Santoyo E, Guevara M, Verma Surendra P
Centro de Investigación en Energía, UNAM, Priv. Xochicalco s/no., Centro, Temixco, Mor. 62580, Mexico.
J Chromatogr A. 2006 Jun 16;1118(1):73-81. doi: 10.1016/j.chroma.2006.01.131. Epub 2006 May 2.
The weighted least-squares (WLS) regression method was successfully applied to establish calibration curves with variable amounts of lanthanides ranging from 0.002 to 0.430 microg. These curves were employed for the analysis of 13 lanthanides (La-Nd, Sm-Tb, and Ho-Lu) in 12 international geochemical reference materials (IGRM). The separation of the lanthanide group was achieved in approximately 15 min. Dysprosium could not be determined in IGRM because of its co-elution with Yttrium. A linear gradient program of alpha-HIBA eluent with a concentration ranging from 0.05 to 0.5 M (0.1 M OS, pH 3.8 with NH(4)OH, and a flow-rate of 1.0 ml/min) was employed. The detection was performed with a UV-vis system at 658 nm using a post-column reagent of Arsenazo III (0.5 ml/min). With this set of RP-HPLC conditions together with the use of both the ordinary least-squares (OLS) and the WLS regressions, we report the results of the measurements along with the total propagated uncertainties in individual concentration values. The uncertainties were obtained by combining standard errors in both regression parameters (slope and intercept) with those related to the chromatographic peak areas. The straight-line slopes and intercepts calculated by the WLS method provided not only considerably smaller errors than the conventional OLS method but also a much better estimation of the limits of detection. The concentrations calculated were compared with the "most probable" concentration values of these reference materials reported in the literature. Statistically significant agreement was consistently observed between the HPLC data and the literature values. The total uncertainties in estimated concentration values for the WLS were consistently smaller than the respective errors for the OLS.
加权最小二乘法(WLS)回归方法成功应用于建立校准曲线,镧系元素含量范围为0.002至0.430微克。这些曲线用于分析12种国际地球化学参考物质(IGRM)中的13种镧系元素(La-Nd、Sm-Tb和Ho-Lu)。镧系元素组的分离在约15分钟内完成。由于镝与钇共洗脱,无法在IGRM中测定镝。采用α-羟基异丁酸(α-HIBA)洗脱液的线性梯度程序,浓度范围为0.05至0.5 M(0.1 M OS,用氢氧化铵调至pH 3.8,流速为1.0 ml/min)。使用偶氮胂III柱后试剂(0.5 ml/min)在658 nm处通过紫外-可见系统进行检测。在这组反相高效液相色谱(RP-HPLC)条件下,结合使用普通最小二乘法(OLS)和WLS回归,我们报告了测量结果以及各个浓度值的总传播不确定度。通过将回归参数(斜率和截距)的标准误差与色谱峰面积相关的标准误差相结合来获得不确定度。WLS方法计算的直线斜率和截距不仅比传统的OLS方法误差小得多,而且对检测限的估计也更好。将计算出的浓度与文献中报道的这些参考物质的“最可能”浓度值进行比较。在HPLC数据和文献值之间始终观察到具有统计学意义的一致性。WLS估计浓度值的总不确定度始终小于OLS的相应误差。