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Determination of selenium in soil samples using high-resolution continuum source graphite furnace atomic absorption spectrometry and direct solid sample analysis

机译:高分辨率连续源石墨炉原子吸收光谱法和直接固体样品分析法测定土壤样品中的硒

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A method has been developed for the determination of Se in soil samples using high-resolution continuum source graphite furnace atomic absorption spectrometry and direct solid sample analysis. The most sensitive absorption line at 196.026 nm has been used for all determinations. Ruthenium, apart from being deposited on the platform as a permanent modifier, was also added in solution on top of each solid sample. All soil samples exhibited a fine structured background caused primarily by the NO and PO molecules. Reference spectra of these molecules were recorded using nitric and phosphoric acids, respectively, which were used for least squares background correction. The limits of detection and quantification were 30 ng g~(-1) Se and 100 ng g~(-1) Se, respectively. Soil samples were collected from untreated experimental farming areas (without addition of fertilizers) in order to obtain representative values of natural selenium distribution. Appropriate areas for sampling were selected in 12 of the 27 Brazilian states, covering 61% of the total area of the country. The results of the certified reference materials MURST-ISS-A1, MESS-3 and PACS-2 Marine Sediments confirmed the validity of the proposed method. The selenium content found in the soil samples varied between 130 ± 10 ng g~(-1) and 630 ± 15 ng g~(-1). The repeatability of the measurements was between 3% and 10% (n = 3).
机译:已开发出一种使用高分辨率连续谱源石墨炉原子吸收光谱法和直接固体样品分析法测定土壤样品中硒的方法。所有测定均使用196.026 nm处最敏感的吸收线。钌除了作为永久性改性剂沉积在平台上之外,还以溶液形式添加到每个固体样品的顶部。所有土壤样品均显示出主要由NO和PO分子引起的精细结构背景。这些分子的参考光谱分别使用硝酸和磷酸记录,用于最小二乘本底校正。检出限和定量检出限分别为30 ng g〜(-1)Se和100 ng g〜(-1)Se。从未经处理的试验农业地区(不添加肥料)收集土壤样品,以获得自然硒分布的代表性值。在巴西的27个州中,有12个州选择了合适的采样区域,覆盖了该国总面积的61%。经认证的参考材料MURST-ISS-A1,MESS-3和PACS-2海洋沉积物的结果证实了该方法的有效性。土壤样品中的硒含量在130±10 ng g〜(-1)和630±15 ng g〜(-1)之间变化。测量的可重复性在3%和10%之间(n = 3)。

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