铁质
菲咯啉
硅酸盐
铁
标准物质
化学
土壤水分
分析化学(期刊)
矿物学
分光光度法
土工试验
氧化还原
核化学
地质学
环境化学
无机化学
色谱法
检出限
土壤科学
有机化学
作者
P. K. Tarafder,Raghbendra Thakur
标识
DOI:10.1111/j.1751-908x.2012.00183.x
摘要
A precise, accurate and rapid method for the sequential determination of FeO and Fe 2 O 3 in rocks, soils and some non‐refractory minerals by 1,10‐phenanthroline spectrophotometry is described. Fe( II ) and Fe( III ) were leached from the sample (−200 mesh) using a mixture of NH 4 HF 2 and H 2 SO 4 at 40–80 °C for 10 min on a hot plate. Both Fe( II ) and Fe( III ) could be conveniently estimated sequentially from the same reaction mixture at the μg g −1 to percentage level. The method is better than the existing wet chemical methods, including the commonly used P ratt's titrimetric redox method, for Fe( II ) and Fe( III ) determinations in rock and soil samples in terms of precision, accuracy and rapidity. The throughput of the method was very high; at least forty to fifty samples could be estimated easily in a day. The results obtained compare favourably with those obtained by P ratt's method, as well as for certified/recommended values of a set of eleven certified reference materials having FeO and Fe 2 O 3 contents in the range 0.21–14.63% and 0.58–8.48%, respectively. The optimised 1,10 phenanthroline method was found to be accurate to within 0.21% m/m FeO and 0.30% m/m Fe 2 O 3 compared with the literature values of the certified reference materials studied.
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