscopic pores of cortical bone has a short T2* but a relatively long T2, and may be detectable with conventional clinical spin echo (SE) or fast spin echo (FSE) sequences. In this study we describe the use of a conventional two-dimensional (2D) FSE sequence to assess cortical bone microstructure and measure cortical porosity using a clinical 3T scanner. Twelve cadaveric human cortical bone samples were studied with MRI and microcomputed tomography (μCT) (downsampled to the same spatial resolution). Preliminary results show that FSE-determined porosity is highly correlated (R(2)=0.83; P<0.0001) with μCT porosity. Bland-Altman analysis suggested a good agreement between FSE and μCT with tight limit of agreement at around 3%. There is also a small bias of -2% for the FSE data, which suggested that the FSE approach slightly underestimated μCT porosity. The results demonstrate that cortical porosity can be directly assessed using conventional clinical FSE sequences. The clinical feasibility of this approach was also demonstrated on six healthy volunteers using 2D FSE sequences as well as 2D ultrashort echo time (UTE) sequences with a minimal echo time (TE) of 8μs, which provide high contrast imaging of cortical bone in vivo.

摘要

在传统的临床磁共振成像(MRI)脉冲序列中,皮质骨通常被认为是“磁共振不可见的”。然而,最近的研究表明,皮质骨微观孔隙中的自由水具有短T2*但相对长的T2,并且可能可以用传统的临床自旋回波(SE)或快速自旋回波(FSE)序列检测到。在本研究中,我们描述了使用传统的二维(2D)FSE序列来评估皮质骨微观结构,并使用临床3T扫描仪测量皮质骨孔隙率。对12个尸体人类皮质骨样本进行了MRI和微观计算机断层扫描(μCT)研究(下采样到相同的空间分辨率)。初步结果表明,FSE测定的孔隙率与μCT孔隙率高度相关(R(2)=0.83;P<0.0001)。Bland-Altman分析表明FSE和μCT之间具有良好的一致性,一致性界限紧密,约为3%。FSE数据也有-2%的小偏差,这表明FSE方法略微低估了μCT孔隙率。结果表明,可以使用传统的临床FSE序列直接评估皮质骨孔隙率。在六名健康志愿者身上也证明了这种方法的临床可行性,使用了2D FSE序列以及最小回波时间(TE)为8μs的2D超短回波时间(UTE)序列,这些序列在体内提供了皮质骨的高对比度成像。

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