The Story of the HeavensBall, Robert S. (Robert Stawell)
History
The Story of the Heavens
Ball, Robert S. (Robert Stawell)
Astronomy
this explanation. They have minutely studied the observations down to
1891, but only to confirm the reality of this diminution in the periodic
time of Encke's comet.
An explanation of these irregularities was suggested by Encke long ago.
Let us briefly attempt to describe this memorable hypothesis. When we
say that a body will move in an elliptic path around the sun in virtue
of gravitation, it is always assumed that the body has a free course
through space. It is assumed that there is no friction, no air, or other
source of disturbance. But suppose that this assumption should be
incorrect; suppose that there really is some medium pervading space
which offers resistance to the comet in the same way as the air impedes
the flight of a rifle bullet, what effect ought such a medium to
produce? This is the idea which Encke put forward. Even if the greater
part of space be utterly void, so that the path of the filmy and almost
spiritual comet is incapable of feeling resistance, yet in the
neighbourhood of the sun it was supposed that there might be some medium
of excessive tenuity capable of affecting so light a body. It can be
demonstrated that a resisting medium such as we have supposed would
lessen the size of the comet's path, and diminish the periodic time.
This hypothesis has, however, now been abandoned. It has always appeared
strange that no other comet showed the least sign of being retarded by
the assumed resisting medium. But the labours of Backlund have now
proved beyond a doubt that the acceleration of the motion of Encke's
comet is not a constant one, and cannot be accounted for by assuming a
resisting medium distributed round the sun, no matter how we imagine
this medium to be constituted with regard to density at different
distances from the sun. Backlund found that the acceleration was fairly
constant from 1819 to 1858; it commenced to decrease between 1858 and
1862, and continued to diminish till some time between 1868 and 1871,
since which time it has remained fairly constant. He considers that the
acceleration can only be produced by the comet encountering periodically
a swarm of meteors, and if we could only observe the comet during its
motion through the greater part of its orbit we should be able to point
out the locality where this encounter takes place.
Public-domain text, read in full here on John Shaqi.
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