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With the same procedure, we calculate the height of equilibrium

L

e

assuming

Q

B

=

120

l/min

=

2

l/s

.

ν

B

=

Q

B

=

2

[l ⁄ s]

=

2 * 10

-3

[m

3

⁄ s]

ν

B

=

20

m ⁄ s

S

1 * 10

-4

[m

2

]

1 * 10

-4

[m

2

]

2

g

*

L

e

ν

A

=

L

e

=

ν

2

A

2

g

20

2

[m ⁄ s]

2

2 * 9,81

[m ⁄ s

2

]

L

e

=

20,38

m

1

L

t

L

t

L

t

L

t

L

2

3

4

L

L

B

B

B

B

A

A

A

A

Fig. 15

Part 2

In the previous section, we observed that bymaintaining a constant input and output flow rate, the height of the

liquid in the tank ismaintained at equilibrium.

Figure 16

Pos. 1

: two pipes, with relative valve sectionswhereby

S

A

1

=

S

A

2

=

S

are connected to the tank filledwithwater

up to the level

L

.We open the valve

B

(

S

B

>

S

) and subsequently the valve

A2

.

Once the equilibrium height

L

is reached, i.e. when the quantity of incoming liquidwill be equal to the quantity of

out-flowing liquid, we position a basin for collecting the liquid at the outlet of the valve

A2

.

After a unit of time

t

we verify the height

h

of the collected liquid.

Pos. 2

: we modify the previous system by also opening the valve

A1

and collecting the liquid in two containers.

Now the time

t

to reach the level

h

in the two basins is greater than the time noted in Pos. 1 (

t

2>

t

1).

We observe that the variation of outflow is not compensated by an appropriate change in the inlet flow, resulting

in changes in the level

L1

and therefore of the pressure.

If the valve

B

had been adjusted in order tomaintain a constant level

L1

=

L

, the same pressure of Pos. 1would

have been exerted on

A1

and

A2

and the filling time of the basinwould have been

t

2=

t

1.

Pos. 3

: let us now consider a single outlet pipe

A

of section

S

A

=2

S

In the time

t

1 a quantity of water equal to the sum of the flow of the valves

A1

and

A2

flows through the valve

A

and the underlying basin is filled up to a level 2

h

.

1

26

CAMOZZI

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PHYSICS