Chillrud Steven N, Hemming N Gary, Ross James M, Wallace Sean, Loiacono Nancy
Lamont-Doherty Earth Observatory of Columbia University, 61 Rt 9W, Palisades, NY 10983, USA.
Appl Geochem. 2005 Apr;20(4):807-813. doi: 10.1016/j.apgeochem.2004.11.002.
Elevated Pb levels in humans through environmental exposure are a significant health concern requiring scientific study of the sources of, and physiological response to this toxin. This requires a simple and precise method for measuring radiogenic Pb isotopes and Pb levels in blood. Presented here is a combination of methods for separation and analysis of Pb previously used predominantly for geologic samples. This includes separation of Pb from the complex matrix of blood samples using an Fe co-precipitation method, followed by isotopic analysis by multi-collector inductively coupled plasma mass spectrometry. Evaluation of the efficacy of this procedure shows that the precision of sample preparations as measured by % difference between the (207)Pb/(206)Pb of duplicate analyses averages 0.064% (n = 48). Using the same preparation and analysis techniques to measure Pb concentrations by isotope dilution resulted in a reproducibility of better than 6%. The method was successfully used to measure uptake of ingested soil Pb in a study of the bioavailability of Pb in contaminated soils.
通过环境暴露导致人体铅水平升高是一个重大的健康问题,需要对这种毒素的来源及其生理反应进行科学研究。这就需要一种简单而精确的方法来测量血液中的放射性铅同位素和铅水平。本文介绍了一种先前主要用于地质样品的铅分离和分析方法的组合。这包括使用铁共沉淀法从血液样本的复杂基质中分离铅,然后通过多接收器电感耦合等离子体质谱进行同位素分析。对该程序有效性的评估表明,通过重复分析的(207)Pb/(206)Pb之间的百分比差异测量的样品制备精度平均为0.064%(n = 48)。使用相同的制备和分析技术通过同位素稀释测量铅浓度,重现性优于6%。该方法已成功用于在一项受污染土壤中铅生物有效性的研究中测量摄入土壤铅的吸收情况。