Jeong Hoon Y, Lee Jun H, Hayes Kim F
Department of Civil and Environmental Engineering, University of Michigan, Ann Arbor, Michigan 48109-2125, Ann Arbor, Michigan 48109, USA.
Geochim Cosmochim Acta. 2008 Jan 15;72(2):493-505. doi: 10.1016/j.gca.2007.11.008.
Iron sulfide was synthesized by reacting aqueous solutions of sodium sulfide and ferrous chloride for 3 days. By X-ray powder diffraction (XRPD), the resultant phase was determined to be primarily nanocrystalline mackinawite (space group: P4/nmm) with unit cell parameters a = b = 3.67 Å and c = 5.20 Å. Iron K-edge XAS analysis also indicated the dominance of mackinawite. Lattice expansion of synthetic mackinawite was observed along the c-axis relative to well-crystalline mackinawite. Compared with relatively short-aged phase, the mackinawite prepared here was composed of larger crystallites with less elongated lattice spacings. The direct observation of lattice fringes by HR-TEM verified the applicability of Bragg diffraction in determining the lattice parameters of nanocrystalline mackinawite from XRPD patterns. Estimated particle size and external specific surface area (SSA(ext)) of nanocrystalline mackinawite varied significantly with the methods used. The use of Scherrer equation for measuring crystallite size based on XRPD patterns is limited by uncertainty of the Scherrer constant (K) due to the presence of polydisperse particles. The presence of polycrystalline particles may also lead to inaccurate particle size estimation by Scherrer equation, given that crystallite and particle sizes are not equivalent. The TEM observation yielded the smallest SSA(ext) of 103 m(2)/g. This measurement was not representative of dispersed particles due to particle aggregation from drying during sample preparation. In contrast, EGME method and PCS measurement yielded higher SSA(ext) (276-345 m(2)/g by EGME and 424 ± 130 m(2)/g by PCS). These were in reasonable agreement with those previously measured by the methods insensitive to particle aggregation.
通过使硫化钠水溶液与氯化亚铁反应3天合成了硫化铁。通过X射线粉末衍射(XRPD),确定所得相主要为纳米晶马基诺矿(空间群:P4/nmm),其晶胞参数a = b = 3.67 Å,c = 5.20 Å。铁K边X射线吸收光谱(XAS)分析也表明马基诺矿占主导地位。相对于结晶良好的马基诺矿,观察到合成马基诺矿沿c轴有晶格膨胀。与相对短龄期的相相比,此处制备的马基诺矿由较大的微晶组成,晶格间距伸长较少。通过高分辨率透射电子显微镜(HR-TEM)对晶格条纹的直接观察证实了布拉格衍射在从XRPD图谱确定纳米晶马基诺矿晶格参数方面的适用性。纳米晶马基诺矿的估计粒径和外部比表面积(SSA(ext))随所使用的方法有显著变化。基于XRPD图谱使用谢乐方程测量微晶尺寸受到谢乐常数(K)不确定性的限制,这是由于存在多分散颗粒。多晶颗粒的存在也可能导致用谢乐方程进行的粒径估计不准确,因为微晶尺寸和颗粒尺寸并不等同。TEM观察得到的最小SSA(ext)为103 m²/g。由于样品制备过程中干燥导致的颗粒聚集,该测量结果不代表分散颗粒。相比之下,乙二醇单甲醚(EGME)方法和光子相关光谱(PCS)测量得到的SSA(ext)更高(EGME法为276 - 345 m²/g,PCS法为424 ± 130 m²/g)。这些结果与先前使用对颗粒聚集不敏感的方法测量的结果合理一致。