Sounding the Ocean of Air: Being Six Lectures Delivered Before the Lowell Institute of Boston, in December 1898Rotch, Abbott Lawrence
Science
Sounding the Ocean of Air: Being Six Lectures Delivered Before the Lowell Institute of Boston, in December 1898
Rotch, Abbott Lawrence
Atmosphere; Balloons; Clouds; Kites (Meteorology)
Having determined that balloons inflated with one hundred and fifty
cubic feet of coal-gas would rise to great heights, simple and light
registering instruments, as well as the postal cards, were attached to
them. As the pressure diminished, an aneroid barometer traced a line
on a smoked glass, and after the descent was placed under the receiver
of an air-pump, and the pressure required to reproduce the trace was
measured by a manometer. From this the height could be computed
approximately. The maximum and minimum thermometer was of the
well-known U-form, and instructions appended asked that it be read as
soon as found. A slow-match was arranged to detach postal cards
successively, so that if they were found and mailed, the track of the
balloon could be determined. These balloons at first were called
_ballons perdus_, or lost balloons, but when it was known that most of
the fourteen balloons liberated from Paris were recovered, the name
_ballons explorateurs_ was given, which was afterwards changed to
_ballons-sondes_, or sounding balloons. The Germans call them,
_Registrir-Ballons_, and in English they have been designated unmanned
balloons also. One of these paper balloons having reached a height of
nearly 30,000 feet, MM. Hermite and BesanÁon proceeded to construct a
balloon of gold-beater's skin, having a capacity of 3960 cubic feet,
in order to carry a better instrumental equipment. The self-recording
instruments made by the French firm of Richard Brothers were well
adapted for this purpose, and a combined barometer and thermometer,
registering in ink on an upright drum that is turned by clockwork
inside, is shown in Fig. 5. The exhausted pair of boxes B of the
barometer actuates the lower pen, while the curved tube C, which is
filled with alcohol, by its change of shape moves the upper pen and
records the temperature. From the indications of the barometer and the
temperature of the mass of air, it is possible by Laplace's formula to
calculate the height at any hour of the registration. The balloon
mentioned was the first of the so-called _AÈrophiles_, and when
inflated with coal-gas it could lift seventy-seven pounds besides its
own weight of forty pounds. It carried two of the baro-thermographs
described, and a package of information cards arranged to be detached
by a slow-match. To mitigate the shock of striking the ground one of
the instruments was hung by rubber cords inside a wicker basket that
in the first ascent was not screened from the sun. It was decided to
liberate these balloons entirely filled with gas (instead of partly
full, to allow for its expansion), and to utilize all possible
ascensional force at first rather than to weight the balloon with an
automatic discharger of ballast (Fig. 6). The trial of the _AÈrophile_
occurred March 21, 1893, and the next day one of the cards was
returned announcing its fall in the department of the Yonne, where the
balloon and the instruments were recovered injured. From the blurred
Public-domain text, read in full here on John Shaqi.
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