1991
DOI: 10.1103/physrevlett.67.3051
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Submarine measurement of the Newtonian gravitational constant

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Cited by 46 publications
(73 citation statements)
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“…High tower experiments [4] have put limits on the variation of G with distance, but provide no direct estimate of the gravitational constant. In mines [5], in boreholes [6], and in the ocean [7] the value of G could be determined with the density of the traversed material. These experiments mainly suer from the insufficient knowledge of local topography and density anomalies in the Earth's crust.…”
mentioning
confidence: 99%
“…High tower experiments [4] have put limits on the variation of G with distance, but provide no direct estimate of the gravitational constant. In mines [5], in boreholes [6], and in the ocean [7] the value of G could be determined with the density of the traversed material. These experiments mainly suer from the insufficient knowledge of local topography and density anomalies in the Earth's crust.…”
mentioning
confidence: 99%
“…The most recent measurement of G, the gravitational constant, on a macroscopic scale of 500 m, done by Zumberge et al (1991), gave a value of G D .6:677˙0:013/ 10 11 m 3 s 2 kg 1 which was consistent, within the experimental uncertainty, with the best laboratory value of 6:6726 10…”
Section: Epiloguementioning
confidence: 55%
“…Thus G(R,) = G(RM). A measurement of G at a length scale of order 5 km was made by measuring g as a function of depth in the ocean (Zumberge et al 1991). They found agreement with the laboratory measurements of G (Luther & Towler 1982) within about 0.2 per cent, so G( 10 cm) = G(5 km) to this accuracy.…”
Section: Absolute Amplitude Of T H E Tidesmentioning
confidence: 91%