Twenty-five of the BDSN sites are equipped with 3 component broadband seismometers
and strong-motion accelerometers, and a 24-bit digital data acquisition
system or datalogger.
Two additional sites (RFSB and SCCB) consist of a strong-motion
accelerometer and a 24-bit digital datalogger. Data from all
BDSN stations are transmitted to UC Berkeley using continuous telemetry.
In order to insure against data loss during utility disruptions,
each site has a 3-day supply of battery power and is accessible
via a dialup phone line. The combination of high-dynamic range
sensors and digital dataloggers ensures that the BDSN has the
capability to record the full range of earthquake motion for
source and structure studies. Table 3.2 lists
the instrumentation at each site.
Most BDSN stations have Streckeisen STS-1 or STS-2 three-component broadband sensors
(Wielandt and Streckeisen, 1982; Wielandt and Steim, 1986).
Guralp CMG-3T downhole broadband sensors contributed by LLNL are
deployed in post-hole installations at BRIB and FARB.
The strong-motion instruments are Kinemetrics FBA-23 or FBA-ES-T
with
2 g dynamic range. The recording systems at all sites are
either Q330, Q680, Q730, or Q4120 Quanterra dataloggers, with
3, 6, 8, or 9 channel systems. The Quanterra dataloggers employ
FIR filters to extract data streams at a variety of sampling rates.
In general, the BDSN stations record continuous data
at .01, 0.1, 1.0, 20.0 or 40.0, and 80 or 100 samples per second,
although some sites send triggered data at the highest sampling rate
using the
Murdock, Hutt, and Halbert event detection algorithm
(Murdock and Hutt, 1983) (Table 3.3).
In addition to the 6-channels of seismic
data, signals from thermometers and barometers are recorded at nearly
every site (Figure 3.2).
Figure 3.2:
Schematic diagram showing the flow of data from the
sensors through the dataloggers to the central acquisition
facilities of the BSL.
 |
In parallel with the upgrade of the broadband network, a grant from
the CalREN Foundation (California Research and Education Network) in 1994
enabled the BSL to convert data telemetry from analog
leased lines to digital frame-relay connections. The frame-relay network
uses digital phone circuits that can support 56 Kbit/s to 1.5 Mbit/s
throughput. Since frame-relay is a packet-switched network, a site may
use a single physical circuit to communicate with multiple remote sites
through the use of ``permanent virtual circuits". Frame Relay Access
Devices (FRADs), which replace modems in a frame-relay network, can
simultaneously support multiple interfaces such as RS-232 async ports,
synchronous V.35 ports, and ethernet connections. In practical terms,
the upgrade to frame relay communication provides faster data
telemetry between the remote sites and the BSL, remote console
control of the dataloggers, additional services such as FTP and telnet
to the dataloggers, data transmission to multiple sites, and the
ability to communicate and transmit data from multiple instruments
such as GPS receivers and/or multiple dataloggers at a single site.
Today, 23 of the BDSN sites use frame-relay telemetry for all or
part of their communications system.
Table 3.1:
Currently operating stations of the Berkeley Digital Seismic Network.
Each BDSN 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
and the elevation (in meters) is relative to the WGS84 reference ellipsoid.
The elevation is either the elevation of the pier (for stations sited
on the surface or in mining drifts) or the elevation of
the well head (for stations sited in boreholes). The overburden is
given in meters. The date indicates either the upgrade or installation
time.
| Code |
Net |
Latitude |
Longitude |
Elev (m) |
Over (m) |
Date |
Location |
| BDM |
BK |
37.9540 |
-121.8655 |
219.8 |
34.7 |
1998/11 - |
Black Diamond Mines, Antioch |
| BKS |
BK |
37.8762 |
-122.2356 |
243.9 |
25.6 |
1988/01 - |
Byerly Vault, Berkeley |
| BRIB |
BK |
37.9189 |
-122.1518 |
219.7 |
2.5 |
1995/06 - |
Briones Reservation, Orinda |
| BRK |
BK |
37.8735 |
-122.2610 |
49.4 |
2.7 |
1994/03 - |
Haviland Hall, Berkeley |
| CMB |
BK |
38.0346 |
-120.3865 |
697.0 |
2 |
1986/10 - |
Columbia College, Columbia |
| CVS |
BK |
38.3453 |
-122.4584 |
295.1 |
23.2 |
1997/10 - |
Carmenet Vineyard, Sonoma |
| FARB |
BK |
37.6978 |
-123.0011 |
-18.5 |
0 |
1997/03 - |
Farallon Island |
| GASB |
BK |
39.6547 |
-122.716 |
1354.8 |
2 |
2004/06 - |
Alder Springs |
| HOPS |
BK |
38.9935 |
-123.0723 |
299.1 |
3 |
1994/10 - |
Hopland Field Stat., Hopland |
| HUMO |
BK |
42.6071 |
-122.9567 |
554.9 |
50 |
2002/06 - |
Hull Mountain, Oregon |
| JCC |
BK |
40.8175 |
-124.0296 |
27.2 |
0 |
2001/04 - |
Jacoby Creek |
| JRSC |
BK |
37.4037 |
-122.2387 |
70.5 |
0 |
1994/07 - |
Jasper Ridge, Stanford |
| KCC |
BK |
37.3236 |
-119.3187 |
888.1 |
87.3 |
1995/11 - |
Kaiser Creek |
| MCCM |
BK |
38.1448 |
237.120 |
-7.7 |
2 |
2005/09 - |
Marconi Conference Center, Marshall |
| MHC |
BK |
37.3416 |
-121.6426 |
1250.4 |
0 |
1987/10 - |
Lick Obs., Mt. Hamilton |
| MNRC |
BK |
38.8787 |
-122.4428 |
704.8 |
3 |
2003/06 - |
McLaughlin Mine, Lower Lake |
| MOBB |
BK |
36.6907 |
-122.1660 |
-1036.5 |
1 |
2002/04 - |
Monterey Bay |
| MOD |
BK |
41.9025 |
-120.3029 |
1554.5 |
5 |
1999/10 - |
Modoc Plateau |
| ORV |
BK |
39.5545 |
-121.5004 |
334.7 |
0 |
1992/07 - |
Oroville |
| PACP |
BK |
37.0080 |
-121.2870 |
844 |
0 |
2003/06 - |
Pacheco Peak |
| PKD |
BK |
35.9452 |
-120.5416 |
583.0 |
3 |
1996/08 - |
Bear Valley Ranch, Parkfield |
| POTR |
BK |
38.2026 |
-121.9353 |
20.0 |
6.5 |
1998/02 - |
Potrero Hill, Fairfield (closed 02/2005) |
| RFSB |
BK |
37.9161 |
-122.3361 |
-26.7 |
0 |
2001/02 - |
RFS, Richmond |
| SAO |
BK |
36.7640 |
-121.4472 |
317.2 |
3 |
1988/01 - |
San Andreas Obs., Hollister |
| SCCB |
BK |
37.2874 |
-121.8642 |
98 |
0 |
2000/04 - |
SCC Comm., Santa Clara |
| WDC |
BK |
40.5799 |
-122.5411 |
268.3 |
75 |
1992/07 - |
Whiskeytown |
| WENL |
BK |
37.6221 |
-121.7570 |
138.9 |
30.3 |
1997/06 - |
Wente Vineyards, Livermore |
| YBH |
BK |
41.7320 |
-122.7104 |
1059.7 |
60.4 |
1993/07 - |
Yreka Blue Horn Mine, Yreka |
|
Table 3.2:
Instrumentation of the BDSN as of 06/30/2005.
Every BDSN station consists of collocated broadband and strong-motion sensors,
with the exception of PKD1, RFSB and SCCB which are strong-motion only, with a 24-bit
Quanterra datalogger and GPS timing. Additional columns indicate the
installation of a thermometer/barometer package (T/B),
collocated GPS receiver as part of the BARD network (GPS), and additional
equipment (Other) such as warpless baseplates or electromagnetic sensors (EM).
The obs station MOBB also has a current meter and differential pressure gauge (DPG).
The main and alternate telemetry paths are summarized for each
station. FR - frame relay circuit, R - radio, Mi - microwave, POTS - plain
old telephone line, VSAT - USGS ANSS satellite link, None - no telemetry
at this time. An
entry like R-Mi-FR indicates multiple telemetry links, in this case, radio
to microwave to frame relay.
| Code |
Broadband |
Strong-motion |
datalogger |
T/B |
GPS |
Other |
Telemetry |
Dial-up |
|
| BDM |
STS-2 |
FBA-23 |
Q4120 |
X |
|
|
FR |
|
|
| BKS |
STS-1 |
FBA-23 |
Q980 |
X |
|
Baseplates |
FR |
X |
|
| BRIB |
CMG-3T |
FBA-23 |
Q980 |
|
X |
Vol. Strain |
FR |
X |
|
| BRK |
STS-2 |
FBA-23 |
Q680 |
|
|
|
POTS |
|
|
| CMB |
STS-1 |
FBA-23 |
Q980 |
X |
X |
Baseplates |
FR |
X |
|
| CVS |
STS-2 |
FBA-23 |
Q4120 |
X |
|
|
FR |
|
|
| FARB |
CMG-3T |
FBA-23 |
Q4120 |
X |
X |
|
R-FR/R |
|
|
| GASB |
STS-2 |
FBA-ES-T |
Q4120 |
X |
|
|
R-FR |
|
|
| HOPS |
STS-1 |
FBA-23 |
Q980 |
X |
X |
Baseplates |
FR |
X |
|
| HUMO |
STS-2 |
FBA-ES-T |
Q4120 |
X |
|
|
VSAT |
X |
|
| JCC |
STS-2 |
FBA-23 |
Q980 |
X |
|
|
FR |
X |
|
| JRSC |
STS-2 |
FBA-23 |
Q680 |
|
|
|
FR |
X |
|
| KCC |
STS-1 |
FBA-23 |
Q980 |
X |
|
Baseplates |
R-Mi-FR |
X |
|
| MCCM |
STS-2 |
FBA-ES-T |
Q4120 |
|
|
|
VSAT |
|
|
| MHC |
STS-1 |
FBA-23 |
Q980 |
X |
X |
|
FR |
X |
|
| MNRC |
STS-2 |
FBA-ES-T |
Q4120 |
X |
|
|
None |
X |
|
| MOBB |
CMG-1T |
|
GEOSense |
|
|
Current meter, DPG |
None |
|
|
| MOD |
STS-1 |
FBA-ES-T |
Q980 |
X |
X |
Baseplates |
VSAT |
X |
|
| ORV |
STS-1 |
FBA-23 |
Q980 |
X |
X |
Baseplates |
FR |
X |
|
| PACP |
STS-2 |
FBA-ES-T |
Q4120 |
X |
|
|
Mi/FR |
|
|
| PKD |
STS-2 |
FBA-23 |
Q980 |
X |
X |
EM |
R-FR |
X |
|
| POTR |
STS-2 |
FBA-ES-T |
Q4120 |
X |
X |
|
FR |
X |
|
| RFSB |
|
FBA-ES-T |
Q730 |
|
|
|
FR |
|
|
| SAO |
STS-1 |
FBA-23 |
Q980 |
X |
X |
Baseplates, EM |
FR |
X |
|
| SCCB |
|
FBA-ES-T |
Q730 |
|
X |
|
FR |
|
|
| WDC |
STS-2 |
FBA-23 |
Q980 |
X |
|
|
FR |
X |
|
| WENL |
STS-2 |
FBA-23 |
Q4120 |
X |
|
|
FR |
|
|
| YBH |
STS-1 & STS-2 |
FBA-23 |
Q980 |
X |
X |
Baseplates |
FR |
X |
|
|
As described in Chapter 9, data from the BDSN are
acquired centrally at the BSL. These data are used for rapid
earthquake reporting as well as for
routine earthquake analysis (Chapters 4 and 10).
As part of routine quality control (Chapter 9),
power spectral density (PSD) analyses are performed weekly and
Figure 3.3 shows a summary of the results for 2004-2005.
The occurrence of a significant teleseism also provides the opportunity
to review station health and calibration. Figure 3.4 displays
BDSN waveforms for a
7.1 deep focus earthquake in the Fiji
region on July 15, 2004.
Figure 3.3:
PSD noise analysis for BDSN stations, by channel, in the period range
from 32-128 sec from 7/1/2004-6/30/2005. BRIB (situation in a shallow
vault that is prone to tilting) and FARB (located on the Farallon Islands)
stand out as sites with high noise levels. HUMO (located in an abandoned
mine) stands out as an exceptionally quiet site.
 |
Figure 3.4:
BDSN broadband vertical-component waveforms for a
7.1 deep
focus earthquake (565 km) which occurred in the Fiji Region on July 15,
2004. The waveforms were deconvolved to absolute ground acceleration,
10-100 second band pass filtered, and plotted in order of increasing
distance from FARB at 76.0 degrees to MOD at 80.1 degrees. Shown are
the P, pP, and sP body wave phases. Note that the body waves are
highly similar across the BK network and that most noticeable
differences are in the coda detail and the absolute amplitudes. This
provides confirmation that the station transfer function and polarities
are correct. The stations MNRC and POTR especially stand out in that
their amplitudes are significantly larger than is observed at the other
BDSN stations, owing primarily to their siting in the proximity of
thick alluvial deposits which amplify the ground motions.
 |
BDSN data are archived at the Northern California Earthquake Data
Center. This is described in detail in Chapter 11.
Table 3.3:
Typical data streams acquired at BDSN stations,
with channel name, sampling rate, sampling mode, and the FIR filter
type. SM indicates strong-motion; C continuous; T triggered; Ac acausal; Ca
causal.
The LL and BL strong-motion
channels are not transmitted over the continuous telemetry
but are available on the Quanterra disk system if needed.
The HH channels are recorded at two different rates, depending
on the dataloger type. Q4120s provide 100 sps and causal filtering;
Q680/980s provide 80 sps and acausal filtering. The BH channels
were changed from 20 to 40 sps this year as described below.
| Sensor |
Channel |
Rate (sps) |
Mode |
FIR |
| Broadband |
UH? |
0.01 |
C |
Ac |
| Broadband |
VH? |
0.1 |
C |
Ac |
| Broadband |
LH? |
1 |
C |
Ac |
| Broadband |
BH? |
20/40 |
C |
Ac |
| Broadband |
HH? |
80/100 |
C |
Ac/Ca |
| SM |
LL? |
1 |
C |
Ac |
| SM |
BL? |
20/40 |
C |
Ac |
| SM |
HL? |
80/100 |
C |
Ac/Ca |
| Thermometer |
LKS |
1 |
C |
Ac |
| Barometer |
LDS |
1 |
C |
Ac |
|
Table 3.4:
Typical MT data streams acquired at SAO and PKD,
with channel name, sampling rate, sampling mode, and FIR
filter type. C
indicates continuous; T triggered; Ac acausal.
| Sensor |
Channel |
Rate (sps) |
Mode |
FIR |
| Magnetic |
VT? |
0.1 |
C |
Ac |
| Magnetic |
LT? |
1 |
C |
Ac |
| Magnetic |
BT? |
40 |
C |
Ac |
| Electric |
VQ? |
0.1 |
C |
Ac |
| Electric |
LQ? |
1 |
C |
Ac |
| Electric |
BQ? |
40 |
C |
Ac |
|
Subsections
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