Baur Andrea, Stäbler Axel, Arbogast Susanne, Duerr Hans Roland, Bartl Reiner, Reiser Maximilian
Departments of Clinical Radiology, University of Munich-Grosshadern, Marchioninistrasse 15, 81377 Munich, Germany.
Radiology. 2002 Dec;225(3):730-5. doi: 10.1148/radiol.2253011413.
PURPOSE: To evaluate the occurrence, location, and shape of the fluid sign in acute osteoporotic and neoplastic vertebral compression fractures at magnetic resonance (MR) imaging. MATERIALS AND METHODS: The study group comprised 87 consecutive patients with acute vertebral compression fractures due to osteoporotic (n = 52) or neoplastic (n = 35) infiltration. The MR imaging protocol included nonenhanced T1-weighted spin-echo and short inversion time inversion-recovery sequences and a 1.5-T system. Readers blinded to the outcome documented the occurrence, shape, and location of the fluid sign with consensus. The fluid sign was correlated with the cause, age, and severity of the fracture. The diagnosis was confirmed with surgery, follow-up MR imaging, clinical follow-up, or unequivocal imaging findings. Wilcoxon and chi(2) tests were used to assess significance. RESULTS: In fractured vertebral bodies, the fluid sign was adjacent to the fractured end plates and exhibited signal intensity isointense to that of cerebrospinal fluid. The fluid sign was linear (n = 16), triangular (n = 5), or focal (n = 2) and was significantly associated with osteoporotic fractures (21 [40%] of 52; P <.001). The fluid sign occurred in two (6%) of 35 neoplastic compression fractures. Histologic examination demonstrated osteonecrosis, edema, and fibrosis at the site of the fluid sign. There was a tendency toward older fractures exhibiting the fluid sign, but this relationship was not significant (P >.05). In osteoporotic fractures, the fluid sign was significantly associated with fracture severity (P <.05). CONCLUSION: The fluid sign is featured in acute vertebral compression fractures that show bone marrow edema. It can be an additional sign of osteoporosis and rarely occurs in metastatic fractures.
目的:评估急性骨质疏松性和肿瘤性椎体压缩骨折在磁共振成像(MR)中的液体信号的出现情况、位置及形态。 材料与方法:研究组包括87例因骨质疏松(n = 52)或肿瘤浸润(n = 35)导致急性椎体压缩骨折的连续患者。MR成像方案包括非增强T1加权自旋回波序列、短反转时间反转恢复序列以及一个1.5T系统。对结果不知情的阅片者一致记录液体信号的出现情况、形态及位置。将液体信号与骨折的病因、年龄及严重程度进行关联分析。通过手术、随访MR成像、临床随访或明确的影像学表现来确诊。采用Wilcoxon检验和卡方检验评估显著性。 结果:在骨折椎体中,液体信号毗邻骨折终板,其信号强度与脑脊液等信号。液体信号呈线性(n = 16)、三角形(n = 5)或局灶性(n = 2),且与骨质疏松性骨折显著相关(52例中有21例[40%];P <.001)。在35例肿瘤性压缩骨折中有2例(6%)出现液体信号。组织学检查显示液体信号部位存在骨坏死、水肿和纤维化。年龄较大的骨折有出现液体信号的趋势,但这种关系不显著(P >.05)。在骨质疏松性骨折中,液体信号与骨折严重程度显著相关(P <.05)。 结论:液体信号在显示骨髓水肿的急性椎体压缩骨折中具有特征性表现。它可以作为骨质疏松的一个附加征象,在转移性骨折中很少出现。
Medicine (Baltimore). 2024-7-5
Diagnostics (Basel). 2023-8-23
Quant Imaging Med Surg. 2018-2
Medicine (Baltimore). 2017-11
J Korean Neurosurg Soc. 2018-1