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FIBEROPTIC SENSOR TECHNOLOGY HANDBOOK

FIBEROPTIC SENSOR TECHNOLOGY HANDBOOK

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Referring once more to Fig. 5.35, if the mass<br />

is given a transverse (cross axis) acceleration, both<br />

optical fibers are strained the same amount. Thus, the<br />

interferometer remains balanced and to first order this<br />

device is insensitive to transverse accelerations.<br />

Cross axis coupling will occur if simultaneously there<br />

are components of acceleration that has components<br />

parallel and perpendicular to the longitudinal axis of<br />

the fiber. The diaphragms indicated in Fig. 5.35 are<br />

provided to essentially eliminate cross-axis coupling.<br />

Tveten et.al. (See Ref. 1 of Subsection 5.3.1)<br />

investigated a single fiber version of this device. The<br />

sensitivity in radians/g versus frequency is shown in<br />

Fig. 5.38 and the value of amin versus frequency in<br />

Fig. 5.39.<br />

100or<br />

y 100 -<br />

v<br />

: 10 -<br />

~<br />

> ~-----<br />

&l -<br />

:<br />

~ 0.1 1<br />

0 100 200 300 400 500<br />

5.4 <strong>FIBEROPTIC</strong> ROTATION-Fb+TE <strong>SENSOR</strong>S<br />

5.4.1 Introduction<br />

The measurement of rotation is of considerable<br />

interest in a number of areaa. For example, inertial<br />

navigation systems as used in aircraft and spacecraft<br />

depend critically on accurate inertial rotation<br />

sensors. The allowable errors in rotation sensor performance<br />

depend on the particular application. Typical<br />

requirements for aircraft navigation lie between 0.01<br />

and 0.001 degreeslhour. In terms of earth rotatio<br />

rate, flE = 15 degrees/hour, this becomes 10-3 to 10 -2<br />

!lE. Fig. 5.40 lists several other applications of rotation<br />

sensors, such as surveying, where the accurate<br />

determination of azimuth and geodetic latitude is important<br />

(see Ref. 1, Subsection 5.4.20). In this case<br />

-6 ~ or less iS needed.<br />

performance of 10<br />

Geophysics<br />

applications include 2t e determination of astronondcal<br />

latitude, and the monitoring of polar motion caused by<br />

wobble, rotation, precession and wandering effects (see<br />

Ref. 1, Subsection 5.4.20). A highly precise rotation<br />

sensor may be used to measure any changes in the length<br />

of the day and to detect torsional oscillation in the<br />

earth caused by earthquakes. Finally, ultraprecise<br />

sensors may find applications in relativity-related<br />

experiments such as the determination of the preferred<br />

frame and dragging of inertial frames (see Ref. 2,<br />

Subsection 5.4.20).<br />

FREQUENCY HZ<br />

Fig. 5.38 The sensitivity in radianslg (g = 9.8m/s2)<br />

of a single-fiber fiberoptic accelerometer<br />

as a function of frequency. The low-frequency<br />

theoretical sensitivity is shown by<br />

the horizontal line.<br />

After A. Tveten et al., Electron Lett., — 16, 854 (1980),<br />

●<br />

●<br />

●<br />

●<br />

NAVIGATION WQESIO –3<br />

SURVEYING<br />

AZIMUTH, GEODETIC LATITUDE N

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