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AE/ME 201-- Procedure -- Lab: Tank Draining Instrumentation and ...

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<strong>AE</strong>/<strong>ME</strong> <strong>201</strong> – Spring 2005<br />

the tank.<br />

7. ρ - density<br />

With 3 locations <strong>and</strong> 7 unknowns at each, there are<br />

a total of 21 unknowns initially.<br />

Using a definition of total pressure from the<br />

Bernoulli equation (not used yet), one definition<br />

links four of the quantities for each location. The<br />

three state equations are:<br />

P T1 = P s1 + ρ 1V1<br />

2<br />

2<br />

+ ρ 1 gh 1 (3)<br />

Fluid Mechanics<br />

Figure 3: Schematic of tank.<br />

Although, this experiment is intended to introduce<br />

you to some different instrumentation techniques<br />

<strong>and</strong> demonstrate experimental methods for obtaining<br />

the constant coefficient in a simple first order<br />

differential equation, a brief introduction to fluid<br />

mechanics is included to help to underst<strong>and</strong> what<br />

you’re measuring <strong>and</strong> why.<br />

Measurements of the liquid height versus time for<br />

the tank draining will provide you with information<br />

on the exit flow fixture (i.e. for your experiment,<br />

this includes the section of pipe <strong>and</strong> the valve). For<br />

example, the valve at the bottom of the tank provides<br />

some resistance to flow <strong>and</strong> controls the rate<br />

of draining <strong>and</strong> the rate of change of height versus<br />

time. Also, the height in the tank sets the water<br />

source pressure that drives the flow through the<br />

valve. Therefore, the measurement of height versus<br />

time provides an indication of both flow rate <strong>and</strong><br />

supply pressure.<br />

There are three locations in question as shown in<br />

Figure 3. At each location, seven quantities are used<br />

to describe the state of the water or conditions:<br />

1. P s - Static pressure<br />

2. P T - Total pressure<br />

3. V - flow velocity<br />

4. h - fluid height<br />

5. ṁ - mass flow<br />

6. A - area<br />

P T2 = P s2 + ρ 2V2<br />

2<br />

2<br />

+ ρ 2 gh 2 (4)<br />

P T3 = P s3 + ρ 3V3<br />

2<br />

+ ρ 3 gh 3 (5)<br />

2<br />

Conservation of mass applies between pairs of locations.<br />

The two conservation of mass equations are:<br />

<strong>and</strong><br />

ṁ 2 = ṁ 3 (6)<br />

dh 1<br />

ρ 1 A 1 = −ṁ 3 (7)<br />

dt<br />

Additional definitions are used to link some of the<br />

quantities. The velocity at location 1 is the free<br />

surface motion:<br />

V 1 = dh 1<br />

(8)<br />

dt<br />

Mass flow rates are defined from surface fluxes as:<br />

<strong>and</strong><br />

ṁ 2 = ρ 2 A 2 V 2 (9)<br />

ṁ 3 = ρ 3 A 3 V 3 (10)<br />

The loss coefficient, K or K 23 , for the exit plumbing<br />

(including the test section) is<br />

K = K 23 = 2(P T 2<br />

− P T3 )<br />

ρ 2 V 2<br />

2<br />

This adds an unknown <strong>and</strong> an equation.<br />

(11)<br />

More equations are obtained by adopting some assumptions.<br />

1. The total pressure loss between stations 1 <strong>and</strong><br />

2 is very small<br />

2. density is constant <strong>and</strong> known - this is three<br />

equations<br />

3. The static pressure at station 1 is the local atmospheric<br />

pressure<br />

4. The static pressure at station 3 is the local atmospheric<br />

pressure<br />

2

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