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Heat of fusion of ice. A revision, Lecture notes of Literature

The results of measurements of the heat of fusion of ice made at the National. Bureau of Standards and published in 1913 and 1915 have been revised by one.

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U.
S.
DEPARTMENT
OF
COMMERCE
NATIONAL
BUREAU
OF
STANDARDS
RESEARCH PAPER RP1260
Part
of
Journal
of
Research
of
the N.ational Bureau
of
Standards,
Volume
23,
December 1939
HEAT
OF
FUSION
OF
ICE.
A
REVISION
By
Nathan
S.
Osborne
ABSTRACT
The
results
of
measurements
of
the
heat
of fusion of ice
made
at
the
National
Bureau
of
Standards
and
published
in
1
913
and
1915
have
been revised
by
one
of
the
original experimenters, usng
more
recent
data
for
the
heat
capacity
of
water, which
is
involved in
the
calculations.
The
revised value,
obtained
by
weighting
the
results of four
independent
series of
measurements
and
expressed
in
terms
of
the
present
calorimetric
unit
of energy, is
333.5
INTERNATIONAL
JOULES
PER
GRAM
with
an
estimated
uncertainty
of 0.2 into j/g.
The
heat
of fusion of ice was determined
at
the National
Bureau
of Standards
about
twenty-five years ago
[1,
2]1.
The
reductions of
the
observations involved the
heat
capacity of water, for which the
values used were chosen from the
data
then
available. Since more
accurate values for
the
heat
capacity of
water
are now
ava
ilable
[3],
the values for
the
heat
of fusion of i
ce
are subject to revision.
It
has
been suggested
that
such a revision, having the benefit of the
inter-
pretation
of
the
experimenters themselves, would be helpful
by
com-
bining all of the results into a single definitive value expressed in
terms of the present calorimetric
unit
of energy, the international
joule.
The
value of
heat
capacity of water does
not
enter as a direct factor
but
affects
parts
of
the
calorimetric process depending on which one
of
the
several methods was used
in
the two original investigations
[1,
2].
This work was done
at
a time when
it
was
not
fully appre-
ciated
that
the use of calories as
heat
units
would complicate
not
only
the
original reductions
but
future revisions as well.
For
this reason
the following description of
the
revisions is likely
to
appear
compli-
cated.
In
these two investigations three essentially different methods were
used.
In
the
first investigation, published in 1913, a calorimeter with
stirred
water
as the calorimetric medium was used. A controlled
jacket permitted
heat
le
ak
to be accounted for. Two series of meas-
urements were made
by
the electric-heating method
and
one series by
the method of mixtures.
The
samples of ice were precooled, so
that
initia.l temperatures were lmown and accolmted for
in
the
reductions.
The
corrections which can be made now
to
the
data
as assembled
in
tables 3 and 5 of the original paper
[1]
are
to
reevaluate
the
heat
supplied to bring
the
ice to C
and
to bring the water formed from
C to
the
final temperatures of the various experiments.
1 Figures in brackets indicate the literature references
at
the end of
th
is
paper. 643
pf3
pf4

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U. S. DEPARTMENT OF COMMERCE NATIONAL BUREAU OF STANDARDS

RESEARCH PAPER RP

Part of Journal of Research of the N.ational Bureau of Standards, Volume 23, December 1939

HEAT OF FUSION OF ICE. A REVISION

By Nathan S. Osborne

ABSTRACT The results of measurements of the heat of fusion of ice made at the National Bureau of Standards and published in 1 913 and 1915 have been revised by one of the original experimenters, usng more recent data for the heat capacity of water, which is involved in the calculations. The revised value, obtained by weighting the results of four independent series of measurements and expressed in terms of the present calorimetric unit of energy, is

333.5 INTERNATIONAL JOULES PER GRAM

with an estimated uncertainty of 0.2 into j/g.

The heat of fusion of ice was determined at the National Bureau of Standards about twenty-five years ago [1, 2]1. The reductions of the observations involved the heat capacity of water, for which the values used were chosen from the data then available. Since more accurate values for the heat capacity of water are now ava ilable [3], the values for the heat of fusion of i ce are subject to revision. It has been suggested that such a revision, having the benefit of the inter- pretation of the experimenters themselves, would be helpful by com- bining all of the results into a single definitive value expressed in terms of the present calorimetric unit of energy, the international joule. The value of heat capacity of water does not enter as a direct factor but affects parts of the calorimetric process depending on which one of the several methods was used in the two original investigations [1, 2]. This work was done at a time when it was not fully appre- ciated that the use of calories as heat units would complicate not only the original reductions but future revisions as well. For this reason the following description of the revisions is likely to appear compli- cated. In these two investigations three essentially different methods were used. In the first investigation, published in 1913, a calorimeter with stirred water as the calorimetric medium was used. A controlled jacket permitted heat le ak to be accounted for. Two series of meas- urements were made by the electric-heating method and one series by the method of mixtures. The samples of ice were precooled, so that initia.l temperatures were lmown and accolmted for in the reductions. The corrections which can be made now to the data as assembled in tables 3 and 5 of the original paper [1] are to reevaluate the heat supplied to bring the ice to 0° C and to bring the water formed from 0° C to the final temperatures of the various experiments.

1 Figures in brackets indicate the literature references at the end of th is paper. 643

~~-- -- -------

644 Journal oj Reseal'ch oj the National Bureau oj Standards [Vol. IS

For the ice correction a tentative value of 0.52 cal/g-O 0 was taken

at the time as an approximation to the specific heat of ice in the range from 0° to -3.78° O. In the second investigation, published in 1915 [2], the heat capacity of ice was measured in international joules per gram degree and was finally expressed by the equation

01'=0 .5057 +0.001863t cal20/g_0 0,

where 01' is specific heat at l-atm pressure, t is centigrade tempera- ture, and the calorie2o was taken as equal to 4.183 into j. For use in the present revision, this equation is now converted back to inter- national joules thus

O1'=2.1153+0.00n9t into j/g_O O.

For recomputing the water correction, the table given in a recent publication by Osborne, Stimson, and Ginnings [3] is used (table 6, page 238). The heat supplied in these two series by the electric method was furnished by current in an electric-heating coil, and was measured by use of a potentiometer, a standard cell, and a standard resistor, thus obtaining the power, which, with the observed time, gave the heat added in international joules. This energy per gram of ice as origi- nally corrected for heat leak, temperature change of calorimeter, stirring energy, and heat capacity of the ice holder is given in column 2 of tables 1 and 2, expressed in a nominal 15-degree calorie of 4. into j. In column 3 these data are converted back to international joules per gram. The heat per gram absorbed by the melted ice, as revised by the new heat-capacity data, is given in column 4, and the

heat absorbed by the ice from the .initial temperature to 0° 0 is given

in column 5. The corrections of -1.52 and -7.94 into jig for -0.72° and -3.78°, respectively, in tables 1 and 2 are next applied giving the final values for heat of fusion in column 6.

TABLE I.-Revision of table 3 (1913)

Final tem- (^) Ice at -0 .72 to water at t, Water 0 to Ice at -0 .72 Ice at 0 to perature, t, t, to water at 0 water at 0

°C call1lu^ Int.^ ilu^ Int.Jlu^ Int.Jlu^ Int.Jlu 15.12 95.15 398 .39 63.57 334 .82 333. 14.83 94.92 397.43 62.36 335.07 333. 14.60 94.67 396.38 61.40 334.98 333. 15.79 95.88 401. 45 66. 37 335.08 333. 15.59 95.67 400.57 65 .54 335.03 333. 14.89 94. 97 397.64 62. 61 335.03 333. 14.87 94. 96 397.60 62.53 335.07 333.

  1. 96 94.98 397.68 62.90 334.78 333. 23.81 103.91 435.07 99.91 335.16 333. 23.67 103.75 434.40 99.32 335.08 333. 15.53 95.

I

400.28 65. 29 334.99 333. 15.76 95.81 401.16 66.25 334.91 333. 15 .65 95.72 400.78 65.79 334.99 333. --~-~ Mean of group 11 _____________________________________________ __ _ (^) 333.

  • In obtaining the final mean, this value was given a weight ot 4.

646 Journal of Research of the National Bureau of Standards [Vol. £

ties given by H. L. Callendar [4] in 1912. These values, as originally given, with corrections applied for heat leak, stirring energy, etc., are shown in column 3 of table 3. In column 4 the ratio is shown of the heat capacity of water according to t.he new NBS data to the heat capacity given by Callendar, at the mean temperature of th e experi- ment, both in 15-degree calories. These factors are applied to the figures in column 3, giving the figures in column 5, which are then converted in column 6 to inter- national joules per gram by use of the equivalent from the NBS

data, i. e., the heat capacity at 15° C is equal to 4.1850 into j/g_oC.

The remainder of the revision is similar to that of table 1. In connection with the later investigation [2], three measurements of heat of fusion were made in the electrically heated heavy-copper calorimeter (aneroid). The main revision of these calcula,tions is th e revaluation of the heat taken up by the water from 0° C to t 2. The old and new values for the entire mass of water are given in columns 3 and 4 of table 4 and their differences in column 5. The correspond- ing corrections per unit mass of ice are given in column 7. The correc- tions for premelting of part of the ice, as determined in the specific- heat measurements, are given in column 8. The sum of the two corrections is applied to the original value, as given in column 9, taken directly from column 15 of the original publication. The revised values are found in column 10. In order to deduce a single figure for the heat of fusion representing an interpretation of the entire amount of experimental data, some relative weighting of experiments or groups must be adopted. This is an arbitrary choice, based on the combined judgment of two of the original authors. Each of the first three groups of measurem ents in the first investigation is taken as an independent lmit with a relative weight of 4. In the second investigation the first two experiments are each given a weight of one and the last a weight of two. According to this weighting, the general weighted mean is 333.48 into jjg. The revised figure can therefore be taken as 333.5 into jjg, with an uncertainty of 0.2 int. jjg, which has been estimated to include both accidental and systematic errors.

[1] D. R. Harper 3d, and N. S. Osborne, Latent heat of fusion of ice, H. C. Dickin- son, Bul. BS 10, 235 (1914) S209. [2] H. C. Dickinson and N. S. Osborne, Specific heat and heat of fusion of ice, Bul. BS 12, 49 (1915-16) S 248. [3] Nathan '-8. Osborne, Harold F. Stimson, and Defoe C. Ginnings, Measure- ments of heat capacity and heat of vaporization of water in the range 0° to 100° C, J. Research NBS 23, 197 (1939) RP1228. [4] H. L. Callendar, On the va riation of the specific he at of water with experiments by a new method. Phil. Trans. Roy. Soc. (London) [AJ 212, 1 (1912).

WASHINGTON, October 17, 1939.