Whitehouse R W, Economou G, Adams J E
Bone Disease Research Centre, University of Manchester, England.
J Comput Assist Tomogr. 1993 Nov-Dec;17(6):945-51. doi: 10.1097/00004728-199311000-00017.
Inaccuracies in quantitative CT (QCT) for vertebral bone mineral measurements may result from differences between the temperature of the vertebrae and the calibration standards. This study aims to quantify these effects by using scans of marrow-equivalent materials and computer simulation.
The CT numbers of fat, water, gelatin suspension, and bone were measured within an anthropomorphic phantom at temperatures between -18 and 38 degrees C. A computer simulation was then performed using these materials to represent marrow fat, soft tissue, and bone in varying proportions over this temperature range. Postprocessing single and dual energy QCT calculations were then performed on the data acquired from the simulation.
A change of 80 HU in the CT number of water on cooling from 38 to -18 degrees C was demonstrated. An increase of 95 HU in the CT number of fat occurred over the same temperature range. Dry cortical bone showed no change in CT number with temperature changes from 24 to -18 degrees C. In the computer simulation, the fat error associated with single energy QCT for trabecular bone mineral densitometry was 20% less for specimens at room temperature than at body temperature. In simulated frozen specimens, varying marrow fat/soft tissue composition had almost no effect on single energy QCT mineral densitometry. Dual energy QCT methods that use a fat-equivalent reference material were significantly influenced by the temperature of the specimen.
The fat error of single energy QCT for mineral densitometry may have been underestimated in previous in vitro studies using vertebral specimens scanned at room temperature. In the simulation, the fat error diminished as the temperature of the specimen was reduced and was negligible when frozen. Fat-equivalent reference materials used for dual energy QCT in vivo should have similar X-ray-attenuating properties at room temperature to those of marrow fat at body temperature.
定量CT(QCT)测量椎体骨矿物质时的误差可能源于椎体温度与校准标准之间的差异。本研究旨在通过使用骨髓等效材料扫描和计算机模拟来量化这些影响。
在温度介于-18至38摄氏度之间的仿真人体模型中测量脂肪、水、明胶悬浮液和骨骼的CT值。然后使用这些材料进行计算机模拟,以在此温度范围内以不同比例代表骨髓脂肪、软组织和骨骼。接着对从模拟中获取的数据进行后处理单能和双能QCT计算。
证明水的CT值在从38摄氏度冷却至-18摄氏度时变化了80HU。在相同温度范围内,脂肪的CT值增加了95HU。干燥皮质骨在温度从24摄氏度变化至-18摄氏度时CT值无变化。在计算机模拟中,室温下小梁骨矿物质密度测定的单能QCT相关脂肪误差比体温下的标本小20%。在模拟冷冻标本中,不同的骨髓脂肪/软组织组成对单能QCT矿物质密度测定几乎没有影响。使用脂肪等效参考材料的双能QCT方法受标本温度的显著影响。
在先前使用室温下扫描的椎体标本进行的体外研究中,单能QCT用于矿物质密度测定的脂肪误差可能被低估了。在模拟中,脂肪误差随着标本温度降低而减小,冷冻时可忽略不计。体内用于双能QCT的脂肪等效参考材料在室温下应具有与体温下骨髓脂肪相似的X射线衰减特性。