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带电多聚 L-氨基酸存在时初始过饱和度对碳酸钙自发沉淀的影响。

Effects of initial supersaturation on spontaneous precipitation of calcium carbonate in the presence of charged poly-L-amino acids.

机构信息

Laboratory for Precipitation Processes, Division of Materials Chemistry, Ruder Bosković Institute, P.O. Box 180, HR-10002 Zagreb, Croatia.

出版信息

J Colloid Interface Sci. 2010 Mar 15;343(2):553-63. doi: 10.1016/j.jcis.2009.12.010. Epub 2009 Dec 6.

Abstract

Spontaneous precipitation of calcium carbonate was investigated in two precipitation systems: (1) with initial supersaturation lower than that corresponding to the solubility of amorphous calcium carbonate (ACC), at which vaterite precipitated, and (2) with initial supersaturation higher than that of ACC solubility, at which a mixture of calcite and vaterite was formed. After the addition of an acidic polypeptide, poly-L-glutamic acid (pGlu) or poly-L-aspartic acid (pAsp), into (1) a significant inhibition of nucleation, expressed as an increase in induction time, and growth of vaterite, perceived as a dead zone, was observed. Extent of inhibition decreased in the order: Inh(pAps)>Inh(pGlu)>>Inh(pLys). The addition of a polypeptide into (2) caused the inhibition of precipitation and changed the morphology and polymorphic composition of the precipitate; only vaterite appeared at approximately c(pAsp)=3 ppm, c(pGlu)=6 ppm, or c(pLys)=7 ppm. This finding is explained as a consequence of kinetic constraints through the inhibition of calcite nucleation and stronger binding of acidic polypeptide by the calcite surfaces than by the vaterite surfaces. Laboratory precipitation studies using conditions that resemble those in living organism should be run at an initial supersaturation corresponding to the solubility of ACC as a limiting condition.

摘要

在两个沉淀体系中研究了碳酸钙的自发沉淀

(1)在初始过饱和度低于无定形碳酸钙(ACC)溶解度的情况下,形成方解石和文石的混合物;(2)在初始过饱和度高于 ACC 溶解度的情况下,形成文石。在(1)中加入酸性多肽聚谷氨酸(pGlu)或聚天冬氨酸(pAsp)后,观察到成核的显著抑制,表现为诱导时间的增加和文石的生长,这被认为是一个死区。抑制程度的顺序为:Inh(pAps)>Inh(pGlu)>>Inh(pLys)。在(2)中加入多肽会导致沉淀的抑制,并改变沉淀的形态和多晶型组成;只有在约 c(pAsp)=3 ppm、c(pGlu)=6 ppm 或 c(pLys)=7 ppm 时才会出现文石。这一发现可以解释为由于动力学限制,通过抑制方解石成核和酸性多肽与方解石表面的结合比与文石表面的结合更强。在与生物体中相似的条件下进行实验室沉淀研究时,应将初始过饱和度控制在 ACC 的溶解度作为限制条件。

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