Yu J S, Chung C, Recht M, Dailiana T, Jurdi R
Department of Radiology, Ohio State University Medical Center, Columbus 43210, USA.
AJR Am J Roentgenol. 1997 Feb;168(2):523-7. doi: 10.2214/ajr.168.2.9016240.
MR imaging is not routinely used for evaluation of tophaceous gout. However, gout may present clinically in an atypical, unusual, or confusing manner. A gouty tophus occasionally mimics an infectious or neoplastic process, and MR imaging may be obtained under these circumstances. The purpose of this study was to determine the MR imaging characteristics of intraosseous and soft-tissue tophi.
We identified 13 MR imaging examinations performed during a 27-month period on nine patients with gouty arthritis. All were men 42-70 years old. T1-, proton density-, and T2-weighted spin-echo MR images were obtained for all the examinations. Nine examinations included contrast-enhanced MR images. The findings were then evaluated, as were the corresponding radiographs.
Five patients presented with articular involvement, three patients with an isolated soft-tissue mass, and one patient with persistent soft-tissue swelling. The duration of symptoms ranged from 3 months to more than 20 years. Nearly all the tophi were of intermediate signal intensity on T1-weighted images. On T2-weighted images, three sites revealed an overall increase in the signal intensity of the tophi, whereas 10 studies showed a heterogeneous decrease in signal intensity. All but one tophus showed homogeneous enhancement. Erosion of adjacent bone, synovial pannus, joint effusion, soft-tissue edema, and bone marrow edema were common associated findings.
The MR appearance of tophi in patients with tophaceous gout is constant on T1- but quite variable on T2-weighted images. This variability in signal intensity could be related to calcium within a tophus. Tophaceous gout should be considered in the differential diagnosis when a mass reveals heterogeneously low to intermediate signal intensity, particularly if the adjacent bone shows typical erosive changes or if other joints are involved. When faced with this situation, radiologists may find it helpful to obtain a further clinical history and recommend evaluating the patient's serum urate level.
磁共振成像(MR成像)通常不用于痛风石性痛风的评估。然而,痛风在临床上可能以非典型、不常见或令人困惑的方式表现。痛风石偶尔会模仿感染或肿瘤性病变,在这些情况下可能会进行MR成像检查。本研究的目的是确定骨内和软组织痛风石的MR成像特征。
我们确定了在27个月期间对9例痛风性关节炎患者进行的13次MR成像检查。所有患者均为42 - 70岁男性。所有检查均获取了T1加权、质子密度加权和T2加权自旋回波MR图像。9次检查包括增强MR图像。然后对检查结果以及相应的X线片进行评估。
5例患者有关节受累,3例患者有孤立的软组织肿块,1例患者有持续性软组织肿胀。症状持续时间从3个月到20多年不等。几乎所有痛风石在T1加权图像上呈中等信号强度。在T2加权图像上,3个部位的痛风石信号强度总体增加,而10项研究显示信号强度不均匀降低。除1个痛风石外,所有痛风石均表现为均匀强化。相邻骨质侵蚀、滑膜血管翳、关节积液、软组织水肿和骨髓水肿是常见的相关表现。
痛风石性痛风患者痛风石的MR表现T1加权像上较为恒定,但在T2加权像上变化较大。这种信号强度的变化可能与痛风石内的钙有关。当肿块显示不均匀的低到中等信号强度时,尤其是相邻骨质出现典型侵蚀性改变或其他关节受累时,鉴别诊断应考虑痛风石性痛风。面对这种情况时,放射科医生进一步了解临床病史并建议检测患者血清尿酸水平可能会有所帮助。