首页> 外文期刊>Urology >Role of cellular oxalate in oxalate clearance of patients with calcium oxalate monohydrate stone formation and normal controls.
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Role of cellular oxalate in oxalate clearance of patients with calcium oxalate monohydrate stone formation and normal controls.

机译:草酸钙在草酸钙一水合物结石形成患者和正常对照中清除草酸的作用。

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OBJECTIVES: To examine the cellular, plasma, and urinary oxalate and erythrocyte oxalate flux in patients with calcium oxalate monohydrate (COM) stone formation vs normal controls. Pathologic oxalate clearance in humans is mostly integrated in calcium oxalate stone formation. An underlying cause of deficient oxalate clearance could be defective transmembrane oxalate transport, which, in many tissues, is regulated by an anion exchanger (SLC26). METHODS: We studied 2 groups: 40 normal controls and 41 patients with COM stone formation. Red blood cells were divided for cellular oxalate measurement and for resuspension in a buffered solution (pH 7.40); 0.1 mmol/L oxalate was added. The supernatant was measured for oxalate immediately and 1 hour after incubation. The plasma and urinary oxalate were analyzed in parallel. RESULTS: The mean cellular oxalate concentrations were significantly greater in the normal controls (5.25 +/- 0.47 micromol/L) than in those with COM stone formation (2.36 +/- 0.28 micromol/L; P < .01). The mean urinary oxalate concentrations were significantly greater in those with COM stone formation (0.31 +/- 0.02 mmol/L) than in the controls (0.24 +/- 0.02 mmol/L; P < .01). The cellular oxalate concentrations correlated significantly with the plasma (r = 0.49-0.63; P < .01) and urinary oxalate (r = -0.29-0.41; P < .03) concentrations in both groups. The plasma oxalate concentrations correlated significantly with the urinary oxalate concentrations (r = -0.30; P < .03) in the controls and with the erythrocyte oxalate flux (r = 0.25; P < .05) in those with COM stone formation. CONCLUSIONS: Our data implicate the presence of a cellular oxalate buffer to stabilize plasma and urinary oxalate concentrations in normal controls.
机译:目的:与正常对照组相比,检查一水草酸钙一水合物(COM)结石患者的细胞,血浆,尿草酸和红细胞草酸通量。人体内的病理性草酸盐清除率主要整合在草酸钙结石形成中。草酸盐清除率不足的根本原因可能是草酸盐的跨膜转运不良,在许多组织中,这是由阴离子交换剂(SLC26)调节的。方法:我们研究了两组:40名正常对照者和41名COM结石形成患者。将红细胞分开进行细胞草酸盐的测定并重悬于缓冲溶液(pH 7.40)中;加入0.1mmol / L的草酸酯。立即和孵育后1小时测量上清液中的草酸盐。同时分析血浆和草酸尿。结果:正常对照组的平均细胞草酸盐浓度(5.25 +/- 0.47 micromol / L)明显高于形成COM结石的细胞(2.36 +/- 0.28 micromol / L; P <.01)。有结石形成者的平均草酸尿浓度(0.31 +/- 0.02 mmol / L)显着高于对照组(0.24 +/- 0.02 mmol / L; P <0.01)。两组中的细胞草酸盐浓度与血浆(r = 0.49-0.63; P <.01)和尿草酸盐(r = -0.29-0.41; P <.03)显着相关。血浆草酸盐浓度与对照组中尿草酸盐浓度(r = -0.30; P <.03)显着相关,而与形成COM结石的人血浆草酸血红素通量(r = 0.25; P <.05)显着相关。结论:我们的数据暗示在正常对照中存在细胞草酸盐缓冲液以稳定血浆和尿中草酸盐的浓度。

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