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Numerical dispersion compensation for Partial Coherence Interferometry and Optical Coherence Tomography

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Abstract

Dispersive samples introduce a wavelength dependent phase distortion to the probe beam. This leads to a noticeable loss of depth resolution in high resolution OCT using broadband light sources. The standard technique to avoid this consequence is to balance the dispersion of the sample by arranging a dispersive material in the reference arm. However, the impact of dispersion is depth dependent. A corresponding depth dependent dispersion balancing technique is diffcult to implement. Here we present a numerical dispersion compensation technique for Partial Coherence Interferometry (PCI) and Optical Coherence Tomography (OCT) based on numerical correlation of the depth scan signal with a depth variant kernel. It can be used a posteriori and provides depth dependent dispersion compensation. Examples of dispersion compensated depth scan signals obtained from microscope cover glasses are presented.

©2001 Optical Society of America

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Figures (1)

Fig. 1.
Fig. 1. Resolution improvement obtained by dispersion compensation using depth-variant numerical correlation. Light of a filtered Hg high pressure lamp (λ 0≅710 nm; Δλ≅210 nm) is incident from left (thick arrow). The object has been synthesized using experimentally obtained non-dispersed front and dispersed back scattered depth scan signals of a single microscope cover slide. Shown are the (direct) auto- and cross-correlation depth scan signals (red) of the two front and the two back interfaces and the corresponding numerically dispersioncompensated correlation signals (black).

Equations (18)

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l c = 4 ln 2 π λ 0 2 Δ λ
n s = c d k d ω = n λ d n d λ .
d n g d λ = λ d 2 n d λ 2 = λ 2 π v 3 c d 2 k d ω 2
f = 1 + 4 d 2 τ 0 4 ( d 2 k d ω 2 ) 2 ,
l C , dispersed = l C · f
G ( τ ) = E ( t ) · E ( t + τ ) = G ( ω ) e i ω π d ω ;
G ( τ + τ 0 ) = G ( ω ) e i Φ 0 e i ω τ d ω
G Disp ( τ + τ 0 ) = G ( ω ) e i ( Φ 0 + Φ Disp ) e i ω τ d ω .
Φ Disp ( ω ω 0 ) = k ( ω ω 0 ) z
= k ( ω 0 ) z + k ( 1 ) ( ω 0 ) ( ω ω 0 ) z + k ( 2 ) ( ω 0 ) ( ω ω 0 ) 2 2 z + k ( 3 ) ( ω 0 ) ( ω ω 0 ) 3 6 z +
v g = [ k ( 1 ) ( ω 0 ) ] 1
E ( t ) = E ̂ ( ω ) e i ω t d ω ,
I I T ( τ ) = G ( τ ) = E ( t + τ ) E * ( t ) = d ω G ( ω ) e i ω τ
I I T ( τ ) = E ( t + τ ) E * Disp ( t ) = d ω G ( ω ) e i ω τ e i Φ Disp ( ω ) .
I Comp ( τ ) = F T { I local ( ω ) exp ( i Φ local ( ω ) } .
I Comp ( τ ) = I local ( τ ) K local ( τ )
K ( t ) = a e t 2 τ 0 2 e i ω 0 t .
n ( λ ) = 1 + B 1 λ 2 λ 2 C 1 + B 2 λ 2 λ 2 C 2 + B 3 λ 2 λ 2 C 3
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