TABLE OF CONTENTS
CHAPTER ONE
INTRODUCTION
1.1 Background to the study
1.2 Problem
Statement
1.3 Aims
and Objectives
1.4 Justification
1.5 Scope
of the Study
1.6 Description
of the Study Area
CHAPTER TWO
2.0 Literature Review
2.1 Hydrology
2.2 Brief Description of Selected Hydrology
Models
2.2.1.
HSPF Model
2.2.2.
AGNPS Model
2.2.3 RIBASIM
2.2.4 SWAT Model
2.3 SWAT input data and management assumptions
2.4 SWAT Model Description
2.5 Sensitivity analysis in watershed
hydrological modeling
2.6 Previous studies on sensitivity analysis of
hydrologic modeling
CHAPTER THREE
METHODOLOGY
3.0 Model Selection and Description
3.1 Model Input Data
3.1.1 Digital Elevation Model (DEM)
3.1.2 Land Use Map of the Watershed
3.1.3 Soil Map
3.2 Weather Data
3.3 Model Setup and Run
3.4 Watershed Delineation
3.4 Sensitivity Analysis of hydrologic
parameters
CHAPTER FOUR
RESULTS AND DISCUSSION
4.1 Results
4.1.1 Stream flow out in the River Reach
4.1.2 Sediment yield in the River Reach
4.1.3 Sensitivity Analysis of Flow out
4.1.4 Sensitivity Analysis of sediment yield
CHAPTER FIVE
CONCLUSION AND RECOMMENDATION
5.1 Conclusion
5.2 Recommendation
REFERENCES
CHAPTER ONE
INTRODUCTION
1.1 Background to the study
The
water is the most important natural resource especially in the arid or
semi-arid zones that face high population growth, scarcity of freshwater,
irregularity of rain- fall, excessive land use change and increasing
vulnerability to risks such of drought, desertification and pollution. Thus,
the availability and the sustainable use of this resource become the core of
the local and national strategies and politics in these regions.
Hydrology
is the main governing backbone of all kinds of water movement and hence of
water-related pollutants. Understanding the hydrology of a watershed and
modeling different hydrological processes within a watershed are therefore very
important for assessing the environmental and economical well-being of the
watershed. These models can offer a sound scientific framework for watershed
analyses of water movement and provide reliable information on the behavior of
the system.
The
degradation of hydrological resources has made it essential to encourage
management practices based on knowledge of spatial and temporal changes in the
quantity and quality of water, in order to ensure the suitability of water
supplied for different uses. This can be assisted by using hydrological and
water quality models to simulate a wide range of processes in hydrographic
basins, such as the production of water and sediments and the dynamics of point
and nonpoint sources of pollution.
Hydrological
models are powerful tools to represent water-resource availability and behavior
in drainage basins under many applications, such as climate change, flood,
drought, runoff and nutrient movement (Abbaspour et al., 2015). They can assist
in the planning and decision-making processes for environment protection and
the guarantee of water availability for future uses (Da Silva et al., 2015;
Fatichi et al., 2016).
The
ability of hydrological model to produce satisfactory predictions is
necessarily correlated to adequate sensitivity analysis and model calibration
(Song et al., 2015). Hydrological models, such as SWAT, incorporate several
parameters (climatic, hydrological and others) obtained theoretically and
through field data collection. Some of these contribute greatly to model
outputs (sensitive parameters), while others have minor relevance
(non-sensitive parameters) (Van Griensven et al., 2006).
Osun
is a river that flow southward through southern Nigeria into Lagos lagoon and
Atlantic Gulf of Guinea. It is one of the several rivers ascribed in local
mythology to have been women who turned into flowing waters after some
traumatic event frightened or angered them. Osogbo GPS coordinates are
7˚46’15.74’’N and 4˚33’25.13’’E. Due to the potential of Osun river basin as a
major source of water supply, this study will develop a plan that will allow
for the sustainable management and treatment of the
water in the catchment area.
1.2 Problem Statement
Osun
River Catchment main source is one of the major sources of water supply,
drinking and commercial purposes. It therefore important to know sensitive
hydrologic parameters that contribute and hinder the stream flow out and
sediment concentration in the catchment area.
1.3 Aims and Objectives
The main aim of this project is to investigate the use
of modeling tool for sensitivity analysis of stream flow hydrologic and
sediment parameters. Specific objectives achieved are:
i. Simulation of the hydrological process of
the watershed using temporal and spatial data.
ii. Prediction of the stream flow and sediments
yield of the watershed.
iii. Determine
the influence of the hydrologic and sediment parameters on stream flow and
sediment yield prediction.
1.4 Justification
Most rivers are ungauged especially in developing
countries and therefore prediction of stream flow for sustainable water
management is regarded as an alternative. Prediction of stream flow and
sediment yield requires many hydrologic and sediment parameters. Also,
calibrating and validating such models are quite cumbersome due to many
parameters to deal with.
Therefore, it is very important to carry out sensitivity
analysis of the modeling parameters to assist modelers in concentrating effort
on most sensitive parameters that affect prediction of stream flow and sediment
yield.
1.5 Scope of the Study
This research work is to carry out the sensitivity analysis of hydrologic parameters in
modelling stream flow of osun river catchment. The analysis will be based on preliminary
modelling results obtained from the modelling of the watershed. Parameters of
interest are stream flow out and sediments yield with
31years meteorological data for the modeling exercises.
Model calibration and validation were not part of the
scope covered in this research work.
1.6 Description of the Study Area
Osun
is a river that flow southward through central Yoruba land in southern Nigeria
into Lagos lagoon and Atlantic Gulf of Guinea. The Osun River is located within
Osogbo Local Government Area of Osun State, Nigeria. It falls within Longitude
7˚46’15.74’’N and latitude 4˚33’25.13’’E. It is one of the several rivers
ascribed in local mythology to have been women who turned into flowing waters
after some traumatic event frightened or angered them. The map of the study
area is as shown in Figure 1.1
Figure 1.1 Map of Nigeria show location of the
Study Area
Click “DOWNLOAD NOW” below to get the complete Projects
FOR QUICK HELP CHAT WITH US NOW!
+(234) 0814 780 1594
Buyers has the right to create
dispute within seven (7) days of purchase for 100% refund request when
you experience issue with the file received.
Dispute can only be created when
you receive a corrupt file, a wrong file or irregularities in the table of
contents and content of the file you received.
ProjectShelve.com shall either
provide the appropriate file within 48hrs or
send refund excluding your bank transaction charges. Term and
Conditions are applied.
Buyers are expected to confirm
that the material you are paying for is available on our website
ProjectShelve.com and you have selected the right material, you have also gone
through the preliminary pages and it interests you before payment. DO NOT MAKE
BANK PAYMENT IF YOUR TOPIC IS NOT ON THE WEBSITE.
In case of payment for a
material not available on ProjectShelve.com, the management of
ProjectShelve.com has the right to keep your money until you send a topic that
is available on our website within 48 hours.
You cannot change topic after
receiving material of the topic you ordered and paid for.
Login To Comment