The use of multicomponent statistical analysis in hydrogeological environmental research
Introduction
Multicomponent statistical analysis is a mathematical technique applied frequently to many problems in geological investigation, such as geochemistry [1], petrography [2], geological engineering [3], and environmental geology [4], [5].
To compare the different chemical parameters of the water analyses and determine the relationships between them, factor analyses were applied to a large number of water quality data samples. This statistical method has several advantages over classical graphical approaches as it takes into consideration more data such as neutral chemical species (e.g. SiO2) and non-chemical data (e.g. temperature) [6], as well as other parameters, such as the distance of a pollutant point from an aquifer. R-Mode factor analysis enables relations among variables, while cluster analysis enables relations among samples to be interpreted in terms of simpler relations that provide an insight into the underlying structure of the data-set [7]. The Discriminant analysis tries to explain why samples should be distinguished in groups according to their characteristics.
In shallow groundwater, increased nitrate concentrations are due to the extensive application of agricultural fertilizers, which are the most common human source of NO3− in groundwater systems [8]. The extent of nitrate leaching from agricultural land is influenced strongly by factors inherent in nature such as soil type and climatic conditions [9]. In groundwater and pore water that is strongly oxidizing, NO3− (the most stable form of dissolved nitrogen) is transported with the groundwater and experiences no chemical transformation and little, or no, retardation [10].
The aim of this paper is to present a simple method based on multicomponent statistical analysis, which could be useful in examining the origin and transport of nitrate ions through the non-saturated and saturated zones of an aquifer. In other words using statistical analysis, we can draw easier conclusions about the factors affecting nitrate transport. Among the most important multicomponent statistical analyses used in this study, Factor analysis (R-mode), Cluster analysis, and Discriminant analysis are presented and proposed as the most efficient.
Section snippets
Hydrogeological setting of the study area
The study area has an extension of 60 Km−2 and is located near the city of Sparta, south Peloponnesus. The shallow aquifer of Sparta (Fig. 1) is developed into the coarse phases of the Plio-Pleistocene sediments, which occupy a broad graben between Mounts Parnon and Taygetos [11]. The bedrock of these formations is composed of crystalline limestones of the zone of Plattenkalk, low metamorphism rocks, phyllites and quartzites, and limestones of the zone of Tripolis [12]. In the pre-orogenic
Determination of used parameters
Selection of the variables on which factor analyses was applied, was carried out in such a way so as to include all possible factors influencing the spread of nitrate ions. The application of the method was based on three data types: (a) data from the unsaturated zone of the aquifer such as the saturated conductivity of the whole thickness of the non-saturated zone and organic matter content (b) data from the saturated zone such as the hydraulic gradient, hydraulic conductivity, transmissivity
Conclusions
From the elaboration of a set of four data groups (hydrogeological, hydrochemical, sedimentary, and environmental), a 4-R-Mode Factor model that explained 74.2% of the total variance was chosen. The following general results can be concluded: The first factor, which accounts for 42.7% of the total variance, is the most significant. It shows clearly the relationship between NO3−, SO42− concentrations and anthropogenic factors such as CROPS and VILDIST, revealing that way the mutual origin of the
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