Biogenic volatile organic compounds (BVOCs) contribute the majority of reactive organic
carbon to the atmosphere and lead to aerosol formation through reaction with atmospheric …

Determining which volatile organic compounds (VOCs) are synthesized by plants and
emitted into the atmosphere and at what rates is a critical component of our understanding of …

Secondary organic aerosol (SOA) is an important constituent of the atmosphere where SOA
particles are formed chiefly by the condensation or reactive uptake of oxidation products of …

Emissions from natural sources are driven by various external stimuli such as sunlight,
temperature, and soil moisture. Once biogenic volatile organic compounds (BVOCs) are …

The largest global source of secondary organic aerosol (SOA) in the atmosphere is derived
from the oxidation of biogenic emissions. Plant stressors associated with a changing …

Biogenic volatile organic compound (BVOC) emissions were studied using vegetation
enclosure experiments. Particular emphasis was given to sesquiterpene compounds (SQT) …

Biogenic Volatile Organic Compounds (BVOC) emitted from plants are the dominant source
of reduced carbon chemicals to the atmosphere and are important precursors to the …

Non-methane volatile organic compounds (VOCs) emitted from boreal peatland microcosms
were semiquantitatively determined using gas chromatography–mass spectrometry …

The concentrations of terpenoids (isoprene; monoterpenes, MTs; and sesquiterpenes,
SQTs) and oxygenated volatile organic compounds (OVOCs; ie aldehydes, alcohols …

Research on biogenic volatile organic compound (BVOC) emissions has mainly focused on
native species in natural ecosystems. However, much of the ozone and aerosol formation …