Status of anthropogenically induced metal pollution in the Kanpur-Unnao industrial region of the Ganga Plain, India

Citation
Aa. Ansari et al., Status of anthropogenically induced metal pollution in the Kanpur-Unnao industrial region of the Ganga Plain, India, ENVIR GEOL, 38(1), 1999, pp. 25-33
Citations number
28
Categorie Soggetti
Environment/Ecology
Journal title
ENVIRONMENTAL GEOLOGY
ISSN journal
09430105 → ACNP
Volume
38
Issue
1
Year of publication
1999
Pages
25 - 33
Database
ISI
SICI code
0943-0105(199906)38:1<25:SOAIMP>2.0.ZU;2-Z
Abstract
The Ganga Plain is one of the most densely populated regions and one of the largest groundwater repositories of the Earth. For several decades, the dr ainage basin of the Ganga Plain has been used for the disposal of domestic and industrial wastes which has adversely affected the quality of water, se diments and agricultural sails of the plain. The concentrations of Al, Cd, Co, Cr, Cu, Fe, Mn, Ni, Pb, Sn, Zn and organic carbon were determined in ri ver sediments and soils of the Ganga Plain in the Kanpur-Unnao industrial r egion in 1994 and 1995 (pre-monsoon period of April-May). High contents (ma ximum values) of C-org (12.0 wt.%), Cr (3.40 wt. %), Sn (1.92 wt. %), Zn (4 000 mg/kg), Pb (646 mg/kg), Cu (408 mg/kg), Ni (502 mg/kg) and Cd (9.8 mg/k g) in sediments (<20 mu m fraction); and C-org (5.9 wt. %), Cr (2.16 wt. %) , Sn (1.21 wt %), Zn (975 mg/kg) and Ni (482 mg/kg) in soils (<20 mu m) in the pre-monsoon period of 1994 were found. From 1994 to 1995 the contents o f Fe and Sn in sediments increase whereas those of C-org, Cd, Cu, Ni and Zn decrease. Considering the analytical errors, Al, Co, Cr, Mn and Pb do not show any change in their concentrations. In soils, the contents of Cd, Fe a nd Sn increase whereas those of Ni decrease from 1994 to 1995. Aluminium, C o, Cr, Cu, Mn, Pb and Zn do not show any change in their concentrations fro m 1994 to 1995. About 90% of the contents of Cd, Cr and Sn; 50-75% of C-org , Cu and Zn; and 25% of Co, Ni and Pb in sediments are derived from the ant hropogenic input in relation to the natural background values, whereas in s oils this is the case for about 90% of Cr and Sn; about 75% of Cd; and abou t 25% of C-org, Cu, Ni and Zn. The sediments of the study area show enrichm ent factors of 23.6 for Cr, 14.7 for Cd, 12.2 for Sn, 3.6 for C-org, 3.2 fo r Zn, 2.6 for Cu and 1.6 for Ni. The soils are enriched with factors of 10. 7 for Cr, 9.0 for Sn, 3.6 for Cd, 1.8 for Ni and 1.5 for Cu and Zn, respect ively.