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A Study to Identify Locations Suitable of Deep Sea Port Operations in the State of West Bengal

  • Bal Krishna
  • B. Chaudhuri
  • P. K. Bhaskaran
Conference paper
Part of the Lecture Notes in Civil Engineering book series (LNCE, volume 23)

Abstract

There is a long pending need for a deep-drafted port in West Bengal which will serve complete East and North East region of India. The port operation in Hooghly estuary starts in Kolkata in the eighteenth century. This is the only riverine port in India which started its operation with an approach channel of around 232 km from the sea (Sand Heads). Thereafter, due to problem of siltation and to accommodate the bigger size of vessels, another Satellite Dock System (Haldia Dock Complex, i.e. HDC) started its operation from 1974 with 9.5 m average draft, whereas the draft available at Kolkata Dock System (KDS) at that time was varying between 7.5 and 8.0 m. Due to adverse morphological transformation, over the decade, at present, the natural depth in and in front of Hooghly estuary varies between 5 and 7 m. So, looking for deep-drafted port in and in front of Hooghly estuary is ruled out. It is required to see the site on East side and West side of Hooghly estuary. Unfortunately, on East and West, the extent of coastline is small. On the East side lies the Sundarban Delta mostly formed by alluvial sediment brought by Hooghly estuary. Subsoil is mostly formed of silty clay unsuitable for port construction. It is also observed that while flood flow enters the estuary with equally distributed over width, the ebb flow moves to East after leaving the estuary. Any attempt to develop a port on East side has to tackle with enormous sediment brought by the estuary. Hence, one has to look towards West for deep-drafted port. Coastline in this stretch is limited. On West side, characteristics of the formation of channels like Eden channel and channel West of Eastern brace, which are wide in deep region and gradually narrows down as they move upstream, indicate that they are flood channels. The advantage of flood channels is that here it is not required to tackle the sediment brought by estuary. They are stable and maintained more or less at same location. Another expectation is that during prehistoric era when reaching of sand to coast through river was not intercepted by dams and movement along coast was not intercepted by port structures and approach channel, West side of Hooghly estuary has intercepted the sand. Outfall of estuary works as sand barrier. There is good chance that subsoil in this area is formed of sand. Existence of number of sand heads for centuries is proof of that. Submerged sands on two sides will give protection from cyclones. Coastal formation dictates that deep-drafted port in this region has to be formed as Island port. Considering all these aspects, the deep flood channel West of eastern brace provides excellent site for deep-drafted Island port. An attempt has been made in this paper to logically reinforce the merits in favour of Island port in reference to other available options, within the jurisdiction of West Bengal.

Keywords

Sedimentation Morphological transformation Tidal range Tidal current Neap/spring Cyclonic time Maintenance dredging Navigational channel VTMS 

Notes

Acknowledgements

The authors are indebted to the competent authorities of CWPRS, KoPT and WAPCOS for providing the required information and wish to convey their sincerest thanks for the constant support and encouragement bestowed towards publication of the paper.

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Copyright information

© Springer Nature Singapore Pte Ltd. 2019

Authors and Affiliations

  1. 1.WAPCOS Ltd.PuneIndia
  2. 2.Kolkata Port TrustKolkataIndia
  3. 3.Department of Ocean Engineering & Naval Architecture IITKharagpurIndia

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