1. Cables
      2. (SPASE)
  1. SPASE
  2. AMANDA DAQ Building (MAPO)
  3. SPASE Building
  4. Antennas
  5. Test array:
  6. NoEvent Event
  7. Pulser Starts Pulse reaches DAQ
  8. MAPO 1 MAPO 2
  9. SPASE 1 SPASE 1
  10. Pulse reaches DAQ
  11. MAPO 1 MAPO 2
  12. SPASE 1 SPASE 1
  13. limin
  14. RMS of reconstruction ~ 3 m
  15. surface
  16. junctionbox
  17. no evident show stopper but impact on detector designs
  18. 2 by factors
  19. shaped pulse
  20. waveform
  21. fully digitized waveform array
  22. Pulse shaping & envelope trigger
  23. “Common Mode” TDA Node:
  24. surface
  25. junctionbox
  26. Countinghouse
  27. Ignition noise transients from idling snowmobile
  28. Transient
  29. Wavefront
  30. Snowmobile(transient source)
  31. tower
  32. tower
  33. Total # of
  34. Sensors
  35. Real-Time, Simplest “Elevation Gating”
  36. TDA (A)
  37. TDA (B)
  38. Reject
  39. Accept
  40. Accept
  41. Active Antennaswith Envelope
  42. Outputs
  43. (TDAs)
  44. Surface Processor Assembly (SPA)
  45. SPA ofNext Hole
  46. Envelopes sent to
  47. surface
  48. Course Time
  49. From
  50. MasterclockLSB= 10nsRange=100us
  51. Fine Times
  52. From Time-Digital-Converter (TDC)
  53. LSB=250psRange=500ns
  54. Hole
  55. Address
  56. TDA1TOT
  57. TDA2Rise
  58. TDA2TOT
  59. “Common Mode” TDA Node:
  60. Envelope
  61. Signals
  62. UpperTDA
  63. LowerTDA
    1. START
    2. STOP CH1
    3. STOP CH2
  64. Coarse Time (x10) Master clock
  65. Settings
  66. Buffered Hit Data
  67. Serializer
  68. Master Clock Pair
  69. Data Pair
  70. Slow Control
  71. AdjacentSPAs
  72. Transient
  73. Wavefront
  74. Snowmobile(transient source)
  75. tower
  76. tower
  77. Disc-A
  78. Disc-B
  79. T= 200ns (Max TDOA for z= 40m)
  80. Variable delay
  81. of PW-A
  82. AND Output
  83. PW-A = PW-B
    1. Variable Delay Range≈ “elevation range”
  84. Rate Output
  85. Envelope
      1. From Hole40m
    1. Pulse width≈ “elevation resolution”

1
R&D working group report
SAC May 2009
Klaus Helbing, Wuppertal & Hagar Landsman, Madison
Goals and tasks
Working group structure
Status of R&D
refraction, attenuation, background
Acoustics
air shower radio
in-ice radio
Conclusions for design of extension
Road forward

2
Common goals
Most general:
Extend IceCube and use unique facility and
environment/infrastructure at SP:
Only place to combine optical & radio &
acoustics & air showers
i.e. imitate the IceTop – InIce relation
Primary motivation:
GZK neutrinos
Expand acceptance of IceCube for EeV neutrinos
by orders of magnitude
Also:
determine EHE neutrino cross section
air shower physics (inclined, composition, EHE)

3
Tasks of R&D working group
work out task distribution amongst
participating institutions
establish Letter Of Intent (LOI)
define interfaces and common infrastructure
for different sensors (in/on ice, methods, ...)
establish milestones for an intermediate
scale detector (~ 5 GZK-
ν
's/year)
establish a road map towards a full scale
detector (~ 50 GZK-
ν
's/year; O(1000) km
2
)
coordinated planning of funding proposals

4
Structure of R&D working group
First common meeting (1-day) at fall meeting 2008
Formation of WG at last collaboration meeting
phone calls on common issues, converging plans
Existing sub-groups continue with dedicated phone
calls (focus: specific instruments):
radio (Dave Besson)
in-ice
air shower
acoustic (Timo Karg)
optical high energy extension (HE, Albrecht K.)
New IC-members and affiliated groups contribute
(e.g. Hawaii and Ohio)
Upcoming R&D workshop in June

5
Relation to standard (optical) IceCube
Benefit from IceCube knowledge and
access to South Pole site
Unique possibilities of combined
observations both in-ice and on-ice
Vision of “guaranteed” neutrino signal ↔
momentum from potential IC discovery
Keep
engineering work force
students with inclination towards hardware
entrepreneurial aspects of early
Amanda/IceCube days

6
Status of ongoing site studies
with ...
SPATS
: South Pole Acoustic Test Setup
RICE
: Radio Ice Cherenkov Experiment
AURA
: Askaryan Underice Radio Array
NARC
: Neutrino Array Radio Calibration
Surface radio antennas
(stand alone)

7
Status Acoustics
SPATS

8
Speed of sound
Also shear waves
are relevant!
helps with
reconstruction
Precision
measurement
ready for journal
publication in
~ weeks

9
Acoustic attenuation
Amplitude
1
st
/2
nd
peak
Energy
time domain
Ball park: 300m ± 100 m
Expectation was kilometers
Unclear whether attenuation is short
because of absorption or scattering

10
Acoustic noise (DC)
Low continuous noise level

11
Acoustic noise, transients
Transients
correlate with
Rod wells for drilling
freeze in of IceCube
holes
No correlation
found with “dry”
rod well
blind analysis proof

12
2
C
a
b
l
e
s
(
S
P
A
S
E
)
125
m

Back to top


SPASE

Back to top


AMANDA DAQ
Building (MAPO)

Back to top


SPASE Building

Back to top


Antennas
Status air shower radio

Back to top


Test array:
4 antennas
read out with
RICE DAQ

13
Surface RFI (DC)
Low continuous noise level

14
Transient surface RFI
- uncalibrated -
GHz
ns

Back to top


NoEvent
Event
GHz
0.
1.
0.
1.
2.
2.
RFI
difference
Event - NoEvent
narrow frequency band of RFI emission
compared to broad band air shower signal
RFI

15
Pinger Data Reconstruction

Back to top


Pulser Starts
Pulse reaches DAQ

Back to top


MAPO 1
MAPO 2

Back to top


SPASE 1
SPASE 1

16
Pinger Data Reconstruction
Pulser Starts

Back to top


Pulse reaches DAQ

Back to top


MAPO 1
MAPO 2

Back to top


SPASE 1
SPASE 1
Pre

Back to top


l
imin
a
ry

Back to top


RMS of reconstruction ~ 3 m

17
Shallow (~300m)
Deep (~1400 m)

Back to top


surface

Back to top


junction
box
Counting
house
Status in-ice radio
AURA cluster:
Digital Radio Module (DRM) – similar to DOM
4 antennas, 1 Antenna Calibration Unit (ACU)
IceCube sphere, DOM main board (waveforms)
5 clusters: 2 in 06/07; 3 in 08/09 (with NARC)
2 channels (“antennas”) down to 100MHz
15/20 channels are working

18
Status in ice radio: Index of refraction
Changing index helps to
reduce surface noise
pickup
... but shadowing for
shallow deployment
No birefringence

19
Radio attenuation
temperature region for shallow deployment
R=1.0 : worst case scenario

20
Forced
Trigger
Trigger - details
In ice RFI transients with AURA
Angular resolution:
few degrees

21
Status summary:
Attenuation
Mostly known
great progress in acoustics with last season
but unfavorable result
known from radio reflection of bed rock,
direct on-site measurements would be nice
confirmation
Negligible for air shower radio

22
Status summary: “
Refraction
Refraction, signal speed, depth
dependence:

Back to top


no evident show stopper but impact
on detector designs
good knowledge in acoustics but needs
additional studies for shallow holes
in radio uncertainties can still influence
detector design
E-field needs further attention to understand
signal strength, B-field configuration wrt veto
coverage of air shower radio.

23
Status summary:
Noise
Noise/EMI/background:
significant
uncertainties wrt transients
potential cost driver (electronics)
Acoustic: constant level of noise favorable
(compared to sea), most transients
from known
sources
In-ice Radio: deserves attention
RICE:
favorable in winter, challenge in summer
transient
background rate O(1/minute) in multiplicity
air showers could be (additional) transient
background
Air shower radio (on-ice antennas) could be
instrumental to get rid of EMI in-ice ... for itself
looks promising, work in progress.

24
Current implications from site exploration
GZK is main science motivation
long attenuation length for radio signals in ice
Askaryan radio detector in ice main
instrumentation and design driver
Pursue integrated approach of air shower radio
detection
together with neutrino detection for
additional (EHE) vetoing
→ increased overlap with optical
EMI reduction and monitoring
air showers may provide test beam for in ice
... and of course air shower physics
use joint infrastructure

25
Role of acoustics
Reevaluation of hybrid option needed in view of
shorter than expected attenuation length
Finish site exploration e.g. understand attenuation
mechanism
In case optimistic scenario prevails
scattering accounts for short attenuation
reduces previously diverging vertical demands
shallow co-deployment in narrow holes feasible
extra cost reasonably small fraction
...
then
Hand full of coincidences that no one else in the
world can do – independent reco + signal
Add independent evidence for neutrinos to radio
signals

26
Drill options for large array
Findings from 2 drilling workshops held in Madison 2008
Current line of thoughts:
down to
200m
depth
at reasonable cost
Dry holes much easier
than wet holes.

27
Road forward
Use last holes/seasons for
prototype sensor co-deployment
tests of digitization strategies
instrumentation for further site studies
e.g. retrievable sensors and radio pingers
find coincidences of air shower radio with IceTop
Aim for dedicated (dry) holes to test
Deployment methods
Couplings of sensors with holes
Assume maximum drilling depth of up to 200m (cost)
acoustic scattering might help reduce previously
diverging vertical demands

28
Clarify role of non-IceCube members 2009
Start „Letter of Intent“ (LOI) at R&D workshop in June and
sign in fall 2009 to demonstrate:
serious intent of signing groups (FAs)
scientific importance
long term time scenario and milestones
Finish basic exploration of ice properties (season 09/10)
Start extensive MC studies (fall 09)
Track down number of different detector options (2010)
Write „Proposal“ for submission to FA‘s early 2011
expand letter of intent based on MC and hardware studies
scalable design plan and 2 phase structure
work out realistic budget plan
Near term time line

29
Hole 36, -250 m
Hole 57, -288 m
Immediate future with AURA
More RFI studies
new stronger transmitter
⇒ first inter-cluster calibration source

30
Radio attenuation: Plans for
direct on-site measurements
AURA
or
AURA
AURA
Options:
2. Frozen-In Tx and Rx
+ good coupling; – fixed position
3. IceCube holes pre-deployment
+ many depths; – water coupling
Previous pinging with RICE
direct signal path
signal path with total reflection

31
Ice attenuation (shallow, horizontal)
Coincidences with IceCube/IceTop
South pole RFI map vs. time
Possibly produce limit on GZK neutrinos:
Sensitivity calibration
Life time
Simulation
To-Do list radio

32
Attenuation (if scattering) strongly frequency
dependent
Test with broadband pinger
Confirm attenuation in perpendicular direction
No transients below ~300 m
No sources? – Unlikely
Mechanism quieting deep sources (relevant to radio?)
Lower pinger to deeper depths (~1000 m)
New set of pinger runs in 2009/2010!
Collect data needed to publish ice properties
Season 09/10 plans for acoustic

33
Detector design considerations
Sensors:
Frequency range and band width
Antennas type
Geometry:
Shadowing effect
→ Deep deployment
Ice Temperature
→ Shallow deployment
Drilling cost and time
→ Shallow deployment
Hole diameter can limit
antenna design
Wet/dry hole
Unique signature of Askaryan:
short pulse, linearly polarized
- Capture polarization?
- Low freq has wider signal
cone but more noise
- Narrow holes effect design
dense shallow versus sparse deep

34
Case study IceRay
– fully digitized waveforms, 50 km
2
Comparison: High density, shallow (50 m) versus sparse, deep (200m )
3-9 GZKs per year (“standard flux”), 0.3-2 coincidences with IceCube
⇒ develop plan to scale beyond 100 km

Back to top


2
by factors

35
Example for technology choices
Pulse shaping and triggering
versus waveform capture

Back to top


shaped pulse
AURA

Back to top


waveform
Short Bipolar Pulse
“Antenna-like” Transient
If only envelope gets sent to surface:
Digitization speed can be lowered
➔ towards demands of air shower radio and acoustic
no interference with several antennas in a hole
➔ use loop through signal cable
Only feasible if RFI is well behaved

36
Data acquisition considerations

Back to top


fully digitized waveform array
Pros:
+ good timing, full frequency info
+ Method proven by ANITA and RICE
Cons:
– Expensive, more complicated units
– power consumption
Challenges:
Handling large amount of data

Back to top


Pulse shaping & envelope trigger
Pros:
+ cheaper units → large array
+ Simpler detector
Cons:
– Limited information
Challenges:
information sufficient to reject
background and detect GZKs ?

37
Look-back buffer read-out for
detector components (here surface)

38
Sensor String Configuration (here: in ice radio)
CM Chokes
(Sets Dipole length)
“Bottle Brush”
Clip-on Antenna Elements
(Allows Reel Deployment)
TDA Node 1
TDA Node 2

Back to top


“Common Mode” TDA
Node:
- Signal Cable Shield = Antenna Element
- Envelope BW minimizes crosstalk
- Multi-sensors on one cable possible
- Azimuthal asymmetry is avoided
~1” diameter bump in cable
~500 mW power consumption
Hole
RF IN
ENV.
OUT
Gain
Envelope
Circuit
PWR
TDA OUTPUTS
Multi-Pair Cable
TDA Rev2

39
Technology choices
DAQ and triggering strategy
pulse shaping versus waveforms
simple local threshold versus local clusters
with phased array type of trigger
Energy distribution
centralized with cables
local with solar panels, wind, peltier effect
Signal propagation to central hub
cable versus wifi (Auger style)
Surface antennas in self trigger mode
versus trigger from IceTop and in ice radio

40
Conclusions & Outlook
Site exploration
very prolific (several publications in pipeline)
Short attenuation length in acoustics
→ Askaryan radio primary driver
Hybrid option being reevaluated
Upcoming seasons to clarify
deployment options (depth, dry/wet)
choice of pulse shaping, trigger, digitization
Institutional responsibilities to be worked
out at upcoming R&D meeting
... head out to extend IceCube and IceTop
by factors at the EHE frontier

41
Thank you!

42
Backup
Backup

43
Use IceCube’s resources: holes, comm. and power
• Each Cluster contains:
Digital Radio Module (DRM) – Electronics
4 Antennas
1 Antenna Calibration Unit (ACU)
Signal conditioning and amplification happen
at the front end
Signal is digitized and triggers formed in DRM
A cluster uses standard IceCube sphere, DOM
main board and surface cable lines.

Back to top


surface

Back to top


junction
box

Back to top


Counting
house
AURA Radio Cluster
A
skaryan Under ice Radio A
rray

44
AURA Radio Cluster
What’s new in the last season
An array of 5 clusters:
2 clusters 2006-2007
+3 clusters 2008-2009
(part of the of the NARC initiative)
2 channels (“antennas”) down to 100MHz
15/20 channels are working
Stronger and/or more sophisticated in ice
pulsers (support CW and pulses)
IceCube-like DAQ (based on pdaq)
Strong surface pulser
Shallow (~300m)
Deep (~1400 m)

45
From Utrecht premeeting
Possible near term timeline:2008-2009-2010
-
Working group and collaboration building -> in progress
-
Write „Letter of Intent“ and sign in spring 2009 to demonstrate:
serious intention of signing groups to in- and out-side world (FA)
scientific importance in comparison to other topics
expected improvement to previous experiments
time scenario and milestones (Hawaii, identify man power)
- Finish basic exploration of ice properties (existing hardware, new deploy?)
-
Agree on deployment scheme already here (?)
-
Start extensive MC studies of different detector options (using above)
-
Start sensor and electronic prototyping
-
Track down number of different detector options based on above
results (earlier?)
- Write „Proposal“ for submission to FA‘s end 2010 (realistic ?)
expand letter of intent to give detailed information
based on extensive MC and hardware studies
still goes with flexible design plan and 2 phase structure
works out realistic budget plan

46
Askaryan Signal
Cherenkov angle=55.8
o
Electric Field angular distributionElectric Field frequency spectrum
A
s
t
r
o
-
ph
/
9
9
0
1
2
7
8
A
l
v
a
r
e
z
-
M
un
i
z,
V
a
z
qu
e
z,
Z
a
s
1
9
9
9

47
Example Transient
(from snowmobile ignition)

Back to top


Ignition noise transients from idling snowmobile
Snowmobile was approximately 100m distance from ICL.
Snowmobile was perpendicular with West tower.
Signals as acquired by ic-scope-ag1
Time Delay=20ns W-E, consistent with Angle-of-Arrival (AOA)

Back to top


Transient

Back to top


Wavefront

Back to top


Snowmobile
(transient source)
West

Back to top


tower
East

Back to top


tower
View of snowmobile
from ICL Door
Delta t =20ns

48
Transient sensor array
Kael Hanson
Perry Sandstorm
Many “simple” sensors to provide a snap shot of an Askaryan pulse.
Wide dynamic range, low power, simple output

49
Case study: Transient Detector Footprints
500m x 500m
sensor
20 km
spacing shown
2
0
k
m
“Kilocube”
100km
2
IceCube
IceRay
18,36
“Kilocube”
# of Sensors vs. Density:
333
1000
1200
333
333
3600
500
500
1600
1000
1000
400

Back to top


Total # of

Back to top


Sensors
Y
Spacing
(meters)
X
Spacing
(meters)

50
Downward Rejection
via Priority, Coincidence

Back to top


Real-Time, Simplest “Elevation Gating”

Back to top


TDA (A)

Back to top


TDA (B)
A
B
A
B
A
B
d
~40m
Lowest Detectable
Neutrino
Trajectory
(93 degree zenith)
Surface
Transients

Back to top


Reject

Back to top


Accept

Back to top


Accept
Time Difference Of Arrival (TDOA)
Highest Detectable
Neutrino Trajectory
(36 degree zenith)
Surface Processor

51
SATRA Functional Blocks
(Sensor Array for Transient Radio
Astrophysics)

52
Radio Transient Sensor Instrumentation
Baseline Configuration
~150m
Surface
Firn
Ice
~190m

Back to top


Active Antennas
with Envelope

Back to top


Outputs

Back to top


(TDAs)

Back to top


Surface
Processor
Assembly
(SPA)
4” Dry
10MHz Clock
Data (RS485)
Slow Ctrl

Back to top


SPA of
Next Hole
1
2
Row
DAQ

Back to top


Envelopes
sent to

Back to top


surface
TDOA =
T
ime-
D
ifference-
O
f-
A
rrival
TOT =
T
ime-
O
ver-
T
hreshold
Elevation ≈
TDOA
Between TDAs (z)
Azimuth ≈
TDOA
Between Holes (d)
Amplitude ≈
TOT
of Envelopes
?
Elevation is determined in real time for each hit at each hole.
?
Azimuth and event signature uses elevation and amplitude
data from all holes hit.
?
Its all in the timing.
“z”
“d”

53
Sensor Array System-Level R&D
Source modeling
Nominal array sizes needed for event detection and/or limits
Array geometry optimization
Vertical, Horizontal spacing
Number of sensors per string
Size of Array
Sensitivity Analysis
Antenna bandwidth
Envelope/discriminator bandwidth
Noise; KT, RFI, CR
Optimized data format for transmission, filtering, storage
Event simulation and filtering
Data processing requirements for online filtering
DAQ for each row and combiner from all row-DAQs

54
Example data from each hole

Back to top


Course Time

Back to top


From

Back to top


Masterclock
LSB= 10ns
Range=100us

Back to top


Fine Times

Back to top


From Time-Digital-Converter
(TDC)

Back to top


LSB=250ps
Range=500ns
8bits
14bits
14bits
8bits

Back to top


Hole

Back to top


Address
TDA1
Rise

Back to top


TDA1
TOT

Back to top


TDA2
Rise

Back to top


TDA2
TOT
14bits
8bits
TDA 3,4, etc
Compare TOT
(amplitudes)
for
“hit quality”
Compare TOAs for
Elevation Angle

55
Sensor String Baseline Configuration
CM Chokes
(Sets Dipole length)
“Bottle Brush”
Clip-on Antenna Elements
(Allows Reel Deployment)
TDA Node 1
TDA Node 2

Back to top


“Common Mode” TDA
Node:
- Signal Cable Shield = Antenna Element
- Envelope BW minimizes crosstalk
- Multi-sensors on one cable possible
- Azimuthal asymmetry is avoided
~1” diameter bump in cable
~500 mW power consumption
Hole
RF IN
ENV.
OUT
Gain
Envelope
Circuit
PWR
TDA OUTPUTS
Multi-Pair Cable
TDA Rev2

56
Sensor String Development
separable activities/disciplines by color
TDA PCB
Circuit topology
Parts selection
Schematic Capture
PCB layout, potting, mechanical attachment
Spice optimization of antenna match
Common Mode Antenna
XFTD modeling of elevation response
NEC modeling of elevation response
Cable
Spice or Qucs simulation of envelope transmission
String fabrication and deployment

57
SPA
(Ele
B
vat
a
ion
s
b
e
y h
l
i
i
-r
n
es
e
TDO
C
A,
o
Am
n
pli
f
tu
i
d
g
e
u
by
r
TO
a
T)
tion
Discriminator
Discriminator

Back to top


Envelope

Back to top


Signals

Back to top


Upper
TDA

Back to top


Lower
TDA
Threshold
START
STOP CH1
STOP CH2
TOT
Time-Digital
Converter (TDC)
4-fold stops/ch
65ps bin size
Min 200ns window
ALU
Hit Processor
Hit Buffer
Elevation
& Coinc.
Fine Time
Data

Back to top


Coarse Time
(x10) Master clock
TDC

Back to top


Settings

Back to top


Buffered Hit Data

Back to top


Serializer
Get Data

Back to top


Master Clock Pair

Back to top


Data Pair

Back to top


Slow Control
Pair
TDOA

Back to top


Adjacent
SPAs

58
SPA Development
separable activities/disciplines by color
Surface Cable and Interface
Discriminator
TDC (or simple elevation gate for ’09-’10
expmt)
Hit Processor (µProcessor or FPGA)
PLL & Course-Time Counter
Data Format and Buffer
DC-DC Converter/ Head-end PSU requirements
Enclosure and Integration

59
SATRA South Pole Testing
Proof of Concept for Envelope Detection
’08-’09 (done)
Goals:
Show feasibility of TDOA technique for background rejection using envelope signals from TDA
Setup:
Two TDAs connected to Horizontally-separated antennas on ICL Towers.
Enables:
Continued transient background monitoring with programmable oscilloscopes
Real-time elevation gating with vertically-separated TDAs
’09-’10
Goals:
Background Rate vs. (elevation & threshold)
Setup:
single test string in multiple IceCube firn and/or rod well holes, simplified SPA. Measure
sensitivity to surface and AURA transmitters
Enables:
comparison of candidate TDA / antenna configurations, verification of envelope discriminator
and basic elevation gating.
Small test array (3km x 1km); (~10x3 holes)
’11-’12
Goal:
(Rate & amplitude) vs (elevation & azimuth & threshold) DAQ verification
Setup:
Upgraded RAM Drill, 30 strings, 30 full-function SPAs, 30 surface links, 3 “Row” DAQs
Enables
: Verification of TDC and course timing circuitry, Optimization of SPA comms, initial sensitivity
calibration. Optimization of RAM drill. DAQ and filter testing, Optimize TDA-TDA and Hole-Hole spacing
Large test array (3km x 2km); (~10x6 holes) ’
12-’13
Goals:
Verify changes to RAM drill and Instrumentation; grid spacing should conform to final geometry
Apparatus:
Upgraded RAM drills, 60 strings, 60SPAs, 60 surface links, 6 Row DAQs
Enables:
verification of configurations and procedures for large-scale drilling and deployment, Establish
Flux Limits and possible event detection.
SATRA KiloCube (20km x 20km); (400-1600 holes)
‘13-’16
Goals:
Detect significant number of GZK events
Apparatus:
$15-20M
Enables:
Event detection and confirmation by spatiotemporal signature.

60
Envelope / TDA Proof-of-Concept Testing
South-Pole 08-09
Ignition noise transients from idling snowmobile
Snowmobile was approximately 100m distance from ICL.
Snowmobile was perpendicular with West tower.
Signals as acquired by ic-scope-ag1
Time Delay=20ns W-E, consistent with Angle-of-Arrival (AOA)

Back to top


Transient

Back to top


Wavefront

Back to top


Snowmobile
(transient source)
West

Back to top


tower
East

Back to top


tower
View of snowmobile
from ICL Door
Delta t =20ns

61
Sensor experiment for ’09-’10
Rate vs. (Threshold, Elevation)
Goals:
Test Common-Mode antenna/TDA design
Optimize envelope/discriminator parameters for rejection of
background transients by virtue of their elevation
Get low-threshold data regarding SP background transients
Basic vertical string with two Rev2 TDAs
Temporary, self-contained apparatus (e.g. battery powered)
Can be moved from hole-hole (e.g. IC firn holes before drilling)
Simplified Surface Processor (SPA)
Acquires background rates vs. (threshold, elevation)
Simplified design allows low thresholds with ~MHz hit rates
Threshold scan is repeated at each elevation increment.
Complete threshold/elevation scan should take a few hours.

62
Simplified SPA -Elevation Scan for ’09-’10

Back to top


Disc-A

Back to top


Disc-B

Back to top


T= 200ns (Max TDOA for z= 40m)

Back to top


Variable delay

Back to top


of PW-A

Back to top


AND Output

Back to top


PW-A = PW-B
Variable Delay Range≈ “elevation range”
Mono ~10ns
Mono ~10ns
Variable Delay
Mono 100ns
Elevation
Setting
Rate
Output
0
Threshold
Setting
2
1
3
4

Back to top


Rate Output
1
2
3
4
5
5
A
B

Back to top


Envelope
s
From
Hole
40m
Resolution
Setting
Pulse width≈ “elevation resolution”
TDOA

63
Askaryan pulses from air
shower core

Back to top