Nbsbulletinv10n2p191 A2b Trubine Windage Loss
Nbsbulletinv10n2p191 A2b Trubine Windage Loss
Nbsbulletinv10n2p191 A2b Trubine Windage Loss
^
j
appears in that
term, all remain indeterminate, i. e., they may have any values
whatever without violating the dimensional requirements. We
may also write equation
(3)
in the simpler form
P-pn>D^<^-^)
(4)
where
^
is an unknown function of (
^y
For wheels of any given shape, the form of the fimction tp is
fixed, but for anyother shape the form of cp will or may be different.
It depends on the values of a number of ratios of lengths sufficient
to fix the shape of the wheel and casing, including the closeness
of the casing to the wheel as part of the "shape." These ratios
determine the values of the A^'s and S's of equation
(3).
The
variable
( V>,
)
has no dimensions, so that its numerical value in
any absolute units is fixed by the physical magnitudes of /x,
/>,
n,
and D, and is independent of the magnitudes of the fundamental
imits.
194
Bulletin
of
the Bureau
of
Standards ivoi.io
2. Remarks on the Function cp.
Equations
(3)
and
(4)
contain
all the information obtainable from the principle of dimensional
homogeneity, and further information must be sought elsewhere.
The resistance offered by a fluid to a solid body in steady motion
through it may be looked upon as a retarding drag due to trans-
verse communication of momentum between currents or layers
of the fluid which are moving over each other with different average
velocities and are maintained by the motion of the solid body.
In quiet stream-Hne motion, this transfer of momentum takes
place by intermixing on a molecular scale, i. e., by interdiffusion of
the different streams of fluid; and the coefficient of viscosity,
/I, is a measure of the activity of this molecular intermixing.
But whenever, by reason of high speed or of roughness or irregu-
larity of the sohd, the motion of the fluid becomes very turbulent,
the lateral transfer of momentum between different streams occurs
mainly by motions of relatively large masses of fluid in all sorts
of irregular cross-currents and eddies. For any given geometrical
arrangement of such a state of tiurbulent motion, this molar trans-
fer of momentum is evidently proportional to the masses involved,
or in other words, to the density of the fluid.
We must therefore expect that when the motion of the fluid
about the solid body is perfectly quiet and regular, which will
usually mean that all the motions are slow, the resistance encoun-
tered by the solid will be directly proportional to the viscosity
of the fluid. But if, on the other hand, the circumstances are
such that the motion of the fluid is very tiurbulent, it is to be
expected that density will play the determining part in the phe-
nomena of resistance, viscosity being of relatively small or even
vanishing importance. The substantial correctness of this general
qualitative reasoning is estabHshed by well-known facts relating
to skin friction, aeroplane and ship resistance, and the flow of
liquids and gases tlurough pipes. Let us now see what it leads
to in connection with equation
(3)
.
If we have to deal with a smooth disk at a low speed of rotation,
we must expect the retarding torque and therefore the power ab-
sorbed at any given speed to be directly proportional to the viscosity
of the medium about the disk. This requires that the second
member of equation
(3)
shall consist of only a single term and
Bucktngham] Wiudage Losscs
of
Steam Turbines
195
that its exponent shall be S =
i . The equation for the power thus
reduces to the very simple form
P
=
Nn^D'/JL
(5)
and the retarding torque is therefore independent of the density
and proportional to the speed of rotation, the viscosity of the
medium, and the cube of the diameter of the disk.
If the speed of rotation is increased, the stream-Hne motion
will become unstable and will break up, at or near a certain definite
critical speed, into a quite different, turbulent motion. At all
events, this is what we should expect from our knowledge of the
flow of fluids through pipes, and otir expectation is confirmed
by experiments on disks. After this abrupt change in the char-
acter of the fluid motion, the density of the fluid must appear
in any equation which is to describe the facts, and if the vis-
cosity fi appears at all it must be, in each term, with a smaller
exponent than that of
p
in the same term. In the Hmiting case,
the viscosity might be of altogether vanishing importance and
then equation
(3)
would necessarily have the form
P
=
Npn'D'
(6)
the retarding torque being proportional, for a given disk, to the
density and the square of the speed, while for disks of different
diameters but geometrically similar
^the experi-
mental accuracy not having been high. Equations
(5)
and
(6)
correspond to the limiting values B=i and S =
o.
The value of A^ depends on the form of the wheel and casing.
For a bladeless disk running in the open, it depends on the pro-
file and the roughness. For a thin flat disk it depends on the
roughness alone; but the roughness is to be measured in terms of
the diameter, so that for a surface with granulations or irregulari-
ties of a certain general absolute size, a large disk is "smoother"
than a small one, in the present sense of the term smooth.
For smooth plane disks of small thickness, the critical speed, at
wliich stream line motion breaks up into turbulent motion and
the exponent B drops suddenly from nearly unity to a much
smaller value, is fairly definite and the change in the law of resist-
ance is sharp. For ordinary tm-bine wheels, consisting of a disk
and blades, the change is less abrupt and there is no definite
critical speed; for the motion about the blades must always be
turbulent at any speeds which are high enough to be of practical
interest. The smaller the ratio,
y^,
of blade length to disk diam-
eter, the more nearly the behavior of the wheel approaches that of
a simple disk, while with long blades, the additional resistance
due to the blades is so much greater than that which would be
encountered by the disk alone, that although the law of resist-
ance is different at high and at low speeds the change is gradual.
In an experimental study of the form of the function
(p we have
first to work with wheels of some one shape, preferably a simple
one, to start with. If we then find, as in fact we do for consider-
able ranges of the variables, that the dissipation P is proportional
to a fixed power of
p,
or of t^, or of Z^, or of fi, we know that equa-
tion
(7)
is adequate for this shape of wheel and our experiments
give us the value of the coefficient N for this shape as well as the
value of 8, no matter which of the four variables we may have
selected for independent variation during the experiments. There
are thus, in principle, four different modes of attacking the prob-
lem which must lead to the same result and may be used for
checking one another. In practice we can not always conven-
Buckingham] Windage Losses
of
Steam Turbines
197
iently vary the density and viscosity of the medium independ-
ently, so that there are often only three modes of attack which
are practicable.
The general procedure is obvious; keeping any three of the
variables at fixed values, we vary the fourth and observe the
corresponding values of P. If the phenomena can be described
by equation
(7),
the values of log P when plotted against the
logarithm of the independent variable will give points which lie
on a straight line, within the experimental errors. The slope of
this line is the exponent with which the independent variable
appears in equation
(7)
; it determines the value of S. The posi-
tion of the line, taken in connection with the fixed values of the
other three variables, determines the value of N. We may now
proceed to examine the experimental data which illustrate the
foregoing statements. Readers who are interested only in the
jSnal result of this somewhat laborious examination may proceed
at once to section
6,
page 214.
3.
The Relation
of
Power Dissipated to Speed
of
Rotation.
j
and it is fortunate that this appears with so small an exponent
since we know almost nothing about the viscosity of steam.
According to measurements by
h.
Meyer and O. Schumann (see
Landolt and Bomstein's tables) the viscosity of sattirated steam
at
100
is about 0.72 times that of air at room temperature. We
may assume as a sufficient approximation, under the circum-
stances, that jji is proportional to the square root of the absolute
temperature and is independent of the density. In applying
equation
(12)
to steam we therefore have
where / is the temperature of the steam on the Fahrenheit scale.
Equation (12)
then takes the form
p-./<i^r
..4)
applicable to dry steam of density
p
Ib./ft.^ and temperature t F.
We may first consider the
15
observations made by I^ewicki in
superheated steam, which was presumably dry and homogeneous
though at the lower temperatures this may not have been quite
true. The data which concern us are collected in Table 2, reduced
to English units.
2IO BtUlettn
of
the Bureau
of
Standards [Voi. w
TABLE 2
Lewicki's Observations in Superheated Steam; n
=
20 000 r.
p. m.
Pressure
[lb./i..]
Temperature
t
[F.]
Density
[lb./ft.3]
Power
P
[U.S.hp.]
P
P
P
pO-9
14.7 221 0.0368 3.02 82 59
14.7 253 0.0350 2.77 79 57
14.7 406 0.0286 2.33 81 57
14.7 462 0.0268 2.30 86 60
14.7 478 0.0263 2.00 76 53
14.7 531 0.0249 1.98 80 55
14.7 556 0.0243 1.87 77 53
14.7 574 0.0239 1.83 77 53
9.56 586 0.0153 1.08 70 46
5.69 462 0.0100 0.88 88 56
5.69 489 0.0097 0.81 84 52
5.68 259 0.0127 0.94 74 48
5.63 561 0.0089 0.60 69 42
5.39 295 0.0115 0.90 78 50
5.39
Means
590 0,0083 0.58 70 43
448 0.0202 78 52
Mean residuals 5.8% 3.5%
1
The values of the density are not very exact, partly because
for the first eight observations the pressure is merely stated to
have been atmospheric, and partly because the densities at high
superheats are not very accurately known.
In view of the unavoidable errors we can probably do no bet-
ter than to average the values and set P
=
'jSp, the mean density
being
p
=
o.o202 and the mean temperature 448 F. Under these
circumstances we therefore have P(obs)
=
1.58 hp. Equation
(14)
with these values of
p
and t gives us P(calc)
=
i.5i hp. The
agreement of the observed and calculated values to within
5
per
cent must be regarded as very satisfactory.
We may also represent the observations fairly well by setting
P(obs) =52 X/^*^^ while equation
(14)
gives us P(calc) =50.5 X/'^
The agreement is a trifle closer but there is no great difference.
The result of the comparison of Stodola's and I^ewicki's wheels
is to show that as nearly as we can tell, equation
(9)
represents
the facts and that dry steam is entirely comparable with air when
the proper physical constants are used.
Buckingham] Windage Losses
of
Steam Turbines 211
We may now consider Ivevvicki's five observations in saturated
steam, the results of which are shown in Table
3.
TABLE 3
Lewicki's Observations in Saturated Steam; n
=
20 000 r. p. m.
Pressure
[lb../m.21
Density
[lb./ft.s]
Power
[U. S. hp.]
P
P
P
14.7 0.03732 3.22 86.2 62.0
10.50 0.02727 2.69 98.3 68.9
8.56 0.02253 2.05 91.1 63.7
6.44 0.01726 1.66 96.0 64.0
5.69
Mean
0.01538 1.49 96.8 63.7
0.02395 93.7 64.5
Mean residuals 4.3% 2.8%
As for superheated steam, we can represent the results approxi-
mately by Poc/o or Pocp^'^, the second being in this case distinctly
the better, as is shown by the fact that the mean residual is only
2.8 per cent as compared with
4.3
per cent.
Not knowing how the viscosity varies with temperature when
the steam is kept saturated, we ignore the last factor of equa-
tion
(14)
which is certainly nearly unity, and we then have
P(calc) =49.7/0^'^ as compared with P(obs)
=
64.5/3*^ The observed
value is thus 1.30 times the calculated. Making the computa-
tion by the mean density we have P
=
93.7/5,
/9
=
0.02395
P(obs)=2.23 hp while equation
(14)
gives us P(calc)
=
1.73,
the ratio being now 1.29 in place of 1.30.
The cause of the discrepancy of 30
per cent is clear. To obtain
dry saturated steam is a difficult matter, requiring elaborate pre-
cautions, though this was not so well known at the date of Lewicki's
experiments. The increase of
30
per cent in the resistance in
passing from air or dry steam to saturated steam, was due to the
wetness of the steam. Not knowing how wet the steam may have
been, we have, perforce, used the density of the steam alone and
not the mean density of the mixture. The mean density would
have been larger and so would, if used in the computations,
have reduced the discrepancy between the observed and calcu-
212 Bulletin
of
the Bureau
of
Standards [Vol. lo
lated values. But it is most unlikely that the steam was so wet
that the whole
30
per cent could be accounted for in this way,
even supposing that the water remained completely suspended.
And under such conditions only a very small amount of water
remains in suspension as fog; most of it is deposited and that is
imdoubtedly what happened here.
Just
how wet the steam was
and why the deposition of water on the wheel should have
increased the resistance
30
per cent it is of course impossible to
say. But it is clear that the steam did not act like an homogene-
ous medium, so that equations developed for homogeneous media,
which, as we have seen, describe the facts satisfactorily for both
air and dry steam, are not strictly apphcable. All we can say
at present is that the resistance to the rotation of a wheel in steam
increases considerably if the steam changes from dry to wet; but
how the amount of the increase depends on the wetness or other
circumstances can only be decided by further experiments.
It remains to examine Holzwarth's results for wheels which
had the same ratio of blade height to disk diameter and so had at
least this one element of geometrical similarity. We have the
figiu-es given in Table
4,
for -^
=
0.05.
TABLE 4
Holzwarth's Results on Wheels with the same Blade Length Ratio
Disk diameter
D (ins.)
Blade
length
/ (ins.)
20
30
40
50
1.0
1.5
2.0
2.5
3.6
3.0
2.9
3.1
2.5
3.5
2.5
2.3
The values of
y3,
taken from the straight lines drawTi on the plot
of log K against log n vary considerably and are rather uncertain
so that the round values yS
=
3
and
7
=
5
have been adopted. The
values in the last column were got by averaging over all the
points which lay distinctly above any indication of a rapid change
in the exponent of n, omitting a few doubtful readings. If these
Buckinoham] Windage Losses
of
Steam Turbines
213
wheels were, together with their casings, all geometrically similar,
and if we had 8 =
0,
the values of
ttW
should all be the same;
it is seen that they are nearly so. The high value for the 30-inch
wheel is consistent with other readings which make it appear that
the 30-inch disks were much rougher than those of the other
diameters.
We have also the following figures for
^^
=0.025
TABLE 5
D 1
P
10iK
n'Ds
20
40
0.5
1.0
3.6
2.5
1.31
1.29
If the readings of K from the published curves really represent
the facts as Holzwarth observed them, the great difference in the
two values of
^
proves that these two wheels were far from geo-
metrically similar. The agreement of the values in the last
column is therefore little better than accidental, though it shows
that the facts may be represented, at least roughly, by the equation
P
=
Npn^D\
5.
The
Effect of
the Density
of
the Medium.All writers on the
subject appear to agree that when a given wheel runs at a given
speed, the power dissipated is directly proportional to the density
of the medium. Holzwarth says that this relation holds for
steam "within limits acctirate enough for practical pturposes,"
and I^asche, in an equation quoted by Stodola,* sets Pocpn^.
Stodola experimented on a multi-disk impulse turbine driven
in stagnant steam of densities of o.i to 1.7
kgm/m^, which
correspond, if the steam was dry satiu-ated, to pressm-es of 2.5 to
45
Ib/in^ absolute. His observations as plotted on a small scale
diagram indicate the existence of a linear relation between P
and
p,
and he sets
Pocp and uses tliis relation without further
question. Lewicki's observations as given in Tables 2 and
3
also indicate that the resistance is approximately proportional
to the density. We may therefore say that within the range
2
1
4
Bulletin
of
the Bureau
of
Standards [Voi. to
and the accuracy of the published experimental data on this
point, the windage of turbine wheels in a given medium is pro-
portional to the density of the medium, but the evidence is not
at all sufficient to show how nearly exact the relation is. We can,
in fact, only regard this evidence as roughly conformatory of that
presented in section
3,
which shows that when the medium is
homogeneous the exponent of
p
in equation
(7)
can not differ
much from imity.
6. Remarks on the Comparison
of
Dissimilar Wheels.
^The
considerations already set forth having shown that an equation
of the form
(7)
describes the behavior of wheels of any one shape,
it remains for us to find out if possible how the coefficient N
depends on the shape of the wheel and its casing.
Since N depends on shape and not on absolute size, any correct
expression for N must contain as variables only ratios of lengths.
An equation for P which can not be reduced to the form
(3),
or
practically to the form
(7),
with the N's satisfying the above
condition, is not a rational equation and can not have any general
validity, even approximate, though it may be satisfactory as an
empirical working formula over limited ranges of the variables.
In attacking the problem of finding a satisfactory expression
for N we are met at the outset by the obvious fact that the shape
of a turbine wheel and its casing, even if confined to general
conformity with commercial practice, may vary in a great many
ways. Thus N must be regarded as a function of a large number
of variables which are, at least within certain limits, all inde-
pendent. But while a complete solution of the problem of pre-
dicting the value of N from geometrical measiurements is thus
out of the question, we may nevertheless make some progress
if it is found that in practice one or a very few variables are of
so much importance that the effects of changing the others are
small or negligible.
It is evident, both a priori and from experiment, that two
very important geometrical elements to be considered are the
blade length and the closeness with which the casing surrounds
the blades, both measured in terms of the disk diameter. Other
important elements are the roughness of the disk; the width,
pitch, and angles of the blades; the number of rows of blades,
Buckinoham] Windage Losses
of
Steam Turbines
215
and whether they are shrouded or not. Of these most evidently
important data, the blade length ratio,
j^,
and the number of rows
of blades are often the only ones given in pubhshed accounts of
experiments, the others either not being given at all or having
been varied so unsystematically that they can not be used. To
start with, we shall of necessity confine our attention to wheels
with one row of blades, together with their Umiting form, bladeless
disks. As regards pitch, width, and angles of the blades, we
can only say that in practice different single-row steam-turbine
wheels are usually somewhere near similar in respect to these
points, as they are also, though perhaps less nearly, in respect
to roughness and profile of the disk.
Stodola's experiments
^
showed that the amount of clearance
between wheel and casing has a large influence on the windage
resistance, and he made a few measurements relating to this
piont. But since his results are not numerous and we have no
other satisfactory data on the effect of altering the casing which
incloses a given wheel, we are reduced to the expedient of elimi-
nating the effect of the casing by removing it altogether; in other
words, we must, at least in starting, use only data obtained from
wheels running in the open without any casing. We may then
hope to get an approximate expression for N in terms of the blade-
length ratio, the hope being founded on the expectation that this
will prove to be much more important in specifying the shape
of the wheel itself than all the other variable elements combined,
so long as these others remain within the Hmits which obtain in
practice.
We then have available for study, Odell's results on disks and
Stodola's results on one disk and five wheels. Tentatively, we
shall also use Holzwarth's results on inclosed wheels in steam,
the assumption being that the casings were similar. Since the
nature of these data does not warrant the use of any refinements
in analyzing them, we shall accept the equation
P^Npn^D^
(15)
as a sufficiently approximate description of the facts for wheels
of any given shape.
2 1
6
Bulletin
of
the Bureau
of
Standards ivoi. to
7.
Expressions
for
N in terms
of
Roughness and Blade Length.
A) against log
y^.
If we can find a
value of A such that the points all lie on a straight line within the
observational errors, equation (22)
is satisfied, the slope of the line
is the value of x, and the position of the Hne gives the value of B.
By this method it was foimd that the observations on foiu* of
the five wheels are satisfactorily represented by writing equation
(22)
in the particular form
P= lor^^prvz>{i+
593(5)]
(24)
Buckingham] Windage Losses
of
Steam Turbines 219
and that no other values oi A,B, and x are sensibly better. Values
computed by equation
(24)
are given in column VII of Table 6
and the agreement of the results mth the observed values in column
V is shown by column VIII to be good except for wheel A. The
value for this wheel can evidently not be brought into accord
with those observed for the others by any simple expression for N
as a function of
y^.
It is possible that the discrepancy may be due
to an experimental error, but this seems very unlikely. Unless it
is merely a typographical error, it probably arises from some geo-
metrical peculiarity of this wheel which is not evident from the
description given. The writer has assumed that the blades of all
the wheels were shrouded, because that is the usual construction;
but if the blades of wheel A were open-ended, the relatively
greater windage would be easily understood.
However, there is no advantage to be gained from splitting
hairs in analysing so small a number of data by means of confess-
edly only roughly approximate assumptions, and we may be
content to say that equation
(24)
represents the results of Stodola's
experiments on single-row wheels of ordinary forms running in
the open air, quite as well as could be demanded of any equation
deduced from so inadequate data.
9.
Deduction
of
an Expression
for N from Holzwarth's Data.
^To avoid
the difficulties of working with large wheels, it may be desirable
to utilize the results of model experiments as is done in determin-
ing ship resistance.
If we limit ourselves to tne use of a single medium, the prac-
ticable range of scale reduction is not great, unless the full-sized
original runs very slowly, and this case is not interesting because
we know that at low speeds the windage losses are too insignificant
to demand much attention. For dynamical similarity in a given
medium, a quarter-scale model must, by equation
(28)
run at 16
times as many revolutions per minute as the full-sized original;
and by equation
(32),
the centrifugal stresses in the wheel will
then be 16 times as great in the model as in the original; an
increase which would usually not be permissible. Furthermore,
the peripheral speed of the model will be
4
times that of the original
and may approach the acoustic speed so closely as to invalidate our
fundamental assumption that the medium behaves sensibly as if it
were
incompressible. There is evidently not much information
to be got from small scale models unless they can be nm in a med-
ium of much less kinematic viscosity than steam, so that the speed
of the model may be reduced, in accordance with equation
(28)
.
Water is such a medium. Using values from I^andolt and Bom-
stein's tables, and comparing water with air which is known to
act like dry steam, we have at
20
C and i atmosphere pressure.
Air Water
p=0. 001205
^=0.0001898
v=0. 1575
p=0.9982
;^
0.01012
y= 0.01014
Buckingham^ Windage Losses
of
Steam Turbines 229
Let it be desired to find the power dissipated by a wheel of diam-
eter Do
running no
revolutions per minute in air, by means of
experiments on a model of diameter D
=
^
running in water,
the temperatiu-e being
20
C in each case and the air being at
normal pressure. We then have to substitute in equations
(6)
to (10)
p
V
=828
=
0.0644
the uncertainty of
being about
3
per cent.
For any given scale ratio r, the ratio of corresponding speeds,
n for the model and no for the original will be, by equation
(28)
,
n
=
o.o644r2
3
per cent
(33)
/fro
The ratio of the powers dissipated at corresponding speeds will
be, by equation
(29)
,
p
p- =0.222 r 6 per cent
(34)
from which Po can be foimd if P has been measured in an experi-
ment on the model.
We must next consider whether the stresses in the wheel and
shaft of the model will rise too high when we make a convenient
reduction of diameter. Taking first the centrifugal stresses in
the wheel, we have by substitution in equation
(32)
^
=
0.00415 r^
(35)
Setting C
=
Co
and solving for r, we find that the stress of any
point in the model will not exceed that at the corresponding point
in the original until r>i5.7. As a 10 to i reduction will usually
be ample, there will be no difficulty regarding the bursting strength
of the model if it is made of the same material as the full-sized
wheel.
230
Bulletin
of
the Bureau
of
Sta^tdards [Vol. lo
For the ratio of the shearing stresses in the shaft, equation
(31)
gives us
5
So
= 3.43^^
(36)
A scale reduction r
=
10 would thus give us
343
times as great a
stress in the shaft of the model as in the original shaft. This, at
first sight, looks quite impracticable. But in fact turbine shafts
are generally made much stronger, for the sake of stiffness, than is
required by torsional strength; and, furthermore, the torque due
to windage when the wheel is driven light is only a few per cent
of the torque of the wheel running at full load. Hence the ratio
343
would probably not always be excessive. However, doubling the
diameter of the shaft of the model would have hardly any effect on
its windage resistance, and by such a small sacrifice of exact geo-
metrical similarity the use of a model in water might always be
made practicable, so far as the strength of the shaft is concerned.
To make the matter more concrete we may carry out the com-
putations for a few typical cases of wheels run in air in comparison
with models of 12 inches diameter run in water. We have the
values given in Table 1 1
.
TABLE 11
FuU-sized
diameter
Do
(inches)
Wheel
. speed
no
(r. p. m.)
Diam-
eter
ratio for
12-inch
model
Do
Speed of
model
n
(r. p. m.)
Power
ratio
P
Po
Stress
ratio in
shafts
S
So
36
60
84
120
3600
1800
900
450
3
5
7
10
2090
2900
2840
2900
0.67
1.11
1.55
2.22
31
86
168
343
It therefore appears that the investigation of such cases as are
commonly met with, by means of
12-inch models run in water,
would be quite practicable so far as the points already treated
are concerned, and only one further point remains to be considered.
This is the question of cavitation.
Buckingham] Windage Losses
of
Steam Turbines
231
If cavitation occurs in the water the similarity of the model
and the original will cease to exist, and equation
(29)
will not give
correct results. To avoid cavitation, the water surrounding the
model must be under pressure and the casing must be constructed
accordingly. At atmospheric pressure and high speeds cavita-
tion will certainly occur. If the pressure on the water is increased
the cavitation will decrease and the torque at a fixed speed will
change until the presstue has been increased so much that cavita-
tion has been eliminated. By observing the variation of torque
or power with the pressure at any given speed we have thus a
means for finding what pressure is needed in order to eliminate
cavitation and make sure that the model in water is comparable
with its original in air or steam. It remains to be seen whether
the pressures required would be impracticably high, but it appears
that the method of model experiments is worth trying.
15.
Summary.I. The power P required to drive a turbine
wheel of diameter D 2it n revolutions per unit time against the
resistance of a homogeneous medium of density
p
and viscosity /x,
when the peripheral speed does not exceed one-half that of soimd,
may be represented by an equation of the general form
in which the form of the unknown function cp depends solely on
the shape of the wheel and its casing.
II. Throughout the practical range of the experimental data,
equation (I) has the simpler form
p^Np'-^n^D^^li^ (II)
the abstract numerical constant N having a value which is deter-
mined solely by the shape of the wheel and casing. All the
reliable data which we have agree with equation (II) or with direct
deductions from it.
III. At low speeds the value of 3 is nearly unity and the resist-
ance is directly proportional to the viscosity of the medium. At
232
Bulletin
of
the Bureau
of
Standards [Voi.io
the speeds at which stationary turbines are usually run, 8 is a
small quantity and we have approximately
P
=
Nfm'D' (III)
A closer approximation is obtained by setting 8
=
o.i whence
IV. For wheels of ordinary shapes, running either in the open
or in casings with fairly large clearances, the "shape coefficient"
A^ may be expressed approximately by the equation
JV=A+b(^J (IV)
in which l/D is the ratio of the blade length to the disk diameter.
The disk coefficient A increases with roughness of the disk; the
blade coefficient B decreases when the clearance round the blades
is decreased, but no more definite statements are warranted.
V. (a) For designing purposes we may first compute the windage
loss by the following equation deduced from Stodola's results
:
P
=
io-^ >^D^[i+59o(0]
(V)
In this equation
P
=
the horsepower dissipated
p
=
the density of the medium, in pounds per cubic foot
w=the speed, in revolutions per minute
D
=
the diameter, in inches, at the root of the blades
/
=
the length of the blades, in inches
The equation is applicable to wheels of ordinary shapes with one
row of shrouded blades, running in the open or in casings which
leave large clearances, in a homogeneous medium such as air or
dry steam.
(b) Reducing the clearances, especially round the blades, reduces
the windage. In some cases the amount of this reduction may be
estimated from Table lo but no general quantitative statement
is possible. The reduction affects mainly the blade term.
(c) Open-ended blades have more resistance than shrouded
blades, to which equation (V) refers, but there are no data to
Buckingham] Windage Losses
of
Steam Turbines
233
show how much. When the radial clearance over the blade tips is
small, the presence or absence of shrouding will have Uttle effect.
(d) A wheel run backward experiences a greater resistance
than the same wheel run forward, i. e., in the normal direction.
When nmning in the open the difference may be considerable,
but if the clearances round the blades are small, the resistance
backward is not much greater than the resistance forward.
(e) Each additional row of blades increases the resistance.
When run in the open, a fotu--row wheel may have two and one-half
times the resistance of a one-row wheel, but there are no adequate
data published. With short blades and fine clearances the effect
of increasing the number of rows will be much less than that
indicated.
(/)
A wheel run in wet steam experiences more resistance
than in dry steam or air of the same density. In Lewicki's experi-
ments the increase was
30
per cent; we have no other informa-
tion on this point.
(g)
Equation (V) gives the power absorbed when the wheel is
driven from without. If the wheel is working in the usual manner
we may reduce the blade term in the ratio of the number of idle
blades to the whole number.
(h) The values given by equation (V) may be too large, espe-
cially for smooth wheels with short blades ; for the disk coefficient
used, viz.: A
= 10-^^,
is larger than the values deduced from
other experiments.
VI. The necessary indefiniteness of many of the statements
made under V is due to lack of experimental data. No formula
based only on our present knowledge can be trusted to give accurate
results, and no formula which has not the general form (II) should
be used for extrapolation beyond the limits of the experiments
from which it was deduced. Equation (V) , if used as indicated,
probably gives safe maximum values.
VII. The method of model experiments is applicable to the
study of the windage losses of steam turbines and might prove very
useful-
by
decreasing some of the difficulties encountered in making
systematic experiments on a large number of full-sized wheels.
Washington,
July 25, 191
3.
234
Bulletin
of
the Bureau
of
Standards vvoi. to
REFERENCES
1. Stodola, Die Dampfturbinen, 4th ed., 1910, pp.
120.
2. Odell, Engineering, 77, p. 30; Jan.
i,
1904.
3.
Osborne Reynolds, Scientific Papers,
2, p. 51;
or Phil. Trans.; March
15, 1883.
4. W. Froude, B. A. Report;
1874.
5.
Zahm, Phil. Mag.
(6), 8, p. 58; 1904
II.
6.
E. Lewicki, Zs. d. Ver. Deutsch, Ingen., 47, p. 492;
Apr.
4, 1903.
7.
Holzwarth, Power, 27, p. 50; Jan. 1907.
8. See Kranz, Lehrb. der Ballistik
1, p. 49,
also Mallock, Proc. Roy. Soc. London,
(A) 79, p. 262; March,
1907.
9. Jude, The Theory of the Steam Turbine, 2nd ed. 1910, p.
221.
10. Jasinsky, Zs. d. Ver. Deutsch. Ingen.,
63, pp. 492, 538; 1909
I.
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