作者: R. L. PARFITT , J. D. RUSSELL
DOI: 10.1111/J.1365-2389.1977.TB02238.X
关键词: Goethite 、 Oxalate 、 Copper 、 Ligand 、 Denticity 、 Adsorption 、 Chemistry 、 Inorganic chemistry 、 Halide 、 Infrared spectroscopy
摘要: Summary Infrared spectroscopy has been used to investigate the complexes that are formed when acids evaporated onto goethite. It is probable that, like HPO2−4, anions SO2−4, SeO2−3, and oxalate adsorbed by ligand exchange form binuclear bridging where two singly coordinated A-type OH groups replaced oxygen atoms of one ligand. There evidence HPO2−4 likely be present in this wet environments, probably also true for SO2−4 SeO2−3. Fluoride ions can completely replace but do not C- or B-type coordinated, respectively, three Fe3+ ions. The other halides, nitrate, benzoate partially groups, being as a monodentate ligand. Copper appear react with zinc on goethite (100) face conjunction carbonate bicarbonate.