2011
DOI: 10.3329/jsr.v4i1.7820
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Seasonal Variations of Arsenic in the Ganges and Brahmaputra River, Bangladesh

Abstract: Dissolved arsenic concentrations in the Ganges, Brahmaputra Rivers and confluence of these two rivers show important seasonal variations and maximum arsenic concentrations are observed during the monsoon season (July–October). These seasonal variations of dissolved arsenic concentrations were closely related to intense river-water discharge during the monsoon season with high arsenic-rich suspended particulate matter (SPM) loads. These arsenic-rich SPM mainly are primarily originated from erosion of agricultur… Show more

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Cited by 10 publications
(6 citation statements)
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“…This is probably due to the presence of many potential ions in shallow aquifer to more extent than those in semi-deep aquifer that accelerated arsenic uptake by plants [36]. This groundwater matrix is in agreement to the general scenario of aquifer conditions of Bangladesh [2,35].…”
Section: Accumulation and Toxicity Of Arsenic In Vegetablessupporting
confidence: 81%
“…This is probably due to the presence of many potential ions in shallow aquifer to more extent than those in semi-deep aquifer that accelerated arsenic uptake by plants [36]. This groundwater matrix is in agreement to the general scenario of aquifer conditions of Bangladesh [2,35].…”
Section: Accumulation and Toxicity Of Arsenic In Vegetablessupporting
confidence: 81%
“…2) and run off from agricultural lands, irrigated with arsenic rich groundwaters. 35 The high summer temperature (maximum 30 C) enhances the biological activity through microbial reduction of As(V) to less particle active As(III) species and contributes to the seasonal variations in arsenic concentrations in river waters. In sea water, arsenic occurs as arsenate (As III) with average As concentrations in open seawater usually showing little variation and typically around 1.5 mg l À1 .…”
Section: Arsenic In Soilsmentioning
confidence: 99%
“…2) and run off from agricultural lands, irrigated with arsenic rich groundwaters. 35 The high summer temperature (maximum 30 C) enhances the biological activity through microbial reduction of As(V) to less particle active As(III) species and contributes to the seasonal variations in arsenic concentrations in river waters.…”
Section: Arsenic In Soilsmentioning
confidence: 99%
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“…The prevalent non-uniformity of As levels may be related to the particular hydrological characteristics of Sundarban wetland which are severely influenced by southeast monsoon and the meso-macrotidal regime . Arsenic may enter the estuary through two potential sources, mainly by (i) anthropogenic sources (such as effluents from multifarious industries located in upper stretch of Hugli estuary as referred earlier as well as from erosion of agricultural land in upstream region irrigated with arsenic-containing shallow waters (Islama et al, 2012) followed by (ii) geogenic processes (transported by Ganges River from weathering of bed rocks in the Himalayan). These values were not particularly high compared to highly contaminated sites cited in the literature and only three of the eleven sites exceeded the ERL of 8 mg kg -1 .…”
Section: Arsenic In Sediment From Sundarbanmentioning
confidence: 99%