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The IUP Journal of Soil and Water Sciences :
Hydrochemistry of Shallow Tubewell Water, Northern Dinajpur District, Bangladesh
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The present study aims at determining the quality of groundwater samples from six Shallow Tubewells (STWs), with special emphasis on drinking and agricultural uses in the northern part of Dinajpur District. The physiochemical properties of water samples were analyzed in order to measure its quality and suitability. Physical analyses involved the measurement of pH, EC, T °C, Total Dissolved Solid (TDS), Dissolved Oxygen (DO), Redox potential (Eh), Arsenic (As), while the chemical analyses included determination of the concentration of selected cations (Ca2+, Mg2+, Na+, K+, NH+4, Mn+2, Fetotal) and anions (Cl_, CO_3, HCO_3, SO_24, NO_3, NO_2, PO_34). Among the cations, the concentration of calcium is highest, and among the anions, bicarbonate concentration is highest. Besides, B+, F_, I_ were determined. Correlation with different guideline values for water use for drinking and public health purposes shows that the groundwater is suitable for the purposes. The groundwater of this area is moderately hard and requires little softening. Plot of analytical values in the Piper Trillinear diagram shows that alkaline earths exceed alkalies, strong acid exceeds weak acids and non-carbonate hardness (secondary salinity) exceeds 50%. Integrated effect of two properties, viz., EC and Sodium-Adsorption Ratio (SAR), shows that the water is of low alkali hazard and low to medium salinity hazard, and the Permeability Index (PI) also indicates that the water is good for irrigation.

 
 
 

Groundwater is one of the most widely distributed resources of earth and is also an essential source of drinking and irrigation water in Bangladesh. It is also considered as one of the most important resources because of the physiological needs of man, animals, plants, stream, navigation, fisheries, salinity control, dilution of pollution and water required for ecological protection and wetland preservation. So the quality of groundwater is as important as is its quantity. All groundwater contains salts in solution that are derived from the location and past movement of the water. The quality required of a groundwater supply depends on its purpose; thus, needs for drinking water, industrial water, and irrigation water vary widely.

The field parameters of water quality, hydrochemical analysis for 25 parameters of groundwater, suitability of the shallow tube well water for domestic, industrial and irrigation use, and comparison of analytical results with national and international standards for drinking and irrigation purpose are the main objectives of this study.

A total of six samples of groundwater from six Shallow Tube Wells (STW) of one each upazilla were collected in clean plastic bottles (500) at different sections in dry season. Before collecting the samples, each well was pumped for 10 min and then two water samples were collected in a new plastic bottle of 500 mL capacity, which was immediately airtightened with stopper tops to protect air bubbles from forming inside. One of the samples was treated with Hydrochloric Acid (HCl) up to the achievement of pH value of 4.0 to avoid any sort of precipitation of the dissolved ions. All samples were stored in a refrigerator. The field parameters, such as Temperature, pH, Redox potential (Eh), Specific Electrical Conductance (SEC), alkalinity and Dissolved Oxygen (DO), were determined during fieldwork by portable instruments. Temperature was measured in the field using a Scientific Thermometer. pH and Eh were measured by using Bench Meter (Hanna pH 211, Portugal). SEC was measured using EC Meter (Lutron CD 4301, Japan). The Arsenic concentrations were investigated using field test kit during work. To carry out a detailed hydrochemical analysis for major parameters such as Ca2+, Mg2+, Na+, K+, Cl_, CO32_, HCO_3, SO42_, NO3_, NO2_, NH4_, Fetotal, Mn2+, B+, F_, I_, PO42_, DO, TDS and SAR, water samples from 6 DTWs were selected on the basis of the results of SEC survey and study of geomorphic features. The chemical analysis of cation and anions were carried out in the Hydrogeology Laboratory of the Department of Geology and Mining, University of Rajshahi and Central Science Laboratory, University of Rajshahi, SRDI and government recognized laboratories. The chemical parameters were determined in the laboratory following the standard analytical procedures.

 
 
 

Soil And Water Sciences Journal, Shallow Tubewell Water, Industrial Water, Electrical Conductance, Scientific Thermometer, Portable Instruments, Standard Analytical Procedures, Absorption Spectrometric Method, Argentomerric Method, Piper Trilinear Diagram, Sensitive Crops.