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by Richard Milton
2007
Ether --- a null result, or an anulled result?
The story of ether, or aether,
is familiar to anyone who has studied the history of science and the seminal
tale from the heroic age of physics of the Michelson-Morley experiment to
establish whether or not light travels through a mysterious medium that
fills space -- the ether. Every high school physics student has taken
down the same notes for more than a century:
1880.
US physicist Albert Michelson invents the Michelson light interferometer --
an instrument that can measure the velocity of a beam of light with great
accuracy by splitting it through a half-silvered mirror and then
re-combining the beams. If the recombined beams interfere with reach other,
causing visible fringes on a screen, then one of them must have been
delayed.
1887.
Michelson and fellow American scientist Edward Morley build an
interferometer with greater accuracy than ever before and use their
instrument in a crucial experiment to determine whether light travels
through the ether, or merely through the vacuum of empty space. The two
physicists set up their instrument to measure the speed of a beam of light
travelling in the same direction as the earth through space, and also a beam
that travels at right angles to the earth’s direction of travel. If the
ether exists there should be a minute – but measurable – drag effect on a
beam of light that will delay it and show up as ‘interference fringes’ in
the interferometer. The experiment shows a 'null result' -- no matter how
the interferometer is orientated with respect to the earth's movement, there
is no measurable ether drag.
1905 - 1915.
This experimental finding throws physics into a quandary for a decade or
more until Albert Einstein comes to the rescue with his Theory of
Relativity. The ether does not exist, says Einstein, and light travels at
constant velocity regardless of the speed of its source. These findings and
the ideas of relativity become the foundation stones of physics in the
twentieth century and are universally accepted.
These are the notes
taken by generations of students. But, as Michelson and Morley’s experiment
affected theoretical physics more than
perhaps any experiments since Galileo
and Newton, then one might expect its results to have been analysed with the
utmost care and the experiment itself to have been replicated many times,
establishing the 'null' result.
Strangely, the real facts of
the Michelson Morley experiment are the very opposite of this oft-told
seminal tale. Michelson and Morley did not in fact obtain a null result in
their original experiment. They found a small, anomalous deviation from the
expected value, but this finding was simply forgotten about. Few attempts
have been made to replicate the experiment itself but several of them have
also found experimental evidence for an ether.
Most extraordinary of all is the series of experiments
carried out over a 30 year period by Dayton Miller, from 1906 to the mid
1930s, using far more accurate apparatus than Michelson and Morley and which
clearly and consistently showed an ether drift effect. But these results
contradicted Einstein and Relativity, so they were first ignored and later,
after Miller’s death, made the subject of a campaign of denigration.
The experiments of Michelson
and Morley and of Dayton Miller, have been repeated and analysed in modern
times by French engineer Maurice Allais, who was awarded the Nobel Prize for
Economic Science in 1988. It is primarily due to the work of Allais that
Miller's discoveries have been brought to a modern audience.
For further details see Allais website here. The story of Dayton Miller
and what happened to his findings has also been researched and told in
considerable detail by Dr James De Meo, Director of the Orgone Biophysical
Research Lab.
His research paper can be found here.
Albert Michelson
became professor of physics at the newly-founded Case School of Applied
Science in Cleveland, Ohio, in 1882. Here he met Edward Morley who was
professor of chemistry at the neighbouring Western Reserve University.
(Today, the two institutions are combined as Case Western University).
Morley had several ideas for improving the Michelson Interferometer and in
1887 a new instrument was built in the basement of Western Reserve's
Adelbert College in Cleveland. The instrument consisted of a 1.5 meter
square block of sandstone on which was mounted the optical apparatus. The
stone block rested on a wooden disk floating on mercury in a cast iron
tank. This made it possible to rotate the instrument through 360 degrees
with virtually no vibration. At each end of the arms of the apparatus were
four mirrors to reflect the light beam back and forth repeatedly, thus
effectively extending the path length for the beam to a total of 11 meters.
If the theory of a stationary
ether through which the earth moved were correct, then pointing one arm of
the apparatus in the direction of the earth's travel through space would
produce a displacement of the observed pattern of interference fringes
amounting to 0.4 of a fringe width. The apparatus was sensitive enough to
detect a displacement much smaller than this amount.
Michelson and Morley made
observations with the instrument for one hour at noon
on 8, 9 and 11 July 1887 and one hour in the evenings of 8, 9 and 12 July --
six hours in all. In each session, the instrument was gradually turned
through 36 rotations, readings being taken at every sixteenth of a turn.
Today, whenever and wherever the results of these six days of observations
are reported -- whether in the popular press or professional scientific
paper -- it is confidently said that the Michelson-Morley experiment
produced a null result.

The real facts were given in
1933 by Dayton C Miller who wrote, "The
indicated effect was not zero; the sensitivity of the apparatus was such
that the conclusions, published in 1887, stated that the observed relative
motion of the earth and ether did not exceed one fourth of the earth's
orbital velocity. This is quite different from a null effect now so
frequently imputed to this experiment by writers on relativity." (The
italics emphasis is Miller's.)
If these words had been written
by a disgruntled amateur, they would merit little attention. However,
Dayton Miller (1866-1941) was a physics graduate from Princeton University,
President of the American Physical Society and Acoustical Society of
America, Chairman of the Division of Physical Sciences of the National
Research Council, Chairman of the Physics Department of Case School of
Applied Science (today Case Western Reserve University), and a Member of the
National Academy of Sciences. Even more significantly, from 1902 onwards
Miller began experiments with Edward Morley using more accurate instruments
and whose own more accurate results clearly show an ether drift effect.
If these words had been written
by a disgruntled amateur, they would merit little attention. However,
Dayton Miller (1866-1941) was a physics graduate from Princeton University,
President of the American Physical Society and Acoustical Society of
America, Chairman of the Division of Physical Sciences of the National
Research Council, Chairman of the Physics Department of Case School of
Applied Science (today Case Western Reserve University), and a Member of the
National Academy of Sciences. Even more significantly, from 1902 onwards
Miller began experiments with Edward Morley using more accurate instruments
and whose own more accurate results clearly show an ether drift effect.
How on earth did the 'null
result' story come about? In their paper of 1887, Michelson and Morley made
an important qualification. 'In what precedes, only the orbital motion of
the earth is considered. If this is combined with the motion of the solar
system, concerning which but little is known with certainty, the result
would have to be modified; and it is just possible that the resultant
velocity at the time of observations was small though the chances are much
against it. The experiment will therefore be repeated at intervals of three
months, and thus all uncertainty will be avoided.'
Unfortunately, this repetition (which later was to prove to be very
important) was never carried out.
In 1889, Michelson left the Case School, first for Clark
University and then for University of Chicago where he remained for 38
years. After 1889, Michelson's interferometry work centred on determining
the unit of [standard] length for which he became world famous.
In the meantime, Einstein had
published his Special Theory of Relativity in 1905, followed by his General
Theory of Relativity in 1915. His theory, which quickly attained widespread
currency and a wide measure of support made two key assumptions; first that
the speed of light is constant, regardless of the speed of the source, and
second, that there is no ether at absolute rest with respect to moving
objects such as the earth. This second assumption is crucial. It requires
that the results of the Michelson-Morley experiment show a NULL result --
that there is absolutely NO difference in the passage of a light beam
whatever its orientation with regard to the earth's motion.
And it is from around this time that people began to speak of a 'null'
result for Michelson-Morley.

Back at Case, Edward Morley and
Dayton Miller continued the ether drift experiments. A new instrument was
constructed using steel girders with arms 4.3 meters long giving a light
path that was effectively 32 meters long -- considerably longer and more
accurate than that of the 1887 experiments. In 1905, the new interferometer
was moved to an unobstructed site on a hill in Cleveland Heights.
Miller's reason for wanting a high point is important. If the ether exists,
some of it may be carried along with the earth as it moves through it, in
the same way that some air is carried along with an aircraft's wing. This
effect, named 'entrainment' could reduce the relative movement by an unknown
amount at ground level -- perhaps a significant amount. If entrainment
occurred then a high point and no obstructions should reduce its effects.
Miller thus wished to avoid concrete basements and dense covering materials
which might affect his readings. On Cleveland Heights
some 230 observations were made in July, October and November 1905. These
showed a very definite positive displacement of fringes corresponding with
the instrument being pointed in certain directions, but again too small to
be reconciled with the ether theory.
For mainly funding reasons, research slowed and halted for a decade or more.
In 1919, an astronomical
expedition to Equatorial Africa made observations of light from a star
occulted by the sun during a total eclipse. The photographs appeared to
shown bending of the starlight around the sun as predicted by Einstein and
relativity theory thus received a major publicity boost, with words like
'scientific confirmation' appearing in daily newspapers.
Because it had now become
central to progress in physics, Miller returned to experiments with the
ether drift in 1921. Albert Einstein visited Miller at Case on 25 May 1921
and urged him to undertake further experiments. The same year, the
Morley-Miller interferometer was transported across the continent to Mount Wilson
observatory and set up at high altitude (1,750 meters above sea level). 67
sets of observations were taken which produced a positive experimental
effect corresponding to a movement of earth relative to the ether of 10 kilometers per second.
The apparatus was returned to Cleveland and the experiments
repeated again between 1922 and 1924 with the same results.
Again in 1925 and 1926,
unobstructed observations were made at high altitude at Mount Wilson. This time,
Miller had a brainwave. All previous observations had been made based on
the assumption that the earth's velocity through the ether was known -- that
it was the resultant of the earth's orbital movement around the sun and the
motion of the solar system towards the constellation Hercules. But what if
we take the interferometer readings at face value -- as telling us the
actual motion of the earth?
During 1925-26 an enormous
number of new readings were taken and computed resulting in some 250,000
observations. Miller presented the results of analysing this mass of data
to a conference in February 1927. The point on the celestial sphere towards
which the earth moves through its absolute motion is named its apex of
motion. Based on the mass of data accumulated, Miller announced to the
conference that he had calculated the earth's apex of motion as lying in the
northern celestial hemisphere at Right Ascension 17 hours and Declination
+68 degrees.
In 1932, Miller revisited the
calculations to consider the possibility that he had correctly calculated
the axis of the earth's movement through space but had got the wrong
direction. His recalculation suggested that an apex of movement in the
southern celestial hemisphere was more probable and was finally determined
to lie at Right Ascension 4 hours 54 minutes and Declination -70 degrees 33
minutes, in the constellation of Dorado (the Swordfish). Moreover, Miller
devised a technique that enabled him to estimate the absolute velocity of
the earth's motion as being some 208 kilometers per second. He was also able to determine from
the data that the disc of the solar system was tilted up almost at right
angles against the direction of motion. He wrote,
'This suggests that the solar
system might be thought of as a dynamic disc that is being pulled through a
resisting medium, and which therefore sets itself perpendicular to the line
of motion.'
A number of other attempts were
made to replicate Miller's findings, some with small positive readings, some
with close to zero. These included an experiment by R J Kennedy in 1926 on
Mount Wilson with the interferometer sealed in helium; an interferometer sealed in a vacuum casing and sent up by balloon to 2,500
meters in 1927; and an interferometer mounted inside a
temperature-constant vault at Mount Wilson by Michelson himself in 1929.
Displacements in each case were almost zero. However, Miller noted
that in each case the instrument was enclosed in metal casings or in a
basement room. He believed that such "opaque" shielding nullified the
experimental effect. [The source of the problem was not the metal casing but
the mere fact that the light was travelling through a vacuum or near-vacuum.
-CR]
Until his death in 1941,
Miller's findings remained uncomfortably in the scientific background --
impossible to refute, equally impossible to accept, since they fatally
undermined Einstein's Relativity which by now had become universally
accepted in physics. After Miller's death his former student Robert S.
Shankland, became Chairman of the Physics Department at Case Western Reserve
University. According to James de Meo, 'Shankland's academic career soared
after he organized a post-mortem on Miller's work, pronouncing it worthless,
and after Einstein later granted him a series of widely-published
interviews. Shankland subsequently became a bureaucrat within the emerging
atomic energy infrastructure. Intimate with Einstein, in a 1981 interview
Shankland claimed Miller's work on ether-drift had probably cost Einstein
the Nobel Prize for relativity theory (Einstein did later get a Nobel Prize,
but for his other theoretical work).'
Shankland and three other
authors published a paper in 1955 which, on the surface, was a critical
review and re-analysis of Miller's long and painstaking observations. In
reality, there was no review and no re-analysis; simply a trawl through the
data looking for possible sources of error. Moreover, neither Shankland nor
his fellow authors actually did any of the work on which the paper was
based. Instead this was left to one of Shankland's students who received no
credit beyond a footnote. The 1955 Shankland paper begins with the
statement that has been repeated so often since, that Michelson and Morley
obtained a "null" result. The paper also claimed that "All trials of this
experiment except those carried out at Mount Wilson by Dayton C. Miller
yielded a null result within the accuracy of the observations."
Says James de Meo, 'This kind
of chronic misrepresentation of the slight positive results of many
interferometer experimenters, including Michelson-Morley, Morley-Miller,
Sagnac, Michelson-Gale, and Michelson-Pease-Pearson, suggests an extreme
bias and deliberate misrepresentation. The fact that this is a very popular
bias does not excuse it. By redefining all the positive results observed by
what may in fact have been the majority of ether-drift researchers, as mere
expressions of "observational inaccuracy", Shankland narrowed his task
considerably'
In the end, Shankland and his
team settled on the notion of seasonal temperature variations as being
responsible for Miller's findings. There was no longer anyone alive to
point out how fatuous this explanation is and Miller's data was safely
interred along with his body. As far as orthodox science is concerned today,
relativity is universally accepted and the ether controversy is dead and
buried.
A curious footnote
James de
Meo points out a curious semantic footnote to this affair. The name for the
hypothetical medium through which light was thought to travel has been
spelled in two ways: as 'ether' and also as 'aether'. In late medieval
times when the word was coined it was spelled aether. In the period
1850-1920 when the topic was current in physics and used regularly by
physicists such as Sir Oliver Lodge, Michael Faraday, Nicola Tesla,
Michelson and Morley, and even by Einstein, the term was spelled 'ether'.
In the 1950s, after Miller's death, when a concerted effort was being made
to denigrate his work, the medieval 'aether' spelling suddenly re-appeared.
On the face of it, the use of this spelling was to avoid confusion with the
anaesthetic fluid ether. But it also appears to have been part of an
attempt to “relegate the ether of space into ancient history, as an unproven
speculation similar to Aristotelian elements of ‘fire, air, water and
earth’.”
* * *
(The above article by Richard
Milton appears on the Cellular Universe website
with the generous consent of its author. The
original was published on the Alternative Science website at
www.alternativescience.com, which is now inactive.)
Back to: The Aether Experiments and the
Impact on Cosmology
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