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胱氨酸、尿酸和草酸钙结石钬:YAG 激光碎石过程中气体形成的观察和比较:色谱和电子显微镜分析。

Observation and comparison of gas formation during holmium:YAG laser lithotripsy of cystine, uric acid, and calcium oxalate stones: a chromatographic and electron microscopic analysis.

机构信息

Department of Urology, Konya City Hospital, Akabe Street, 42020, Konya, Turkey.

Department of Urology, School of Meram Medicine, Necmettin Erbakan University Medical Faculty, Konya, Turkey.

出版信息

Urolithiasis. 2024 Jan 8;52(1):23. doi: 10.1007/s00240-023-01517-4.

Abstract

The primary aim of the present in vitro study is to analyze the chemical content of the bubbles occurring during the fragmentation of cystine stones with both the high-power and low-power holmium:YAG (Ho:YAG) lasers. The secondary aim is to discuss their clinical importance. Three types of human renal calculi calcium oxalate monohydrate (COM), cystine, and uric acid were fragmented with both low-power and high-power Ho:YAG lasers in separate experimental setups at room temperature, during which time it was observed whether gas was produced. After laser lithotripsy, a cloudy white gas was obtained, after the fragmentation of cystine stones only. A qualitative gas content analysis was performed with a gas chromatography-mass spectrometry (GC-MS) device. The fragments in the aqueous cystine calculi setup were dried and taken to the laboratory to be examined by scanning electron microscopy with energy dispersive X-ray spectroscopy (SEM-EDX) and X-ray diffraction analysis. No gas production was observed after fragmentation in the COM and uric acid stones. Free cystine, sulfur, thiophene, and hydrogen sulfide gas were produced by both low-power and high-power Ho:YAG laser lithotripsy of the cystine stones. In the SEM-EDX mapping analysis, a free cystine molecule containing 42.8% sulfur (S), 21% oxygen (O), 14.9% carbon (C), and 21% nitrogen (N) atoms was detected in the cystine stone experimental setup. The evidence obtained, which shows that hydrogen sulfide emerges in the gaseous environment during Ho:YAG laser fragmentation of cystine stones, indicates that caution is required to prevent the risk of in vivo production and toxicity.

摘要

本体外研究的主要目的是分析胱氨酸结石在高功率和低功率钬

钇铝石榴石(Ho:YAG)激光碎石过程中产生的气泡的化学成分。次要目的是讨论它们的临床重要性。在室温下,将三种类型的人类肾结石(一水合草酸钙(COM)、胱氨酸和尿酸)分别用低功率和高功率 Ho:YAG 激光在单独的实验装置中进行粉碎,同时观察是否产生气体。激光碎石后,仅在胱氨酸结石粉碎后获得混浊的白色气体。使用气相色谱-质谱(GC-MS)设备进行定性气体含量分析。将含水胱氨酸结石装置中的结石碎片干燥并带到实验室,用扫描电子显微镜和能量色散 X 射线光谱(SEM-EDX)以及 X 射线衍射分析进行检查。COM 和尿酸结石碎石后均未观察到气体产生。低功率和高功率 Ho:YAG 激光碎石均可产生游离胱氨酸、硫、噻吩和硫化氢气体。在胱氨酸结石实验装置的 SEM-EDX 图谱分析中,检测到含有 42.8%硫(S)、21%氧(O)、14.9%碳(C)和 21%氮(N)原子的游离胱氨酸分子。该研究表明,在 Ho:YAG 激光碎石过程中,胱氨酸结石会在气态环境中产生硫化氢,这表明需要谨慎以防止体内产生和毒性的风险。

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