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Spectrophotometric Flow Injection Analysis of Silicates for Manganese

机译:锰硅酸盐的分光光度流动注射分析

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A flow injection Spectrophotometric method has been developed for the determination of manganese in silicate rocks with formaldoxime as a chromogenic reagent. A rock solution is prepared by fusion with a mixture of lithium carbonate and boric acid and subsequent dissolution of the cake in 1M hydrochloric acid. An aliquot of the sample solution is treated with hydrofluoric and perchloric acids and passed through a cellulose phosphate column to remove polyvalent cations like iron(III) and aluminum(III). A definite portion of the filtrate is injected into the flow system where the manganese-formaldoxime complex allows to be formed and monitored at 452nm. Nickel is masked with 2-aminoethanethiol by a merging zone technique. The flow injection analysis system permits throughput of 45 samples per hour. The relative standard deviations (n=10) for 0.5 and 2.0ppm manganese solutions are 0.80 and 0.33%, respectively. The procedure has been applied to a variety of standard silicate rocks of the U.S.Geological Survey and of the Geological Survey of Japan, yielding the results which are in satisfactory agreement with the recommended or reported values.
机译:流动注射分光光度法已被开发出来,以福尔多肟为生色剂测定硅酸盐岩石中的锰。通过与碳酸锂和硼酸的混合物熔融并随后将滤饼溶解在1M盐酸中来制备岩石溶液。将样品溶液的等分试样用氢氟酸和高氯酸处理,并通过磷酸纤维素柱以去除多价阳离子,如铁(III)和铝(III)。将一定量的滤液注入流动系统,在该流动系统中可以形成锰-甲醛肟配合物,并在452nm处进行监测。通过合并区技术,镍被2-氨基乙硫醇掩盖。流动注射分析系统允许每小时处理45个样品。 0.5和2.0ppm锰溶液的相对标准偏差(n = 10)分别为0.80和0.33%。该程序已应用于美国地质调查局和日本地质调查局的各种标准硅酸盐岩,其结果与建议值或报告值相符。

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