G-whizzes disagree over gravity
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By Eugenie Samuel Reich
The Newtonian constant of gravitation -- known in the finely tuned business of metrology as 'big G' -- has come a long way since British physicist Henry Cavendish first measured the gravitational attraction of Earth in 1798. Although G derived from Cavendish's measurements had an uncertainty of about 1%, modern measurements have tightened that to just a couple of tens of parts per million.
But the relentless honing of G may have hit a stumbling block. Two recent experiments are in striking disagreement with earlier findings, and the overall uncertainty in the value of the constant may be set to increase.
In Newton's equations of gravity, G represents the size of the gravitational force. The constant is involved in the quest to unify the theories of gravity and quantum mechanics, and efforts to determine G have contributed to progress in areas of experimental physics: elements of the apparatus first developed to measure the constant, for example, are now used in gravitational-wave detectors. But for some researchers, measuring G is an end in itself. "It's the ultimate precision experiment," says James Faller, a physicist at the University of Colorado at Boulder.
Metrologists have traditionally measured G using a torsion balance -- a rod suspended from a wire. When masses are placed near the ends of the rod, their minute gravitational pull causes it to rotate by an amount proportional to G. In 2000, Jens Gundlach and Stephen Merkowitz at the University of Washington in Seattle used a new torsion-balance method to make the most precise measurement to date: 6.674215 × 10^−11 cubic metres per kilogram per square second, with an uncertainty of 14 parts per million (p.p.m.).
But that value is being challenged by two different methods that have now been developed to a level of precision comparable to Gundlach and Merko witz's. In a paper accepted by Physical Review Letters2, Faller and Harold Parks at Sandia National Laboratories in Albuquerque, New Mexico, used a laser interferometer to measure the displacement of pendulum bobs by various masses. Their result (6.67234 × 10^−11 m3 kg−1 s−2, with an uncertainty of 21 p.p.m.) is an enormous 10 standard deviations lower than the value measured by Gundlach and Merko witz. And in a paper3 published in 2009 in Physical Review Letters, researchers led by Jun Luo of Huazhong University of Science and Technology in Wuhan, China, measured G by comparing the time it took for a torsion pendulum to swing past masses placed at varying distances from it. They obtained a value of 6.67349 × 10^−11 m^3 kg^−1 s^−2, with an uncertainty of 26 p.p.m., about three standard deviations below Gundlach and Merkowitz's value. Metrologists had expected much smaller disagreements among the results -- probably no more than a couple of standard deviations.
Stephan Schlamminger of the University of Washington, who measured G while at the University of Zurich in Switzerland and reported4 a result consistent with that of Gundlach and Merkowitz, says he cannot explain the inconsistency. It may be down to systematic error, which is why it is so important to measure G in a variety of ways, he says. "People are obviously overlooking effects and not taking that into account in their experiments," adds Barry Taylor of the National Institute of Standards and Technology in Gaithersburg, Maryland.
The latest results mean that the Paris-based Committee on Data for Science and Technology (CODATA), which recommends values of physical constants every four years, will probably revise G in its next set of values, finalized in early 2011. "Those new values will pull the value down," says Taylor, who sits on the committee. "The final uncertainty will be the same or larger."
Faller says the fear of being wrong can cause investigators to wait many years before publishing results that don't agree with previous measurements. He and Parks ran their experiment in 2004, and have spent the time since then searching for effects they might have missed. But he's sure their measurement is sound: "I feel like I've checked everything and I have to wash my hands."
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6 Comments
Add CommentAccording to General Relativity, gravity is the effect mass-energy has in curving space-time. Static experiments with torsion balances and pendulums measure the spatial curvature. Perhaps other methods could measure that of time. Are available clocks precise enough measure the time-slowing effect of massive objects at varying distances?
Reply | Report Abuse | Link to thisAtomic clocks are more precise than the measurement of G.
Reply | Report Abuse | Link to thisFrom Wikipedia:
During the 1970s it was realized that gravitational time dilation caused the second produced by each atomic clock to differ depending on its altitude. A uniform second was produced by correcting the output of each atomic clock to mean sea level (the rotating geoid), lengthening the second by about 1 × 10−10. This correction was applied at the beginning of 1977 and formalized in 1980. In relativistic terms, the SI second is defined as the proper time on the rotating geoid.
If gravity constant differs in different experiments, it is maybe due to our error in understanding the gravity and not the problem with the methods of measurements. I would not be surprised if the value of G would differ for different locations of the measurement, time at which the measurement was conducted and orientation relative to the universe.
Reply | Report Abuse | Link to thisBLACK HOLE PUNCTUATION
Reply | Report Abuse | Link to this-- James Ph. Kotsybar
“Amusing,”
thinks God,
”that My weakest force
ironically becomes the strongest.
The meek shall inherit, over due course --
the last become first, the shortest, longest.
“So gravity, most obvious, shall be
the greatest ever unsolved mystery
which, though its effects everyone can see,
can’t be described satisfactorily –
a force that’s both uniform and mundane,
predictable yet able to allude
a simple explanation that sounds sane
of its ever attractive attitude.
“And action at a distance? Let men try
to come to terms with what they most deny.”
This may sound funny, But I do not believe that we are held to this earth as Newton states . we are pressured down by our atmosphere as Einstein stated a 100 years ago . And you can't manipulate something thats not real.
Reply | Report Abuse | Link to thisYou do remember we walked on the moon, don't you? There's no atmosphere there to hold anything down (nor make it buoyant).
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