A large source of low-volatility secondary organic aerosol. - Wikidata - wikimedia - TriplyDB

A large source of low-volatility secondary organic aerosol.

A large source of low-volatility secondary organic aerosol.

http://www.wikidata.org/entity/Q46927137

about

Identification and quantification of carbonyl-containing alpha-pinene ozonolysis products using O-tert-butylhydroxylamine hydrochloride Diel Variation of Biogenic Volatile Organic Compound Emissions--A field Study in the Sub, Low and High Arctic on the Effect of Temperature and Light Unexpected seasonality in quantity and composition of Amazon rainforest air reactivity The future of airborne sulfur-containing particles in the absence of fossil fuel sulfur dioxide emissions Perturbations in the carbon budget of the tropics Polluted dust promotes new particle formation and growth.Highly functionalized organic nitrates in the southeast United States: Contribution to secondary organic aerosol and reactive nitrogen budgets.Atmospheric science: Unexpected player in particle formation.Oil sands operations as a large source of secondary organic aerosols.Combustion Chemistry Diagnostics for Cleaner Processes.Reduced anthropogenic aerosol radiative forcing caused by biogenic new particle formation.Global distribution of particle phase state in atmospheric secondary organic aerosols Secondary organic aerosol formation and organic nitrate yield from NO3 oxidation of biogenic hydrocarbons.Production of extremely low volatile organic compounds from biogenic emissions: Measured yields and atmospheric implications.Kinetics of a Criegee intermediate that would survive high humidity and may oxidize atmospheric SO2 Triggering of myocardial infarction by increased ambient fine particle concentration: Effect modification by source direction.Formation and evolution of molecular products in α-pinene secondary organic aerosol The quasi-unchanged gas-phase molecular structures of the atmospheric aerosol precursor β-pinene and its oxidation product nopinone.Atmospheric gas-to-particle conversion: why NPF events are observed in megacities?The effect of acid-base clustering and ions on the growth of atmospheric nano-particles Characterization of Highly Oxidized Molecules in Fresh and Aged Biogenic Secondary Organic Aerosol Photosensitized Formation of Secondary Organic Aerosols above the Air/Water Interface.Molecular-scale evidence of aerosol particle formation via sequential addition of HIO3.Hydroxyl radical-induced formation of highly oxidized organic compounds.Influence of vapor wall loss in laboratory chambers on yields of secondary organic aerosol.Sesquiterpene emissions from Alternaria alternata and Fusarium oxysporum: Effects of age, nutrient availability, and co-cultivation.Cloud Activation Potentials for Atmospheric α-Pinene and β-Caryophyllene Ozonolysis Products.Health effects of carbon-containing particulate matter: focus on sources and recent research program results.Introductory lecture: atmospheric chemistry in the Anthropocene.Water diffusion in atmospherically relevant α-pinene secondary organic material.The effect of gas-phase polycyclic aromatic hydrocarbons on the formation and properties of biogenic secondary organic aerosol particles.Spiers Memorial Lecture. Introductory lecture: chemistry in the urban atmosphere.OH reactivity in urban and suburban regions in Seoul, South Korea - an East Asian megacity in a rapid transition.New particle formation and growth from methanesulfonic acid, trimethylamine and water.Atmospheric fates of Criegee intermediates in the ozonolysis of isoprene.Molecular composition of organic aerosols at urban background and road tunnel sites using ultra-high resolution mass spectrometry.Traffic is a major source of atmospheric nanocluster aerosol.Surface behavior of amphiphiles in aqueous solution: a comparison between different pentanol isomers.Long-term (2001-2013) observations of water-soluble dicarboxylic acids and related compounds over the western North Pacific: trends, seasonality and source apportionment.Environmental conditions regulate the impact of plants on cloud formation.

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P2860

A large source of low-volatility secondary organic aerosol.

http://www.wikidata.org/entity/Q46927137

description

2014 nî lūn-bûn

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2014年の論文

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2014年学术文章

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2014年学术文章

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2014年学术文章

@zh-cn

2014年学术文章

@zh-hans

2014年学术文章

@zh-my

2014年学术文章

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2014年學術文章

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2014年學術文章

@zh-hant

name

A large source of low-volatility secondary organic aerosol.

@en

A large source of low-volatility secondary organic aerosol.

@nl

type

label

A large source of low-volatility secondary organic aerosol.

@en

A large source of low-volatility secondary organic aerosol.

@nl

prefLabel

A large source of low-volatility secondary organic aerosol.

@en

A large source of low-volatility secondary organic aerosol.

@nl

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P1476

A large source of low-volatility secondary organic aerosol.

@en

P2093

Douglas R Worsnop

http://www.w3.org/2001/XMLSchema#string

Einhard Kleist

http://www.w3.org/2001/XMLSchema#string

Felipe Lopez-Hilfiker

http://www.w3.org/2001/XMLSchema#string

Iida Pullinen

http://www.w3.org/2001/XMLSchema#string

Ismail-Hakki Acir

http://www.w3.org/2001/XMLSchema#string

Jürgen Wildt

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Lasse B Nielsen

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Manjula Canagaratna

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Monika Springer

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Ralf Tillmann

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476-479

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scholarly article

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10.1038/NATURE13032

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7489

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506

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Matti P Rissanen

Juha Kangasluoma

Heikki Junninen

Veli-Matti Kerminen

Tuukka Petäjä

Siegfried Schobesberger

Henrik G Kjaergaard

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2014-02-01T00:00:00Z

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24572423

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