Volume 13 Issue 4 May - July 2018
Research Paper
Dhiman Kumar*, Vinod Kumar Tripathi**,
Prabeer Kumar Parhi***
* Senior Research
Fellow, ICAR-Indian Institute of Water Management, Bhuabaneswar, Odisha, India.
** Assistant Professor, Department of Farm Engineering,
Institute of Agricultural Science, IIT-BHU, Varanasi, Uttar Pradesh, India.
*** Assistant Professor, Centre for Water Engineering and
Management, Central University of Jharkhand, Ranchi, Jharkhand, India.
Kumar, D.,
Tripathi, V. K., & Parhi, P. K. (2018). Flood Flow Modelling and Embankment
Protection of Mahanadi River Using HEC-RAS. i-manager’s
Journal on Future Engineering and Technology, 13(4), 1-13. https://doi.org/10.26634/jfet.13.4.14470
Abstract
India
has such a diverse geographical area that there are floods in some parts and
droughts in other parts of the country and same time they co-exist. Large
numbers of severe and devastating floods are endangering life and properties.
In the state of Odisha, flooding is caused primarily due to Mahanadi River. The
flow of water and its level in the river Mahanadi having a catchment area
141000 km2 is
controlled by Hirakud dam. The entire deltaic region of Mahanadi River
intercepting a catchment of 48700 km2 gets
affected by medium to severe flood almost every year causing immense loss to
life and property. Study was done to find out reduced level of flood water in
different locations of Mahanadi river reach between Hirakud dam and Naraj for
10, 25, 50, and 100 years return period using Hydrologic Engineering
Center-River Analysis System (HEC-RAS) model. The study has been accomplished
by preparing the basin map for Mahanadi river in HEC-RAS readable format and
computing the peak flood for 10 years, 25 years, 50 years, and 100 years return
period using Gumbel's distribution. Improvements for the channel cross-section,
bank embankment modification, height of flood protection structure such as
dikes, levees in the flooded zone were suggested. The peak flood discharge of
Mahanadi river at 10 years, 25 years, 50 years, 100 years return have been
calculated as 37535.026 m3/s,
45067.19m3/s,
50656.19 m3/s,
and 56203.24 m3/s,
respectively. Flood flow hydrograph has been prepared for the year 2008 by
unsteady flood flow simulation. Around 10 marked location of river stations are
prone to flood under 20 year return period. Eight such points were observed to
be overtopping the existing banks with a varying height of 1 m to 10 m with
reference to existing banks reduced level in subsequent 10 years to 100 years
return period in increasing order. The findings of present study suggest the
minimum height of dikes, levees to provide protection from flood at different
locations of existing banks to be 2 m to 10 m.
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