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Textural Studies of the Surficial Sediments of Muvattupuzha River and Central Vembanad Estuary, Kerala


Affiliations
1 Marine Geology Division, School of Marine Sciences, Cochin University of Science and Technology, Kochi - 682 016, India
     

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The Muvattupuzha river and the Central Vembanad estuary have been studied mainly for grain size spectrum and textural parameters such as phi mean, standard deviation, skewness and kurtosis. In general, the grain size spectrum shows a marked gradation downstream. The observed variation is in consonance with the energy conditions controlled by the profile of the river as wellas the natural and man-made obstacles encountered in the river channel. In the estuary, the textural pattern is highly complicated owing to the fluctuation in the physico-chemical conditions prevailing in the system. Further, seasonal maintenance dredging activities by the Port authorities also have a considerable bearing on the sediment dispersal pattern of the estuary. The CM model worked out for the fluvial system perfectly agrees with the transportational and depositional regimes of the river and the estuary.

Keywords

Sedimentology, Muvattupuzha River, Vembanad Estuaty, Kerala.
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  • Textural Studies of the Surficial Sediments of Muvattupuzha River and Central Vembanad Estuary, Kerala

Abstract Views: 200  |  PDF Views: 1

Authors

P. Seralathan
Marine Geology Division, School of Marine Sciences, Cochin University of Science and Technology, Kochi - 682 016, India
D. Padmalal
Marine Geology Division, School of Marine Sciences, Cochin University of Science and Technology, Kochi - 682 016, India

Abstract


The Muvattupuzha river and the Central Vembanad estuary have been studied mainly for grain size spectrum and textural parameters such as phi mean, standard deviation, skewness and kurtosis. In general, the grain size spectrum shows a marked gradation downstream. The observed variation is in consonance with the energy conditions controlled by the profile of the river as wellas the natural and man-made obstacles encountered in the river channel. In the estuary, the textural pattern is highly complicated owing to the fluctuation in the physico-chemical conditions prevailing in the system. Further, seasonal maintenance dredging activities by the Port authorities also have a considerable bearing on the sediment dispersal pattern of the estuary. The CM model worked out for the fluvial system perfectly agrees with the transportational and depositional regimes of the river and the estuary.

Keywords


Sedimentology, Muvattupuzha River, Vembanad Estuaty, Kerala.