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The determination of atmospheric pressure and its influence on analytical weighings
The demands in respect to the accuracy of analytical and especially of micro-analytical weighings
are often extreme. Even though the accuracy required for the end result is usually only 1 %, the
requirement of a much higher accuracy is conditioned by the necessity of also having to weigh the
mass of the tare which often exceeds to a considerable degree that of the proper sample.
In Order to improve accuracy, it is necessary to systematically eliminate all sources of errors. One
of the most critical factors in this respect is the elimination of the influence of the air buoyancy. To
what extent it may be necessary to take this factor into account, depends — aside from the
required tolerances - on the specific weight of the sample in relation to that of the weights used.
Felgentraeger1) in “Feine Waagen, Waegungen und Gewichte" draws attention to the fact that
most chemists either are not aware of the significance of air buoyancy or fall to do anything about it
because the procedure seems too complicated.
The tables provided by that author furnish the necessary information for all respective calculations
up to the most exacting requirements. Lately, H. Ulbricht has published two papers on the
significance of air buoyancy2). These publications give information only on the importance of air
buoyancy without furnishing data on how to determine it. It is exactly this point, however, which
causes difficulties.
The tables found in Kohlrausch and D'Ans/Lax3) can be used only for a coarse reduction of mass
relative to vacuum at normal air pressures. They cannot be used for determining changes in
buoyancy caused by variations of atmospheric pressure.
This paper presents an attempt at furnishing to the chemist information which will enable him in a
simple manner to determine atmospheric pressure and to use this information for analytical
weighings. lt is hoped that in this way a contribution is being made towards the full utilization of the
inherent accuracy of modern analytical balances by those who need it.
One must first distinguish between the determination of the absolute mass i.e. the reduction of the
found values to vacuum atmosphere and the determination of the influence of changes of air
buoyancy. The latter are significant also in „relative" weighings.
Usually, only the second case will be of practical interest. Since the required corrections in this
case amount to only 1/10th of those required in the first instance, it may, sometimes, be
unnecessary to apply these corrections at all. This does not mean that one should not be aware of
the magnitude of correction and consider the questions of its application.