Archivos espanoles de urologia · 2002
[Intra-scrotal lithiasis. Crystallographic analysis].
Клинический случайСтатьяНазвание и аннотация: Перевод в очереди
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Sánchez Merino José María, Lancina Martín Alberto, Grases Freixedas Félix, Parra Muntaner Luis, Gómez Cisneros Sergio Carlos, García Alonso Jesús
Аннотация
OBJECTIVE: To present two cases of intrascrotal lithiasis associated with hydrocele and the results of the crystallographic study.
METHODS: Three intrascrotal calculi in two patients aged 72 and 75 years that underwent surgery for hydrocele were analyzed. Two 2-mm. calculi were incidentally discovered during surgery for a right hydrocele in one patient. An ultrasound scan of the other patient showed a left hydrocele with a free-floating, round, hyperechoic, 6-mm. calculus, with posterior acoustic shadow. None of the patients had a previous history of trauma. The 3 calculi were white and smooth, but turned yellow and rough after removal. Scanning electron microscopy and x-ray dispersion studies were performed.
RESULTS: All 3 calculi had a center comprised of hydroxyapatite and white organic matter, and an exterior of yellow organic matter. The mineral portion of the center of the 6-mm. calculus and one of the 2-mm. calculi was composed of 33% phosphorus and 67% calcium, and the other 2-mm. calculus contained 32% phosphorus and 68% calcium by x-ray dispersion analysis.
CONCLUSIONS: Intrascrotal lithiasis is rare. In the two cases described herein, we observed abundant organic matter, particularly on the stone surface, and hydroxyapatite, particularly in the center. Among the possible etiologic causes, the deposit of organic matter in the presence of high oversaturation of calcium phosphates and absence of crystallization inhibitors, can initiate calcification and the subsequent collection of organic matter makes the process irreversible.
METHODS: Three intrascrotal calculi in two patients aged 72 and 75 years that underwent surgery for hydrocele were analyzed. Two 2-mm. calculi were incidentally discovered during surgery for a right hydrocele in one patient. An ultrasound scan of the other patient showed a left hydrocele with a free-floating, round, hyperechoic, 6-mm. calculus, with posterior acoustic shadow. None of the patients had a previous history of trauma. The 3 calculi were white and smooth, but turned yellow and rough after removal. Scanning electron microscopy and x-ray dispersion studies were performed.
RESULTS: All 3 calculi had a center comprised of hydroxyapatite and white organic matter, and an exterior of yellow organic matter. The mineral portion of the center of the 6-mm. calculus and one of the 2-mm. calculi was composed of 33% phosphorus and 67% calcium, and the other 2-mm. calculus contained 32% phosphorus and 68% calcium by x-ray dispersion analysis.
CONCLUSIONS: Intrascrotal lithiasis is rare. In the two cases described herein, we observed abundant organic matter, particularly on the stone surface, and hydroxyapatite, particularly in the center. Among the possible etiologic causes, the deposit of organic matter in the presence of high oversaturation of calcium phosphates and absence of crystallization inhibitors, can initiate calcification and the subsequent collection of organic matter makes the process irreversible.