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扁桃体周围结石

Peritonsillolith.

作者信息

Samant H C, Gupta O P

出版信息

Oral Surg Oral Med Oral Pathol. 1975 Jul;40(1):56-60. doi: 10.1016/0030-4220(75)90346-1.

Abstract

Peritonsillolith appears to be an unknown entity. Two cases of lithiasis in the peritonsillar region following spontaneous rupture of peritonsillar abscesses have been reported. The authors have speculated concerning the cause of stone formation in the peritonsillar region, which has been designated "peritonsillolith," on the basis of lithiasis in other regions of the body, such as gallbladder, kidneys, and salivary glands. Peritonsilloliths most likely form as a result of incomplete evacuation of pus, the dead bacteria and the pus cells providing the nidus for their formation. The salts of these stones are undoubtedly derived from the inflammatory exudates and saliva.

摘要

扁桃体周围结石似乎是一种尚不为人所知的病症。已有报道称,两例扁桃体周围脓肿自发破裂后出现了扁桃体周围区域结石症。作者根据身体其他部位(如胆囊、肾脏和唾液腺)的结石症,推测了扁桃体周围区域结石形成的原因,这种结石被称为“扁桃体周围结石”。扁桃体周围结石很可能是由于脓液未完全排出而形成的,死亡的细菌和脓细胞为其形成提供了病灶。这些结石的盐分无疑来自炎性渗出物和唾液。

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