Dipartimento di Chimica, Università di Roma La Sapienza, Piazzale Aldo Moro 5, 00185 Roma, Italy.
Phys Chem Chem Phys. 2010 Jan 7;12(1):227-38. doi: 10.1039/b915182f. Epub 2009 Nov 9.
Fe-doped synthetic geomimetic chrysotile nanocrystals represent a reference standard to investigate the health hazard associated with asbestos fibers and constitute interesting inorganic nanotubes for specific technological applications in light harvesting systems, optoelectronics and photonics. As the fiber toxicity is catalyzed by iron ions in specific crystallographic sites and the mechanical behaviour of synthetic chrysotile nanotubes is strongly affected by the iron doping extent, the characterization of Fe substitution to Mg and/or Si sites in the chrysotile structure appears highly important. By EPR, DRS spectroscopic analyses and magnetic investigations, Mg and/or Si ion replacement by Fe(3+) in a synthetic geomimetic chrysotile structure has been investigated. The results highlight that, as a function of the Fe doping extent and of the Fe doping process, iron can replace both Mg and Si sites. The contemporary iron substitution into the octahedral and tetrahedral sheets is associated with the presence of both of isolated Fe(3+) centres in high-spin 3d(5) configuration (S = 5/2, (6)A(1)((6)S)) in O(h) and T(d) symmetry and of intra-lattice clustered species. Increasing the Fe doping extent increases the concentration of aggregated species, while magnetic susceptibility confirms a paramagnetic anisotropy. The results allow to define the opportunity of using or not metallic Fe during the synthesis to obtain doped chrysotile nanocrystals with tailored morphological and structural properties suitable as a reference to study asbestos toxicity and apt to prepare new inorganic nanotubes and quantum wires for innovative technological applications.
掺铁合成仿地质纤蛇纹石纳米晶体是研究与石棉纤维相关的健康危害的参考标准,同时也是在光收集系统、光电学和光子学等特定技术应用中具有有趣的无机纳米管。由于纤维毒性是由特定晶体学位置的铁离子催化的,并且合成纤蛇纹石纳米管的机械性能受到铁掺杂程度的强烈影响,因此,对纤蛇纹石结构中 Mg 和/或 Si 位取代 Fe 的特性进行表征显得非常重要。通过 EPR、DRS 光谱分析和磁性研究,研究了在合成仿地质纤蛇纹石结构中 Mg 和/或 Si 离子被 Fe(3+)取代的情况。结果表明,随着铁掺杂程度和掺杂过程的变化,铁可以取代 Mg 和 Si 位。同时,八面体和四面体层中同时存在孤立的 Fe(3+)中心,其具有高自旋 3d(5)组态(S = 5/2,(6)A(1)((6)S))的 O(h)和 T(d)对称性和晶格内的聚集态物种,这与同时存在的孤立 Fe(3+)中心有关。增加铁掺杂程度会增加聚集态物种的浓度,而磁化率则证实了顺磁各向异性。这些结果为在合成过程中是否使用金属 Fe 来获得具有所需形貌和结构特性的掺杂纤蛇纹石纳米晶体提供了机会,这些纳米晶体可用作研究石棉毒性的参考标准,并适合于制备新的无机纳米管和量子线,以用于创新性的技术应用。