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Essay on water importance
The importance of water
The importance of water
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1. INTRODUCTION 1.1 Introduction “Anyone who can solve the problems of water will be worthy of two Nobel Prizes - one for Peace and one for Science”, stated by John F. Kennedy. Since the beginning of civilization, mankind has faced tribulations allied with river and its flow. With increase in utilization of water resources; flow in river channels are gaining significant importance among the research scholars. More and more complicated problems are encountered due to multipurpose use of alluvial rivers. Flow velocity, Shear stress, and Unit Stream Power are important characteristics for the measurement of the behavior of the river. Quantification of flow velocity, shear stress, and Unit Stream Power is important both for engineering problems and for ecological assessments. All these characteristics depend on resistance which is due to roughness, area of the flow and slope of the channels and the relation between these four parameters is known as resistance relationship. In simple form, flow velocity is defined as the displacement of water particles with respect to the time; shear stress refers to the force which is exerted by water on the channel bed; and stream power refers to the rate of energy dissipation against the bed and banks of a river per unit downstream length. If the slope of the channel is steep, then the flow velocity is high. And in Gravel bed-rivers, if the discharge is increased due to high intensity rainfall, then this high velocity of flow results in large boulder movements, which may cause heavy destruction. So, if some obstruction is provided in the course of the river then the flow velocity and thus shear stress is reduced and less rate of energy dissipation. In response to any change in the environ... ... middle of paper ... ... destruction caused to movement of heavy boulders, in case of high intensity rainfall. 1.4 Organisation Of Thesis The chapters are organized in the following way: Chapter-1- Description of introductory aspects of the topic studied, underlying objectives and description of the study area and the layout of the thesis. Chapter-2- Presentation of a comprehensive review of literature Chapter-3- Description of data collection and methodology adopted Chapter-4- Study of flow velocity and its results and conclusion Chapter-5- Study of Shear stress and its results and conclusion Chapter -6- Study of Energy gradient slope and its results and conclusion Chapter-7- Study of Stream Power and its results and conclusion Chapter -8-Preliminary Structural Detailing and cost analysis of the piano key weir Chapter-9- Presentation of conclusions and scope for future work
Exploring the Channel Characteristics of the River Chess The aim of this investigation is to explore the channel
Depending on the type of path that was created, it would largely influence the rate and distance to which the sediment was transported.
Allow land close to the river to be used for economic gain · Concrete levees are a barrier to the river draining away naturally · Expensive to build & repair · Restrict access to the river Channel straightening Straight channel is cut between two necks of a meander -shortens river. · Shortens river - cuts transport costs · Controls the flow of the river more closely · Evidence now suggests that river Mississippi too powerful - re-cut back to original meander course breaking away from artificial channel. Wing Dikes Structures built out into river to force faster current to midstream.
As can be seen from the photo( Image 1), looking downstream, there were steep sections of bank where it appeared the erosive forces of the river when high have cause part of the bank to fall away leaving steep about 1m high drops on the bank with exposed rocky soil visible. The phenomenon also illustrate that it is an alluvial landforms, which will find erosional feature from fluvial
This report is to see the effects of stream erosion and transportation of sediment caused by running water in the North Fork Cosumnes River California. The field repot was conducted on July 9, 2014 by Joel Morsey and John Morsey. I chose this location because I used to go there with my family when I was younger to swim in the river. I was interested to see how low the river was, because of the drought California has been having and to see the effects of erosion in more detail because the water would be much lower.
This course is found closest to the sea where the river has its mouth. The flat area of land by the riverbanks is known as a floodplain. Sometimes a river can also have an estuary or a delta as its mouth. This is due to the following. Rivers and its landforms are formed and moulded over time chiefly by the processes of erosion, and by the transport and deposition of sedim... ...
A river or “stream, ribbons of water confined to channels, or troughs, cut into the land,” (Marshak, 2009) is formed from a drainage network or “the array of interconnecting streams” that form tributaries. (Marshak, 2009). The amount of water that flows down a stream is its discharge. The discharge measurement takes the width and depths or cross sectional area of a river as well as the downstream velocity to get a numeric value for amount of water moving down stream. (Marshak, 2009)
The interactive force between the fluid and the porous medium is due to the frictional forces only and this force proportional to the flow velocity which represents by the term , where is the Darcy's coefficient, is the fluid viscosity and is the permeability of the porous medium.
...f the streams and drainage basins were found using the Calculate Geometry tool in ArcMap. This information gave us the minimum, maximum, average, and total stream lengths, along with the area of the drainage basins. Once this information was obtained it was used to calculate morphometric relationships (table 1). The sinuosity of the BRV was determined through a custom built tool in ArcMap that took the length of the stream over the length of the valley.
One of the largest geographic physical structures in the United States is the Colorado River. Human activity and its interaction with this great river have an interesting history. The resources provided by the river have been used by humans, and caused conflict for human populations as well. One of these conflicts is water distribution, and the effects drought conditions have played in this distribution throughout the southwestern region. Major cities such as Las Vegas, Los Angeles, San Diego, and other communities in the southwest depend on the river. It provides water for over 20 million people, irrigation for 2 million acres of land, four thousand megawatts of hydroelectric energy, and over twenty million annual visitors for recreation purposes. Also, once in Mexico, the river provides water to irrigate half a million acres of farmland, and municipal and industrial water for 2 million people living in this delta region. The river distributes its flow from lakes and canals along its journey as well. Due to climate change, human demand, natural forces like evaporation and human-induced climate change this water supply is in conflict. Also, a recent change that began in March of 2014 will bring a temporary water surge to the delta of the Colorado River for the first time in many years to help restore this region, and it’s possible it could reach the Sea of Cortez once again.
during normal conditions. Dam-like ridges form along the banks of rivers on flood plains and under normal conditions keep the river in its channel. During floods rivers flow over the tops of levees and flood the flood plains that lie adjacent to the river channel. Man has constructed channel walls to "beef up" the natural levees to protect the flood plains. However, all of New Orleans and the flood plain beyond the city is constantly threatened by flooding of the Mississippi River (Madsi, July 99).
A Flood Hydrograph and the Factors That Affect its Form A flood hydrograph is a graph of two axis, 'discharge' and 'time'. Plotted on the graph is the amount of discharge over a period of time. By looking at a hydrograph, a lot of information and data can be gathered about the river, the precipitation, the surrounding area and vegetation etc. The gradient, height and length of a line can tell you a lot of this information. There are many different factors that can affect the appearance and shape of a hydrograph.
Salt dilution method is used in mountain rivers with rough cross section, big boulders and turbulent flow. An electrical conductivity (EC) meter was used for discharge measurement. Salt dilution method is particularly used for measurement of flow in mountainous stream and any other sites where high degree of turbulence exists to ensure complete mixing of injected solution in the pre-determined length of the channel. Under such condition of flow, the conventional approach to flow gauging such as current meter or calibrated structure are not feasible. NaCl was used for discharge measurement with the salt dilution methods. The amount of salt to be injected depends on flow estimation flow (generally 5 g/l). The salt was dissolved properly in a bucket. Then this solution was injected at once in the stream water almost 100 m from point of measurement. Base level conductivity of water was noted. As the salt reached to the place of measurement, the conductivity value started changing. The conductivity values were noted with 5 second interval. This was done until the measured value reached the base level conductivity again (Hofer, 1998). The rate of flow in channel (Q) can then be calculated by:
Problems during transportation or relocation of water can occur. Water can be lost through evaporation while rerouting waterways. This too Involves human intervention, which presents many more problems. Man made waterways, dams, pumps, these things require energy, creates wastes, and ruin the natural environment. They interrupt marine ecosystems as well as marsh areas and swamps. Huge river projects displace people, cultures and livelihoods and put species in danger. For example in Iraq, the days of reed built houses and long wooden boats are over.
Water is an integral part of not only human beings but all other creatures in the world. We use it every day for different purposes such as domestic, agricultural and industrial. Water has always been a prestigious resource. However, the majority of people do not appraise water’s worth since they do not face water scarcity; whereas, in third world countries it is one of the most serious problems. Nearly 2.4 billion people have a lack of water resources in the world, shows the investigation done by the Pacific Institute, an Oakland, California-based non-profit scientific research group. Moreover, every year this number is growing gradually and more people are suffering (Bloomberg News, 2010). There are certain causes which deteriorate current situation. The most influential reasons are global warming, pollution by human-beings and overpopulation. It is known that India is one of the countries which face water scarcity so this essay will consider the possible ways of solutions of water shortage in India.