Université de Paris, INSERM UMR 1132, Hôpital Lariboisière, AP-HP, Paris, France.
Vien Gut Medical Center and French-Vietnamese Research Center on Gout and Chronic Diseases, Ho Chi Minh City, Vietnam.
Arthritis Rheumatol. 2021 Feb;73(2):324-329. doi: 10.1002/art.41515. Epub 2020 Dec 5.
The coexistence of calcium pyrophosphate dihydrate (CPPD) and monosodium urate monohydrate crystals in gouty tophi has rarely been reported. We undertook this study to investigate CPPD crystal deposits in a series of surgically removed gouty tophi and to identify factors associated with these deposits.
Twenty-five tophi from 22 gout patients were analyzed using polarized light microscopy, field emission scanning electron microscopy (FESEM), and μ Fourier transform infrared (μFTIR) spectroscopy.
Tophi consisted of multiple lobules separated by fibrous septa and surrounded by a foreign-body giant cell reaction. CPPD crystal aggregates were identified in 9 of 25 tophi from 6 patients. CPPD crystals were dispersed or highly compacted, localized at the edge or inside the tophus lobules, with some lobules completely filled with crystals. Both monoclinic and triclinic CPPD crystal phases were identified using FESEM and μFTIR. Compared to patients without CPPD, those with CPPD-containing tophi were older (mean 60.5 years versus 47.2 years; P = 0.009), and had longer-term gout duration (mean 17.0 years versus mean 9.0 years; P < 0.05) and tophi duration (mean 10.0 years versus mean 4.6 years; P < 0.01). None of the patients had radiographic chondrocalcinosis of the knee or wrist.
CPPD crystal formation seems to be a late and frequent event of tophus maturation, occurring more frequently with aging, and could contribute to the speed of tophus dissolution and the apparent persistence of tophus sometimes observed even after effective, long-lasting urate-lowering therapy.
焦磷酸钙二水合物(CPPD)和单水尿酸单钠晶体在痛风性痛风石中的共存很少有报道。我们进行这项研究,以调查一系列手术切除的痛风石中 CPPD 晶体沉积物,并确定与这些沉积物相关的因素。
使用偏光显微镜、场发射扫描电子显微镜(FESEM)和 μ 傅里叶变换红外(μFTIR)光谱分析了 22 例痛风患者的 25 个痛风石。
痛风石由纤维隔分开的多个小叶组成,周围有异物巨细胞反应。在 6 名患者的 9 个 25 个痛风石中发现 CPPD 晶体聚集体。CPPD 晶体分散或高度致密,位于痛风石小叶的边缘或内部,有些小叶完全充满晶体。FESEM 和 μFTIR 均鉴定出单斜和三斜 CPPD 晶体相。与无 CPPD 患者相比,含有 CPPD 的痛风石患者年龄更大(60.5 岁比 47.2 岁;P = 0.009),痛风持续时间更长(17.0 年比 9.0 年;P < 0.05)和痛风石持续时间更长(10.0 年比 4.6 年;P < 0.01)。没有患者有关节膝或腕部放射学软骨钙质沉着症。
CPPD 晶体形成似乎是痛风石成熟的晚期和常见事件,随着年龄的增长而更频繁发生,并且可能有助于痛风石溶解的速度,以及即使在有效的、长期的尿酸降低治疗后有时仍然存在的痛风石的明显持续存在。