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原子发射光谱分析中的撒样法,是苏联光谱学家捏得莱尔于1936年首先提出来的。后经鲁萨诺夫等人的逐步改进,到1957年即发展成为一种比较完善的分析手段。我国于1957年首先在冶金部地质研究所(现中国有色金属工业总公司矿产地质研究院)由苏联光谱专家克列斯基扬尼诺夫介绍应用了这种方法。随后,在整个地质部门得到了广泛的应用。撒(吹)样法与垂直电极孔穴蒸发法相比,具有检出限低(易挥发元素),再现性好,快速和成本低廉等优点,是一
Spattering in atomic emission spectroscopy was first proposed by the Soviet spectroscopist Lehrer in 1936. After the gradual improvement of Rousanov and others, it developed into a comparatively perfect analysis method in 1957. China first applied this method in 1957 by the Soviet spectral expert Klitschyaninov at the Institute of Geology, Ministry of Metallurgy (now the Institute of Mineral Geology, China Nonferrous Metals Industry Corporation). Subsequently, the entire geological department has been widely used. Compared with the vertical electrode hole evaporation method, the sampling method has the advantages of low detection limit (volatile elements), good reproducibility, fastness and low cost, and is one