Professional Committee of Rock and Mineral Testing Technology of the Geological Society of China, National Geological Experiment and Testing CenterHost
2012 Vol. 31, No. 5
Article Contents

YU Zhao-shui, ZHANG Qin, LIU Ling. Determination of Water Soluble As(Ⅲ) and As(Ⅴ) in Soil by Hydride Generation-Atomic Fluorescence Spectrometry[J]. Rock and Mineral Analysis, 2012, 31(5): 838-841.
Citation: YU Zhao-shui, ZHANG Qin, LIU Ling. Determination of Water Soluble As(Ⅲ) and As(Ⅴ) in Soil by Hydride Generation-Atomic Fluorescence Spectrometry[J]. Rock and Mineral Analysis, 2012, 31(5): 838-841.

Determination of Water Soluble As(Ⅲ) and As(Ⅴ) in Soil by Hydride Generation-Atomic Fluorescence Spectrometry

  • Based on the determination method of Sb(Ⅲ) and Sb(Ⅴ) in soil, a method for the determination of water soluble As(Ⅲ) and total arsenic in soil has been established by using Hydride Generation-Atomic Fluorescence Spectrometry (HG-AFS) in the media of 0.3 mol/L NaH2PO4-Na2HPO4. An amount of As(Ⅴ) was obtained by subtracting As(Ⅲ) from total arsenic. The hydrogen was provided from a hydrogen generator instead of chemical reaction to ignite a H2-Ar flame. Therefore, arsenic in any media was measurable since the arsenic was reduced into AsH3. Effects on the determination of As(Ⅲ) and As(Ⅴ) were investigated for concentrations of NaH2PO4-Na2HPO4 from 0.02 mol/L to 0.4 mol/L. The results show As(Ⅴ) can be screened by 0.3 mol/L NaH2PO4-Na2HPO4. The detection limits were 2.92 ng/g for As(Ⅲ) and 2.35 ng/g for total As. The recoveries of As(Ⅲ) and As(Ⅴ) are 96%-104% and 101%-103%, respectively. The method was simple and highly accurate, meeting the requirements for multiple sample analysis.
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