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E. T. Arakawa

Researcher at Oak Ridge National Laboratory

Publications -  115
Citations -  3717

E. T. Arakawa is an academic researcher from Oak Ridge National Laboratory. The author has contributed to research in topics: Surface plasmon & Plasmon. The author has an hindex of 31, co-authored 115 publications receiving 3603 citations.

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Optical constants of organic tholins produced in a simulated Titanian atmosphere: From soft x-ray to microwave frequencies

TL;DR: In this paper, the real and imaginary parts of the complex refractive index of thin films of the dark reddish organic solids called tholins, produced by continuous D.C. discharge through a 0.9 N2/0.1 CH4 gas mixture at 0.2 mb, were determined from a combination of transmittance, specular reflectance, interferometric, Brewster angle, and ellipsometric polarization measurements.
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Amino acids derived from Titan tholins

TL;DR: The results suggest that episodes of liquid water in the past or future of Titan might lead to major further steps in prebiological organic chemistry on that body.
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Optical and dielectric properties of DNA in the extreme ultraviolet

TL;DR: In this article, the optical constants of dry films of deoxyribonucleic acid (sodium salt of calf thymus DNA) have been determined in the 2 −82 eV region of photon energy.
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Production and Optical Constants of Ice Tholin from Charged Particle Irradiation of (1:6) C2H6/H2O at 77 K

TL;DR: In this article, 50 separate irradiations of a 6:1 mixture of H2O/C2H6 ice conducted over a 5-month period have yielded sufficient tholin for the determination of its physical constants in the 006 to 40 micron range while the imaginary part of the refractive index k was obtained by transmission measurements on thin-film samples and Kramers-Kronig analysis (KKA).
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Polycyclic aromatic hydrocarbons in the atmospheres of Titan and Jupiter.

TL;DR: Incompletely characterized complex organic solids (tholins) produced by irradiating simulated Titan atmospheres reproduce well the observed UV/visible/IR optical constants of the Titan stratospheric haze.