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Surface Wave Propagation
Preliminary work developing a method for surface wave detection
Amy ZhengAndrew Johnanneson
Ultrahigh Energy Neutrino Detection•Particles with velocity >
will emit radiation due to the Askaryan effect [1]
•Detection is difficult due to internally reflected waves dying off quickly[2]
phasev
Surface Waves as an Detection Tool
•Radiation from Askaryan cascade is trapped in Air-dielectric layer between ice and firn [2]
•In tandem with existing experiments RICE [3]
and ANITA [4]
Why Use Surface Waves?
•Surface waves travel between two mediums[5]
▫Amplitudes fall at the rate ▫Attenuation length times > bulk
waves•~800 times more efficient than bulk
waves•If detection is viable, expanding existing
experiments would be far less expensive•Surface waves may carry information
about neutrinos and their interactions with ice better than the current method
r
1
22
Procedure
•1 sending + 2 receiving antennas displayed waveshape
•Physically moved antennas to determine wavelength and thus index of refraction
Translating to refractive index
fc
v
cn
phase
n
n
C
Bn
2
2
1
(1)
(2)
Definition of Refractive Index
Sellmeier Equation
Refractive Index of Air
T1 T2 T3 T4
Avera
ge
Calcu
late
d Ave
rage
Adjus
ted
Calcu
late
d Ave
rage rm
s0
0.4
0.8
1.2
1000 MHz1500 MHz
Calculated (2) 1000MHz & 1500MHz n=1.000273[6]
Single or Half λ
λ (
cm)
Refractive Index of Water (rms)
Surface Surface Surface
Surface Surface
Half
Surface In In
Surface Half Half
Surface Half In
0
0.2
0.4
0.6
0.8
1
1.2
1.4
1.6
1.8
2
750 MHz1000 MHz1500 MHz
Calculated (2) n~1.3333[7]
Single or Half λ
λ (
cm)
Refractive Index of NaCl (rms)
Surface Surface Surface
In Surface In In Air In0
0.2
0.4
0.6
0.8
1
1.2
1.4
1.6
1.8
1000 MHz1500 MHz
Single or Half λ
λ (
cm)
Calculated (2) n~1.544[8]
Refractive Index of Granulated Fused Silica (sand)
Surface Surface Surface
In Surface In In Air In0
0.2
0.4
0.6
0.8
1
1.2
1.4
1.6
1.8
2
1000 MHz1500 MHz
Calculated (2)1000MHz n= 1.73251 [9]Calculated (2) 1500MHz n= 1.73317
Single or Half λ
λ (
cm)
Refractive Index of Granulated Fused Silica (sand)
Surface Surface Surface
In Surface In In Air In0
0.2
0.4
0.6
0.8
1
1.2
1.4
1000 MHz1500 MHz
Calculated (2) 1000MHz n= 1.73251 [9]Calculated (2) 1500MHz n= 1.73317
Multiple λ
λ (
cm)
Measurement Complications•Mechanical water waves appeared to alter EM
waveform•Imprecise measurements due to hand & eye
observation•Sand and water tend to collect in the connectors•Angular error from planar disparity•Waveforms disappeared & reappeared on and off•Waveforms constantly shift amplitude•Background EM noise & reflections often
interfered
Future Steps
•Experiment using ice as a medium•Change antenna size; more precision•Change experimental scale
References
• [1] G.A. Askaryan, Sov. Phys. JETP 14, 441 (1961)• [2]J.P. Ralston, Phys. Rev. D 71, 011503 (2005)• [3] RICE Collaboration, I. Kravchenko et al., Astropart. Phys. 19, 15 (2003); S.
Razzaque, Sseunarine, D.Z. Besson, D.W. McKay, J.P. Ralston, and D. Seckel, Phys. Rev. D 65, 103002 (2002); Phys. Rev. D 69, 047101 (2004).
• [4] For information on ANITA, see http://www.phys.hawaii.edu/anita/.• [5] J. P. Ralston “An Experiment to Detect Surface Waves on Polar Ice” (2005)• [6] Philip E. Ciddor. Refractive index of air: new equations for the visible and
near infrared, Appl. Optics 35, 1566-1573 (1996) doi:10.1364/AO.35.001566• [7]P. Schiebener, J. Straub, J.M.H. Levelt Sengers and J.S. Gallagher, J. Phys.
Chem. Ref. Data 19, 677, (1990)• [8] Faughn, Jerry S., Raymond A. Serway. College Physics, 6th Edition. Toronto:
Brooks/Cole, 2003: 692.• [9] I. H. Malitson. Interspecimen Comparison of the Refractive Index of Fused
Silica, J. Opt. Soc. Am. 55, 1205-1208 (1965) doi:10.1364/JOSA.55.001205• [misc] Colloquium Notes from John P. Ralston• Refractive index calculations for relative reference only:
▫ n found for granulated fused silica was found using Sellmeier constants for solid fused silica; granulation affects density.
▫ Calculated n for water is for λ of 589.29 nm ▫ Calculated n for NaCl is for λ of 589 nm