dc.description.abstract |
Water is one of the precious and vital resources essentially required for the sustenance
of life and for the economic and social progress of any country. Scientific water management
is a must to sustain the domestic, irrigation and other water needs. Quantifying the hydrologic
responses at micro watershed scale plays an important role for water resources development
of a locality. For understanding the watershed characteristics and behavior, models play an
important role which are also useful for extrapolating the current conditions to potential future
conditions. Hydrological modeling is considered as a powerful technique for water resources
management. In this study, the hydrology of two small sub watersheds of Bharathapuzha river
basin near Valanchery town, were modeled using GIS and SWAT watershed model. The study
aims to quantify the morphometric characteristics using GIS, simulate the hydrologic elements
and stream flow using SWAT model and to suggest water conservation measures for the study
area.
First, a comparison of different commonly available DEMs were made to assess their
suitability to perform morphometric analysis and it was found that SRTM DEM gives best
result. Further studies were carried out using SRTM DEM. The W1 sub watershed is devided
into six micro watersheds and W2 sub watershed is devided into four micro watersheds and
prioritized the micro watersheds using morphometric analysis. Further, datasets required for
the SWAT model were collected through primary and secondary sources and calibrated the
model by generated two years (2019 to 2020) of stream flow. An NSE = 0.87 and R 2 = 0.92
for W1 sub watershed and NSE=0.91 and R 2 = 0.91 for W2 sub watershed were obtained. With
the calibrated model, simulations were made to predict the hydrologic elements of both the sub
watersheds. The whole sub watersheds characteristics and behavior and that of micro
watersheds were determined and predicted.
It was found that ET values of sub watersheds were varying in the range of 16 to 28 %
of the annual rainfall, surface flow and base flow were in the range of 36 to 44 % and 25 to 27
% for W1 and W2 sub watersheds respectively. Relationship between morphometric
characteristics and water balance components were determined and it was found that drainage
density has got direct relationship with surface runoff (SURQ) and total runoff (WYLD) is
having inverse relationship with base flow. Similarly, the relationship with relief ratio, stream
frequency and texture ratio were also found out. Further, regression analysis was done between
the morphometric characteristics viz. drainage density, relief ratio, stream frequency and
texture ratio with that of hydrologic responses viz. surface runoff (SURQ), lateral flow (LAT_Q), baseflow (GW_Q) and water yield (WYLD). It was found that drainage density,
stream frequency and texture ratio was having good positive correlation with total runoff
(WYLD) generated from the watershed. Drainage density was having negative correlation with
baseflow (GW_Q). Using these vital information, soil and water conservation measures have
been suggested scientifically and objectively at micro watershed scale. |
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