Heavy metal distribution and environmental status of Doon Valley soils, Outer Himalaya, India

Citation
Kk. Purohit et al., Heavy metal distribution and environmental status of Doon Valley soils, Outer Himalaya, India, ENVIR GEOL, 40(6), 2001, pp. 716-724
Citations number
44
Categorie Soggetti
Environment/Ecology
Journal title
ENVIRONMENTAL GEOLOGY
ISSN journal
09430105 → ACNP
Volume
40
Issue
6
Year of publication
2001
Pages
716 - 724
Database
ISI
SICI code
0943-0105(200103)40:6<716:HMDAES>2.0.ZU;2-6
Abstract
Doon Valley is surrounded by two major river systems (Ganga and Yamuna) on either side, with a water divide passing nearly across the centre of the va lley, and is sandwiched between two mountain ranges in the fragile ecologic al systems of the Himalayan foothills. In total 398 soil samples were colle cted from the valley in a grid pattern (similar to1 sample per 2 km(2)) and investigated for their heavy metal (Cr, Cu, Ni, Pb and Zn) abundances that are environmentally sensitive. Comparison of the heavy metal abundances wi th the contamination threshold values (CTV) revealed that most of these ele mental abundances in Doon Valley soils fall well within the range of the un contaminated to slightly contaminated category. In the case of Cr and Ni, a sizeable number of samples exceeded the CTV (250 and 100 mg kg(-1) respect ively) with an overall background value of 109 and 52 mg kg(-1) respectivel y. Sites of high Cr and Ni mostly occur in the Ganga Catchment (GC) sector that includes even relatively undisturbed forestland. The source of this co ntamination is attributed to geological factors which indicate contribution from the mafic volcanics of the Lesser Himalaya. This is also con sistent with the distribution pattern of Mn and Fe, though their abundance levels a re not alarming. The background concentration of Pb is low (22 mg kg(-1)) i n Doon Valley soils; however, signs of gradual Pb contamination are palpabl e in and around the centre of the Dehra Dun city and along the highways. Al uminium normalized heavy metal ratios were found to exhibit narrow variabil ity in the case of Cu, Ni and Cr and had good correlation with Al, indicati ng their affinity and association with the clay minerals. On the other hand , Pb and Zn seem to be associated with non-silicate sources.