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Martin Hewitson and the GEO team

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DRMI gives 2 output signals, each containing GW information P(t) and Q(t) There is a transfer function from h(t) ... Undoing the effect of the optical response ... – PowerPoint PPT presentation

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Title: Martin Hewitson and the GEO team


1
Measuring gravitational waves with GEO600
  • Martin Hewitson and the GEO team

2
Introduction
  • DRMI gives 2 output signals, each containing GW
    information P(t) and Q(t)
  • There is a transfer function from h(t) to P(t)
    and from h(t) to Q(t)
  • Tp(f) P(f) / h(f) and Tq(f) Q(f)/h(f)
  • Each comprise an optical part and an electronic
    part
  • Each vary (slowly?) in time
  • We want to calibrate P(t) and Q(t) to h(t)
    on-line
  • Need to estimate Tp(f) and Tq(f) ? hp(t) and
    hq(t)
  • Combine hp(t) and hq(t) to get optimal h(t)

3
In the steady state.
4
Transfer functions h(t)?P,Q
5
Optical transfer function - equations
  • For each quadrature, P and Q,
  • Overall gain
  • Pole frequency
  • Pole Q
  • Zero frequency

6
Measured optical response - P
7
Calibration overview
8
Calibration software tasks
9
On-line measurement of Tp(f)
10
Optimisation routine
  • Fit models of the transfer functions to the
    measured ones
  • 8 parameter fit
  • Gp, Ppf, Ppq, Pzf, Gq, Qpf, Qpq, Qzf
  • Electronic parameters are fixed
  • Algorithm uses various minimisation methods to
    find the best parameter set that describes the
    data
  • It also returns a measure of success c2

11
Undoing the effect of the optical response
  • The parameters from sys id can be used to
    generate inverse optical response
  • Poles to zeros, zeros to poles, invert gains
  • IIR filters are designed for these inverted
    responses
  • Overall gains are treated separately
  • Filters are applied to up-sampled error-point to
    give better filter response

Inverse P
12
Generating loop-gain correction signals
  • A full set of IIR filters has be constructed to
    match the response of the feedback electronics in
    the detection band
  • One set for fast feedback, one set for slow
    feedback
  • Error-point signal is filtered through these
    electronics filters and then through actuator
    filters
  • This produces two displacement signals that
    correct for the loop gain of the MI servo

13
Fast path (UG 100 Hz) electronics model
14
Slow path (UG 8 Hz) electronics model
15
Calibration pipeline hp(t)
16
Parameter estimation results - P
17
Parameter estimation results - Q
18
c2 behaviour
  • The measure of success from the optimisation
    routine tells us something about data quality
  • c2 depends on SNR of calibration lines in P

19
Quality channel
  • One 16-bit sample per second
  • Encodes information from
  • Lock status
  • Maintenance status
  • c2 threshold crossings
  • So far, c2 thresholds have been chosen arbitrarily

This will be extended soon see data quality
indicators talk ? 32 bit sample per sec
20
Measured c2 behaviour
21
Measured c2 behaviour
22
Measured c2 behaviour
noise estimation (s2)
23
hp(f) and hq(f) validation I
24
ESD calibration - Validation II
Labbook pages 1587, 1596, 1602
25
Combining hp(t) and hq(t)
  • With correct hp(t) and hq(t) we can try to
    combine them to get some optimal h(t)
  • Both signals represent (apparent) strain
  • Each contain some differential arm-length change
    information (real strain)
  • So, far only tried a couple of simple examples
  • Simple mean
  • High/low pass filter combination

26
Simple mean combination
h(t) hp(t) hq(t) / 2
27
Simple mean combination phase check
28
Filtered combination highpasslowpass
h(t) lowpasshp(t) highpasshq(t)
29
Filtered combination results
h(t) lowpasshp(t) highpasshq(t)
30
Filtered combination phase check
31
Current and future work
  • Q quadrature parameters are now successfully
    estimated and signal is calibrated to hq(t)
  • Updating of the optical filters needs more
    extensive studies to look for artefacts
  • More studies of c2 values for PQ simulations
  • More studies of c2 values for PQ real data
  • How to combine h(t)_P and h(t)_Q ?
  • Some simple ideas already exist
  • Other possibilities should be explored
  • The combined h(t) needs studied for artefacts
  • Include more automation
  • MI loop gains read from LabVIEW
  • Add more data quality checks extend quality
    channel bits
  • Try using recorded feedback signals for loop-gain
    correction

32
Pros and cons
  • Pros
  • Calibration is updated once per second
  • Accuracy to 10 from 50Hz to 6kHz
  • Runs on-line with 2 min latency time-domain
  • Produces calibrated time-series hp(t), hq(t)
  • Cons
  • Fast (gt1Hz) optical gain fluctuations ignored
  • Outwith valid frequency range, accuracy is poorer
  • Bottom line is ESD calibration good to about 5
  • Need independent check of ESD
  • Photon pressure calibrator

33
Intermission (Pause)
34
Introducing GEO Summary Pages
  • Track fixed measurements over lock stretches
  • Same set of measurements is performed on each
    data segment
  • Lock stretches can be overnight runs, weekend
    runs, science runs
  • A report is produced (web page) for each data
    segment
  • Quick-look way of comparing detector status over
    days
  • Also gives information about data quality
  • Q Should this data segment be analysed?

35
GEO Summary Pages calibration quality
  • GEO Summary pages focus primarily on calibration
    quality and sensitivity measures so far
  • Min/Max spectra
  • BLRMS sensitivity
  • Data quality channel locked?, Maintenance?
  • Recovered parameters
  • c2 values
  • Lock lists and duty cycle
  • Will be extended to include GEO monitor outputs
    (see Ajiths talk)

36
Where to look
  • Index of reports appears at
  • http//www.geo600.uni-hannover.de/georeports/index
    .html
  • The list of reports is split into months
  • Each entry is a summary of the full report
  • Links take you to the full report

Lets have a look
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