Optical reflectance, optical refractive index and optical conductivity measurements of nonlinear optics for l-aspartic acid nickel chloride single crystal

2013 ◽  
Vol 291 ◽  
pp. 304-308 ◽  
Author(s):  
G. Anbazhagan ◽  
P.S. Joseph ◽  
G. Shankar
Keyword(s):  
Refractive Index ◽  
Nonlinear Optics ◽  
Single Crystal ◽  
Aspartic Acid ◽  
Optical Conductivity ◽  
Nickel Chloride ◽  
Conductivity Measurements ◽  
Optical Reflectance

Refractive index measurements on bismuth tellurium oxide (Bi2TeO5) single crystal

1992 ◽  
Vol 1 (3) ◽  
pp. 161-164 ◽  
Author(s):  
G. Mandula ◽  
L. Kovács ◽  
Á. Péter ◽  
E. Hartmann
Keyword(s):  
Refractive Index ◽  
Single Crystal ◽  
Tellurium Oxide

scholarly journals Free-carrier dynamics in Au2Pb probed by optical conductivity measurements

2018 ◽  
Vol 30 (48) ◽  
pp. 485403 ◽  
Author(s):  
R Kemmler ◽  
R Hübner ◽  
A Löhle ◽  
D Neubauer ◽  
I Voloshenko ◽  
...  
Keyword(s):  
Optical Conductivity ◽  
Free Carrier ◽  
Carrier Dynamics ◽  
Conductivity Measurements

An Ocean Refractometer: Resolving Millimeter-Scale Turbulent Density Fluctuations via the Refractive Index

2006 ◽  
Vol 23 (1) ◽  
pp. 121-137 ◽  
Author(s):  
Matthew H. Alford ◽  
David W. Gerdt ◽  
Charles M. Adkins
Keyword(s):  
Refractive Index ◽  
Density Fluctuations ◽  
Inertial Subrange ◽  
Conductivity Measurements ◽  
Velocity Fluctuations ◽  
Fiber Motion ◽  
Turbulent Spectrum ◽  
Ocean Measurements ◽  
Fiberoptic Sensor ◽  
Better Than

Abstract A fiberoptic sensor has been constructed to measure oceanic density fluctuations via their refractive index signature. The resolution (Δz = 1 mm, Δt = 0.2 ms) and precision (Δn < 10−8, Δρ = 3.4 × 10−5 kg m−3) of the device are far better than other methods and are sufficient to resolve the entire turbulent spectrum. Spectra show the salinity Batchelor rolloff at levels undetectable via conductivity measurements. However, the low-wavenumber portion of the spectrum occupied by the turbulent inertial subrange (≈1 m–1 cm scales) is marred by noise resulting from fiber motion in response to turbulent velocity fluctuations. The technique is described, and the first ocean measurements are reported.

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