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Science of Water : Concepts and Applications

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<strong>Water</strong> Hydraulics 59<br />

With regard to fl ow, continuity <strong>of</strong> fl ow <strong>and</strong> the continuity equation have been discussed (i.e.,<br />

Equation 3.15). Along with the continuity <strong>of</strong> fl ow principle <strong>and</strong> continuity equation, the law <strong>of</strong> conservation<br />

<strong>of</strong> energy, piezometric surface, <strong>and</strong> Bernoulli’s theorem (or principle) are also important<br />

to our study <strong>of</strong> water hydraulics.<br />

CONSERVATION OF ENERGY<br />

Many <strong>of</strong> the principles <strong>of</strong> physics are important for the study <strong>of</strong> hydraulics. When applied to problems<br />

involving the fl ow <strong>of</strong> water, few principles <strong>of</strong> physical science are more important <strong>and</strong> useful to<br />

us than the law <strong>of</strong> conservation <strong>of</strong> energy. Simply put, the law <strong>of</strong> conservation <strong>of</strong> energy states that<br />

energy can neither be created nor destroyed, but it can be converted from one form into another. In<br />

a given closed system, the total energy is constant.<br />

ENERGY HEAD<br />

Two types <strong>of</strong> energy—kinetic <strong>and</strong> potential—<strong>and</strong> three forms <strong>of</strong> mechanical energy—potential<br />

energy due to elevation, potential energy due to pressure, <strong>and</strong> kinetic energy due to velocity—exist<br />

in hydraulic systems. Energy has the unit <strong>of</strong> foot pounds (ft-lb). It is convenient to express hydraulic<br />

energy in terms <strong>of</strong> energyhead, in feet <strong>of</strong> water. This is equivalent to foot-pounds per pound <strong>of</strong> water<br />

(ft-lb/lb = ft).<br />

PIEZOMETRIC SURFACE<br />

As mentioned earlier, we have seen that when a vertical tube, open at the top, is installed onto a<br />

vessel <strong>of</strong> water, the water will rise in the tube to the water level in the tank. The water level to which<br />

the water rises in a tube is the piezometric surface. That is, the piezometric surface is an imaginary<br />

surface that coincides with the level <strong>of</strong> the water to which water in a system would rise in a piezometer<br />

(an instrument used to measure pressure).<br />

The surface <strong>of</strong> water that is in contact with the atmosphere is known as free water surface.<br />

Many important hydraulic measurements are based on the difference in height between the free<br />

water surface <strong>and</strong> some point in the water system. The piezometric surface is used to locate this free<br />

water surface in a vessel, where it cannot be observed directly.<br />

To underst<strong>and</strong> how a piezometer actually measures pressure, consider the following example.<br />

If a clear, see-through pipe is connected to the side <strong>of</strong> a clear glass or plastic vessel, the water will<br />

rise in the pipe to indicate the level <strong>of</strong> the water in the vessel. Such a see-through pipe, the piezometer,<br />

allows you to see the level <strong>of</strong> the top <strong>of</strong> the water in the pipe; this is the piezometric surface.<br />

In practice, a piezometer is connected to the side <strong>of</strong> a tank or pipeline. If the water-containing<br />

vessel is not under pressure (as is the case in Figure 3.8), the piezometric surface will be the same<br />

Free water<br />

surface<br />

Open end<br />

Piezometric surface<br />

Piezometer<br />

FIGURE 3.8 A container not under pressure where the piezometric surface is the same as the free water<br />

surface in the vessel.

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