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N. Chandramohanakumar

Researcher at Cochin University of Science and Technology

Publications -  52
Citations -  979

N. Chandramohanakumar is an academic researcher from Cochin University of Science and Technology. The author has contributed to research in topics: Organic matter & Mangrove. The author has an hindex of 17, co-authored 46 publications receiving 808 citations.

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Distribution and sources of sedimentary organic matter in a tropical estuary, south west coast of India (Cochin estuary): a baseline study.

TL;DR: It is found that the dynamic cycling of nitrogen through various biogeochemical and organic matter degradation processes modifies the OC/TN ratios and δ¹⁵N to a considerable degree.
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Toxic Metals Enrichment in the Surficial Sediments of a Eutrophic Tropical Estuary (Cochin Backwaters, Southwest Coast of India)

TL;DR: Concentrations and distributions of trace metals in surficial sediments of the Cochin backwaters were studied during both monsoon and pre-monsoon periods and showed that metal contamination was the product of anthropogenic activities.
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Dynamics of polycyclic aromatic hydrocarbons (PAHs) in surface sediments of Cochin estuary, India

TL;DR: Polycyclic aromatic hydrocarbons showed significant seasonal dynamics in surface sediments of a tropical ecosystem (Cochin estuary, south west coast of India), indicating land/river runoff as the major transport pathway.
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Spatial variability and contamination of heavy metals in the inter-tidal systems of a tropical environment

TL;DR: In this article, the degree of anthropogenic influence on heavy metal concentration in the sediments of the mangrove and adjacent estuarine stations using enrichment factor and geoaccumulation index was assessed.
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Formation of anoxia and denitrification in the bottom waters of a tropical estuary, southwest coast of India

TL;DR: In this paper, the authors studied the hydrographic characteristics of the southwest coast of India and its adjoining Cochin backwaters (CBW) during the summer monsoon period and observed anomalous formation of anoxia and denitrification were observed in the bottom layers of CBW, which have not been previously reported elsewhere in any tropical estuarine systems.