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The top documents tagged [faraday discussions]
Atmospheric Aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions Keith Heidecorn Graduate Seminar in Atmospheric
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An Alamethicin Channel in a Lipid Bilayer(1)
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Biosphere Atmosphere Exchange 1) Directly emitted GHGs CO 2, CH 4, N 2 O 2) Chemical sources of GHGs and SOA BVOCs CO CO 2 BVOC aerosol 3) Effects
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Metal Catalyst Particles Smaller than 8 nm Have Properties That Depend Strongly on Size Charles T. Campbell, D. E. Starr, J. T. Ranney, J. Larsen, S. C
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Time-of-flight Analysis of Hemispherical Deflection Analyzers Omer SISE 1 and Theo J.M. ZOUROS 2,3 1 Dept. of Science Education, Faculty of Education,
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Laboratory Studies of VUV CH 4 Photolysis and Reactions of the Resulting Radicals Robin Shannon, Mark Blitz, Mike Pilling, Dwayne Heard, Paul Seakins University
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Keith Heidecorn Graduate Seminar in Atmospheric Sciences April 7, 2014
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Electrons at Saturn’s moons: selected CAPS-ELS results A.J. Coates 1,2. G.H. Jones 1,2, C.S.Arridge 1,2, A. Wellbrock 1,2, G.R. Lewis 1,2, D.T. Young 3,
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Wetting Dynamics of Hydrophobic and Structured Surfaces
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Royal Society of Chemistry RSC Journals and Databases CALIS 2nd Imported Database User Training Week, Dalian 11 May 2004 Dr Mike Hannant Key Account Manager
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Nucleation Mechanism Most common model: ¯Methane solvation shell is dodecahedral hydrate cage ¯Nucleation occurs by aggregation of dodecahedral water cages
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