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    Murshidabad District is one of the worst affected areas of arsenic contamination

    in groundwater in the world. The other affected areas are Malda, Nadia, and North and

    South 24 Parganas districts of West Bengal. According to the water test report of Public

    Health Engineering Department in Murshidabad District 28,357 water samples have

    arsenic concentration above 0.05 mg/l in groundwater. 22 out of 26 blocks have arsenic

    concentration 9(Samaddar and Subbarao, 2007). This district is also one of the worst

    affected areas in the world by arsenicosis.

    6Abhijit Mukherjee et. al., 2007 had documented the groundwater flow and a

    regional- scale hydrostratigraphy for a ~ 21,000 km2 area of the arsenic affected

    districts of West Bengal. These districts include Murshidabad District, Nadia, North 24-

    Parganas and South 24- Parganas (including Kolkata). Eight 22- layer model scenarios

    of regional groundwater flow were developed based on the observed topography,

    seasonal conditions and inferred hydrostratigraphy. A comparative picture is drawn

    between the existence of seasonally variable, regional north- south flow across the basin

    prior to the onset of extensive pumping and severe pumping, therefore, distorting the

    flow pattern, inducing high vertical hydraulic gradients across wide cones of depression

    after 1970’s, a landmark period of Green Revolution. Downward flows of irrigational

    return flow and inflow from rivers have resulted in arsenic contamination in shallow

    ground water. Previously safe aquifers appear to have contaminated by a combination

    of mechanical mixing and chemical equilibrium.

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    Stuben 13(2003) had made a study in a small watershed at and around

    Berhampore block in ‘bagri’ region of Murshidabad District. Groundwater from wells

    and the main rivers crossing the area (Bhagirathi and Gobra) have been sampled in the

    north of Murshidabad District covering an area about 200 square kilometers. The

    concentration of major cations including Ca, Mg, K, Na and Fe were measured.

    Fluoride, Cl-, NO3 - and SO4

    -2 concentration were also determined. According to the

    relative molar portion of the dissolved ionic species, all samples are of Ca – HCO3 type.

    River and groundwater samples are similar in their main hydro-geochemical

    compositions, but the total amount of dissolved solids in river water is slightly lower in

    Bhagirathi about 300 mg/l, Gobra about 500 mg/l and ground water is 700 mg/l

    symptomatic of anthropogenic interference into the groundwater through soil due to

    infiltrating, surface run-off. In this chapter the geo-chemical mechanism of arsenic

    contamination in groundwater has been discussed, and emphasis on the effect of

    changing land-use on groundwater since Green Revolution.

    Mobilization of As (arsenic) in groundwater is mainly governed by low

    temperature geochemical processes that involve leaching of naturally occurring ores.

    Accumulation of As (arsenic) in soil and groundwater especially under anoxic

    conditions, due to anthropogenic input or human activity (Bowell et. al., 1994; Azcue

    et. al., 1995; Mariner et. al., 1997; Chakraborty et. al., 1998; Ashley and Lottermoser,

    1999; Madhavan and Subramaniam, 2000; Stuben 2001 in 9Stuben 2003).

    According to Mallick and Rajagopal, 1996; Das, 1996; Mandal 1996;

    Chowdhury et. al.; 1999) arsenic is released to the groundwater from sulfides mostly

    pyrite which were oxidized primarily due to water level drawn down as a consequence

    of intensive irrigation and groundwater exploitation. A group of scientist opines that

    arsenic is released by the oxidation of pyrite or arseno-pyrite following the lowering of

    water ground water level. The other view is that arsenic is released due to desorption

    from or reductive dissolution of ferric oxy-hydroxide in reducing aquifer in

    environment (KMPC, 2006). The widely accepted hypothesis by a group of researchers

    from the Division of Land and Water Resources, Royal Institute of Technology,

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    Sweden is, arsenic is fixed on Fe-oxyhydroxides (FeOOH). Fe-oxyhydroxides

    scavenges and immobilized arsenic in an aerated aquatic system but in the presence of

    organic material and as a released; again due to the microbial mediated reductive

    dissolution of Fe-oxyhydroxides arsenic is released from such Fe- oxyhydroxides under

    reducing condition. The flooding method of irrigation gradually sealed the aquifer from

    diffusion of oxygen.

    A.K. Singh, (2006)11 has explained the organo-arsenic cycles in sediments with

    a flow diagram. He had explained how natural arsenic rises in quantity in groundwater

    due to anthropogenic factor.

    Figure no.: 5.i Organo-arsenic cycles in sediments (after Singh A.K., 2006)

    Concern has been raised by Bangladeshi and international scientist about

    elevated levels of arsenic in Bengali food particularly in rice grain cultivation. The

    highest level of As (arsenic) in the southwest of Bangladesh (district -Nawabganj,

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    Faridpur, Rajbari and Gopalganj) share a common international boundary with

    Murshidabad District of West Bengal therefore the soil and aquifer are quite similar. In

    the rice survey both wet season crop ‘aman’ and dry season crop ‘boro’ were sampled

    and observed. 8Roy Chowdhury, 2002, surveyed Domkal blocks in Murshidabad

    District where the arsenic level is above 0.05 mg/l in many places. According to the

    study many million cubic meter of groundwater is extracted daily by shallow big

    diameter tubewells for agricultural irrigation. The mean concentration of As is 10.7

    mg/kg, Fe is 7860 mg/kg and Mg is 733 mg/kg in higher side of agricultural land soils

    compared to the fallow land soils and lower sides of the agricultural land soils. This

    arsenic indirectly gets included in the daily food chain of the common people. Those

    consume less protein in their daily food habit are worse affected by intestinal problems.

    Table no. 4.xvi shows the case study of arsenic contamination in food items in Domkal

    and Jalangi block of Murshidbad District in a report by The National Institute of Health

    Sciences, Japan, published in journal of Centre for Science and Environment (CSE),


    Table no: 5.i Mean concentration of arsenic in food items in Domkal, Jalangi block.

    Species As concentration micron/gram

    Garlic 0.04

    Coriander 0.049

    Tumeric 0.27 to 0.43

    Source: Roy Chowdhury 2002, pp: 605-618.

    Groundwater occurs under unconfined conditions particularly in the ‘bagri’

    region of Murshidabad District. The ‘rarh region shares partly unconfined and partly

    semi-confined aquifer condition. The unconfined aquifer occurs along the tectonic

    troughs through which the major rivers flow. Arsenic gets contaminated within 20-80

    meters intermediate aquifer within the meander belt of the upper deltaic plain. The

    aquifer in the West Bengal part of the basin probably belong to a) Late Pleistocene to

    Holocene Ganges sediments and b) Early to Middle Pleistocene coastal and moribundh

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    Ganges delta deep aquifers composed of stacked, main- channel, medium to coarse

    sands at depths more than 130 m.

    Mukherjee, et. al. (2007), had tried to explain the flow and mechanism of groundwater

    due to irrigation since the introduction of green revolution. The extensive exploitation

    of groundwater after 1970’s in the up–gradient of mature delta, flushes and dilutes the

    arsenic present at very slow rate. The regional flow occurs within the major system

    from north to south down- gradient during the dry season probably due to the low

    topographic gradient (~0.1 m/km). Very frequent pumping centers in the agricultural

    fields and aquifer architectures dictated the hydraulic gradient of the study area. The

    absence of continuous confining layers, pumping induces between relatively shallower

    and deeper groundwater, which may lead to arsenic enriched water to spread downward.

    The arsenic contaminated water when spread over the land surface partially gets

    accumulated in crops and partially re-circulate in to the sub surface via enhanced

    recharge. This mechanism of repeated extraction and recharging may worsen the

    scenario of Murshidabad District in future.

    Mukherjee (2006), has opined that the smaller rivers in the study area were

    found to be mostly gaining from groundwater discharge. Presumably the groundwater

    discharge to rivers has decreased because of pumping by deep tubewells and shallow

    tubewells. As a consequence, the outflow from the shallow aquifers may have impacted

    the chemistry of smaller rivers. River Bhairab, Dwarka, Pagla, Mayurakhi and many

    other rivers may have the same story.

    Mineralogical investigations


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