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• Basic properties of the Fourier transform• Discrete form and the FFT • Simple example applications
• Applications in radio astronomy;– Synthesis imaging and the u-v plane – Frequency conversion– The Sampling Theorem– Advanced signal processing (DSP)– filter-banks, spectroscopy
Fourier Integral Transform
dtethfH ift
2)()(
dfefHth ift
2)()(Fourier integral transform
Inverse transform
Mutant forms;
i j (Engineering) 2πf ω (Pure maths or theoretical physics) f,t x,y Individual cosine, sine transforms
Basic Properties I
a . h(t) a . H(f) linearity h(t) + g(t) H(f) + G(f) linearity
h(t) is real H(-f) = H(f)* symmetry
h(t) is imag’ry H(-f) = -H(f)*
h(-t) = h(t) H(-f) = H(f)
h(t) real,even H(f) real,even
Basic Properties II
Scaling; “broad narrow” h(at) H(f/a) / |a|
Shifting; “shift phase roll/gradient”
h(t-t0) H(f) * exp(2πi f t0)
Convolution; “convolution multiplication”
h(t) * g(t) H(f) G(f)
Scaling; “broad narrow”
h(at) H(f/a) / |a|
Shifting; “shift phase roll/gradient”
h(t-t0) H(f) * exp(2πi f t0)
Convolution; “convolution multiplication”
H(f) G(f)
Basic Properties II
')'()'()(*)( dttgtthtgth
More convoluted example
After J. J. Condon and S. M. RansomESSENTIAL RADIO ASTRONOMYhttp://www.cv.nrao.edu/course/astr534
Parseval and correlation theorems
dhtghgCorr )()(),(
Corr (g,h) G(f)H(-f) = G(f)H(f)* for real g(t),h(t)
Corr (g,g) |G(f) |2 (Wiener-Khinchin)
Correlation function:
dffHdtth22
)()(
(Parseval)
Consumer applications
Fourier Transform Processing With ImageMagick
IntroductionOne of the hardest concepts to comprehend in image processing is Fourier Transforms.There are two reasons for this. First, it is mathematically advanced and second, resulting images, which do not resemble the original image, are hard to interpret.
Practical realisation
Periodic Discrete (“Fourier series”)
perioddf = 1/period
Periodic & Discrete Periodic & Discrete
period = N.dt period = N.dfN.dt.df = 1
DFT: Discrete Fourier Transform
Periodic, discretely sampled functions with; t = k.dt, f = n.df, (where N.dt.df = 1)
Replace indefinite integral with summation over N values;
NiknN
k kn ehH /21
0
NiknN
n nNk eHh /21
01
21
01
21
0
N
n nN
N
k k Hh Discrete form of Parseval
All aforementioned properties of Fourier integrals carry over, e.g.;
* One or other of h(t), H(f) function is generally “band-limited”
FFT – the Fast Fourier Transform
Simple DFT requires ~N2 multiplicationsGets very slow with large N
Decompose the NxN matrix intoa product of N sparse matrices
Have reduced to 2 DFTs of order N/2Keep going until you get to order 1.Number of mults now ~N.logN
Why phase is important
),( vuF
Originalimage
2D (3D) Transform
),(
),(
vuF
vuF
Amplitude only
Phase only
Filter:
Filter:
SpatialFrequencydomain
Applications in radio astronomy
• Aperture synthesis imaging
• Frequency conversion
• Sampling theorem
• Signal processing (spectrometers, PFBs)
u-v plane
East
Synthesis interferometer: we cross-correlate each pair of antennas
2-1 1-2 2-3 1-33-1 3-2321
Distribution function A(x,y) in antennas Transfer function W(u,v)
For n antennas n(n-1)/2 baselines (points) in u-v plane
u
1-1, 2-2 etc excluded!
aperture plane u-v plane
spatialauto-correlation
Complex visibility
dmdlemlBmlAvuV mvuli .),(),(),( )(2
B(l,m) := sky brightness in direction l,m
A(l,m) := antenna reception pattern
Mixing it down – Frequency Conversion
Signal 1
Signal 2
Signal 1 × Signal 2
Mixer (Multiplier)
Frequency Frequency
cos(ω1t)cos(ω2t)=½[cos((ω1+ω2)t)+ cos((ω1-ω2)t)]
Δf Δf
1*2
Difference Sum
cos(ωt) = ½[exp(iwt)/2 + exp(-iwt)]
Mixing it down II– Frequency Conversion (aka superheterodyne principle)
Signal 1
Mixer (Multiplier)
Frequency Frequency
Δf Δf
Local Oscillator
flo
Band pass filter
Image rejection
CSIRO. Receiver Systems for Radio Astronomy
Frequency
Frequency
Δf
flo* -flo
2flo-2flo
Unwanted image response
Negative frequencies: learn to love them!
titi eet 21)cos(
ω-ω
Analytic signal of real f(t);
h(t) h(t) + i.H(f)(t)
H(f) := Hilbert transform
cos(ωt) cos(ωt) + i.sin(ωt)
Single Sideband Mixers
CSIRO. Receiver Systems for Radio Astronomy
Signal
2√2cos(ω1t) √2cos[(ωLO- ω1)t] (USB) 0 (LSB)
SignalLocal Oscillator
Lower sideband
Upper sideband
Sampling Theorem – History
The theorem is commonly called the Nyquist sampling theorem; since it was also discovered independently by E. T. Whittaker, by Vladimir Kotelnikov, and by others, it is also known as Nyquist Shannon–Kotelnikov, Whittaker–Shannon–Kotelnikov, Whittaker–Nyquist–Kotelnikov–Shannon, WKS, etc., sampling theorem, as well as the Cardinal Theorem of Interpolation Theory.
It is often referred to simply as the sampling theorem.
(From Wikipedia)
Sampling Theorem (Shannon)
If a function x(t) contains no frequencies higher than B hertz, it is completely determined by giving its ordinates at a series of points spaced 1/(2B) seconds apart.
tsamp < 1 / 2B
Sampling Theorem continued
Also;
Radiotelescopes – Christiansen and Högbom
Radio Astronomy – J.D. Kraus
Principles of Interferometry and Synthesis in Radio Astronomy - Thompson, Moran, Swenson
Aliased sampling
Frequency
fs = 1/tsamp
*
2fs
B
Sampling theorem: fs = 1/tsamp > 2B
3fs -fs -2fs
Baseband 3rd Nyquistzone
Recent Trends
• Faster, cheaper, samplers
• Faster, cheaper processing, data storage
Wider sampled bandwidthsFewer downconversion stages
“direct conversion” (no downconversion)
e.g. DRAO receiver at Parkes)