signals and trends in borehole strainmeter data strainmeter short course 2009 earthscope meeting,...
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Signals and Trendsin Borehole Strainmeter Data
Signals and Trendsin Borehole Strainmeter Data
Strainmeter Short Course2009 Earthscope Meeting, Boise
May 12, 2009
Strainmeter Short Course2009 Earthscope Meeting, Boise
May 12, 2009
Signals and Trends
• State of borehole compression
• Earth tides
• Barometric pressure response
• Seismic signals
• Non-tectonic signals
• Strain transients
Trends: Borehole• Dominant signal over months is borehole relaxation.
• Long term trend should be areal compression.
3 gauge areal strain = (CH0+CH1+CH2)/3
120° 120°
90°
CH0
CH2 CH1
30°
Trends: Borehole
Extension +ve
areal strain=(CH0+CH2+CH3)/3
“Classic Trends”
Dig
ital C
ou
nts
(x1
03)
21
.3 M
icro
stra
in
Compression -ve
B087, Ford Ranch
Trends: Borehole
Extension +ve
Dig
ital C
ou
nts
(x1
03)
0.4
Mic
rost
rain
Compression -ve
B087, Ford Ranch
Network State of Compression
Extension +ve
Com
pre
ssio
n R
ate
(n
an
ost
rain
/day)
Compression -veDecember 15, 2008 - April 15, 2009
Extension +ve
Compression -ve
PBO BSM Network, Compression Rate74% in compression
Days since installation
Extension and steps
B040 , York, Northern California
GTSM21 designed to operate under compression
Dig
ital C
ounts
(x1
03)
14
7.3
M
icro
stra
in
16
.6 M
icro
stra
in
Extension and steps
B040 , York, Northern California
Dig
ital C
ounts
(x1
03)
More likely to see steps in non-compressional BSM
21% of BSMs record steps58% of non compressional BSMs record steps
Extension and steps
B040 , York, Northern California
Rate of steps decrease as BSM turns to compression
Dig
ital C
ou
nts
Dig
ital C
ounts
(x1
03)
2.7
Mic
rost
rain
Extension and steps
Source of step unknown:Nothing on other gaugesNothing on B009 or B011
16
.8
Mic
rost
rain
B010, PGC, Vancouver Island, Canada
Dig
ital C
ou
nts
(x1
03)
B009
B010
B011168m
250m
Trends: Seasonal
B009, PGC
B009, PGC, Vancouver Island, Canada
mic
rost
rain
Herb Dragert reports farmer irrigating fields
Hydrostatic CouplingB006, Shores, Washington
Possibly hydrologically coupled• Little or no shear strain• Drifting phase in tidal signal• Little strain accumulated over 3.5 years
4.3
M
icro
stra
in
Dig
ital C
ou
nts
(x1
03)
Tidal signal
• Expect optimal performance in the tidal band
• M2 and O1 peaks should be visible in the spectrum
• Areal and shear consistency
Tidal Consistency
120° 120°
CH0
CH2 CH1
120°90°
CH3
CH1
3 gauge areal strain(CH0+CH1+CH2)/3
2 gauge areal strain(CH1+CH3)/2
Tidal Consistency
Areal ±10° 69% Shear ±10° 65%
Areal ±25 44% Shear ±25% 65%
Strainmeters
M2
Pha
se D
iffer
ence
M2
Am
plit
ude
Rat
io
B018, Delphi, Seattle, WA
Barometric Response
Barometric Pressure
mbar
Pressure increase = gauge compression
CH0
CH1
CH2
CH3
mic
rost
rain
Tides removed
Barometric Response
Barometric Pressure
mbar
CH0
CH1
CH2
CH3
mic
rost
rain
B018, Delphi, Seattle, WA
Pressure increase = gauge compression
Tides & barometric response removed
Barometric Response
Average barometric response coefficients
ParkfieldOlympic P.
Strainmeters
Anza MSH YSOR N.C Mojave
• Typical Range 2-10 nanostrain/millibar
9-12 second calibration signal, 30 minutes past the hourNull point before and after signal
9-12 second calibration signal, 30 minutes past the hourNull point before and after signal
High frequency signalsD
igit
al C
ou
nts
(x1
06)
B022 , May 31, 2008, 1-sps data
B022 Spectrogram, May 31, 2008
B006
M6.6 Mid Indian Ridge
Calibration spikes
MicroseismCH1
CH2
CH0
CH3
Noise: Rainfall
• Several of the PBO BSMs show strain signals
correlated with rainfall
• When looking at transients check the rainfall
measurements, all PBO sites have rain gauges
Noise: B022 RainfallB022, Oregon CoastB022, Seaside, Oregon Coast
Site in river flood plain, prone to floodingD
igita
l Cou
nts
Rainfall (m
m/hr)
Noise: Pathfinder, Anza
Co-located, Pathfinder strainmeters
Mic
rost
rain
B082
B089
Mic
rost
rain
CH0 CH1 CH2 CH3
Noise: B001 PumpingB001, Golbeck, Washington
Dig
ital C
ou
nts
0.1
M
icro
stra
in
2 gauges compression2 gauge in extension
PNW: B001 B045 Anza: B082 B089 B088
Noise: StormsD
igit
al C
ou
nts
(x1
03)
B012, Ucluelet, Vancouver Island, Canada
February 4, 2006 February 4, 2006 February 5, 2006
Noise: Downhole TemperatureB022, Seaside, Portland
Cou
nts
Tem
perature °C
Downhole Temperature
Dig
ital C
ou
nts
(x1
03)
Increase in downhole temperature=> compression
Noise: Downhole TemperatureB012 restart, February 11, 2009
Tem
perature °CDownhole Temperature
Dig
ital C
ou
nts
(x1
03)
Instrument restart
Increase in downhole temperature=> compression
Solar Noise
• Noise is introduced when solar panels start to
charge up in early morning.
• Visible in the 1 and 20-sps data set.
• PBO engineers found that rerouting cables helped.
A Strain Transient: Cascadia ETS
B012 B009
B004
B003
B005-7 B001
B018
Cascadia Episodic Tremor and Slip
B004, Hoko Falls, WA
2Ene Strain
Eee-Enn
Cascadia Episodic Tremor and Slip
2Ene Strain
2Ene Strain
Eee-Enn
2007 Tremor
2005 TremorB004
B004
mic
rost
rain
mic
rost
rain
Spring 2008 Cascadia ETS
B012 B009
B004
B003
B005-7 B001
B018
mic
rost
rain
Pacific Northwest BSMs: Shear strain
propagation of tremor (www.pnsn.org)
May 4
May 15
May 31
April 2008 May 2008
2009 Cascadia ETS ?
B012 B009
B004
B003
B005-7 B001
B018
Pacific Northwest BSMs: Shear strain
mic
rost
rain
April 2009 May 2009
ETS March 2009, B012, Vancouver Island
B012, Ucluelet, March 2009: Processed Gauge Data
mic
rost
rain
Detrended gauge dataTide removedTide and pressure removed
ETS March 2009, B012, Vancouver Islandm
icro
stra
in
Tensor Strain
Detrended gauge dataTide removedTide & pressure removed
Creep Events, Parkfield
Middle Mountain Area, Parkfield
PBO-BSM
PBO-BSM
2Ene Strain
Eee-Enn
B073 Varian, Parkfield
mic
rost
rain
Right lateral creep events