Ground Water Essay

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5.1 INTRODUCTION

Ground water is one of the Nation's most important natural resources. As groundwater moves underground it tends to develop a chemical equilibrium by chemical reactions. With the rising of groundwater levels the salinity of groundwater also increases due to dissolution of rock or mineral salts (Ballukraya and Ravi 1995; Subba Rao 2008). Hydrogeochemical processes of groundwater studied in coastal aquifers (Jagannadha Sarma and Narayana Swamy 1981; Somasundaram et al. 1993; Manjusree et al. 2009), hard rock areas (Sreedevi 2002; Srinivasamoorthy et al. 2008; Gupta et al. 2009), fluoride regions (Ravindra and Garg 2006; Mor et al. 2009; Vikas et al. 2009) for suitability of groundwater quality in respect of drinking and irrigation purposes. Various geo-statistical concepts are also used for the interpretation of complex data sets which may be allows a better understanding of the water quality parameters (Suk and Lee 1999; Suvedha et al. 2009; Yidana and Yidana 2010). In recent years, due to the advent of industrial growth, large-scale application of synthetic fertilizers for agriculture production and use of pesticides and insecticides for production has caused serious concern regarding the susceptibility of groundwater contamination.

5.2 GROUNDWATER SAMPLING AND CHEMICAL ANALYSIS

The technical literature on ground-water sampling provides a great deal of information on selected aspects of an efficient sampling program. A high quality set of hydrologic and chemical data is accurate, precise, comparable, and complete. Groundwater contains a variety of chemical constituents at different concentrations. The greater part of the soluble constituents in groundwater comes from soluble minerals in soils and sedimentary ...

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...unction of TDS (Gibbs, 1970). The Gibbs plotting (Figure 5a-b) of chemical data were mainly around the chemical weathering of rock-forming mineral zone and therefore indicated that the chemical composition of these water were mainly controlled by weathering reactions and can be modified from the underlying biotite gneisses, biotite schists and granite as well as from dissolution of both carbonate and silicate minerals from them and by the interaction between the aquifer rocks and groundwater.

PIPER’S TRI-LINEAR DIAGRAM

The waters were classified into hydrochemical facies indicating water types based on the subdivisions of the Piper-trilinear diagram suggested by Back (1961) and Hanshaw (1965).

Legend
A- Calcium type
B- No Dominant type
C- Magnesium type
D- Sodium and potassium type
E- Bicarbonate type
F- Sulphate type
G- Chloride type

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