Search results for "Ultra violet"

showing 3 items of 3 documents

Electrodeless HF-lamps as UV and VUV light sources

2002

The paper is devoted to problems of employment of high- frequency electrodeless lamps as ultra violet (UV) and vacuum ultra violet (VUV) light sources. Some aspects of lamp preparation technology for UV and VUV are considered. The technology, developed in our laboratory, allows to prepare HFEL-s filled with wide spread of chemical elements. Our experience shows that most important filling elements for UV and VUV spectral regions are Zn, Cd, Hg, Se, As, Sn and Pb, Sb, Bi, Tl, Te, I, H, Hg-Cd, Hg-Zn, Se-Te. The requirements for generators are discussed. Some important spectral characteristics of lamp examples are presented.

Cadmiumbusiness.industryAnalytical chemistrychemistry.chemical_elementUltra violetZincHafniumMercury (element)Vacuum ultravioletchemistryOptoelectronicsbusinessTelluriumSeleniumSPIE Proceedings
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2000

We report on lifetime measurements of the 3d(5)(S-6)4s4p(P-3)y P-6 degrees states of Fe II using time-resolved vacuum ultraviolet (VUV) laser spectroscopy. A laser-produced plasma has been used as the source of free Fe+ ions. The tunable VUV radiation was obtained employing resonantly enhanced sum-difference four-wave-mixing of short laser pulses. We obtained tau((6)P(3/2)degrees) = 3.90(20) ns, tau((6)P(5/2)degrees) = 3.80(20) ns and tau((6)P(7/2)degrees) = 3.65(20) ns.

PhysicsUltra violetPlasmaRadiationCondensed Matter PhysicsLaserAtomic and Molecular Physics and OpticsIonlaw.inventionVacuum ultravioletlawRadiative transferAtomic physicsSpectroscopyJournal of Physics B: Atomic, Molecular and Optical Physics
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Exploring the explosive-effusive transition using permanent ultraviolet cameras

2017

Understanding the mechanisms that cause effusive eruptions is the key to mitigating their associated hazard. Here, we combine results from permanent ultra-violet (UV) cameras, and from other geophysical observations (seismic very long period, thermal, and infrasonic activity), to characterize volcanic SO2 flux regime in the period prior, during, and after Stromboli's August-November 2014 effusive eruption. We show that, in the two months prior to effusion onset, the SO2 flux levels are two times average level. We explain this anomalously high SO2 regime as primarily determined by venting of rapidly rising, pressurized SO2-rich gas pockets, produced by strombolian explosions being more frequ…

event.disaster_typegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesExplosive materialUltra violetGeophysics010502 geochemistry & geophysics01 natural sciencesStrombolian eruptionVolcanic GasesGeophysicsEffusive eruptionFlux (metallurgy)VolcanoSpace and Planetary ScienceGeochemistry and PetrologyMagmaEarth and Planetary Sciences (miscellaneous)eventPetrologyGeology0105 earth and related environmental sciencesJournal of Geophysical Research: Solid Earth
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