The five MPBO sites have 3-component borehole geophone packages. All
the remaining HFN sites have six-component borehole sensor packages.
The packages were designed and fabricated at LBNL's Geophysical
Measurement Facility by Don Lippert and Ray Solbau, with the exception
of site SFAB. For the HFN sites, three channels of acceleration are
provided by Wilcoxon 731A piezoelectric accelerometers and three
channels of velocity are provided by Oyo HS-1 4.5 Hz geophones.
Velocity measurements for the MPBO sites are provided by Mark Products
L-22 2 Hz geophones (Table 5.2). The 0.1-400 Hz Wilcoxon
accelerometers have lower self-noise than the
geophones above about 25-30 Hz, and remain on scale and linear to 0.5
g. In tests performed in the Byerly vault at UC Berkeley, the Wilcoxon
is considerably quieter than the FBA-23 at all periods, and is almost
as quiet as the STS-2 between 1 and 50 Hz.
Sensors are generally
installed at depths of about 100 m, but several sites have sensors
emplaced at depths of over 200 m and the Dumbarton bridge sites have
sensors at multiple depths (Table 5.1). During initial
stages of the project, the NHFN sensors provided signals to on-site
Quanterra Q730 and RefTek 72A-07 data loggers.
Today, twelve of the NHFN sites currently have Quanterra data loggers with
continuous telemetry to the BSL. Similar to BDSN sites, these stations
are capable of on-site recording and local storage of all data for more
than one day and have batteries to provide backup power. Signals from
these stations are digitized at a variety of data rates up to 500 Hz at
24-bit resolution (Table 5.3). In contrast to the BDSN
implementation, the NHFN data loggers employ casual FIR filters at high
data rates and acausal FIR filters at lower data rates. Because of
limitations in telemetry bandwidth and disk storage, 8 of these sites
transmit triggered data at 500 sps, using the Murdock, Hutt, and
Halbert (MHH) event detection algorithm (Murdock and Hutt, 1983),
and continuous data at reduced rates (100, 20 and 1 sps) to the BSL,
while the four MPBO sites transmit continuous data at 100 sps (one MPBO
site does not have telemetry yet).
The remaining 12 sites of the NHFN have in the past recorded data using
RefTek data loggers. These sites do not have continuous telemetry for
acquisition and required visits from BSL staff for data recovery.
Collection of data from these sites has been discontinued, but efforts
are underway to upgrade them with Quanterra Q4120 data loggers and
continuous telemetry.
Signals from the 5 SHFN stations are digitized by Nanometrics data
loggers at 100 sps and transmit continuous data to Menlo Park by
radio. These digital data streams are processed by the Earthworm
system with the NCSN data and waveforms are saved when the Earthworm
detects an event.
Table 5.1:
Stations of the Hayward Fault Network. Each HFN station is listed with
its station code, network id, location, operational dates, and site
description. The latitude and longitude (in degrees) are given in the
WGS84 reference frame. The elevation of the well head (in meters) is
relative to the WGS84 reference ellipsoid. The overburden is given in
meters. The start dates indicate either the upgrade or installation
time.
The abbreviations are:
BB - Bay Bridge;
BR - Briones Reserve;
CMS - Cal Memorial Stadium;
CB - Carquinez Bridge;
DB - Dumbarton Bridge;
MPBO - mini-Plate Boundary Observatory
RFS - Richmond Field Station;
RSRB - Richmond-San Rafael Bridge;
SF - San Francisco;
SMB - San Mateo Bridge;
SMC - St. Mary's College;
and, YB - Yerba Buena.
The * for stations indicates that the stations are not currently
recording data. RSRB is shut down while Caltrans is retrofitting the
Richmond-San Rafael bridge (as of April 19, 2001) and YBIB has been
off-line since August 24, 2000 when power cables to the site where shut
down. Other off-line stations are in the process of being upgraded as
funding for equipment becomes available. The table also includes 2
MPBO stations which became operational in the last 2 years, and 3 MPBO
borehole sensors that have recently been installed.
| Code |
Net |
Latitude |
Longitude |
Elev (m) |
Over (m) |
Date |
Location |
| CRQB |
BK |
38.05578 |
-122.22487 |
-25.0 |
38.4 |
1996/07 - current |
CB |
| HERB |
BK |
38.01250 |
-122.26222 |
-25.0 |
217.9 |
2000/05 - current |
Hercules |
| BRIB |
BK |
37.91886 |
-122.15179 |
219.7 |
108.8 |
1995/07 - current |
BR, Orinda |
| RFSB |
BK |
37.91608 |
-122.33610 |
-27.3 |
91.4 |
1996/01 - current |
RFS, Richmond |
| CMSB |
BK |
37.87195 |
-122.25168 |
94.7 |
167.6 |
1994/12 - current |
CMS, Berkeley |
| SMCB |
BK |
37.83881 |
-122.11159 |
180.9 |
3.4 |
1997/12 - current |
SMC, Moraga |
| SVIN |
BK |
38.03325 |
-122.52638 |
|
158.7 |
2003/08 - current |
MPBO, St. Vincent's school |
| OHLN |
BK |
38.00742 |
-122.27371 |
|
196.7 |
2001/07 - current |
MPBO, Ohlone Park |
| MDHL |
BK |
37.84227 |
-122.49374 |
|
160.6 |
in progress |
MPBO, Marin Headlands |
| SBRN |
BK |
37.68562 |
-122.41127 |
|
157.5 |
2001/08 - current |
MPBO, San Bruno Mtn. |
| OXMT |
BK |
37.498 |
-122.425 |
|
194.2 |
2003/12 - current |
MPBO, Ox Mtn. |
| BBEB |
BK |
37.82167 |
-122.32867 |
|
150.0 |
2002/05 - current |
BB, Pier E23 |
| E17B |
BK |
37.82086 |
-122.33534 |
|
160.0 |
1995/08 - current * |
BB, Pier E17 |
| E07B |
BK |
37.81847 |
-122.34688 |
|
134.0 |
1996/02 - current * |
BB, Pier E7 |
| YBIB |
BK |
37.81420 |
-122.35923 |
-27.0 |
61.0 |
1997/12 - current * |
BB, Pier E2 |
| YBAB |
BK |
37.80940 |
-122.36450 |
|
3.0 |
1998/06 - current * |
BB, YB Anchorage |
| W05B |
BK |
37.80100 |
-122.37370 |
|
36.3 |
1997/10 - current * |
BB, Pier W5 |
| W02B |
BK |
37.79120 |
-122.38525 |
|
57.6 |
2003/06 - current |
BB, Pier W2 |
| SFAB |
BK |
37.78610 |
-122.3893 |
|
0.0 |
1998/06 - current * |
BB, SF Anchorage |
| RSRB |
BK |
37.93575 |
-122.44648 |
-48.0 |
109.0 |
1997/06 - current * |
RSRB, Pier 34 |
| RB2B |
BK |
37.93 |
-122.41 |
|
133.8 |
2003/07 - current * |
RSRB, Pier 58 |
| SM1B |
BK |
37.59403 |
-122.23242 |
|
298.0 |
not recorded |
SMB, Pier 343 |
| DB3B |
BK |
37.51295 |
-122.10857 |
|
1.5 |
1994/09 - 1994/11 |
DB, Pier 44 |
| |
|
|
|
|
62.5 |
1994/09 - 1994/09 |
|
| |
|
|
|
|
157.9 |
1994/07 - current * |
|
| DB2B |
BK |
37.50687 |
-122.11566 |
|
|
1994/07 - current * |
DB, Pier 27 |
| |
|
|
|
|
189.2 |
1992/07 - 1992/11 |
|
| DB1B |
BK |
37.49947 |
-122.12755 |
|
0.0 |
1994/07 - 1994/09 |
DB, Pier 1 |
| |
|
|
|
|
1.5 |
1994/09 - 1994/09 |
|
| |
|
|
|
|
71.6 |
1994/09 - 1994/09 |
|
| |
|
|
|
|
228.0 |
1993/08 - current * |
|
| CCH1 |
NC |
37.7432 |
-122.0967 |
226 |
|
1995/05 - current |
Chabot |
| CGP1 |
NC |
37.6454 |
-122.0114 |
340 |
|
1995/03 - current |
Garin Park |
| CSU1 |
NC |
37.6430 |
-121.9402 |
499 |
|
1995/10 - current |
Sunol |
| CYD1 |
NC |
37.5629 |
-122.0967 |
-23 |
|
2002/09 - current |
Coyote |
| CMW1 |
NC |
37.5403 |
-121.8876 |
343 |
|
1995/06 - current |
Mill Creek |
|
Table 5.2:
Instrumentation of the HFN as of 06/30/2005. Every HFN downhole
package consists of co-located geophones and accelerometers, with the
exception of MPBO sites. 6 HFN sites also have dilatometers (Dilat.)
and the 5 MPBO sites have tensor strainmeters (Tensor.) 12 NHFN sites
have Quanterra data loggers with continuous telemetry to the BSL. The
remaining sites are being upgraded to Quanterra data loggers. The 5
SHFN sites have Nanometrics data loggers with radio telemetry to the
USGS. The orientation of the sensors (vertical - Z, horizontals - H1
and H2) are indicated where known or identified as "to be determined"
(TBD). The azimuths of the horizontal component geophones have a 180
degree ambiguity owing to the dead vertical component geophone.
| Site |
Geophone |
Accelerometer |
Z |
H1 |
h2 |
Data logger |
Notes |
Telem. |
| CRQB |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
251 |
341 |
Q4120 |
|
FR |
| HERB |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
TBD |
TBD |
Q4120 |
|
FR |
| BRIB |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
79 |
349 |
Q4120 |
Acc. failed, Dilat. |
FR |
| RFSB |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
256 |
346 |
Q4120 |
|
FR |
| CMSB |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
19 |
109 |
Q4120 |
|
FR |
| SMCB |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
76 |
166 |
Q4120 |
Posthole |
FR |
| SVIN |
Mark L-22 |
|
-90 |
298 |
28 |
Q4120 |
Tensor. |
FR/Rad. |
| OHLN |
Mark L-22 |
|
-90 |
313* |
43* |
Q4120 |
Tensor. |
FR |
| MDHL |
Mark L-22 |
|
-90 |
TBD |
TBD |
None at present |
Tensor. |
|
| SBRN |
Mark L-22 |
|
-90 |
347 |
77 |
Q4120 |
Tensor. |
FR |
| OXMT |
Mark L-22 |
|
-90 |
163 |
253 |
Q4120 |
Tensor. |
FR |
| BBEB |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
TBD |
TBD |
Q4120 |
Acc. failed |
Radio |
| E17B |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
TBD |
TBD |
None at present |
|
|
| E07B |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
TBD |
TBD |
None at present |
|
|
| YBIB |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
257 |
347 |
None at present |
Z geop. failed |
FR/Rad. |
| YBAB |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
TBD |
TBD |
None at present |
|
|
| W05B |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
TBD |
TBD |
None at present |
|
|
| W02B |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
TBD |
TBD |
Q4120 |
|
Radio |
| SFAB |
None |
LLNL S-6000 |
TBD |
TBD |
TBD |
None at present |
Posthole |
|
| RSRB |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
50 |
140 |
None at present |
2 acc. failed |
FR |
| RB2B |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
TBD |
TBD |
None at present |
1 acc. failed |
|
| SM1B |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
TBD |
TBD |
None at present |
|
|
| DB3B |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
TBD |
TBD |
None at present |
Acc. failed |
|
| DB2B |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
TBD |
TBD |
None at present |
|
|
| DB1B |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
TBD |
TBD |
None at present |
Acc. failed |
|
| CCH1 |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
TBD |
TBD |
Nanometrics HRD24 |
Dilat. |
Radio |
| CGP1 |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
TBD |
TBD |
Nanometrics HRD24 |
Dilat. |
Radio |
| CSU1 |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
TBD |
TBD |
Nanometrics HRD24 |
Dilat. |
Radio |
| CYD1 |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
TBD |
TBD |
Nanometrics HRD24 |
Dilat. |
Radio |
| CMW1 |
Oyo HS-1 |
Wilcoxon 731A |
-90 |
TBD |
TBD |
Nanometrics HRD24 |
Dilat. |
Radio |
|
Experience has shown that the MHH detector does not provide uniform
triggering across the NHFN on the smallest events of interest. In
order to insure the recovery of 500 sps data for these earthquakes, a
central-site controller has recently been implemented at the BSL using
the 500 sps vertical component geophone data for event detection.
Originally the 100 sps vertical component geophone data was used for
event detection but the bandwidth proved to be inadequate for detection
of the smaller events where most of the seismic wave energy was at
frequencies above 40 Hz. Triggers from this controller are being used to
recover the 500 sps data from the NHFN data loggers.
Data from the NHFN and SHFN are archived at the NCEDC. At this time,
the tools are not in place to archive the Hayward fault data together.
The NHFN data are archived with the BDSN data, while the SHFN are
archived with the NCSN data (Chapter 11). However, the
new central-site controller will provide the capability to both include
SHFN data in the event detection and extract SHFN waveforms for these
events in the future.
As originally planned, the Hayward Fault Network was to consist of 24
to 30 stations, 12-15 each north and south of San Leandro, managed
respectively by UCB and USGS. This is not happening quickly, although
west of the fault, Caltrans has provided sites along the Bay bridges.
This important contribution to the Hayward Fault Network has doubled
the number of sites with instrumentation. At times, Caltrans provides
holes of opportunity away from the bridges (e.g., HERB), so we have
plans for additional stations that will bring the network geometry to a
more effective state for imaging and real-time monitoring of the
fault.
As a check on the calibration and an example of the capabilities of a
borehole installed network, we compare the bandpass filtered (0.3-5 Hz)
ground velocity data recorded at NHFN and MPBO stations for a M 7.8
intermediate focus teleseism that occurred in Chile at a depth of 116
km in Figure 5.2.
Figure 5.2:
Plot of the P-wave waveforms, recorded by the NHFN/MPBO borehole
stations, for a major intermediate focus Chilean earthquake
(2005/06/13; 22:44 UT; 116 km deep;
7.8; 8460 km S51E of
Berkeley). The waveform data were deconvolved to ground velocity,
0.3-5.0 Hz band pass filtered to enhance the P-wave signal and
normalized prior to plotting. For comparison, the traces are plotted
in order of distance. The waveforms are highly similar at all stations
except W02B where there the trace is inverted.
 |
Table 5.3:
Typical data streams acquired at each NHFN site, with channel name,
sampling rate, sampling mode and FIR filter type. C indicates
continuous; T triggered; Ca causal; and Ac acausal. The 100 sps
channels (EP & HL) are only archived when the 500 sps channels are not
available.
| Sensor |
Channel |
Rate (sps) |
Mode |
FIR |
| Accelerometer |
CL? |
500.0 |
T |
Ca |
| Accelerometer |
HL? |
100.0 |
C |
Ca |
| Accelerometer |
BL? |
20.0 |
C |
Ac |
| Accelerometer |
LL? |
1.0 |
C |
Ac |
| Geophone |
DP? |
500.0 |
T |
Ca |
| Geophone |
EP? |
100.0 |
C |
Ca |
| Geophone |
BP? |
20.0 |
C |
Ac |
| Geophone |
LP? |
1.0 |
C |
Ac |
|
Berkeley Seismological Laboratory
215 McCone Hall, UC Berkeley, Berkeley, CA 94720-4760
Questions or comments? Send e-mail: www@seismo.berkeley.edu
© 2005, The Regents of the University of California