Rodgers A L, Webber D, Hibberd B
Department of Chemistry, University of Cape Town, Rondebosch, Cape Town, 7701, South Africa.
Urolithiasis. 2015 Nov;43(6):479-87. doi: 10.1007/s00240-015-0802-4. Epub 2015 Jul 22.
Nephrolithiasis is thought to be governed by urinary thermodynamic and kinetic risk factors. However, identification of one or more of these factors which consistently and unambiguously differentiates between healthy subjects (N) and calcium oxalate (CaOx) renal stone patients (SF) remains elusive. The present study addresses this challenge. 24 h urines were collected from 15 N and 10 SF. Urine compositions were used to compute thermodynamic risk indices including urinary ratios, quotients and supersaturation (SS) values, while CaOx metastable limits (MSL) were determined experimentally. Crystallisation kinetics was determined by measuring rates of particle formation (number, volume, size) using a Coulter counter multisizer (CC) and a Coulter flow cytometer (FC). Particle shapes were qualitatively differentiated by FC and were viewed directly by scanning electron microscopy. Several urinary composition ratios and risk quotients were significantly different between the groups. However, there were no significant differences between CaOx MSL or SS values. Using transformed FC data, the rate of CaOx crystallisation in SF was significantly greater than in N. This was not supported by CC measurements. There were no significant differences between the groups with respect to particle size or CaOx crystal growth rates. Single and aggregated CaOx dihydrate crystals were observed in both groups with equal frequency and there were no differences in the kinetic properties of these deposits. A few CaOx monohydrate crystals were observed in SF. Although several risk factors were found to be significantly different between the groups, none of them were consistently robust when compared to other cognate factors. Arguments were readily invoked which demonstrated inter-factor inconsistencies and conflicts. We suspect that a unique discriminatory factor, such as any of those which we investigated in the present study, may not exist.
肾结石被认为受尿液热力学和动力学风险因素的控制。然而,确定一个或多个能持续且明确地区分健康受试者(N)和草酸钙(CaOx)肾结石患者(SF)的因素仍然难以实现。本研究应对了这一挑战。从15名健康受试者和10名草酸钙肾结石患者中收集了24小时尿液。尿液成分用于计算热力学风险指数,包括尿液比率、商和过饱和度(SS)值,同时通过实验确定草酸钙亚稳极限(MSL)。通过使用库尔特计数器多通道粒度分析仪(CC)和库尔特流式细胞仪(FC)测量颗粒形成速率(数量、体积、大小)来确定结晶动力学。通过FC对颗粒形状进行定性区分,并通过扫描电子显微镜直接观察。两组之间的几种尿液成分比率和风险商有显著差异。然而,草酸钙MSL或SS值之间没有显著差异。使用转换后的FC数据,SF组中草酸钙结晶速率显著高于N组。CC测量结果不支持这一点。两组在颗粒大小或草酸钙晶体生长速率方面没有显著差异。两组中观察到单晶体和聚集的二水草酸钙晶体的频率相同,并且这些沉积物的动力学性质没有差异。在SF组中观察到少量一水草酸钙晶体。尽管发现两组之间有几个风险因素有显著差异,但与其他相关因素相比,没有一个因素始终具有稳健性。很容易找到证据表明因素之间存在不一致和冲突。我们怀疑可能不存在像我们在本研究中所研究的任何一个独特的鉴别因素。