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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.
After the Civil War, America was in a lot of turmoil, especially in the southern states. A goal of the U.S was to bring the southern states back into the union and fix up all the physical damage that tore apart the south. Reconstruction had a couple main goals to bring America back together and that was to fix the southern states of all the damage that was done, explain how the southern states could be readmitted into the union, and also implement how whites and blacks could live together without slavery. Also during reconstruction, black and white teachers would help teach former slaves who were illiterate how to read and write. Thought the main goal of reconstruction was to rebuild America, there were three different plans on how America
North Fork Cosumnes River is what you call a bedrock channel. A bedrock channel is a channel in which the stream is actively cutting into solid rock. Evidence of this is the visible erosion of potholes in the bedrock like the picture to the left shows lots of potholes. How does this happen to the bedrock, according to the text, by sand and pebbles large and small caught in swirling eddies that act like drills and bore circular potholes into the bedrock channel
Why Depositional Landforms Occur Along the Course of A River Rivers have three courses. The course is the journey the river makes to reach the sea. Rivers never have a straight course from source to mouth. Their course is always irregular. Along this course depositional landforms can occur.
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).
...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.
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)
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.
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.
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
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.
If the gradient is steep (like the example on the right) then this can indicate that the amount of rainfall becoming overland flow is very high, the result of this is that all the water reaches the river very quickly and all in a short period of time, this gives the immediate steep ascending limb on the hydrograph. Reasons for large amounts of rainfall becoming overland flow can be little vegetation and maybe impermeable rock below the surface. Being impermeable rock, the water cannot infiltrate through this and become ground water, instead it flows over the ground to the river. Urban development and agricultural practices contribute to overland flow.
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.