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The time-dependent mantle up- and downwellings induce a time-dependent vertical forcing on the plate floating above, which causes topography at the lithosphere-asthenosphere boundary (LAB).
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The uplift pressures reduce the vertical force resultant promoting sliding.
The actuators transform the torque into vertical forces.
For the discs, vertical forces decreased with increased working depth.
The vertical force decreased linearly with these angles.
The disturbance was also well shown by the vertical force magnetometer.
In this system, beside vertical force versus vertical motion, lateral and vertical force versus lateral motion measurements, the vertical force versus temperature at the fixed distance between permanent magnet PM and superconducting sample SC, and the vertical force versus time measurements were performed at any temperatures from 20 K to 300 K.
Non-linearity was from 0.2% (left vertical force) to 1.4% (right antero-posterior force).
Unlike the leaf spring but like the coil spring, the air spring is capable of withstanding only vertical forces.
Patients applied less than 25% BW of peak vertical forces on the cane.
Vertical force could be estimated in the Type-I model with an accuracy of 13.75% BW.
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