122
Boundary
conditions
lch.4
fitted a number of check
valves which
open and
permit
a
restricted
flow into
the
tank.
When the flow direction reverses,
somewhat
smaller
check
valves, fitted
in the
leaves
of
the main
check
valves,
open and
permit flow
out of the surge tank into the
pipeline.
The
flow
is restricted
in both directions, less
for
flow in and more for
flow
out
of the tank. This restriction
dissipates
and attenuates the
mass oscillation and
also tends to
prevent
resonance. The flow in the
pipeline
just
upstream of the
junction
must
equal
the
flow into
the surge tank
plus
the flow
that
travels on down the
pipeline
away from the
junction.
So
A(i)u*,'
or#+ A(i+
1)u* .
(This
is the
same equation
as
was
used for the air
vessel
case.)
Ndenotes
the nodes at
the
junction
with
the surge
tank at time level /. From this
equation the
value
of.dhldt
can be obtained.
d/,
_
A(i)ul(i,
netno(i))
-
A(t + 1, 1)u1(t + 1,
1)
AT
where
i is the
pipe
number of the upstream
pipe
and
i * 1 is the number of the
pipe
downstream
of
the surge tank.
From dhldt
the
depth of liquid in the tank at the
end of a Ar
period
can be
calculated.
hrr: hr,+fftt .
Now
the head
in
the tank must be less than the
head
in the
pipe
at
the
junction
by the
amount of
kuluf2g
where u is the
velocity
through the
choke.
The
energy loss at
the
choke
due to the expansion
of flow
after it is
given
by this term and it
can be
seen that
it will reverse its direction
when
the flow reverses.
The
head
at the
junction
becomes
h2(i,netn'o(i))
=
Z +
hr +
h^ + Or,*
ry
where
fto is
the
height
of
the
water
barometer. This is the absolute
head at the
junction.
The value
of
k will have one
value when the
surge is rising
and
a
larger when
the
surge
is
falling.
This
is
because the larger chokes are in use when
the
surge
is rising
and
the smaller chokes
when
the surge is
falling. The
two characteristic
equations can
then
be used
to obtain the
values of the two
velocities
at the surge tank
junction
at the
t + Lt
time level.
dt
Sec.
4.141
Line
pack
and
attenuation
123
4.13.4
The
Johnson
differential
surge
tank
The Johnson
differential
tank is
a
surge
tank
with
special
qualities
in
that it is capable
of
causing rapid
attenuation
of
an oscillation
and is
unlikely to
generate
consequen-
tial frequencies
which
are
liable
to resonate
with the
governor
of
the
turbine
(see
Fig.
4.14).
open
top
(weir
flow)
orif
ices
Fig.
4.14
-
The
Johnson
differential
surge tank.
When shut-down
of
the
pipeline occurs,
forwhatever
reason,
the
level rises
in the
surge tank
and initially
in the
riser
only.
As it rises,
however,
flow out
through
the
base orifices
occurs
and
the
level starts
to
rise
in the concentric
outer
riser. When
the
level reaches
the top
of
the
inner riser,
a
weir flow occurs over
the
circumference
of
the top
edge of
it.
Eventually
the flow occupies
the entire
cross-section
of the tank
and the surge
reacies
its
maximum
amplitude.
The
surge
then
starts
to
fall but the
sequence
of events
is
not the
reverse
of the
events
that
occurred
during
the rising
surge.
The surge
falls,
at
first like
that in
a simple surge
tank;
then,
as
the surface
approaches
the level
of
the
central
riser, a
weir flow
will develop
down into
the
riser
of
smaller
diameter.
Once
a level
difference
between the surface
over
the outer
riser
and
the inner
riser
develops,
a flow
out of the
base
orifices into
the
inner
riser starts.
The level
in
the inner
riser falls
rapidly
and
the flow out of
the
orifices
is needed
to
stop
the level
from
falling
too far
and letting
air out of
the
surge
tank
into the
pipeline.
This sequence,
although
complex,
can
be
programmed
using
methods
similar
to those
demonstrated
in the
analysis
of
the choke
ring surge
tank.
Surge
tanks can
be used
in
the control
of
transients in
pipe networks
and also in
stabilizing
hydroelectric
systems.
As a
generalization it is
possible
to say that surge
tanks
are
more usually
encountered
in hydroelectric
schemes
and
air
vessels in
pipe
networks but
this
is a
very
general
statement
and
many exceptions
exist.
4.I4
LINE
PACK
AND
ATTENTUATION
When a
valve closes
rapidly
at the
downstream
end
of a
pipeline,
a steep-fronted
wave travels
upstream
at the
local acoustic
velocity.As it starts
off
to travel
upstream,