Scientific American Supplement, No. 633, February 18, 1888Various
Science
Scientific American Supplement, No. 633, February 18, 1888
Various
Science -- Periodicals
In Fig. 4 a machine is represented in which the field is external to the
armature.
[Illustration: Fig. 4.]
In Fig. 5 we have a thermo-magnetic generator, which corresponds to the
disk machine in dynamos. Similar parts are indicated by the same letters
in each of these figures, so that no further detailed description is
necessary.
[Illustration: Fig. 5.]
In another modification M. Menges proposes to rotate the burners and
leave the armature and distributor at rest. But in this case it is
evident that the E.M.F. produced would be much less, because the
magnetization of the core would only undergo a variation of intensity,
and would nowhere be reversed, except, perhaps, just in front of the
poles. In machines modeled on the Brush type it is evident that the
distributor need not be continuous.
Enough has, however, been said to indicate the extent of the field upon
which the principle may be applied.--_The Electrician._
* * * * *
OBSERVATIONS ON ATMOSPHERIC ELECTRICITY.[1]
[Footnote 1: Abstract of a paper read before the British
Association meeting at Manchester, September, 1887.]
BY PROF. L. WEBER.
I will try to give a short report of some experiments I have made during
the last year in regard to atmospheric electricity. It was formerly
uncertain whether the electrostatic potential would increase by rising
from the surface of the earth to more elevated region of the atmosphere
or not, and also whether the potential in a normal--that is,
cloudless--state of the atmosphere was always positive or sometimes
negative. Sir William Thomson found by exact methods of measuring that
the increase of the potential with elevation is very important, and
values about 100 volts per meter. That fact is proved by many other
observers, especially lately by Mr. F. Exner, at Vienna, who found an
increase of 60 to 600 volts per meter. The observations were made by
means of an electrometer. In respect of many inconveniences which are
connected with the use of an electrometer, I have tried the measurements
with a very sensitive galvanometer. In this case it is necessary to
apply a separating air exhaust apparatus, for example flame, or a system
of points at the upper end of the conductor, which is elevated in the
atmosphere. In order to get a constant apparatus, I have used 400 of the
finest needles inserted in a metallic ribbon. This system I have raised
in the air by means of a captive balloon, or by a kite, which was
attached to a conductor of twine or to a twisted line of the finest
steel wire. In this way I have attained a height of 100 to 300 meters.
When the lower end of the kite line was communicating with the
galvanometer whose other terminal was in contact with the earth, a
current passed through the galvanometer. For determining the strength of
this current I proposed to called a micro-ampere the 10^{-9} part of an
ampere. At the height of about 100 meters in the average the current
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