2013
DOI: 10.1016/j.pce.2013.04.009
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Is organic matter a source or redox driver or both for arsenic release in groundwater?

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Cited by 50 publications
(22 citation statements)
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“…Similarly, mean concentration of sulphate is twice the permissible limit (250 mg/L) of WHO for drinking water Table 4. Very high sulphate content in the groundwater of study area suggests the gypsum dissolution, use of inorganic fertilizer and the recent recharge of saline water [20,21]. High concentration of sulphate in study area is consistent with the study of Mashiatullah, et al [18] in Ghizri creek which is 5.6 km away from Qayyumabad.…”
Section: Major Anionssupporting
confidence: 88%
“…Similarly, mean concentration of sulphate is twice the permissible limit (250 mg/L) of WHO for drinking water Table 4. Very high sulphate content in the groundwater of study area suggests the gypsum dissolution, use of inorganic fertilizer and the recent recharge of saline water [20,21]. High concentration of sulphate in study area is consistent with the study of Mashiatullah, et al [18] in Ghizri creek which is 5.6 km away from Qayyumabad.…”
Section: Major Anionssupporting
confidence: 88%
“…However, organic/sulfide fraction of As in peat layers was higher than 1.4 mg/kg. This indicates that As content was affected by organic matter content as pointed out by Anawar et al (2013).…”
Section: Arsenic Sequential Extractionmentioning
confidence: 58%
“…Elevated bicarbonate (mean > 285) is reported from all three union councils where it is almost same (mean: 289 mg/L) in the UC-1 and 2 and relatively less in UC-3. Very high content of bicarbonate in the groundwater generally occur either due to carbonate mineral dissolution or organic matter decomposition (Anawar et al, 2013) in flood plain setting. Since the alluvial sediments brought by the Indus River are mainly comprised of silt and clay (non carbonate grains) the source of bicarbonate seems to be organic matter decomposition.…”
Section: Prevalence Of Anoxiamentioning
confidence: 99%
“…Strong positive loading of major ions and TDS explains intense water-sediment interaction. Similarly, significant loading of As and HCO 3 depicts organic matter decomposition due to which arsenic is being released both from organic matter itself and aquifer sediments (Anawar et al, 2013) very strong loading of Cl, SO 4 and Na indicates sewage mixing with groundwater which is triggering the arsenic release process (Cole & Ryan, 2005). The second component (F2) (19%) shows strong positive loadings of As, PO4, NO3, Fe, K coupled with strong negative association of pH, SO4 and F-.…”
Section: Principle Component Analysis (Pca)mentioning
confidence: 99%