Guerra Angela, Meschi Tiziana, Schianchi Tania, Allegri Franca, Novarini Almerico, Borghi Loris
Department of Clinical Sciences, University of Parma, Italy.
Acta Biomed. 2002;73(1-2):11-26.
The formation of calcium oxalate (CaOx) crystals, their growth and above all their agglomeration tendency are considered to be decisive factors in the renal stone formation. The aim of this study was to verify whether the formation in vitro of crystalline macroaggregates, induced by increasing loads of oxalate, is different in normal subjects as opposed to CaOx stone formers, free from urinary metabolic abnormalities. The possible interference of the urinary micromolecular environment on the activities of macromolecules with molecular weight greater than 10,000 Daltons was also evaluated. Formation of crystalline macroaggregates took place in controls at a relative CaOx supersaturation equivalent to 32.6 +/- 12.9 and in stone formers at 34 +/- 12.3 (NS); the CaOx RS aggregation--CaOx RS nucleation delta was 11.4 +/- 12.2 in controls and 15.8 +/- 13.9 in stone formers (NS). Leaving aside the stone disease variable, the urine characterized by high baseline CaOx saturation, high ionic strength and high levels of citrate, magnesium and calcium, seemed particularly predisposed to macroaggregates formation; the opposite was true for urine characterized by a totally different micromolecular environment. A very close relationship was found between the CaOx RS aggregation--CaOx RS nucleation delta in urine filtered at 0.22 mu and in metastable solutions containing macromolecules in similar concentrations to those found in the native urine (r = 0.74, P < 0.0001). In conclusion the formation of crystalline macroaggregates in vitro does not present differences in normal subjects compared to CaOx stone formers free from urinary metabolic abnormalities. The urinary macromolecules seem to participate in the formation of the crystalline macroaggregates and their action seems to be affected by the urinary micromolecular environment and, even when they are re-suspended in a completely different medium, their action seems to be preserved intact.
草酸钙(CaOx)晶体的形成、生长,尤其是其聚集倾向被认为是肾结石形成的决定性因素。本研究的目的是验证在草酸盐负荷增加诱导下,正常受试者与无尿代谢异常的CaOx结石形成者相比,体外结晶大聚集体的形成是否存在差异。还评估了尿微分子环境对分子量大于10,000道尔顿的大分子活性的可能干扰。对照组在相对CaOx过饱和度相当于32.6±12.9时发生结晶大聚集体的形成,结石形成者在34±12.3时发生(无显著性差异);对照组的CaOx相对过饱和度聚集 - CaOx相对过饱和度成核差值为11.4±12.2,结石形成者为15.8±13.9(无显著性差异)。抛开结石病变量不谈,以高基线CaOx饱和度、高离子强度以及高柠檬酸盐、镁和钙水平为特征的尿液似乎特别易于形成大聚集体;而以完全不同的微分子环境为特征的尿液则相反。在0.22μm过滤的尿液以及含有与天然尿液中浓度相似的大分子的亚稳溶液中,发现CaOx相对过饱和度聚集 - CaOx相对过饱和度成核差值之间存在非常密切的关系(r = 0.74,P < 0.0001)。总之,与无尿代谢异常的CaOx结石形成者相比,正常受试者体外结晶大聚集体的形成没有差异。尿大分子似乎参与了结晶大聚集体的形成,其作用似乎受尿微分子环境的影响,并且即使将它们重新悬浮在完全不同的介质中,其作用似乎仍能完整保留。