

Author: Robertson D. S.
Publisher: IOP Publishing
ISSN: 0026-1394
Source: Metrologia, Vol.38, Iss.2, 2001-04, pp. : 147-153
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Abstract
The position versus time data from a free-fall absolute gravimeter can be used to estimate the vertical gravity gradient in addition to the gravity value itself. Hipkin has reported success in estimating the vertical gradient value using a data set of unusually good quality. This paper explores techniques that may be applicable to a broader class of data that may be contaminated with "system response" errors of larger magnitude than were evident in the data used by Hipkin. This system response function is usually modelled as a sum of exponentially decaying sinusoidal components. The technique employed here involves combining the
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