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It was reported a clear temporal and seasonal variability of As concentrations in different water samples of Ballia district of eastern U. P. During post monsoon season As concentration decreases in Samples. A definite relationship exists between the behavior of arsenic and rainfall intensity. With increasing rainfall intensity rate of dilution increases which minimizes the arsenic concentration in the groundwater. During monsoon period there is considerable decrease in the arsenic concentration. Groundwater stream design is influenced by water level surface and subsurface redox potential because of seasonal rainfall. During monsoon seasons groundwater level is increased due to its low-land shallow basin and flooding condition also help in rising its groundwater level. For an extensive stretch of the year, the land remains water-logged and this prompts low groundwater flushing rates. In this manner, the watched varieties in mean As concentrations during storm season contrasted with pre rainstorm season. During monsoon time arsenic goes into groundwater by disintegration of Fe(III)- oxy hydroxides and in pre monsoon time arsenic reversibly adsorb on Fe(III)- oxyhydroxides. So these two processes control arsenic concentration during pre monsoon and post monsoon time.

Temporal and seasonal variability, pre and post monsoon, groundwater stream, rainfall intensity, oxy hydroxides, seasonal rainfall.

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AZAM, A. (2020). TEMPORAL AND SEASONAL VARIATION OF ARSENIC IN BALLIA DISTRICT OF EASTERN U. P. Asian Journal of Advances in Research, 2(1), 22-29. Retrieved from https://mbimph.com/index.php/AJOAIR/article/view/1475
Original Research Article


Singh Rajesh, Dadhibal Prasad Gond, Amit Pal. Assessment of ground water quality of Ghazipur District, Eastern Uttar Pradesh, India, special reference to arsenic contamination. Recent Research in Science and Technology. 2010;2(3).

Pathak Vinay Kumar, et al. Hydrochemistry of groundwater with special reference to arsenic in Lakhimpur Khiri District, Uttar Pradesh, India. IOSR J. Appl Chem. 2013;6:61-68.

Acharya SK. Arsenic levels in groundwater from quaternary alluvium in the Ganga Plain and the Bengal Basin, Indian subcontinent: Insights into influence of stratigraphy. Gondwana Res. 2005;8:55–66.

Owa FW. Water pollution: Sources, effects, control and management. International Letters of Natural Sciences. 2014;3.

Shankar Shiv, Uma Shanker. Arsenic contamination of groundwater: A review of sources, prevalence, health risks and strategies for mitigation. The Scientific World Journal; 2014.

Namrata Pandey, et al. Arsenic pollution scenario in Eastern UP, India: A review. International Research Journal of Environment Sciences. 2015;4(11):83-86.

Singh Ashalata, Vipin Kumar Singh. Arsenic contamination in ground water of Ballia, Uttar Pradesh State, India. Journal of Applied Geochemistry. 2015;17(1):78.

Bhattacharya P, Mukherjee A, Mukherjee AB. Arsenic in groundwater of India. 2011;150-164.

Acharya SK, Shah BA. Risk of arsenic contamination in groundwater affecting the Ganga Alluvial Plain, India. Environ. Health Persp. 2004;Corr. 112:A-19–A-20.

Acharya SK, Shah BA. Genesis of arsenic contamination of ground water in alluvial Gangetic aquifer in India. In: Bundschuh J, Bhattacharya P, Chandrasekharam D, (Eds.), Natural Arsenic in Groundwater. Balkema/Taylorand Francis, Leiden/London. 2005;17–23.

Acharya SK, Shah BA. Groundwater arsenic contamination affecting different geologic domains in India – a review: Influence of geological setting, fluvial geomorphology and quaternary stratigraphy. J. Environ. Sci. Health. 2007;A42:1795–1805.

Ahamed S, Sengupta MK, Mukherjee A, Amir Hossain M, Das B, Nayak B, Pal A, Chakraborti D. Arsenic groundwater contamination and its health effects in the state of Uttar Pradesh (UP) in upper and middle Ganga plain, India: A severe danger. Sci. Total Environ. 2006;370:310–322.

Acharya SK, Lahiri S, Raymahashay BC, Bhowmik A. Arsenic toxicity of groundwater in parts of the Bengal basin in India and Bangladesh: The role of quaternary stratigraphy and Holocene sea-level fluctuation. Environ. Geol. 2000;39:1127–1137.

Rotiroti M, Bonomi T, Sacchi E, McArthur JM, Stefania GA, Zanotti C, Fumagalli L. The effects of irrigation on groundwater quality and quantity in a human-modified hydro-system: The Oglio River basin, Po Plain, Northern Italy. Science of the Total Environment. 2019;672:342-356.

Chowdhury TR, Basu GK, Mandal BK, Biswas BK, Samanta G, Chowdhury UK. Arsenic poisoning in the Ganges Delta. Nature. 1999;401:545–546.

Datta DV, Kaul MK. Arsenic content of tube well water I villages in Northern India. A concept of arsenicosis. J. Assoc. Physicians India. 1976;24:599–604.

Dhar RK, Biswas BK, Samanta G, Mandal BK, Chakraborti D, Roy S, Jafar A, Islam A, Ara G, Kabir S, Khan AW, Ahmed SA, Hadi SA. Groundwater arsenic calamity in Bangladesh. Curr. Sci. India. 1997;73:48–59.

Farooq A, Arshad MJ, Shah A. A layered approach for similarity measurement between ontologies. Journal of American Science. 2010;6(12):12.

Dixit S, Hering JG. Comparison of arsenic (V) and arsenic (III) sorption onto iron oxide minerals: Implications for arsenic mobility. Environ. Sci. Technol. 2003;37:4182–4189.

Dowling CB, Poreda RJ, Basu AR, Peters SL, Aggarwal PK. Geochemical study of arsenic release mechanisms in the Bengal Basin groundwater. Water Resour. Res. 2002;38: 1173–1190.