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Eötvös experiment
The Eötvös experiment was a famous physics experiment that measured the correlation between inertial mass and gravitational mass, demonstrating that the two were one and the same, something that had long been suspected but never demonstrated with any sort of accuracy. The primary experiment was carried out by Roland von Eötvös starting around 1885, with further improvements in a lengthy run between 1906 and 1909. Eötvös' team followed this with a series of similar but more accurate experiments, as well as experiments with different types of materials and in different locations around the Earth, all of which demonstrated the same equivalence in mass. In turn, these experiments led to the modern understanding of the equivalence principle encoded in general relativity, which essentially states that there is no "gravitational mass" at all, and that inertial mass is all that really exists.
Eötvös' original experimental device consisted of two masses on either end of a rod, hung from a thin fiber. A mirror attached to the rod, or fiber, reflected light into a small telescope. Even tiny changes in the rotation of the rod would cause the light beam to be deflected, which would in turn cause a noticeable change when magnified by the telescope.
Two primary forces act on the balanced masses, gravity and the centripetal force due to the rotation of the Earth. The former is calculated by Newton's law of universal gravitation, which depends on gravitational mass. The later is calculated by Newton's laws of motion, and depends on inertial mass. The experiment was arranged so that if the two types of masses were different, the two forces will not exactly cancel, and over time the rod will rotate.
Initial experiments around 1885 demonstrated that there was no apparent difference, and he improved the experiment to demonstrate this with more accuracy. In 1889 he used the device with different types of sample materials to see if there was any change in gravitational force due to materials. This experiment proved that no such change could be measured, to a claimed accuracy of 1 in 20 million. In 1890 he published these results, as well as a measurement of the mass of Gellért Hill in Budapest.[1]
The next year he started work on a modified version of the device, which he called the "horizontal variometer". This modified the basic layout slightly to place one of the two rest masses hanging from the end of the rod on a fiber of its own, as opposed to being attached directly to the end. This allowed it to measure torsion in two dimensions, and in turn, the local horizontal component of g. It was also much more accurate. Now generally referred to as the Eötvös balance, this device is commonly used today in prospecting by searching for local mass concentrations.
Using the new device a series of experiments taking 4000 hours was carried out with Pekár and Fekete starting in 1906. These were first presented at the 16th International Geodesic Conference in London in 1909, raising the accuracy to 1 in 100 million.[2] Eötvös died in 1919, and the complete measurements were only published in 1922 by Pekár and Fekete.
Eötvös also studied similar experiments being carried out by other teams on moving ships, which led to his development of the Eötvös effect to explain the small differences they measured. These were due to the additional accelerative forces due to the motion of the ships in relation to the Earth, an effect that was demonstrated on an additional run carried out on the Black Sea in 1908.
In the 1930's a former student of Eötvös, J. Renner, further improved the results to between 1 in 2 to 5 billion.[3] Robert H. Dicke with P. G. Roll and R. Krotkov reran the experiment much later using improved apparatus and further improved the accuracy to 1 in 100 billion.[4] They also made several observations about the original experiment which suggested that the claimed accuracy was somewhat suspect. Reexamining the data in light of these concerns led to an apparent very slight effect that appeared to suggest that the equivalence principle was not exact, and changed with different types of material.
In the 1980s several new physics theories attempting to combine gravitation and quantum physics suggested that matter and antimatter would be affected slightly differently by gravity. Combined with Dicke's claims there appeared to be a possibility that such a difference could be measured, and this led to a new series of Eötvöstype experiments (as well as timed falls in evacuated columns) that eventually demonstrated no such effect. A sideeffect of these experiments was a reexamination of the original Eötvös data, including detailed studies of the local stratigraphy, the physical layout of the Physics Institute (which Eötvös had personally designed), and even the weather and other effects. The experiment is therefore well recorded.[5]
Loaded Eötvös balance rotor hanging (top) from a tungsten filament 1/4 the diameter of a human hair. All surfaces are gold plated to dissipate static electricity.
Equivalence Principle Tests
Researcher  Year  Method  Difference/Average Sensitivity 
John Philoponus  500 AD?  Drop Tower  "small" 
Simon Stevin  1585  Drop Tower  5x10^{2} 
Galileo Galilei  1590?  Pendulum, Drop Tower  2x10^{2} 
Isaac Newton  1686  Pendulum  10^{3} 
Friedrich Wilhelm Bessel  1832  Pendulum  2x10^{5} 
Southerns  1910  Pendulum  5x10^{6} 
Zeeman  1918  Torsion Balance  3x10^{8} 
Loránd Eötvös  1922  Torsion Balance  5x10^{9} 
Potter  1923  Pendulum  3x10^{6} 
Renner  1935  Torsion Balance  2x10^{9} 
Dicke, Roll, Krotkov  1964  Torsion Balance  3x10^{11} 
Braginsky, Panov  1972  Torsion Balance  10^{12} 
Shapiro  1976  Lunar Laser Ranging  10^{12} 
Keiser, Faller  1981  Fluid Support  4x10^{11} 
Niebauer, et al.  1987  Drop Tower  10^{10} 
Heckel, et al.  1989  Torsion Balance  10^{11} 
Adelberger, et al.  1990  Torsion Balance  10^{12} 
Baeßler, et al.  1999  Torsion Balance  5x10^{13} 
MiniSTEP, MICROSCOPE, Galileo Galilei 
2010?  Satellite Orbit  10^{17}? 
Eötvös experiments are rational inquiries. Noether's theorem: For each continuous symmetry in physics there must be a conserved observable, and viceversa. A list of symmetries (easy) is then a list of fundamental properties (otherwise difficult to identify) to be tested.
Internal symmetries' observables transform fields amongst themselves leaving physical states (translation, rotation) invariant. Internal symmetries' observables are default null results in any Eötvös experiment.
Parity is unique for being absolutely discontinuous, a mirror reflection along each axis. Parity is not a Noetherian symmetry. Covariance with respect to reflection in space and time is not required by the Poincaré group of Special Relativity or the Einstein group of General Relativity. Parity Eötvös experiment net output may be observed without contradicting orthodox theory or prior observations in any venue at any scale.
Class  Invariance  Conserved quantity 
Proper orthochronous Lorentz symmetry 
translation in time (homogeneity) 
energy 
translation in space (homogeneity) 
linear momentum  
rotation in space (isotropy) 
angular momentum  
Discrete symmetry  P, coordinates' inversion  spatial parity 
C, charge conjugation  charge parity  
T, time reversal  time parity  
CPT  product of parities  
Internal symmetry
(independent of 
U(1) gauge transformation  electric charge 
U(1) gauge transformation  lepton generation number  
U(1) gauge transformation  hypercharge  
U(1)_{Y} gauge transformation  weak hypercharge  
U(2) [U(1)xSU(2)]  electroweak force  
SU(2) gauge transformation  isospin  
SU(2)_{L} gauge transformation  weak isospin  
PxSU(2)  Gparity  
SU(3) "winding number"  baryon number  
SU(3) gauge transformation  quark color  
SU(3) (approximate)  quark flavor  
S((U2)xU(3)) [U(1)xSU(2)xSU(3)] 
Standard Model 
Berylliummagnesium and berylliumtitanium test mass contrasts respectively give 0.1919% and 0.2398% difference/average nuclear binding energies. These are among the largest net active mass composition Eötvös experiments possible. 420+ years of Equivalence Principle tests have given zero net output within experimental error. The largest possible amplitude Eötvös experiment is a parity Eötvös experiment  assay of spacetime geometry with test mass geometry.
Test Masses' Divergent Property  Fraction of Rest Mass 
rest mass 
100%

crystal lattice geometric parity 
99.9726%^{a} alphaQuartz 99.9771%^{a} Cinnabar 
nuclear binding energy (low Z)  00.76% (^{4}He) 
neutron versus proton mass  00.14% 
electrostatic nuclear repulsion  00.06% 
electron mass  00.03% 
unpaired spin mass  00.005% (^{55}Mn^{b}) 
nuclear antiparticle exchange  00.00001% 
Weak Force interactions  00.0000001% 
Gravitational binding energy, Nordtvedt effect and lunar laser ranging 
00.000000046% Earth^{c} 00.0000000019% Moon 
^{a}(nuclear mass)/(atomic mass), corrected for isotopic abundance
_{b}globally aligned undecatiplet
^{c}iron core rather than homogeneous body
Chemically identical, opposite parity mass distributions have never been tested in an Eötvös experiment. Do metaphoric left and right shoes vacuum free fall along identical trajectories? A parity Eötvös experiment opposes crystallographic opposite parity space groups P3121 (righthanded screw axes) and P2221 (lefthanded screw axes) cultured alphaquartz (average atomic weight = 20.03) or cinnabar (average atomic weight = 116.33) solid single crystal spheres or other solid shapes with all identical moments of inertia (no directional bias).
General relativity (postulated) and string theory (BRST invariance demanded) require parity Eötvös experiment zero net output. Affine (EinsteinCartan theory), teleparallelism (Weitzenböck), and noncommutative (Connes) gravitation theories predict measurable parity Eötvös experiment output. If the vacuum is reproducibly demonstrated to contain a chiral anisotropic background then angular momentum need not be conserved for opposite parity mass distributions (Noether's theorem). Lorentz invariance would be broken. Somebody should look.
References
1. ^ R. v. Eötvös, Mathematische und Naturwissenschaftliche Berichte aus Ungarn, 8, 65, 1890
2. ^ R. v. Eötvös, in Verhandlungen der 16 Allgemeinen Konferenz der Internationalen Erdmessung, G. Reiner, Berlin, 319,1910
3. ^ J. Renner, Matematikai és Természettudományi Értesítõ, 13, 542, 1935, with abstract in German
4. ^ P. G. Roll, R. Krotkov, R. H. Dicke, Annals of Physics, 26, 442, 1964.
5. ^ One Hundred Years of the Eötvös Experiment
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