Abstract
We amplified the geomagnetic influence on torsion pendulum experiment by producing an additional horizontal magnetic field, and obtained the dissipation, which is proportional to B 2 in the disc-shaped torsion pendulum experiment. The geomagnetic influence should be considered due to the inelasticity correction in G measurement in high Q-factor torsion pendulum experiments. 2001 Elsevier Science B.V. All rights reserved.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have