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handbook of modern sensors

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304 8 Velocity and Acceleration<br />

Fig. 8.2. A frequency response <strong>of</strong> an accelerometer. f n is a natural frequency and f ref is the<br />

reference frequency.<br />

where a is the time-dependent impulse <strong>of</strong> the<br />

√<br />

accelerometer body and g(t) is the<br />

inverse transform L −1 {G(s)}.Ifwesetω = ω 0 1 − ζ 2 , then Eq. (8.6) has two solutions.<br />

One is for the underdamped mode (ζ < 1),<br />

x(t)=<br />

∫ t<br />

whereas for the overdamped mode (ζ > 1),<br />

x(t)=<br />

0<br />

∫ t<br />

0<br />

− 1 ω e−ζω 0(t−τ) sin ω(t − τ)a(t)dτ, (8.7)<br />

− 1 ω e−ζω 0(t−τ) sinh ω(t − τ)a(t)dτ, (8.8)<br />

√<br />

where ω = ω 0 ζ 2 − 1. The above solutions can be evaluated for different acceleration<br />

inputs applied to the accelerometer base [1].<br />

A correctly designed, installed, and calibrated accelerometer should have one<br />

clearly identifiable resonant (natural) frequency and a flat frequency response at which<br />

the most accurate measurement can be made (Fig. 8.2). Within this flat region, as the<br />

vibrating frequency changes, the output <strong>of</strong> the sensor will correctly reflect the change<br />

without multiplying the signal by any variations in the frequency characteristic <strong>of</strong><br />

the accelerometer. Viscous damping is used in many accelerometers to improve the<br />

useful frequency range by limiting the effects <strong>of</strong> the resonant. As a damping medium,<br />

silicone oil is used quite <strong>of</strong>ten.<br />

When calibrated, several characteristics <strong>of</strong> an accelerometer should be determined:<br />

1. Sensitivity is the ratio <strong>of</strong> an electrical output to the mechanical input. It is usually<br />

expressed in terms <strong>of</strong> volts per unit <strong>of</strong> acceleration under the specified conditions.<br />

For instance, the sensitivity may be specified as 1 V/g (unit <strong>of</strong> acceleration:<br />

g = 9.80665 m/s 2 at sea level, 45 ◦ latitude). The sensitivity is typically measured

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