Department of Bioenvironmental Systems Engineering, National Taiwan University, Taipei 106, Taiwan, ROC.
J Hazard Mater. 2011 Jan 30;185(2-3):1458-66. doi: 10.1016/j.jhazmat.2010.10.069. Epub 2010 Oct 25.
Redox couples approach and multivariate statistical techniques, including factor analysis, cluster analysis and discriminant analysis, were applied to evaluate and to interpret the complex groundwater quality in the blackfoot disease endemic area, Taiwan. Most groundwater samples were characterized as Na-Ca-HCO(3) with HCO(3)(-) as the dominant anion. Total arsenic (As) concentration, predominantly as As(3+), ranged from <1.0 to 562.7 μg/L. The patterns of measured reducing potential were consistent with those values calculated from As couple, revealing the in situ environment enhanced the accumulation of As concentration in the groundwater. Factor analysis proposed a four-factor model, comprising salination, reductive dissolution of Fe/Mn oxyhydroxides, As reduction and chemical potential factor, and explained 89.94% of total variance in groundwater. Furthermore, two factors, reductive dissolution of Fe/Mn oxyhydroxides and As reduction, suggested that the decoupled reductive processes accounted for high As concentration in this area. Cluster analysis was adopted to spatially categorize the sampled wells into three main clusters and characterized by the factor scores of the four-factor model. Two-parameter (pH and Eh) model derived from discriminant analysis can be used for preliminary assessment to determine whether the As concentration exceeds 10 μg/L with simple field measurements in this area.
采用氧化还原对方法和多元统计技术,包括因子分析、聚类分析和判别分析,评估和解释了台湾黑脚病流行区复杂的地下水质量。大多数地下水样本的特征为 Na-Ca-HCO3,HCO3-为主要阴离子。总砷(As)浓度主要以 As(3+)形式存在,范围从 <1.0 至 562.7μg/L。实测还原电位的模式与从 As 对计算得出的模式一致,表明原位环境促进了地下水 As 浓度的积累。因子分析提出了一个四因子模型,包括盐化作用、Fe/Mn 氢氧化物的还原溶解、As 还原和化学势因子,解释了地下水总方差的 89.94%。此外,两个因子,即 Fe/Mn 氢氧化物的还原溶解和 As 还原,表明脱耦的还原过程导致了该地区高浓度的 As。聚类分析采用空间方法将采样井分为三个主要类群,并根据四因子模型的因子得分进行特征描述。判别分析得到的双参数(pH 和 Eh)模型可用于初步评估,以便用简单的现场测量确定该地区的 As 浓度是否超过 10μg/L。