Graphical methods (e.g., Piper diagram) and statistical cluster analysis (e.g., hierarchical clustering) have been used to cluster water samples as an initial step to interpret hydrochemical processes (natural versus anthropogenic) controlling groundw...
Graphical methods (e.g., Piper diagram) and statistical cluster analysis (e.g., hierarchical clustering) have been used to cluster water samples as an initial step to interpret hydrochemical processes (natural versus anthropogenic) controlling groundwater quality. However, these conventional approaches can be unsatisfactory for reasonable interpretation because 1) groundwater quality can be too complex to successfully analyze using conventional graphical methods, 2) hydrochemical properties of the natural groundwater system can vary continuously, and 3) statistically, the geometrical space of compositional data makes up the simplex and therefore the distance between two compositional observations should be measured by the Aitchison distance, whereas most of statistical clustering methods are based on Euclidean space. This study aims 1) to classify hydrochemical data (compositional data), which was difficult to classify by using hard clustering, through Fuzzy C-menas clustering after performing ilr transformation of hydrochemical data for using strictly statistical methods (fuzzy c-means clustering, PCA, modified piper diagram) in Anseong area. Additionally, 2) we suggest a new quantitative criteria named ANSI (Anthropogenic and Natural Source Identification) to distinguish whether groundwater quality is affected by natural or anthropogenic sources. For this study, hydrochemical data of 77 groundwater samples were collected in an agricultural area of Anseong, South Korea. The ilr (isometric log-ratio)-transformed data of the concentrations of ion (Na+K, Ca, Mg, HCO3, SO4, NO3+Cl, Si) were interpreted using the soft clustering method (i.e., Fuzzy C-means clustering). Then, the fuzziness of the samples belonging to specific groups was plotted on modified Piper diagram for the visualization of quantitative clustering results. In addition, the principal component analysis (PCA) was conducted to understand the factors determining hydrochemical facies. The results yielded three well-defined water types: 1) Ca-HCO3, 2) Ca-SO4, and 3) Ca-Cl-NO3 types. Each group is interpreted to represent distinct groundwater masses: 1) Ca-HCO3 type represents the groundwater quality that affected by natural processes and rarely affected by anthropogenic pollution. 2) Ca-SO4 type describes the groundwater quality that affected by human activities and shows especially highest SO4 concentration, and 3) Ca-Cl-NO3 type represents the groundwater quality that affected by anthropogenic pollutants such as agriculture practices and industrial effluents and indicates highest NO3 concentration. In order to understand the water quality, we plotted groundwater samples at modified piper diagram. We suggest a new quantitative criteria named ANSI (Anthropogenic and Natural Source Identification) to distinguish whether groundwater quality is affected by natural or anthropogenic sources. ANSI index is the ratio of HCO3 versus the geometric mean of SO4 and Cl+NO3. The average value of ANSI indices of overlapping range between natural groundwater (Cluster 1) and polluted groundwater (Cluster 2 and 3) is 1.55. Groundwater with ANSI index≥1.55 is regarded as non-polluted natural groundwater, while groundwater with ANSI index≤1.55 is regarded as polluted groundwater affected by anthropogenic activities. The spatial distribution of ANSI index is well explained by the land use patterns of the study area. Therefore, ANSI index can be proposed as a useful tool to identify the origin of natural and anthropogenic sources of groundwater.