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www.etasr.com Bhatti et al.: Ground Water Quality Assessment of Daur Taluka, Shaheed Benazir Abad 
 

Ground Water Quality Assessment of Daur Taluka, 
Shaheed Benazir Abad 

 

Nadeem-ul-Karim Bhatti 

Department of Civi Engineering 
Quaid-e-Awam University of Engineering, Science & 

Technology 
Larkana, Pakistan  

knadeem_b@quest.edu.pk 

Salem Raza Samo 
Department of Energy & Environment  

Quaid-e-Awam University of Engineering, Science & 
Technology 

Nawabshah, Pakistan 
sfaizsamo@yahoo.com 

Abdullah Saand 
Department of Civil Engineering 

Quaid-e-Awam University of 
Engineering, Science & Technology 

Nawabshah, Pakistan  
abdullah@quest.edu.pk 

Manthar Ali Keerio 
Department of Civil Engineering 

Quaid-e-Awam University of 
Engineering, Science & Technology 

Larkana, Pakistan 
mantharali99@quest.edu.pk 

Ahsan Ali Bhuriro 
Department of Civil Engineering 

Quaid-e-Awam University of 
Engineering, Science & Technology 

Larkana, Pakistan 
ahsanone@gmail.com 

 

 
Abstract—The aim of this study was to assess the ground water 
quality of Daur Taluka of district Shaheed Benazir Abad for 
drinking purposes. Forty groundwater samples were collected 
from different locations and brought to Pakistan Council of 
Research in Water Resources (PCRWR) for analyzing various 
groundwater physical, chemical and biological parameters. The 
results of this study revealed that color, pH, magnesium, 
alkalinity and nitrate of all samples were found within the 
permissible limits of World Health Organization (WHO). 
Analytical results revealed that the percentage of samples that 
were beyond WHO standards was 15% regarding taste, 42.5% 
regarding TDS, 20% regarding chlorine, 12.5% regarding sulfate 
12.5 regarding sodium and 32.5% regarding hardness. 
Microbiological contamination was found positive in the 25% of 
samples. The findings of this study revealed that the most 
(82.5%) of the samples of the study area belong to the category of 
hard to very hard water and their nature were alkaline. 

Keywords-water quality parameters; arsenic; Taluka Daur; 
Shaheed Benazir Abad; WHO standards 

I. INTRODUCTION 
Water is one of the most important ecosystem and climate 

components. Water quantity and quality determine the 
biodiversity of an ecosystem. Water quantity and quality is not 
distributed evenly in the world [1, 2]. Safe drinking water is not 
only a fundamental requirement of all living organisms but also 
an indispensable human right [3, 4]. Insufficient availability of 
fresh water coerces people to use ground water for meeting 
their needs. About 70% of Pakistan households use ground 
water for domestic purposes [5 ,6]. Water also becomes a vital 
source of increasing demand for agriculture and industry [7]. 
The quality of ground water in Sindh region is worsening due 
to overuse of fresh water layer. Sindh is an arid region, so 

ground water is recharged only during flooding time along the 
water channel sides [8, 9]. About 78% of Sindh province has 
saline ground water whose salinity varies and at maximum is 
9dS/m [7, 10]. The groundwater is polluted due to various 
natural and anthropogenic factors. The disposal of untreated 
effluents from industries and household sewage, seepage of 
fertilizers and land degradation are the main sources of 
groundwater pollution [11-14]. The quality of ground water of 
Sindh urban and suburban areas is very poor and chemically 
and bacteriologically not fit for drinking purposes [15]. The 
consumption of contaminated water causes various diseases 
[16]. About 98% of the households of Shaheed Benazir Abad 
are using ground water [17]. The aim of this study is to assess 
the ground water quality of four sites of Taluka Daur of 
Shaheed Benazir Abad for drinking purposes. 

II. METHODOLOGY 
Forty groundwater samples were collected from different 

locations of four union councils of Taluka Daur (Daur, Bandhi, 
Jam Sahib and Bucheri) of district Shaheed Benazir Abad. Ten 
water samples have been taken from each union council. 
Sterilized plastic bottles were used for collecting the samples 
which were washed with distilled water twice prior to 
sampling. The samples were collected by using standard 
methods suggested in [18, 19]. The collected water samples 
were brought to Pakistan Council of Research in Water 
Resources (PCRWR) regional laboratory for analyzing 
regarding the following selected physical and chemical 
groundwater parameters (methods of analysis and concerned 
instruments employed for each water quality parameter are 
summarized in Table I). 



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A. Physical Water Parameters under Study 
These parameters of water are turbidity, electrical 

conductivity, pH, taste and color. 

B. Chemical Water Parameters under Study 
These parameters were bicarbonate (HCO3), chlorine (Cl), 

sulfate (SO4), hardness, calcium (Ca), magnesium (Mg), 
sodium (Na), potassium (K), alkalinity (CaCo3), total dissolved 
solids (TDS) and nitrate (NO3). 

C. Biological Water Aspects under Study 
Presence-absence test kit was used to evaluate the water 

samples for microbiological contamination. American Public 
Health Association's guidelines were followed for examining 
the water samples and calibrating the equipment and 
instruments [20]. 

TABLE I.  WATER QUALITY PARAMETERS AND METHODS OF ANALYSIS 

S. No. Water Quality Parameter Method of analysis 

1 TDS 2540C, Standard method (1992) 

2 Conductivity (µS/cm) 
E.C. meter, Syber Scan CON 11 

Singapore 

3 PH Jenco Handheld pH meter, Model 6230N 
4 Color (TCU) Sensory Test 
5 Taste Sensory Test 
6 Bicarbonate (mg/l) 2320, Standard method (1992) 
7 Chloride(mg/l) Titration Standard method (1992) 

8 Sulfate Spectrophotometer Optizen 2120UV plus Korea 

9 Hardness (mg/l) EDTA Titration Standard method (1992) 
10 Calcium (mg/l) 3500-Ca-D, Standard method (1992) 
11 Magnesium (mg/l) 234-C, Standard method (1992) 
12 Sodium (mg/l) Flame photometer Italy 
13 Potassium Flame photometer 
14 Alkalinity 2320, Standard method (1992) 

15 Turbidity Turbidity meter Lovibond PC check kit Germany 
16 Nitrate Colorimeter, Hach- DR2800, USA 
17 B.C Presence /absence test kit 

 
Statistical methods were used to find the minimum, 

maximum, mean and range of all water quality parameters. The 
results were compared and evaluated with the help of WHO 
guidelines for physical and chemical water characteristics. 

III. RESULTS AND DISCUSSION 

A. Color 
Pure water is usually considered as colorless but it actually 

possesses a slightly blue hue. The sources of color in ground 
water are natural and anthropogenic. The particular geological 
formation or some metallic species of the region or seepage of 
effluent impact the groundwater color. WHO set the 15 TCU 
limit for the color of drinking water. All samples were 
aesthetically good and clear. 

B. Taste and Odor 
The taste and odor of 34 samples are non-objectionable. 

Only 6 samples possessed objectionable taste. 

C. TDS 
TDS level is a good indicator of taste. Less than 300mg/l is 

excellent, in the range between 300 and 600mg/l is good, from 
600 to 900mg/l is fair, between 900 and 1200mg/l is poor and 
greater than 1200mg/l is not acceptable [19]. The upper limit of 
TDS of drinking water should be 1000mg/l according to WHO 
standards. Figure 1 shows the results of TDS for all samples. 
Results indicate that the TDS of 23 (57.5%) samples is within 
the permissible limits. The range of TDS of the entire samples 
was 100-3290mg/l and the average value was 1273mg/l. 
Further analysis showed that 3 samples were excellent, 7 were 
good, 5 were fair and 7 were poor in taste while the remaining 
samples were not acceptable.  

 

 
Fig. 1.  Comparison of results of TDS of the entire samples 

D. Electrical Conductivity (EC) 
No guide line value has been given by WHO and USEPA 

for EC. The range of EC of all 40 samples was found as 389-
5140μS/cm and the average value was 2103.7μS/cm. 

E. pH 
pH is a very important water quality parameter which 

describes its acidic or alkaline nature. Drinking water pH 
should range from 6.5 to 8.5 according to WHO standards. 
Results show that the pH of all samples is within permissible 
limits. The range of pH of all samples was 6.7-7.6 and the 
average value was 7.2. The pH values of 8 samples were below 
7 and the values of the remaining samples were greater than 7. 
This shows that the nature of most of the ground water in the 
study area is alkaline. 

F. Bicarbonate 
Bicarbonate is the main anion in ground water. It derives 

from CO2 released as a consequence of organic decay in the 
soil. No guide line value of bicarbonate (HCO3) has been given 
by WHO. The range of HCO3 of all tested 40 samples was 60-
680mg/l and the average value was 295.25mg/l. 



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G. Chlorine (Cl) 
There are the various Cl sources in groundwater. These 

sources are leaching from mineral rock or soil, seepage of 
domestic and industrial effluent, sea water intrusion etc. [21]. 
Ground water shows higher Cl concentration compared to 
surface water. Cl is essential for metabolic activity and other 
physiological processes of human body but excess 
concentration of Cl is also detrimental [5]. The highest 
desirable limit of chloride in drinking water is accredited as 
250mg/l by WHO. Results of Cl concentration for all study 
area samples are shown in Figure 2 

 

 
Fig. 2.  Comparison of results of Cl of all samples 

Figure 2 indicates that the Cl concentration of 32 samples is 
within the limit given by WHO while 20% of the samples are 
exceeding it. Water containing Cl in concentration greater than 
250mg/l has salty taste. The range of Cl of all the samples was 
25-437mg/l and the average value was 172.47mg/l. 

H. Sulfate (SO4) 
Laxative effect is associated with water ingestion 

containing elevated sulfate level [22]. The highest desirable 
limit of sulfate is acknowledged as 250mg/l in drinking water 
by WHO. Figure 3 shows the results of Sulfate (SO4) 
concentration in the study area samples.  

 

 
Fig. 3.  Comparison of results of SO4 of all 40 samples 

Results exhibit that the Sulfate (SO4) concentration of 35 
samples is within the maximum permissible limit specified by 
WHO. The sulfate concentration of 12.5% of the samples is 
above the permissible limit while the sulfate concentration of 
10 samples was lower than the desirable limit of 50mg/l. The 
range SO4 of the samples was 20-302mg/l and the average 
value was 115mg/l. 

I. Magnesium(Mg) 
Mg is one of the important minerals of water and is very 

essential for human health. The content of Mg in water is used 
to determine the quality of water for various purposes [5]. 
WHO has specified 150mg/l of Mg for drinking water. Mg 
concentrations of all samples are within the maximum 
permissible limit. The magnesium content varied from 10 to 
121mg/l and the average value was 50.65mg/l. 

J. Calcium (Ca) 
Calcium is one of the most significant minerals of water 

which is indispensable for bones, teeth and cell physiology. 
Excess calcium consumption is very detrimental for human 
health [5]. WHO has not set any guide line value of Ca for 
drinking water. The range of Ca of all samples was 16-160mg/l 
and the average value was 71.5mg/l.  

K. Hardness 
Water hardness is a very important parameter determining 

its potential use. Various minerals are dissolved in water 
impacting its hardness. Water hardness is often calculated as 
calcium carbonate concentration. It should be 500mg/l in 
drinking water according to WHO. Drinking water has been 
classified on the basis of hardness as follows: Soft :between 0 
and 75mg/l, moderately hard: between 75 and 150mg/l, hard: 
between 150 and 300mg/l and very hard: greater than 300mg/l 
[21]. The results of degree of hardness are shown in Figure 4. 

 

 
Fig. 4.  Comparison of results of hardness of all 40 samples 

Results indicate that the hardness of 27 samples is within 
the permissible limit, while 32.5% of the samples have 
hardness above the permissible WHO limit. The range of 
hardness of all 40 tested samples was 11-900mg/l and the 



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average value was 384.27mg/l. Only one groundwater sample 
was soft according to the above criteria. While 6 samples were 
moderately hard, 14 samples belonged to hard and the 
remaining 19 samples comprised very hard water. The 
analytical result shows that 82.5% of ground water samples of 
the study area fall in the category of hard to very hard water. 
Elevated level of water hardness creates heart and kidney 
problems [23]. 

L. Sodium (Na) 
Sodium is one of the most common water metallic 

elements. Proper quantity of Na is very essential for the human 
body. Elevated Na level imparts its flavor to water and can be 
harmful for human health [24]. Its concentration should be 
200mg/l in drinking water according to WHO. The results of 
Na concentration are shown in Figure 5. 

 

 
Fig. 5.  Comparison of results of Na of all samples 

Results indicate that the sodium concentration of 35 
samples was found within the permissible limit given by WHO 
The remaining 12.5% of the samples possessed higher Na 
concentration. The range of Na concentration of all samples 
was 14-301mg/l and the average value was 115.32 mg/l. 

M. Potassium (K) 
Potassium is an alkali element. It is very essential for all 

living organisms, it is particularly found in cell tissues and 
helps in hydration [25]. WHO has not specified a permissible 
value of K. However European Commission set 12mg/l in 
water for drinking purpose. The results of K of all samples are 
shown in Figure 6. Results indicate that K concentrations of 39 
samples are within the permissible limit given by EC and only 
1 sample is beyond it. The range of K of all samples was 1-
13mg/l and the average value was as 4.61mg/l.  

N. Alkalinity 
Alkalinity is the presence of different components in water 

which make it alkaline. Alkalinity elevated level may create 
various health problems. No guide line value of alkalinity has 
been given by WHO. The range of alkalinity of the samples 

was 1.2-13.6m.mol/1 and the average value was calculated as 
5.96m.mol/1. 

 

 
Fig. 6.  Comparison of results of potassium of all samples 

O. Nitrate (NO3) 
Nitrate is an inorganic and water soluble compound derived 

from nitrogen and essential for plant life. The natural source of 
nitrate in groundwater is the atmosphere through the nitrogen 
cycle. Anthropogenic sources are leaching from industrial 
effluent, agricultural chemicals and sewage [26]. The 
consumption of groundwater having elevated level of nitrate 
may cause diabetes, thyroid disease, gastric cancer and 
methemoglobinemia [27]. WHO set the maximum permissible 
limit of nitrate as 10mg/l in drinking water. The results show 
that nitrate levels of all samples are within this limit. The range 
of nitrate of the samples was 0.25-2.7mg/l and the average 
value was 1.27mg/l.  

P. Microbiological Contamination 
The microbial contamination of groundwater is a severe 

cause of health concern. Dysentery, diarrhea, cholera, typhoid 
and polio are diseases which can be transmitted through 
contaminated water. The main sources of microbial 
contamination of water are human or animal feces and 
agricultural activity [27, 28]. Presence-absence test kit was 
used to evaluate the ground water samples for microbiological 
contamination. The results indicate that 75% of samples were 
free from microbiological contamination while 25% of samples 
showed positive results.  

IV. CONCLUSIONS 
Results of this study revealed that 82.5% of groundwater 

samples of the study area belong to the category of hard to very 
hard water and the most (82.5%) of the samples are alkaline in 
nature. Color, pH, magnesium, alkalinity and nitrate of all the 
samples are found within the permissible limits of WHO. The 
analytical results revealed that the percentage of samples 
beyond permissible limits, regarding the tested parameters were 
taste (15%), TDS (42.5%), Cl (20%), sulfate (12.5%), Na 
(12.5%) and hardness (32.5%). The microbiological 
contamination of 25% of the samples was found positive. 



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Groundwater with parameters beyond permissible limits should 
not be used for drinking purpose. 

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