1995
DOI: 10.1103/physrevd.51.4005
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Determination of the gravitational constant with a lake experiment: New constraints for non-Newtonian gravity

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Cited by 27 publications
(17 citation statements)
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“…It is based on a beam balance which is a suitable device for measuring the gravitational force [12]. The idea of this experiment and the experience on how to operate the balance is based on our successful storage lake experiment, where the gravitational force of water has been measured in order to test Newton's inverse-square law [13,14]. This new experiment is a modern variation of the method used by von Jolly [5] and Richarz and Krigar-Menzel [6].…”
Section: (Received 19 August 1997)mentioning
confidence: 99%
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“…It is based on a beam balance which is a suitable device for measuring the gravitational force [12]. The idea of this experiment and the experience on how to operate the balance is based on our successful storage lake experiment, where the gravitational force of water has been measured in order to test Newton's inverse-square law [13,14]. This new experiment is a modern variation of the method used by von Jolly [5] and Richarz and Krigar-Menzel [6].…”
Section: (Received 19 August 1997)mentioning
confidence: 99%
“…The balance and the basic weighting technique is discussed in more detail in Refs. [12][13][14][15][16], for example.…”
Section: (Received 19 August 1997)mentioning
confidence: 99%
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“…5 As the accuracy of lunar laser ranging improves, one can expect this limit on M dm to improve. Added Note Gary Gibbons [16] has pointed out that if one assumes that there is no dark matter bound to the earth, then the comparison of GM ⊕ as determined by LAGEOS, with that determined by lunar ranging, gives a bound on possible non-Newtonian modifications to the gravitational force, and he has alerted me to several references [17], [18], [19] where the use of satellite orbits to restrict non-Newtonian force models has been discussed. To illustrate with the numbers employed above in the dark matter discussion, if one assumes G = G far for the G value relevant both for lunar ranging and for the asteroid determination of the earth to moon mass ratio, and G = G near for the G value relevant for the LAGEOS orbit, and takes M dm = 0, then one has 4 The LAGEOS orbit is usually described in terms of its altitude of 5, 900 km above the earth's surface, which lies about 6, 400 km from the earth's center.…”
mentioning
confidence: 99%
“…Fujii pointed out (Fujii 1971) that the addition of a Yukawa-type potential to the conventional gravitational potential, forming modified Newtonian gravitational potential, can describe the phenomenon of non-Newtonian gravity. Also, some scientists have referred to it as a new fundamental intermediate-range force (Hubler et al 1995), i.e., the fifth force.…”
Section: Introductionmentioning
confidence: 99%