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Algorithm for deriving the value of the Earth's gravity using the ZZG ballistic absolute gravimeter

Z Zabek1, T Knap1 and W Kielek2,3

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We describe an original algorithm for extraction of the local value of the Earth's gravity from the measured trajectory, h(t), of a test mass thrown up vertically. This algorithm relies upon separate adjustment of the rising and the falling parts of the test mass motion to an assumed model of the trajectory, and then connecting both limbs at the apex to obtain a complete ballistic curve. This complete curve is adjusted finally to the motion model to obtain the values of g, other trajectory parameters and the height residuals versus time curve. Within the procedure for connecting the two limbs at the apex, the two limbs are adjusted separately; some mechanisms are included that allow partial elimination of errors arising from microseisms and other disturbances. Standard methods of adjustment calculus used in geodesy are used in the fitting process.


PACS

91.10.Pp Gravimetric measurements and instruments

04.80.Nn Gravitational wave detectors and experiments

06.20.Dk Measurement and error theory

93.85.-q Instruments and techniques for geophysical research: Exploration geophysics

Subjects

Instrumentation and measurement

Environmental and Earth science

Gravitation and cosmology

Dates

Issue 6 (December 2004)

Received 3 June 2004

Published 5 November 2004



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