about
Elemental composition and clustering behaviour of α-pinene oxidation products for different oxidation conditionsAtmospheric benzenoid emissions from plants rival those from fossil fuelsDetection of plant volatiles after leaf wounding and darkening by proton transfer reaction "time-of-flight" mass spectrometry (PTR-TOF)Effect of dimethylamine on the gas phase sulfuric acid concentration measured by Chemical Ionization Mass SpectrometryAn ecosystem-scale perspective of the net land methanol flux: synthesis of micrometeorological flux measurementsGap-filling strategies for annual VOC flux data setsLeaf and ecosystem response to soil water availability in mountain grasslands.Oxidation products of biogenic emissions contribute to nucleation of atmospheric particles.Facing the Future: Effects of Short-Term Climate Extremes on Isoprene-Emitting and Nonemitting Poplar.Effects of heat and drought stress on post-illumination bursts of volatile organic compounds in isoprene-emitting and non-emitting poplarIon-induced nucleation of pure biogenic particles.Reduced anthropogenic aerosol radiative forcing caused by biogenic new particle formation.Airborne observations of vegetation and implications for biogenic emission characterization.Insight into acid-base nucleation experiments by comparison of the chemical composition of positive, negative, and neutral clusters.Role of sulphuric acid, ammonia and galactic cosmic rays in atmospheric aerosol nucleation.Neutral molecular cluster formation of sulfuric acid-dimethylamine observed in real time under atmospheric conditions.Characterization of a BAHD acyltransferase responsible for producing the green leaf volatile (Z)-3-hexen-1-yl acetate in Arabidopsis thaliana.Global atmospheric particle formation from CERN CLOUD measurements.Practical approaches to plant volatile analysis.Organosulfates as tracers for secondary organic aerosol (SOA) formation from 2-methyl-3-buten-2-ol (MBO) in the atmosphereThe effect of acid-base clustering and ions on the growth of atmospheric nano-particlesMolecular understanding of atmospheric particle formation from sulfuric acid and large oxidized organic moleculesBVOC fluxes above mountain grasslandDealing with disjunct concentration measurements in eddy covariance applications: a comparison of available approaches.Qualitative and quantitative characterization of volatile organic compound emissions from cut grass.Eddy covariance VOC emission and deposition fluxes above grassland using PTR-TOF.Biotic, abiotic and management controls on methanol exchange above a temperate mountain grasslandMeasuring eddy covariance fluxes of ozone with a slow-response analyser.Acetaldehyde exchange above a managed temperate mountain grassland.Deposition Fluxes of Terpenes over GrasslandThe role of low-volatility organic compounds in initial particle growth in the atmosphere.First observation of a potential non-invasive breath gas biomarker for kidney function.Real-time monitoring of herbivore induced volatile emissions in the field.On-line monitoring of microbial volatile metabolites by proton transfer reaction-mass spectrometry.On the use of Tedlar® bags for breath-gas sampling and analysis.Buffered end-tidal (BET) sampling-a novel method for real-time breath-gas analysis.Quantitative determination of biogenic volatile organic compounds in the atmosphere using proton-transfer reaction linear ion trap mass spectrometry.Molecular understanding of sulphuric acid-amine particle nucleation in the atmosphere.Contribution of different carbon sources to isoprene biosynthesis in poplar leaves.Transient release of oxygenated volatile organic compounds during light-dark transitions in Grey poplar leaves.
P50
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P50
description
hulumtues
@sq
onderzoeker
@nl
researcher
@en
հետազոտող
@hy
name
Armin Hansel
@ast
Armin Hansel
@en
Armin Hansel
@es
Armin Hansel
@nl
Armin Hansel
@sl
type
label
Armin Hansel
@ast
Armin Hansel
@en
Armin Hansel
@es
Armin Hansel
@nl
Armin Hansel
@sl
prefLabel
Armin Hansel
@ast
Armin Hansel
@en
Armin Hansel
@es
Armin Hansel
@nl
Armin Hansel
@sl
P1053
F-3915-2010
P106
P21
P31
P3829
P496
0000-0002-1062-2394