A sapphire monolithic differential accelerometer as core sensor for gravity gradiometric geophysical instrumentation

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Abstract

Gradiometric gravimetry is a survey technique widely used in geological structure investigation. This work demonstrates the feasibility of a new class of low frequency accelerometers for geodynamics studies and space applications. We present the design features of a new low noise single-axis differential accelerometer; the sensor is suitable to be used in a Gravity Gradiometer (GG) system for land geophysical survey and gravity gradient measurements. A resolution of 1 Eötvös (1 Eö = 10-9s-2) at one sample per second is achievable in a compact, lightweight (less than 2 kg) portable instrument, operating at room temperature. The basic components of the sensor are two identical rigidly connected accelerometers separated by a 15-cm baseline vector and the useful signal is extracted as the subtraction of the two outputs, by means of an interferometric microwave readout system. The structure will be engraved in a monocrystal of sapphire by means of Computer-Numerically-Controlled (CNC ultrasonic machining: the material was chosen because of its unique mix of outstanding mechanical and dielectric properties.

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APA

Bertolini, A., Beverini, N., De Michele, A., Fidecaro, F., & Mango, F. (2006). A sapphire monolithic differential accelerometer as core sensor for gravity gradiometric geophysical instrumentation. Annals of Geophysics, 49(4–5), 1095–1103. https://doi.org/10.4401/ag-3111

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