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二氧化硅在羧基和胺基封端表面上的成核动力学:对生物矿化的见解

Kinetics of silica nucleation on carboxyl- and amine-terminated surfaces: insights for biomineralization.

作者信息

Wallace Adam F, DeYoreo James J, Dove Patricia M

机构信息

Department of Geosciences, Virginia Polytechnic Institute & State University, Blacksburg, Virginia 24061, USA.

出版信息

J Am Chem Soc. 2009 Apr 15;131(14):5244-50. doi: 10.1021/ja809486b.

Abstract

An in situ, atomic force microscopy- (AFM-)-based experimental approach is developed to directly measure the kinetics of silica nucleation on model biosubstrates under chemical conditions that mimic natural biosilica deposition environments. Relative contributions of thermodynamic and kinetic drivers to surface nucleation are quantified by use of amine-, carboxyl-, and hybrid NH(3)(+)/COO(-)-terminated surfaces as surrogates for charged and ionizable groups on silica-mineralizing organic matrices. The data show that amine-terminated surfaces do not promote silica nucleation, whereas carboxyl and hybrid NH(3)(+)/COO(-) substrates are active for silica deposition. The rate of silica nucleation is approximately 18x faster on the hybrid substrates than on carboxylated surfaces, but the free energy barriers to cluster formation are similar on both surface types. These findings suggest that surface nucleation rates are more sensitive to kinetic drivers than previously believed and that cooperative interactions between oppositely charged surface species play important roles in directing the onset of silica nucleation. Further experiments to test the importance of these cooperative interactions with patterned NH(3)(+)/COO(-) substrates, and aminated surfaces with solution-borne anionic species, confirm that silica nucleation is most rapid when oppositely charged species are proximal. By documenting the synergy that occurs between surface groups during silica formation, these findings demonstrate a new type of emergent behavior underlying the ability of self-assembled molecular templates to direct mineral formation.

摘要

开发了一种基于原位原子力显微镜(AFM)的实验方法,以在模拟天然生物硅沉积环境的化学条件下,直接测量模型生物底物上二氧化硅成核的动力学。通过使用胺基、羧基和混合NH(3)(+)/COO(-)端基表面作为硅矿化有机基质上带电和可电离基团的替代物,定量了热力学和动力学驱动因素对表面成核的相对贡献。数据表明,胺基端基表面不促进二氧化硅成核,而羧基和混合NH(3)(+)/COO(-)底物对二氧化硅沉积具有活性。混合底物上二氧化硅成核的速率比羧化表面快约18倍,但两种表面类型上团簇形成的自由能垒相似。这些发现表明,表面成核速率对动力学驱动因素比以前认为的更敏感,并且带相反电荷的表面物种之间的协同相互作用在指导二氧化硅成核的开始中起重要作用。用图案化的NH(3)(+)/COO(-)底物以及带有溶液中阴离子物种的胺化表面测试这些协同相互作用重要性的进一步实验证实,当带相反电荷的物种靠近时,二氧化硅成核最快。通过记录二氧化硅形成过程中表面基团之间发生的协同作用,这些发现证明了自组装分子模板指导矿物形成能力背后的一种新型涌现行为。

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