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A laser sensor of a seismic slope of the Earth surface

  • Methods of Physical Experiment
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Abstract

A principally new method of the measurement of a seismic slope of the Earth surface is suggested. The method makes it possible to stabilize the position of the laser beam as a highly extended coordinate axis in the metrological support of the precision construction of large-scale physical installations. The method has been tested experimentally: for the first time, low-frequency periodic angular oscillations have been registered with an amplitude of 5 × 10−7 rad and the noise registration value of 2.5 × 10−8 rad. The measurements were taken at CERN, during the construction of the spectrometric complex ATLAS.

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Batusov, V., Budagov, J. & Lyablin, M. A laser sensor of a seismic slope of the Earth surface. Phys. Part. Nuclei Lett. 10, 43–48 (2013). https://doi.org/10.1134/S1547477113010020

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