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Last modified
1/25/2010 6:47:57 PM
Creation date
10/5/2006 1:10:52 AM
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Floodplain Documents
County
Statewide
Community
State of Colorado
Basin
Statewide
Title
State Of Colorado Dam Safety Manual
Date
6/1/1983
Prepared By
Colorado State Engineers Office
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br />10 <br /> <br />2.9 <br /> <br />FLOW PATH <br /> <br />29-1 Flow Path is the approximate line or path <br />droplet or molecule of water takes whe <br />moving tlucugh a material. <br /> <br />These comparisons are intended to rank or order the <br />materials in terms of how much area or how many <br />pathways are available for water to flow through. A <br />larger void area reduces the soil's ability to resist the flow <br />of water. <br /> <br />2.8 WATER PRESSURE <br />An understanding of two aspects of water behavior is <br />important in understanding why water tends to flow <br />through a soil. These are: <br /> <br />1. The pressure exerted at any point in a body of <br />water increases with increased depth below the <br />water surface. <br /> <br />2. The water pressure exerted at a point can act in <br />any direction. <br /> <br />Figure 2.8-1 shows a container with three holes of the <br />same size along one side. Water flowing from the bot- <br />tom hole moves much further horizontaIly because of <br />the increased pressure at that exit point. <br /> <br /> <br />FIGURE 2.11-1 WATER PRESSURE VARIES WITH DEPTH <br /> <br />Figure 2.8-2 shows several smaIl pipes originating at <br />approximately the same point. The water flows in the <br />various directions. This illustrates that water pressure at <br />any point can cause flow in any direction if a path is <br />available. <br /> <br /> <br />FIGURE 2.11-2 WATER PRESSURE AT ANY POINT ACTS IN ALL <br />DIRECTIONS <br /> <br />'\ <br /> <br /> <br />A <br /> <br />. . , <br /> <br />~-......; . .. <br />~.. ~.' 4'w ''..-.:~;'~'-~:,.~ ". <br />.: .. . ~ .... <br />. ...... . <br />.,.f . . ~ . .....: . . <br />'''.,. <br /> <br />B <br /> <br />. <br /> <br />. <br /> <br /> <br />FIGURE 2.!H FLOW PATH OF WATER MOVING THROUGH SAND- <br />FILLED CONTAINER. <br /> <br />In the above figure water is introduced into a <br />sand-filled container at the top and exits <br />through the pipe in the side. The path water . <br />takes through the container is caIIed the flow <br />path. <br /> <br />A droplet of water moves along a flow path <br />from an initial contact point A with a material <br />or combination of materials to some exit point <br />B from those materials. <br /> <br />Point A, Figure 2.9-1, is where the water <br />droplet contacts the sand material and <br />Point B is where that same droplet exits <br />the material and begins moving under the <br />influence of gravity alone. <br /> <br />2.10 LENGTHENING THE FLOW PATH <br />In the experiment shown here the quantity of flow <br />through a compacted sand material contained in a j's- <br />inch diameter tube was reduced about 5y\% for each <br />I-inch unit of increased flow path when subjected to a <br />constant water pressure. llJis illustrates that lengthen- <br />ing of the flow path can help red'Jce flow through the <br />material. <br /> <br /> <br /> <br />FIGURE 2.10.1 <br />REDUCED AMOUNT OF FLOW CAUSED BY LENGTHENING THE <br />FLOW PATH <br />By increasing the length of the path through the same material, tbe amount of <br />flow is reduced. <br />Another example of increased flow path is shown here. <br /> <br />Two identicaIIy sized tanks are made. One of the tanks is <br />equipped with a series of alternating baftIes which are <br />waterproof. Both tanks are filled with sand. Each tank is <br />
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