Top Banner
Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National Laboratory
37

Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Jan 18, 2018

Download

Documents

Melinda Hancock

Uranus and Titan Courtesy: De Pater Courtesy: Team Keck.
Welcome message from author
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
Page 1: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Fundamentals of adaptive optics and wavefront reconstruction

Marcos van Dam

Institute for Geophysics and Planetary Physics, Lawrence Livermore National Laboratory

Page 2: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Outline

1. Introduction to adaptive optics2. Wavefront sensors

• Shack-Hartmann sensors• Pyramid sensors• Curvature sensors

3. Wavefront reconstructors• Least-squares• Modal reconstructors

4. Dynamic control problem

Page 3: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Uranus and Titan

Courtesy: De Pater Courtesy: Team Keck.

Page 4: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Adaptive optics

Page 5: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Effect of the wave-front slope

• A slope in the wave-front causes an incoming photon to be displaced by xzWx

x

z

W(x)

Page 6: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Shack-Hartmann wave-front sensor

• The aperture is subdivided using a lenslet array.• Spots are formed underneath each lenslet.• The displacement of the spot is proportional to the

wave-front slope.

Page 7: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Shack-Hartmann wave-front sensor• The centroid (center-of-mass) is proportional to the mean

slope across the subaperture.• Centroid estimate diverges with increasing detector area

due to diffraction and with increasing pixels due to measurement noise.

• Correlation or maximum-likelihood methods can be used.

0

5

10

15

20

0

5

10

15

20-10

0

10

20

05

1015

20

0

5

10

15

200

0.02

0.04

0.06

0.08

Page 8: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

• Wave-front x- and y-slope measurements are usually made in each subaperture using a quad cell (2 by 2).

• Quad cells are faster to read and to compute the centroid.

Quad cells

Page 9: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

• These centroid is only linear with displacement over a small region.

• Centroid is proportional to spot size.

Quad cells

Displacement

Cen

troid

Cen

troid

vs.

dis

plac

emen

t for

diff

eren

t spo

t siz

es

Page 10: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

• Similar to the Shack-Hartmann, it measures the average slope over a subaperture.

• The subdivision occurs at the image plane, not the pupil plane.

• Less affected by diffraction.

Pyramid wave-front sensor

Page 11: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Wave-front at aperture

Aperture

Image 1

z

-z Image 2

Curvature sensing

Page 12: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Curvature sensing

• Practical implementation uses a variable curvature mirror (to obtain images below and above the aperture) and a single detector.

Page 13: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Curvature sensing

WIWIzI

.2

IIWzWz

IIII

.2

12

12

Where I is the intensity, W is the wave-front and z is the direction of propagation, we obtain a linear, first-order approximation,

• Using the irradiance transport equation,

which is a Poisson equation with Neumann boundary conditions.

Page 14: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Curvature sensing

)(21

21yyxx WWz

IIII

• Solution inside the boundary,

• Solution at the boundary,

)()()()(

21

21

xx

xx

zWRxHzWRxHzWRxHzWRxH

IIII

+ -

I1

I2

I1- I2

Page 15: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Curvature sensing

As the propagation distance, z, increases,

• Sensitivity increases.• Spatial resolution decreases.• Diffraction effects increase.• The relationship between the signal, (I1- I2)/(I1+ I2) and the curvature, Wxx + Wyy, becomes non-linear.

Page 16: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Faint companions

Page 17: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Wave-front reconstruction

• There is a linear relationship between wave-front derivative and a measurement.

• Don’t want to know the wave-front derivative, but the wave-front or, better, the actuator commands.

• Need to know the relationship between actuator commands and measurement.

Page 18: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Actuators: Shack-Hartmann

• The lenslets are usually located such that the actuators of the deformable mirror are at the corners of the lenslets.• Piston mode, where all the actuators are pushed up, is invisible to the wave-front as there is no overall slope.• Waffle mode, where the actuators are pushed up and down in a checkerboard pattern, is also invisible.

Page 19: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

System matrix

• The system matrix, H, describes how pushing each actuator, a, affects the centroid measurements, s

.• It is created by pushing one actuator at a time and

measuring the change in centroids.

Actuators

Centroids

Has

Page 20: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

System matrix

• Alternatively, the system matrix can be computed theoretically using finite differences to approximate the derivatives:

• Another formulation is using Fourier transforms (faster than matrix multiplication).

daass jiji

xji

xji ,,1,1,

2

d

daass jiji

yji

yji ,1,1,,

2

Page 21: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Actuators: Curvature

• Bimorph mirrors are usually used, which respond to an applied voltage with a surface curvature.• The electrodes have the same radial geometry as the subapertures.• Curvature sensors tend to be low order.

Page 22: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Reconstruction matrix• We have the system matrix:• We need a reconstruction matrix to convert from centroid measurements into actuator voltages:• Need to invert the 2N (centroids) by N (actuators) H matrix. • For well-conditioned H matrices a least-squares algorithm suffices: unsensed modes, such as

overall piston, p, and waffle, w, are thrown out.

• Equivalently, use singular value decomposition.

Rsa

Has

TTTT HwwppHHR 1)(

,...]1,1,1,1,1[,...]1,1,1,1,1,1[

wp

Page 23: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Reconstruction

matrix

• Most modes have local waffle but no global waffle.• Hence, must regularize before inverting.

Page 24: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Reconstruction

matrix

1. Penalize waffle in the inversion, e.g., using the inverse covariance matrix of Kolmogorov turbulence, and a noise-to-signal parameter, (Bayesian reconstructor).

TT HCHHR 11)(

C

SVD Bayesian

Page 25: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Reconstruction

matrix

• Comparison of reconstruction matrices

SVD Bayesian

Page 26: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Reconstruction

matrix

• Comparison of reconstruction matrices

SVD Bayesian

Page 27: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Reconstruction

matrix

2. Only reconstruct certain modes, zi, (modal reconstruction).

TT HZHZHZZR )()]()[( 1

...],,[ ,321 zzzZ

Page 28: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Keck I I AO + NI RSPEC (J une/ 00)

HST: J,H,K composite

1.6 arc sec

Bright nucleus

Faint nucleus

Gas in betweenx

2.00 m 2.08 m 2.17 m

H2 emission line f rom shocked or ionized gas (v=580 km/ s)

Keck: K-band Active galaxyNGC6240:Max et al.

R = 12.5 NGS,35” separation

Page 29: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Control problem

• Wave-front sensing in adaptive optics is not only an estimation problem, it is a control problem.

• There are inherent delays in the loop due to• Integration time of the camera• Computation delays

• The AO system should minimize bandwidth errors while maintaining loop stability.

• The propagation of measurement noise through the loop also needs to be minimized.

Page 30: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Modeling the system dynamics

• Model the dynamic behavior of the AO system using the transfer function of each block.

Deformable mirror Centroid measurements

Page 31: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Modeling the system dynamics

• The turbulence rejection curve can be calculated from a model of the AO system.

0 50 100 150 200 250 300 3500

0.5

1

1.5

2

2.5

3

Frequency (Hz)

Rej

ectio

n

Page 32: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Modeling the system dynamics

• We can calculate the bandwidth and noise terms from a combination of data from the telescope and modeling the system.

Noise

Bandwidth errors

Page 33: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Laser guide stars

• Shine a 589 nm 10-20 W laser in the direction of the atmosphere.

• Sodium atoms at an altitude of 90 km are excited by this light and re-emit.

• The return can be used as a guide star.

Page 34: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Laser guide stars• The laser is equally deflected on the way up and

down, so can’t be used to measure tilt.• The guide star is not at infinity, so the focus is

different.• Hence, need a natural guide star as well (but can

be much fainter).

Page 35: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

• This work was performed under the auspices of the US Department of Energy by the University of California, Lawrence Livermore National Laboratory, under contract W-7405-Eng-48.

• The work has been supported by the National Science Foundation Science and Technology Center for Adaptive Optics, managed by the University of California at Santa Cruz under cooperative agreement No. AST-9876783.

• W. M. Keck Observatory has supported this work.

Acknowledgements

Page 36: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

90 sec integration90 sec integration

Page 37: Fundamentals of adaptive optics and wavefront reconstruction Marcos van Dam Institute for Geophysics and Planetary Physics, Lawrence Livermore National.

Thank you!