Possibility of a geophysical determination of the Newtonian gravitational constant

Physics

Scientific paper

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Density Measurement, Gravimetry, Gravitational Constant, Sea Water, Flotation, Gravitation Theory, Gravity Anomalies, Ocean Surface, Spheres, Symmetrical Bodies

Scientific paper

Measurement of sea-water density and gravity variations from the ocean surface to a depth of about five km may provide a method for the geophysical determination of the Newtonian gravitational constant. The density measurements could be derived from the flotation force on a hollow silica sphere of near-neutral buoyancy and known compressibility. The chief technical challenge of the geophysical determination is to make precise gravity measurements at sea; uncertainty due to localized gravity anomalies may limit the accuracy of the determination.

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