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Application and Optimisation of the Spatial Phase Shifting ...

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168 Improvements on SPS<br />

6.7.2 Long-term observation <strong>of</strong> biological object<br />

Many industrial ESPI experiments allow to predict <strong>the</strong> number <strong>and</strong> shape <strong>of</strong> fringes with which a test<br />

object will respond to a certain load. On <strong>the</strong> o<strong>the</strong>r h<strong>and</strong>, being a non-destructive examination technique,<br />

ESPI is particularly useful for unique objects about whose properties little is known. Therefore it is in<br />

general difficult to foresee changes in <strong>the</strong> fringe pattern, all <strong>the</strong> more when <strong>the</strong> objects are not subjected to<br />

test sequences or cycles but left to fluctuations – or attempts <strong>of</strong> stabilisation – <strong>of</strong> ambient parameters. In<br />

such cases, eventful periods may alternate with hours <strong>of</strong> little or no changes. A "good" experiment<br />

requires that <strong>the</strong> object motion be adequately tracked in time, this is, nei<strong>the</strong>r fringe density nor speckle<br />

decorrelation must grow too large between <strong>the</strong> capturing <strong>of</strong> consecutive interferograms; <strong>and</strong> on <strong>the</strong> o<strong>the</strong>r<br />

h<strong>and</strong>, no redundant data should be produced. While <strong>the</strong>re may be tasks where a human operator can make<br />

such decisions, this is undesirable from an economical point <strong>of</strong> view. Also, some observations exclude <strong>the</strong><br />

presence <strong>of</strong> a person.<br />

Temporal phase unwrapping is well suited to utilise <strong>the</strong> fringe order count n(x, y, t) to generate matched<br />

data storage intervals ∆t: from <strong>the</strong> continuously updated values Φ(x, y, t), <strong>the</strong> extreme values Φ max <strong>and</strong><br />

Φ min can be extracted in every run <strong>of</strong> <strong>the</strong> temporal phase unwrapping loop. When <strong>the</strong> difference exceeds a<br />

certain threshold Φ T , it is assumed that <strong>the</strong> corresponding sawtooth phase map ∆ϕ(x, y) = ϕ O (x, y, t f ) –<br />

ϕ O (x, y, t i ) between <strong>the</strong> present phase distribution ϕ O (x, y, t f ) <strong>and</strong> <strong>the</strong> stored initial one, ϕ O (x, y, t i ), has<br />

acquired m fringes with m = Φ T /2π. In that case ϕ O (x, y, t f ) is stored <strong>and</strong> re-labelled ϕ O (x, y, t i ), Φ(x, y, t)<br />

is cleared <strong>and</strong> <strong>the</strong> procedure begins anew. This technique yields a sequence <strong>of</strong> few-fringe sawtooth images<br />

that constitute no problem for spatial unwrapping. Note, however, that this method <strong>of</strong> fringe counting<br />

does not limit <strong>the</strong> fringe density: when small defects generate high local phase gradients, it may possibly<br />

come to unresolvable sawtooth fringe patterns. The phase gradient is easily accessible with <strong>the</strong> help <strong>of</strong> <strong>the</strong><br />

co-ordinates <strong>of</strong> Φ max <strong>and</strong> Φ min ; but this procedure was omitted for <strong>the</strong> sake <strong>of</strong> simplicity.<br />

Of course, <strong>the</strong> most convenient data evaluation would be to accumulate Φ(x, y, t) throughout <strong>the</strong> whole<br />

observation, whereby it may even become obsolete to save phase maps ϕ(x, y) regularly. But with <strong>the</strong> type<br />

<strong>of</strong> filter used here (6.26), it is safer to eliminate accumulated noise or accidental errors (e.g. by abrupt<br />

stress relaxation in <strong>the</strong> interferometer) by clearing Φ(x, y, t) when a phase map is stored. Thereby <strong>the</strong><br />

continuous tracking <strong>of</strong> phases Φ(x, y, t) is given up, but <strong>the</strong> propagation <strong>of</strong> errors is being limited to one<br />

measurement <strong>of</strong> Φ(x, y, t), corresponding to only one storage interval ∆t. Never<strong>the</strong>less, <strong>the</strong> whole series <strong>of</strong><br />

k phase maps Φ k (x, y, t) may be stored <strong>and</strong>, if usable, added up later on to yield Φ(x, y, t total ) = ΣΦ k (x, y, t).<br />

To test this approach <strong>of</strong> dynamic data storage, I examined a biological test object whose likely<br />

deformation is not known in advance. The white spot on a fresh chestnut, as shown in Fig. 6.26, was<br />

found to be quite co-operative for interferometry: its surface is reasonably reflective <strong>and</strong> maintains<br />

speckle correlation over sufficient time intervals. We can expect <strong>the</strong> displacements to proceed most<br />

rapidly at <strong>the</strong> beginning <strong>of</strong> <strong>the</strong> experiment because <strong>the</strong> object will relax in its holder. Also, <strong>the</strong> loss <strong>of</strong><br />

water from <strong>the</strong> surface should result in a constant shrinking, relatively fast initially <strong>and</strong> <strong>the</strong>n levelling <strong>of</strong>f.

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