1 S4 Environmental Disturbances Robert Schofield, U of O John Worden, Richard McCarthy, Doug Cook, Hugh Radkins, LHO Josh Dalrymple, SU I.Pre-S4 “fixes”

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Presentation transcript:

1 S4 Environmental Disturbances Robert Schofield, U of O John Worden, Richard McCarthy, Doug Cook, Hugh Radkins, LHO Josh Dalrymple, SU I.Pre-S4 “fixes” II.Some S4 veto issues III. Early coupling results from S4 PEM injections

2 In E12, H2 AS_Q was dominated by FMY roll mode when excited by chiller FMY roll mode peak in AS_Q increases when chiller matches frequency drifting chiller seismic peak ? staging building chiller Solution: resonant gain at FMY roll mode, seismic isolation of chiller. D.Q. flag for Hz glitches produced by 16 Hz? Office building chiller LVEA

3 10 Hz seismometer (etc.) peaks from RF card reader original set up after improving ground isolation of RF reader

4 Transformers near test-masses contribute to 60 Hz AS_Q peak AS_Q peak produced by transformer-sized magnetic field Recommendation: keep transformers at least 15 feet away from chambers (annulus ion pumps?).

5 Protecting sensitivity to the crab pulsar Crab GW frequency Pump shut downPump left on Coherence between LVEA seismic and H1, H2 AS_Q

6 Up-conversion of low frequency seismic noise seismic noise from distant excavation night spectrum excites stack modes in AS_Q up-conversion reduces interferometer sensitivity night spectrum

7 Up-conversion experiments Mechanical shaker at EX produces up-conversion in AS_Q But matched injection into DARM and optical lever servo (pitch and yaw) does not produce up-conversion. This suggests that up-conversion is not produced in servo systems or by optic motion.

8 Up-conversion of low frequency seismic transients Produces large in-band event (and event triggers) coincident on both interferometers. Small fast-traveling seismic transient

9 time series of same transient, 0.7 to 2 Hz steep band-pass, seismometers at all stations H2 AS_Q, 0.7 to 2 band-pass H2 AS_Q, 70 to 200 Hz band-pass

10 Coincident 1-3 Hz seismic, and Hz AS_Q spikes MY Seis Z 1-3 Hz MZ Seis Z 1-3 Hz H1 AS_Q Hz H2 AS_Q Hz This event does not produce up- conversion. However, this event does not show up in a sharper 0.7 to 2 Hz band.

11 Why are airplanes signals so bursty in AS_Q? Continuous acoustic sources can produce 5x bursts in AS_Q. Microphone signal (BP) from sound injection at REFL port Band Pass on resulting acoustic peak in AS_Q Bursts correspond with slight drops in arm power Makes vetoing more complex!

12 S4 LHO LVEA acoustic coupling from PEM injections

13 S4 LHO out-station acoustic coupling

14 S4 LLO corner and EY acoustic coupling

15 S4 LHO EX, EY magnetic coupling With predicted upper limits to displacement noise from coupling of ambient fields.

16 PEM burst injection logs (also in elog) LHOLLO

17 Summary I.Pre-S4 partial fixes a. Wandering chiller seismic peak (D.Q. flag for 16 Hz?) b. 10 Hz from RFID c. Transformers near test masses (ion pump supplies?) d. Crab protection (LHO out-stations, LLO?) II.Some S4 Issues a. Up-conversion of low frequency “continuous” seismic noise b. Veto up-converting Hz seismic transients c. Continuous environmental sources can produce AS_Q bursts III.Preliminary coupling results from S4 PEM injections a. LHO LVEA ambient sound level generally less than 1/5 SRD above 60 Hz b. LHO out-station ambient sound level generally less than 1/10 SRD c. 60 Hz peak in AS_Q may be dominated by direct coupling of ambient magnetic fields

18 Mechanical shaker near corner of chamber produces pitch, yaw and displacement motion as well as causing up-conversion in AS_Q. Mechanical shaker beside chamber produces side motion, but little pitch, yaw or displacement, and does not produce up-conversion.

19