Ghosh Subhendu, Maurya Ashok Kumar, Barman Piyali Deb, Roy Ankit, Madaan Mukul, Choudhury Utpal Roy
Geological Survey of India, Eastern Region, Salt Lake Sector II, Kolkata, 700091, India.
Geological Survey of India, Nothern Region, Aliganj Sector-E, Lucknow, 226024, India.
Anal Sci. 2023 Sep;39(9):1531-1539. doi: 10.1007/s44211-023-00367-9. Epub 2023 May 29.
The presence of arsenic in ground waters of many countries has been a subject of global concern due to its toxicity. Primary sources of arsenic are geogenic, i.e. weathering and erosion of rocks and soils containing arsenic. This paper presents a rapid method for determination of arsenic in solid geological samples by wavelength dispersive X-ray fluorescence spectrometer. To achieve the best LLD (lower limit of detection), the most intense X-ray fluorescence line Kα is preferably used for determination of elemental concentrations because it pertains to the most probable transition. But the greatest challenge in arsenic estimation is the serious line overlap of AsKα lines with the equi-energy PbLα lines. By using the conventional line overlap correction methods, uncertainty and detection limits in arsenic determination are degraded to an unacceptable degree in samples which contains high lead and low arsenic concentrations. The proposed method bypasses the line overlap issue in employing a novel concept of arsenic-lead concentration equivalence factor for the cumulative peak of AsKα and PbLα fluorescence lines. The constancy of this factor for all geological matrices facilitates arsenic determination in samples universally irrespective of matrix elements. For the method validation, 22 international certified reference materials have been analysed and the results proved to be propitious wherein only one value out of 22 determinations showed relative error more than 20% of the certified values. This attests to the high accuracy of the proposed method which can effectively determine arsenic below 5 mg/kg in the presence of high lead concentration up to 1000 mg/kg.
由于砷的毒性,许多国家地下水中砷的存在已成为全球关注的问题。砷的主要来源是地质成因的,即含砷岩石和土壤的风化和侵蚀。本文提出了一种用波长色散X射线荧光光谱仪测定固体地质样品中砷的快速方法。为了获得最佳的检测下限(LLD),最好使用最强的X射线荧光线Kα来测定元素浓度,因为它涉及最可能的跃迁。但是,砷含量估算中最大的挑战是AsKα线与等能量的PbLα线严重的谱线重叠。通过使用传统的谱线重叠校正方法,在高铅低砷浓度的样品中,砷测定的不确定度和检测限会降低到不可接受的程度。所提出的方法通过采用AsKα和PbLα荧光线累积峰的砷-铅浓度等效因子这一新颖概念,绕过了谱线重叠问题。该因子在所有地质基质中的恒定性便于普遍测定样品中的砷,而与基质元素无关。为了验证该方法,分析了22种国际认证参考物质,结果证明是有利的,其中22次测定中只有一个值的相对误差超过认证值的20%。这证明了所提出方法的高精度,该方法能够在高达1000mg/kg的高铅浓度下有效测定低于5mg/kg的砷。