Department of Urology, Center for the Study of Lithiasis and Pathological Calcification, University of Florida, Gainesville, Florida, USA.
Urology. 2011 Sep;78(3):721.e13-721.e17. doi: 10.1016/j.urology.2011.04.046. Epub 2011 Jul 13.
To evaluate the factors that affect the enzymatic dissolution rate of calcium oxalate monohydrate (COM), calcium phosphate (brushite), and magnesium ammonium phosphate (struvite) crystals as enzymatic digestion of kidney stones could enhance lithotripsy or provide alternatives to surgical removal.
At pH 4.2, pelleted COM crystals were combined with oxalate decarboxylase (ODC from Bacillus subtilis), oxalate oxidase (from Hordeum vulgare), or control. Crystal dissolution was followed by measuring increases in solution calcium ion concentration. For phosphate-based crystals, the rates of phosphorolysis by the enzyme purine nucleoside phosphorylase (PNP, assay form) were compared to the control solution using spectrophotometry.
The addition of ODC to COM crystals resulted in production of highly soluble calcium formate and a 15-fold increase in COM solubility. By adding a formate-catabolizing enzyme (formate dehydrogenase), dissolution increased 47-fold compared with controls with nearly one half of the mineral dissolved. Oxalate oxidase showed much lower activity than ODC in COM dissolution. Using inorganic phosphate as a substrate, PNP was able to dissolve both brushite and struvite minerals in water at concentrations near saturation. Measuring dissolution by adding more PNP was not possible because of equilibrium and assay detection restraints.
Stone dissolution using enzymes appears to be viable, particularly for oxalate-based minerals. In a closed system, product inhibition by calcium formate appeared to limit the extent of COM crystal dissolution using ODC. Although phosphate-containing minerals appear to be suitable phosphate sources for PNP, the reversibility of the reaction limits the use of this enzyme.
评估影响一水合草酸钙 (COM)、磷酸钙 (brushite) 和磷酸镁铵 (struvite) 晶体酶解速率的因素,因为肾结石的酶解可以增强碎石术或提供手术切除的替代方法。
在 pH 4.2 下,将沉淀的 COM 晶体与草酸脱羧酶 (来自枯草芽孢杆菌的 ODC)、草酸氧化酶 (来自大麦) 或对照物一起孵育。通过测量溶液中钙离子浓度的增加来监测晶体溶解情况。对于磷酸盐基晶体,使用分光光度法比较酶嘌呤核苷磷酸化酶 (PNP,测定形式) 对晶体的磷解作用与对照溶液的速率。
向 COM 晶体中添加 ODC 会产生高度可溶的甲酸钙,并使 COM 的溶解度增加 15 倍。通过添加一种甲酸分解酶 (甲酸脱氢酶),与对照相比,溶解率增加了 47 倍,几乎有一半的矿物质溶解。与 ODC 相比,草酸氧化酶在 COM 溶解中表现出的活性要低得多。使用无机磷酸盐作为底物,PNP 能够在接近饱和浓度的水中溶解 brushite 和 struvite 矿物质。由于平衡和测定检测限制,无法通过添加更多 PNP 来测量溶解情况。
使用酶进行结石溶解似乎是可行的,特别是对于基于草酸盐的矿物质。在封闭系统中,钙甲酸盐的产物抑制作用似乎限制了 ODC 对 COM 晶体溶解的程度。尽管含磷酸盐的矿物质似乎是 PNP 的合适磷酸盐来源,但反应的可逆性限制了该酶的使用。