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Intrinsic hydrated defects in calcium carbonate: A solid state NMR spectroscopic study.

机译:碳酸钙中的固有水合缺陷:固态NMR光谱研究。

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摘要

Common biogenic materials constructed with calcium carbonate mineral phases and an organic matrix exhibit delicate structure with unusual mechanical properties, and have inspired ideas for the design and synthesis of biomimetic functional materials. The organic templates play an important role in directing assembly of the mineral/organic composites, and in controlling the nucleation and subsequent crystallization. Consequently, knowledge about the molecular interactions at mineral/organic interfaces is essential for understanding the principles of the organic-matrix-mediated biomineralization process. Double resonance NMR techniques based on nuclear spin dipole-dipole interactions can provide local structural information about the mineral/organic interface. NMR studies of natural biogenic materials have relied on the assumption that H occurs principally in the organic matrix. However, even abiogenic nominally anhydrous calcium carbonate phases can contain significant amounts of H-containing defects, which could interfere with interpretation of spectroscopic results. Therefore, the occurrence of intrinsic hydrated defects in CaCO3 must be considered in studies of biomineralized and biomimetic materials. The purpose of this work is to determine the nature of the H environments in CaCO3 phases.;The research reported in this thesis focuses primarily on synthetic, additive-free calcium carbonate materials, including calcite, aragonite, and an amorphous phase which is now thought to be a common precursor to crystallization in inorganic and biotic systems. The single pulse and double resonance (mostly CP and HETCOR) 13C and 1H NMR spectra were obtained systematically for these phases, giving qualitative information about the H-bearing species involved in the intrinsic defects. These NMR studies provide a baseline for further NMR analysis of biogenic materials or synthesized mineral/organic composites. A correlation based on 13C{1H} cross-polarization kinetics was also established, from which more quantitative geometrical information can be obtained at low 13C/1H abundance. This method was applied to a synthetic calcite/citrate composite, providing evidence for the close association of citrate with carbonate ions in the calcite host.
机译:由碳酸钙矿物相和有机基质构成的常见生物材料具有微妙的结构和不寻常的机械性能,并为仿生功能材料的设计和合成提供了灵感。有机模板在指导矿物/有机复合物的组装以及控制成核和随后的结晶中起重要作用。因此,有关矿物/有机界面分子相互作用的知识对于理解有机基质介导的生物矿化过程的原理至关重要。基于核自旋偶极-偶极相互作用的双共振NMR技术可以提供有关矿物/有机界面的局部结构信息。天然生物材料的NMR研究基于H主要存在于有机基质中的假设。但是,即使是非生物名义上的无水碳酸钙相也可能包含大量的含H缺陷,这可能会干扰光谱结果的解释。因此,在生物矿化和仿生材料的研究中必须考虑到CaCO3中固有水合缺陷的发生。这项工作的目的是确定CaCO3相中H环境的性质。本论文报道的研究主要集中在合成的,无添加剂的碳酸钙材料上,包括方解石,文石和无定形相,现在人们认为成为无机和生物系统中结晶的常见前体。系统地获得了这些相的单脉冲和双共振(主要为CP和HETCOR)13C和1H NMR光谱,从而给出了与固有缺陷有关的含H物种的定性信息。这些NMR研究为生物材料或合成的矿物/有机复合物的进一步NMR分析提供了基线。还建立了基于13C {1H}交叉极化动力学的相关性,从中可以在低13C / 1H丰度下获得更多定量的几何信息。该方法应用于合成方解石/柠檬酸盐复合材料,为方解石主体中柠檬酸盐与碳酸根离子的紧密结合提供了证据。

著录项

  • 作者

    Feng, Jian.;

  • 作者单位

    State University of New York at Stony Brook.;

  • 授予单位 State University of New York at Stony Brook.;
  • 学科 Chemistry Analytical.;Geochemistry.
  • 学位 Ph.D.
  • 年度 2009
  • 页码 184 p.
  • 总页数 184
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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