WKU Radio Jove Remote Station
Overview
In the basic Radio Jove setup, incoming radio waves close to the 20 MHz
resonant frequency (15 meter wavelength) of two horizontal dipole antennas
induce small (microvolt) electrical signals in the antenna wires that are
transmitted down coaxial feed lines to a radio receiver, where they are
amplified, mixed down to audio frequencies, filtered and amplified further, and
finally output to standard audio jacks for live listening or recording. The
direction in which the dipole array is most sensitive can be adjusted in
azimuth by the orientation of the individual dipole antennas and in elevation
by adjusting the antenna heights and the relative lengths of their feed lines.
The area of maximum sensitivity (the "beam") is huge by radio astronomy
standards (about 120° × 60° = 2.2 steradians in the
configuration used here), but the low gain of such a broad beam is offset by
the ability to monitor emissions from Jupiter or other targets for several
hours without having to track their motion across the sky, which would carry
them through a narrower beam more quickly.
WKU's Radio Jove experiment was adapted for remote operation to minimize
contamination of the received signal by radio frequency interference (RFI) from
power lines, computers, and other artificial sources commonly found where
people live or work. The WKU RJ remote station was thus completely
battery-operated and as isolated from RFI sources as was practical. It was
located on private land near WKU's Bell Observatory, approximately 10 km SW of
the city limits of Bowling Green, KY. The antenna array and receiving
equipment were located 150 meters ESE of the optical telescope dome, which has
its own power lines coming in from the west and a small microwave tower for
internet connectivity. The nearest residential property was 800 meters to the
west, over a hill. The nearest cell tower was 2 km SSE.
Equipment
- Antenna + Feed Line: Assembled from RJ 1.2 Antenna Kit
(RJA). Includes two horizontal, parallel, center-fed dipole antennas made of
#14 gauge 7-strand copper wire, suspended 10 feet above ground by four aluminum
masts, and connected by RG59U coaxial cable feed lines, with 3/8 wave delay on
one for phasing, through a power combiner/splitter. Line losses are estimated
at 1.5 dB (factor of sqrt(2) in signal amplitude). Beam directivity is
described above; particular configurations are described below.
- Noise Source + Bandpass Filter: An RF-2080 C/F calibrated
noise source and bandpass filter was placed between the feed line and the
receiver. When switched on, this replaced the antenna signal with a known
amount of noise power, which could compared to the antenna input to determine
how much power was being received in normal observations. Both the noise and
antenna signals were sent through a bandpass filter to eliminate RFI from
strong broadcast stations. This filter added another 1.5 dB of
attenuation to the signal path.
- Receiver: The RJ 1.1 receiver (RJB kit, pre-assembled) has a
tunable bandwidth of 300 kHz centered at 20.1 MHz and an instantaneous
bandwidth of 7 kHz at radio frequencies (half of this at audio
frequencies, since it is a
direct-conversion
design). A gain (volume) setting of 0.5 was normally used, which sufficed for
capturing both faint Jupiter storms and loud Solar bursts; terrestrial
broadcast signals can be even stronger but are still within the dynamic range
of the recording equipment. The RJ receiver draws 0.72 W of power.
- Audio Output: The receiver has two audio jacks, allowing
simultaneous live monitoring and recording. Auvio 3300090 Headphones were used
for live monitoring and for later playback of recordings. For the latter, a
TASCAM DR-40 portable digital recorder samples audio output from the receiver
at 44.1 kHz with 16-bit depth in a single (mono) channel, writing this to
consecutive uncompressed WAV files, in which format it can store up to 100
hours of continuous observations on its 32-GB SDHC memory card. Data
extraction and processing are described below. The DR-40 draws about 0.78 W of
power as used here, so the total power drain of the receiver + recorder was
about 1.5 W.
- Power: Starting in 2013, a QuickCable Rescue 1800 Jump Pack
rechargeable 12-volt, 40 amp-hour battery powered all electronic gear,
including the receiver, noise source, and digital recorder, via an assembly of
Enercell cigar-lighter plug adapters with 2A, 250V slo-blow fuses. Both the
receiver and noise source are designed for 12V power. In 2011 and 2012, the
recorder was run off 3 internal AA cells or 6 AA cells in an external pack
(model BP-6AA), but the latter was adapted to accept 12V input to its DC
switching power converter in 2013; field tests show no measurable RFI increase
from this arrangement (the 12V power for the receiver was also run through an
alternator
whine filter to minimize noise feeding back from the BP-6AA converter).
The 12V battery can power both the
receiver and recorder for 10 days of continuous operation in cold weather with
75% charge capacity (the noise source was run only for brief field
calibrations).
This was a great
improvement over AA battery life for the DR-40, which ranged from about 8 hours
for 3 alkaline cells to about 30 hours for 6 lithium cells.
- Housing: All electronic gear was housed in a tent to shield it
from the elements and kept in plastic storage tubs that both cover from above
in case of a tent breach and protect from below in case of flooding. The most
durable tent was a Springbar 7'×8' Outfitter 3 canvas model. Inexpensive
nylon dome tents were used for shelter initially, but these (a) had screened
areas that could not be fully sealed, letting in rainwater that pooled on the
tent floor, and (b) were not robust against long-term exposure to wind and
sunlight, necessitating regular replacement and risking equipment damage.
Aside from the tent and storage tubs, no environmental controls were provided
for temperature or moisture, but the equipment performed well in dry and wet
weather, from 20° to 90° Fahrenheit.
Procedure
During a "campaign" of continuous observations, local weather forecasts were
checked daily for possible thunderstorm activity, in which case the equipment
was disconnected from the antenna feed line until the threat was past.
Otherwise, data were retrieved from the digital recorder every few days, and the
12V battery was replaced once per week (typically every other data visit) by a
recharged twin unit. During each site visit, the antenna, feed lines, and tent
were inspected for wear and tear, the receiver audio output was monitored for
RFI, and a recording was made of the calibrated noise source and of broadcast
station
WWV, which was used
to correct the time calibration of the recorded data for any drift in the
DR-40's internal clock. The data were then read to a laptop computer disk and
cleared from the DR-40 memory card before making another set of noise source
and WWV recordings and resuming "sky" observations.
The WAV files written by the
DR-40 encode the raw signal wave-form as a digital representation of the
voltage as a function of time. These were read with a C code using the
libsndfile package,
squared, and averaged over a set of equal time intervals (typically a second or
more) to obtain an uncalibrated estimate of the received power, which by Ohm's
Law is proportional to the square of the signal voltage. The power could then
be calibrated by comparing sky observations to others of the calibrated noise
source and assuming simple proportionality (tests of different receiving gear
configurations indicate that this is reasonable). The standard calibration is
in temperature units, but these can be
converted into flux units or received power if the antenna beam is well
understood. The data timestamps were also calibrated against recorded WWV time
announcements. Plots of received power vs. time could then be generated from
the calibrated data using custom routines in C, CSH,
and Supermongo. As an
option, some brief RFI spikes from radiosonde band sweeps could be excised from
these plots (but not the WAV recordings) by median filtering of the waveform
data with 3-sigma clipping before squaring the voltages to get power.
Both plots and audio recordings were subsequently reviewed for Jupiter and
Solar activity. The Radio Jove email list is a valuable resource for checking
the local results against those of other RJ observers.
Development
The WKU Radio Jove remote station was run on an intermittent basis since
first established in the fall of 2011 as part of the Honors General Astronomy
214 course.
Several attempts were required for the station to
attain full operations.
- The original 2011 setup used two east-west dipoles at 10-ft. elevation,
with a 3/8-wave (135° phase) delay in the southern dipole feed directing
the beam to a point 50° above the southern horizon to observe Jupiter
crossing the local
meridian (a weaker secondary beam pointed 35° above the north horizon,
but Jupiter does not pass through this part of the sky as viewed from the
northern hemisphere).
The experiment was limited by not having long-term power for the DR-40 recorder
(6-9 hours for internal alkali AA batteries, or twice this for the external
BP-6AA pack), nor any power for the noise source in the field.
In addition, data could only be listened to as audio
playbacks or by viewing signal amplitudes inside audio-manipulation software
like Audacity (the standard
software for handling RJ data
is Radio SkyPipe, but
it requires a Microsoft Windows platform that could not be supported locally).
Even so, several short observations were made over a period of weeks,
and Jupiter S- and L-burst activity was captured. The
electronic gear was removed during the winter, and the antenna array was taken
down and stored in late spring.
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The experiment was repeated in the fall of 2012 with a new ASTR 214 class.
The same antennas were put up again in the same configuration, and the same
equipment was used, but a new tent was needed to house the gear, since the
previous tent had not survived the spring 2012 storm season. Although the fall
2012 observations were heavily time-constrained, some
Jupiter activity was again captured. Observations were also taken in a
more continuous mode by visiting the site frequently to replace batteries, and
by using lithium cells in the BP-6AA, which enabled the DR-40 to run for up to
30 hours. In parallel, code was developed to read the WAV files and compute
(still uncalibrated) received power vs. time for analysis. At the end of the
season, gear was stowed as before, but the tent and antennas were left in
place.
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In the fall of 2013, the experiment was repeated again for ASTR 214, but
with the ability to power the receiver, calibration noise source, and recorder
together off the 12V battery. This allowed for the first true long-term
observations, spanning 8 continuous days. Bad luck intervened however. First,
signal quality was hobbled by feed line damage from a lawn mower at the start
of the season. Then the antenna array was damaged in a severe storm. Later,
the tent (a replacement for the 2012 tent, which had also not survived the
off-season) was torn loose from its moorings and deposited intact in the woods
east of the site. It was moved back and anchored more securely but was torn
beyond repair in subsequent storms.
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In 2014, the experiment was revived for a fourth ASTR 214 class,
but on a much more solid footing. First, in place of the prior nylon dome
tents used to house equipment, a new high-quality canvas tent was purchased to
allow for longer-term stability of operations.
Second, a new antenna array (dipole wires, insulators, masts, feed lines, etc.)
was assembled from scratch. The array was configured as in 2011-2013, but with
the two dipoles oriented north-south and a 3/8-wave delay in the eastern dipole
to capture Jupiter in the early morning sky, since it would not cross the local
meridian before sunrise until very late in the year. This setup proved very
successful, recording almost continuously for many weeks and capturing
numerous Jupiter storms, Solar
flares, and sudden ionospheric disturbances. As a
result, students were able to carry out in-depth data analyses in addition to
the hands-on experience of setting up the station that they had in prior years.
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- In 2015, more observations were made with the same experimental setup
in the spring and summer and also for a few days in the fall with a new
ASTR 214 class. The equipment continued to perform well, adding to the
growing body of recorded data, which had multiplied greatly in the past year.
To address this data glut, new methods were developed to plot large masses of
continuous data. The combination of broad time coverage and the means to
visualize it at last enabled the positive detection of
Galactic emission and, quite unexpectedly, the tracking
of long-term changes in Solar activity.
- In the spring of 2016, the station was dismantled and its components
placed in storage to allow the land to be used for other purposes. Jupiter's
location in its orbit placed it on the far side of the Sun during the fall
semester when ASTR 214 was taught, visible only briefly before or after
sunset, so that fresh observations for the course would be difficult. Instead,
efforts were focused on processing, visualizing, and reviewing the backlog of
the many hundreds of hours of RJ observations accumulated in the previous 5
years.
Plots of these data are available for viewing.
Future observations are planned as circumstances allow.
Please see the credits page for a
list of the many individuals who have helped with this project.
The photo gallery gives many more
photos of the station and the people involved.
The history page describes earlier
radio astronomy experiments at WKU.
Radio Projects
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Radio Jove