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IOSR Journal of Environmental Science, Toxicology and Food Technology (IOSR-JESTFT)
e-ISSN: 2319-2402,p- ISSN: 2319-2399.Volume 9, Issue 1 Ver. I (Jan. 2015), PP 05-08
www.iosrjournals.org
DOI: 10.9790/2402-09110508 www.iosrjournals.org 5 | Page
Arsenic in Tube Well Water in Six Blocks of Supaul
District, Bihar
A.Nath1
*, Shailendra Kumar2
, Priyanka1
, Preety Sinha2
, Aseem Kumar Anshu1
,
And Manisha Singh1
1
Research Centre, Mahavir Cancer Institute and Research Centre, Patna.
2
Department of Zoology, A. N. College, Patna.
Abstract: An experimental estimation of arsenic in a large number of samples by Field Test Kits and by
Hydride Generation Atomic Absorption Spectrophotometer (HGAAS) was done. Water samples were collected
from the following blocks of Supaul district, viz., Raghopur, Basantpur, Supaul, Nirmali, Saraigarh-Bhaptiyahi
and Triveniganj. The aim of this study was to analyze the total arsenic concentration in tube well water of these
regions at different locations. Twenty water samples were randomly selected from each block (n=120) for the
determination of Arsenic concentration, using Field Test Kits. Few samples (n=11) found with higher
concentration of arsenic, were also estimated and confirmed by HGAAS method for comparative observation.
The maximum concentration of arsenic was found to be 0.10 mg/l by using Field Test Kits method and the
average concentration of arsenic of the selected samples was 0.02 mg/l, whereas around 20% of these tube
wells had arsenic concentration above 0.05 mg/l. It was observed that the results obtained by usingField Test
Kits showed less measurement as compared to those obtained by HGAAS method for the same samples, when
the arsenic concentration measured ≤0.10 mg/l. Arsenic concentration was significantly (p<0.0001) higher in
HGASS results than the value obtained by Field Test Kit method.
Keywords: Arsenic, Tube well water, Field Test Kit, HGAAS
I. Introduction
Environmental pollution has become one of the most serious concerns these days. Arsenic (As) is
among the top 20 most toxic known substances, which have become serious concerns for the human health.
Arsenic is described as a metalloid and a ubiquitous element in the environment. Toxicity of arsenic depends on
the form in which it is present. Inorganic arsenic, typical in drinking water, is much more toxic than organic
arsenic. The toxicity of arsenic is determined by its oxidation state, thus the toxicity of different As species
changes depending on the biotic and abiotic conditions in water [1]. Incidences of arsenic in groundwater have
been reported in many countries of the world [2,3,4,5,&6]. In 1984, ground water arsenic contamination was
identified in lower Gangetic plains of West Bengal [7]. Arsenic contamination in the middle Gangetic plain of
Bihar was first reported in June 2002 [8&9]. It was reported that the Ganga-Meghan-Brahmaputra (GMB) plain,
which had an area of approximately 500,000 km2
and the population over 500 million, was at risk from ground
water arsenic contamination. According to Public Health Engineering Department, Government of Bihar and
UNICEF - Bihar, arsenic contamination of ground water was found in several districts of Bihar, viz. Patna,
Saran, Vaishali, Katihar, Purnea, Araria, Supaul, Kishanganj, Madhubani, Sitamarhi, East and West Champaran,
Khagaria, Begusarai and Bhagalpur. Extensive exposure to high level of arsenic in drinking water may cause
serious health hazard [10, 11, 12, 13 & 14]. Hydride Generation Atomic Absorption Spectrophotometer
(HGAAS) is widely used technique for trace metal analysis. With the help of this HGAAS technique, metal
toxicity in water, soil and other biological samples can be examined easily. The aim of the present work was to
make comparative study of existing methods for detection of arsenic in water samples of the selected region by
Field Test Kits and by Hydride Generation Atomic Absorption Spectrophotometer (HGAAS).
II. Materials And Methods
Sample containers were cleaned scrupulously with 1% HCl.
2.1 Materials and reagents of Test Kit:
Field Test Kit (Merck, Germany) contained two test bottles, One red spoon, One green Spoon, reagent
1st
(As-1), Reagent 2nd
(As-2), Reagent 3rd
(As-3) and arsenic test strips.
2.2 Method for detection of arsenic using test kit:
60 ml water sample was taken in the test bottle. Thereafter two drops of As-1 reagent was mixed with
the sample water collected in the testing bottle. After that, one red spoon As-2 reagent was added and vigorously
swirled. Then one green spoon As-3 reagent was mixed with the sample. Thereafter, one As-test strip was
Arsenic in tube well water in six blocks of supaul district, bihar
DOI: 10.9790/2402-09110508 www.iosrjournals.org 6 | Page
inserted into the test bottle to develop the color. Thereafter it was kept at room temperature for 20 minutes. After
20 minutes the strip was matched with arsenic color chart.
2.3 Reagents of AAS:
3% (w/v) NaBH4 in 1% (w/v) NaOH, 3% (w/v) KI in 5% ascorbic acid, Conc. HCl, Conc. HNO3 and
Distilled water
2.4 Digestion of water samples:
100 ml water sample was taken in a Griffin beaker and 5 ml HNO3 was added into it. Then the sample
was covered with watch glass and it was placed on a hot plate at 90 0
C for evaporation to allow volume to
reduce to up to 5ml. After that, the sample was cooled at room temperature and volume made up to 50 ml with
2% HNO3. Finally, that solution was filtered by using filter paper.
2.5 Preparation of water sample for AAS:
10 ml digested sample was taken in a 50 ml volumetric flasks and 5 ml conc. HNO3 was added, after
that 5 ml prepared KI with ascorbic acid solution was added. Thereafter the solution was kept for 45 minutes at
room temperature. After 45 minutes the volume of solution was made up to 50 ml by adding DI water.
2.6 Instrument Used:
In this study model number PinAAde900T Atomic Absorption Spectrophotometer (AAS) with Hydride
Generation was used.
III. Results And Discussion
Arsenic concentration range in water (mg/l) of different blocks of Supaul district was found as
following: Raghopur block from 0.02-0.10, Basantpur block from 0.01 - 0.10, Supaul block from 0.01-0.10,
Nirmali block from 0.005-0.05, Saraigadh-Bhaptiyahi block from 0.005-0.05 and of Triveniganj block from
0.005-0.025 mg/l (Table 1).
Table-1. Mean, SD and SEM Values of Arsenic Concentration
Name of Blocks Range(mg/l) Arsenic Level(mg/l)
Mean SD SEM
Raghopur 0.02-0.10 0.04275 0.03397 0.00760
Basantpur 0.01-0.10 0.04575 0.03661 0.00819
Supaul 0.01-0.10 0.03275 0.03374 0.00754
Nirmali 0.005-0.05 0.01950 0.01799 0.00402
Saraigadh-Bhaptiyahi 0.005-0.05 0.01925 0.01823 0.00408
Triveniganj 0.005-0.025 0.00975 0.00881 0.00197
Seventeen out of twenty water samples from Raghopur, sixteen out of twenty water samples from
Basantpur, fifteen out of twenty water samples from Supaul, fourteen out of twenty water samples from Nirmali,
thirteen out of twenty water samples from Saraigadh-Bhaptiyahi and eleven out of twenty water samples from
Triveniganj blocks crossed the permissible limit of arsenic in drinking water (0.01mg/l = 10 ppb) as prescribed
by WHO (1999) [21], which are shown in Table - 2.
Table-2. Summary of Arsenic concentration in the six blocks of Supaul district
Name of Blocks No. of Samples ≤0.01mg/l >0.01-0.2 mg/l 0.025-0.1 mg/l
Numbers % Numbers % Numbers %
Raghopur 20 03 15 04 20 13 65
Basantpur 20 03 15 05 25 11 55
Supaul 20 05 25 06 30 09 45
Nirmali 20 06 30 6 30 08 40
Saraigadh-
Bhaptiyahi
20 07 35 06 30 07 35
Triveniganj 20 09 45 08 40 03 15
There may be various explanations for such arsenic concentration in ground water in blocks of Supaul
district. The four geochemical mechanisms of natural arsenic pollution are reductive dissolution; alkali
desorption; sulphide oxidation and geothermal activity [15]. Nickson et al., (2000) [16] have suggested anoxic
reduction of arseniferous iron-oxyhydroxides as the promising source of arsenic in ground water. According to
another theory [17,5 & 18], on the basis of sediment analysis high volume pulling out of ground water favours
the oxidation of arsenic rich iron sulphide and mobilization of arsenic to the aquifer. River Koshi originates
from the Himalayas and crosses Tibet reaching plains at Chatra in Nepal and in India on the border of
Arsenic in tube well water in six blocks of supaul district, bihar
DOI: 10.9790/2402-09110508 www.iosrjournals.org 7 | Page
Madhubani and Darbhanga. It flows through Supaul, Saharsa and Madhepura and joins the river Ganga near
Kursela. Supaul was one of the districts that were affected by Koshi flood in 2008. McArthur et al. (2004) and
Ravenscroft et al. (2005) [19&20] have reported that arsenic contained in relatively unweathered alluvial
sediments are imitative of igneous and metamorphic rocks in the Himalayas and associated young mountain
chains. The variation of arsenic concentration in ground water of six blocks under Supaul district is to be related
to regional and local variations of the amount of organic matter in aquifer sediments. Weathering of rocks from
Himalayas in Koshi River and the widespread use of rodenticides and pesticides might be other aspects
accountable for arsenic contamination in ground water of the study area.
Eleven samples out of one hundred twenty samples having the highest concentration were further
observed by Hydride Generation Atomic Absorption Spectrophotometer (HGAAS) for the comparison of
results, which are shown in Table-3, Table-4 and Fig.-1
Table-3. Water sample of tube wells detected with high concentration of Arsenic
Sample ID Owner of the Tube well Locality of Block Depth of Tube well (ft.)
R03 Sajjan Pandit Raghopur 20
R10 LalBahadur Mehta Raghopur 35
R17 Jaynarayan Mandal Raghopur 25
R20 Lalit Sada Raghopur 25
B06 Nagendra Mishra Basantpur 15
B09 Santosh Singh Basantpur 15
B18 Dularchandra Sada Basantpur 20
B19 India-Nepal Border Basantpur 25
S07 Amal Sada Supaul 45
S15 Ganesh Mandal Supaul 35
S20 Anirudh Chopal Supaul 35
The highly concentrated water samples from eleven different tube wells (Table-3) were collected in
separate sample container (glass) of 250 ml capacity for further observation under Hydride Generation Atomic
Absorption Spectrophotometer (HGAAS) at Mahavir Cancer Institute & Research Center, Patna in the DST
Lab. When the samples were analyzed for arsenic content by HGAAS, it was found that there were differences
in values as compared to the Field Test Kit method values. Differences in the values have been shown in Fig.-1
and Table-4.
Table-4. Mean, Std. Deviation (SD) & Std. Error of Mean (SEM) of Fig. 1
IV. Conclusion
Nowadays, Arsenic content in water is measured by either of the two methods: Laboratory based
instrumental method like AAS or by Field Test Kit method at the site. In this work, a comparative study of Field
Test Kit method with HGAAS has been done. It was observed that the results obtained by using Field Test Kit
Sample ID Mean SD SEM
R03 0.1050 0.0071 0.0050
R10 0.1085 0.0120 0.0085
R17 0.1045 0.0063 0.0045
R20 0.1075 0.0106 0.0075
B06 0.1030 0.0042 0.0030
B09 0.1105 0.0148 0.0105
B18 0.1045 0.0063 0.0045
B19 0.1060 0.0084 0.0060
S07 0.1115 0.0162 0.0115
S15 0.1120 0.1696 0.1200
S20 0.1080 0.0113 0.0080
Arsenic in tube well water in six blocks of supaul district, bihar
DOI: 10.9790/2402-09110508 www.iosrjournals.org 8 | Page
showed less measurement as compared to that by AAS method (p<0.0001). The water samples having arsenic
concentration ≤0.10 mg/l were further analysed by AAS. 86 samples out of 120 samples collected from the
different blocks of Supaul district were found to have arsenic concentration more than the permissible limit of
0.01mg/l as recommended by WHO (1999).
Acknowledgement
The authors are very thankful to the Department of Science & Technology (DST), Government of
India, for financial support (No.SSTP/LSR/Bihar/12/12th Plan, dated 04/02/2013) and Mahavir Cancer Institute
and Research Centre for their cooperation. We also extend our thanks to Mr. Naresh Kumar assistant professor
NIT, Patna for statistical calculations.
References
[1]. Yan-Chu, H. (1994) Arsenic in Environment. Part I: Cycling and Characterization. Johnwiley & sons Inc., 26:17-49.
[2]. Robertson, F.N. 1986. Occurrence and solubility control to trace elements in groundwater in alluvial basins of Arizona. In: Regional
aquifer system of United States, Southwest alluvial basin of Arizona. American Water Resource association Monograph, Series. 7, 69-
80.
[3]. Robertson, F.N. (1989). Arsenic in groundwater under oxidation conditions, Southwest United States. Environmental Geochemistry
and Health.11, 171-185.
[4]. Wang, L. and Huang, J. (1994). In: Arsenic in the Environment, Plant II: Human health and ecosystem effects (eds. Nriagu, J.O.),
Wiely, NewYork, 159-172.
[5]. Das, D., Samanta, G., Mandal, B.K., Chowdhury, R.T., Chandra, C.R. and Chowdhury, P.P. (1996). Arsenic in ground water in six
district of West Bengal, India. Environ. Geochem. Health 18, 5-15.
[6]. Chatterjee, A., Das, D., Mandal, B.K., Chowdhury, T.R., Samanta, G. and Chakraborty, D. (1995). Arsenic in ground water in six
districts of West Bengal, India: the biggest arsenic calamity in the world. Part I. Arsenic species in drinking water and urine of the
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[7]. Garai, R., Chakraborti, A.K, Dey, S.B. and Saha, K.C. (1984).Chronic arsenic poisoning from tube-well water. J. Indian Med.
Assoc.82, 34-35.
[8]. Chakraborti, D., et al. (2003). Arsenic groundwater contamination in middle Ganga Plains, Bihar, India: a future danger. Environ.
Health Perspect.111, 1194-1201.
[9]. Chakraborti, D., et al. (2004). Groundwater arsenic contamination and its health effects in the Ganga-Meghna-Brahmaputra Plain. J
Environ. Monit. 6,74N-83N.
[10]. WHO. (1981). International Programme on Chemical Safety (IPCS).Environmental Health Criteria-18, Arsenic, World Health
Organization, Geneva.
[11]. Mandal, B.K, et al. (1996). Arsenic in ground water in seven district of West Bengal, India: the biggest arsenic calamity in the world.
Curr. Sci. 70(11), 976-986.
[12]. Chakraborti, D. et al. (1998). Calcutta’s industrial pollution: groundwater arsenic contamination in a residential area and sufferings of
people due to industrial effluent discharge –An-eight-year study report. Curr.Sci.74 (4), 346-355.
[13]. 13.Morales, K.H., Ryan, L., Kuo, T.L.,Wu, M.M. and Chen, C.J. (2000). Risk of internal cancers from arsenic in drinking water.
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[14]. Chen Yu., et al. (2013). Arsenic exposure from Drinking water and QT-Interval Prolongation: Results from the Health Effects of
Arsenic Longitudinal Study.Environ. Health Perspect. 121(4), 427-432.
[15]. Ravenscroft, P., Brammer, H. and Richards, K.S. (2009). Arsenic pollution: a global synthesis. Wiley-Blackwell, U.K.
[16]. Nickson, R.T., McArthur, J.M., Ravenscroft, P., Burgess, W.G and Ahmed, K.M. (2000). Mechanism of arsenic release to
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[17]. Chowdhury, T.R., Basu, G. K., Mandal, B.K., Biswas, B.K., Samanta, G. and Chowdhury, U.K. (1999). Arsenic poisoning in the
Ganga Delta. Nature.401, 545-546
[18]. Chakraborti, D., Basu, G. K., Biswas, B. K., Chowdhury, U. K, Rahman, M. M. and Paul K. (2001). Charecterisation of arsenic
bearing sediments in Gangatic Delta of west Bengal, India. In: Arsenic Exposure and Health effects. Eds (Chappell W.R., Abernathy
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[19]. McArthur, J.M., et al. (2004). Natural organic matter in sedimentary basin and its relation to arsenic in anoxic ground water: the
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Arsenic in Tube Well Water in Six Blocks of Supaul District, Bihar

  • 1. IOSR Journal of Environmental Science, Toxicology and Food Technology (IOSR-JESTFT) e-ISSN: 2319-2402,p- ISSN: 2319-2399.Volume 9, Issue 1 Ver. I (Jan. 2015), PP 05-08 www.iosrjournals.org DOI: 10.9790/2402-09110508 www.iosrjournals.org 5 | Page Arsenic in Tube Well Water in Six Blocks of Supaul District, Bihar A.Nath1 *, Shailendra Kumar2 , Priyanka1 , Preety Sinha2 , Aseem Kumar Anshu1 , And Manisha Singh1 1 Research Centre, Mahavir Cancer Institute and Research Centre, Patna. 2 Department of Zoology, A. N. College, Patna. Abstract: An experimental estimation of arsenic in a large number of samples by Field Test Kits and by Hydride Generation Atomic Absorption Spectrophotometer (HGAAS) was done. Water samples were collected from the following blocks of Supaul district, viz., Raghopur, Basantpur, Supaul, Nirmali, Saraigarh-Bhaptiyahi and Triveniganj. The aim of this study was to analyze the total arsenic concentration in tube well water of these regions at different locations. Twenty water samples were randomly selected from each block (n=120) for the determination of Arsenic concentration, using Field Test Kits. Few samples (n=11) found with higher concentration of arsenic, were also estimated and confirmed by HGAAS method for comparative observation. The maximum concentration of arsenic was found to be 0.10 mg/l by using Field Test Kits method and the average concentration of arsenic of the selected samples was 0.02 mg/l, whereas around 20% of these tube wells had arsenic concentration above 0.05 mg/l. It was observed that the results obtained by usingField Test Kits showed less measurement as compared to those obtained by HGAAS method for the same samples, when the arsenic concentration measured ≤0.10 mg/l. Arsenic concentration was significantly (p<0.0001) higher in HGASS results than the value obtained by Field Test Kit method. Keywords: Arsenic, Tube well water, Field Test Kit, HGAAS I. Introduction Environmental pollution has become one of the most serious concerns these days. Arsenic (As) is among the top 20 most toxic known substances, which have become serious concerns for the human health. Arsenic is described as a metalloid and a ubiquitous element in the environment. Toxicity of arsenic depends on the form in which it is present. Inorganic arsenic, typical in drinking water, is much more toxic than organic arsenic. The toxicity of arsenic is determined by its oxidation state, thus the toxicity of different As species changes depending on the biotic and abiotic conditions in water [1]. Incidences of arsenic in groundwater have been reported in many countries of the world [2,3,4,5,&6]. In 1984, ground water arsenic contamination was identified in lower Gangetic plains of West Bengal [7]. Arsenic contamination in the middle Gangetic plain of Bihar was first reported in June 2002 [8&9]. It was reported that the Ganga-Meghan-Brahmaputra (GMB) plain, which had an area of approximately 500,000 km2 and the population over 500 million, was at risk from ground water arsenic contamination. According to Public Health Engineering Department, Government of Bihar and UNICEF - Bihar, arsenic contamination of ground water was found in several districts of Bihar, viz. Patna, Saran, Vaishali, Katihar, Purnea, Araria, Supaul, Kishanganj, Madhubani, Sitamarhi, East and West Champaran, Khagaria, Begusarai and Bhagalpur. Extensive exposure to high level of arsenic in drinking water may cause serious health hazard [10, 11, 12, 13 & 14]. Hydride Generation Atomic Absorption Spectrophotometer (HGAAS) is widely used technique for trace metal analysis. With the help of this HGAAS technique, metal toxicity in water, soil and other biological samples can be examined easily. The aim of the present work was to make comparative study of existing methods for detection of arsenic in water samples of the selected region by Field Test Kits and by Hydride Generation Atomic Absorption Spectrophotometer (HGAAS). II. Materials And Methods Sample containers were cleaned scrupulously with 1% HCl. 2.1 Materials and reagents of Test Kit: Field Test Kit (Merck, Germany) contained two test bottles, One red spoon, One green Spoon, reagent 1st (As-1), Reagent 2nd (As-2), Reagent 3rd (As-3) and arsenic test strips. 2.2 Method for detection of arsenic using test kit: 60 ml water sample was taken in the test bottle. Thereafter two drops of As-1 reagent was mixed with the sample water collected in the testing bottle. After that, one red spoon As-2 reagent was added and vigorously swirled. Then one green spoon As-3 reagent was mixed with the sample. Thereafter, one As-test strip was
  • 2. Arsenic in tube well water in six blocks of supaul district, bihar DOI: 10.9790/2402-09110508 www.iosrjournals.org 6 | Page inserted into the test bottle to develop the color. Thereafter it was kept at room temperature for 20 minutes. After 20 minutes the strip was matched with arsenic color chart. 2.3 Reagents of AAS: 3% (w/v) NaBH4 in 1% (w/v) NaOH, 3% (w/v) KI in 5% ascorbic acid, Conc. HCl, Conc. HNO3 and Distilled water 2.4 Digestion of water samples: 100 ml water sample was taken in a Griffin beaker and 5 ml HNO3 was added into it. Then the sample was covered with watch glass and it was placed on a hot plate at 90 0 C for evaporation to allow volume to reduce to up to 5ml. After that, the sample was cooled at room temperature and volume made up to 50 ml with 2% HNO3. Finally, that solution was filtered by using filter paper. 2.5 Preparation of water sample for AAS: 10 ml digested sample was taken in a 50 ml volumetric flasks and 5 ml conc. HNO3 was added, after that 5 ml prepared KI with ascorbic acid solution was added. Thereafter the solution was kept for 45 minutes at room temperature. After 45 minutes the volume of solution was made up to 50 ml by adding DI water. 2.6 Instrument Used: In this study model number PinAAde900T Atomic Absorption Spectrophotometer (AAS) with Hydride Generation was used. III. Results And Discussion Arsenic concentration range in water (mg/l) of different blocks of Supaul district was found as following: Raghopur block from 0.02-0.10, Basantpur block from 0.01 - 0.10, Supaul block from 0.01-0.10, Nirmali block from 0.005-0.05, Saraigadh-Bhaptiyahi block from 0.005-0.05 and of Triveniganj block from 0.005-0.025 mg/l (Table 1). Table-1. Mean, SD and SEM Values of Arsenic Concentration Name of Blocks Range(mg/l) Arsenic Level(mg/l) Mean SD SEM Raghopur 0.02-0.10 0.04275 0.03397 0.00760 Basantpur 0.01-0.10 0.04575 0.03661 0.00819 Supaul 0.01-0.10 0.03275 0.03374 0.00754 Nirmali 0.005-0.05 0.01950 0.01799 0.00402 Saraigadh-Bhaptiyahi 0.005-0.05 0.01925 0.01823 0.00408 Triveniganj 0.005-0.025 0.00975 0.00881 0.00197 Seventeen out of twenty water samples from Raghopur, sixteen out of twenty water samples from Basantpur, fifteen out of twenty water samples from Supaul, fourteen out of twenty water samples from Nirmali, thirteen out of twenty water samples from Saraigadh-Bhaptiyahi and eleven out of twenty water samples from Triveniganj blocks crossed the permissible limit of arsenic in drinking water (0.01mg/l = 10 ppb) as prescribed by WHO (1999) [21], which are shown in Table - 2. Table-2. Summary of Arsenic concentration in the six blocks of Supaul district Name of Blocks No. of Samples ≤0.01mg/l >0.01-0.2 mg/l 0.025-0.1 mg/l Numbers % Numbers % Numbers % Raghopur 20 03 15 04 20 13 65 Basantpur 20 03 15 05 25 11 55 Supaul 20 05 25 06 30 09 45 Nirmali 20 06 30 6 30 08 40 Saraigadh- Bhaptiyahi 20 07 35 06 30 07 35 Triveniganj 20 09 45 08 40 03 15 There may be various explanations for such arsenic concentration in ground water in blocks of Supaul district. The four geochemical mechanisms of natural arsenic pollution are reductive dissolution; alkali desorption; sulphide oxidation and geothermal activity [15]. Nickson et al., (2000) [16] have suggested anoxic reduction of arseniferous iron-oxyhydroxides as the promising source of arsenic in ground water. According to another theory [17,5 & 18], on the basis of sediment analysis high volume pulling out of ground water favours the oxidation of arsenic rich iron sulphide and mobilization of arsenic to the aquifer. River Koshi originates from the Himalayas and crosses Tibet reaching plains at Chatra in Nepal and in India on the border of
  • 3. Arsenic in tube well water in six blocks of supaul district, bihar DOI: 10.9790/2402-09110508 www.iosrjournals.org 7 | Page Madhubani and Darbhanga. It flows through Supaul, Saharsa and Madhepura and joins the river Ganga near Kursela. Supaul was one of the districts that were affected by Koshi flood in 2008. McArthur et al. (2004) and Ravenscroft et al. (2005) [19&20] have reported that arsenic contained in relatively unweathered alluvial sediments are imitative of igneous and metamorphic rocks in the Himalayas and associated young mountain chains. The variation of arsenic concentration in ground water of six blocks under Supaul district is to be related to regional and local variations of the amount of organic matter in aquifer sediments. Weathering of rocks from Himalayas in Koshi River and the widespread use of rodenticides and pesticides might be other aspects accountable for arsenic contamination in ground water of the study area. Eleven samples out of one hundred twenty samples having the highest concentration were further observed by Hydride Generation Atomic Absorption Spectrophotometer (HGAAS) for the comparison of results, which are shown in Table-3, Table-4 and Fig.-1 Table-3. Water sample of tube wells detected with high concentration of Arsenic Sample ID Owner of the Tube well Locality of Block Depth of Tube well (ft.) R03 Sajjan Pandit Raghopur 20 R10 LalBahadur Mehta Raghopur 35 R17 Jaynarayan Mandal Raghopur 25 R20 Lalit Sada Raghopur 25 B06 Nagendra Mishra Basantpur 15 B09 Santosh Singh Basantpur 15 B18 Dularchandra Sada Basantpur 20 B19 India-Nepal Border Basantpur 25 S07 Amal Sada Supaul 45 S15 Ganesh Mandal Supaul 35 S20 Anirudh Chopal Supaul 35 The highly concentrated water samples from eleven different tube wells (Table-3) were collected in separate sample container (glass) of 250 ml capacity for further observation under Hydride Generation Atomic Absorption Spectrophotometer (HGAAS) at Mahavir Cancer Institute & Research Center, Patna in the DST Lab. When the samples were analyzed for arsenic content by HGAAS, it was found that there were differences in values as compared to the Field Test Kit method values. Differences in the values have been shown in Fig.-1 and Table-4. Table-4. Mean, Std. Deviation (SD) & Std. Error of Mean (SEM) of Fig. 1 IV. Conclusion Nowadays, Arsenic content in water is measured by either of the two methods: Laboratory based instrumental method like AAS or by Field Test Kit method at the site. In this work, a comparative study of Field Test Kit method with HGAAS has been done. It was observed that the results obtained by using Field Test Kit Sample ID Mean SD SEM R03 0.1050 0.0071 0.0050 R10 0.1085 0.0120 0.0085 R17 0.1045 0.0063 0.0045 R20 0.1075 0.0106 0.0075 B06 0.1030 0.0042 0.0030 B09 0.1105 0.0148 0.0105 B18 0.1045 0.0063 0.0045 B19 0.1060 0.0084 0.0060 S07 0.1115 0.0162 0.0115 S15 0.1120 0.1696 0.1200 S20 0.1080 0.0113 0.0080
  • 4. Arsenic in tube well water in six blocks of supaul district, bihar DOI: 10.9790/2402-09110508 www.iosrjournals.org 8 | Page showed less measurement as compared to that by AAS method (p<0.0001). The water samples having arsenic concentration ≤0.10 mg/l were further analysed by AAS. 86 samples out of 120 samples collected from the different blocks of Supaul district were found to have arsenic concentration more than the permissible limit of 0.01mg/l as recommended by WHO (1999). Acknowledgement The authors are very thankful to the Department of Science & Technology (DST), Government of India, for financial support (No.SSTP/LSR/Bihar/12/12th Plan, dated 04/02/2013) and Mahavir Cancer Institute and Research Centre for their cooperation. We also extend our thanks to Mr. Naresh Kumar assistant professor NIT, Patna for statistical calculations. References [1]. Yan-Chu, H. (1994) Arsenic in Environment. Part I: Cycling and Characterization. Johnwiley & sons Inc., 26:17-49. [2]. 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