4.2 Article

Evaluation of environmental status and geochemical assessment of sediments, Manasbal Lake, Kashmir, India

Journal

ARABIAN JOURNAL OF GEOSCIENCES
Volume 10, Issue 4, Pages -

Publisher

SPRINGER HEIDELBERG
DOI: 10.1007/s12517-016-2826-7

Keywords

Manasbal Lake; Environment assessment indices; Lake bottom sediments; Geochemistry; Provenance; Organic matter; C/N ratio

Funding

  1. Anna University, Chennai
  2. UGC, New Delhi

Ask authors/readers for more resources

The present study was conducted on the Manasbal Lake ( 34 degrees 14'N: 74 degrees 40'E) to assess the geochemical characteristics of the lake bottom sediments, its environmental implications and its response in the local catchment area. This study tracks the spatial distribution of grain size, geochemical analysis, C/N ratio, calcium carbonate ( CaCO3) and organic matter ( OM) of the lake bottom sediments. It is observed that the clay fraction ( 49.79%) is predominant in the lake bottom sediments, followed by silt ( 35.88%) and sand ( 14.33%) and its spatial distribution is controlled by water depth. Geochemistry and normalized diagrams for the major oxides and trace elements reveal enrichment of CaO, K2O, P2O5, S, Cl, Ni, Zn and Sr. Chemical index of alteration ( CIA) reflects low to moderate weathering intensity and near compositional similarity with the bedrock exposed in the catchment area around the lake. Environmental indices ( EF, Igeo) suggest that the sediments are enriched in Cu, Ni, Zn, Cr, Co, Pb followed by Mn content. Pollution load index ( PLI) reveal that all the sampling sites reflect low to moderately polluted category except for few stations that are towards the southern and southeastern side of the lake. OM ( 16.85%), CaCO3 ( 14.04%) and C/N ratio ( 15.5) of the lake bottom sediments is attributed to high organic activity within the lake, shell fragments, contributions from the lake flora and fauna adhering to the clayey silty sediments. The C/N ratio of 15.5 suggests a mixed source of organic matter both terrestrially and in situ formation within the lake. Sulphur and chlorine are high amongst the trace elements suggesting anthropogenic detritus input into the lake and this is due to the chemical fertilizers from the agricultural runoff and organic load into the lake. Thus, the present study suggests that in order to preserve the pristine lake ecology and the environment; continued monitoring and restoration efforts need to be undertaken.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.2
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available