It has been postulated that secondary organic particulate matter plays a pivotal role in the early growth of newly formed particles in forest areas. The recently detected class of extremely low volatile organic compounds (ELVOC) provides the missing organic vapors and possibly contributes a significant fraction to atmospheric SOA (secondary organic aerosol). The sequential rearrangement of peroxy radicals and subsequent O2 addition results in ELVOC which are highly oxidized multifunctional molecules (HOM). Key for efficiency of such HOM in early particle growth is that their formation is induced by one attack of the oxidant (here O3), followed by an autoxidation process involving molecular oxygen. Similar mechanisms were recently observed a...
Oxidation by hydroxyl radical (OH) and ozonolysis are the two major pathways of daytime biogenic vol...
We present a hypothesis that autoxidation (inter- and intramolecular hydrogen abstraction by peroxy ...
Aromatic hydrocarbons contribute significantly to tropospheric ozone and secondary organic aerosols ...
It has been postulated that secondary organic particulate matter plays a pivotal role in the early g...
It is generally assumed that isoprene-derived secondary organic aerosol (SOA) precursors are mainly ...
Terpenes are emitted by vegetation, and their oxidation in the atmosphere is an important source of ...
Terpenes are emitted by vegetation, and their oxidation in the atmosphere is an important source of ...
Recent advances in chemical ionization mass spectrometry have allowed the detection of a new group o...
It is generally assumed that isoprene-derived secondary organic aerosol (SOA) precursors are mainly ...
Explaining the formation of secondary organic aerosol is an intriguing question in atmospheric scien...
Highly oxygenated organic molecules (HOM) are found to play an important role in the formation and g...
Recent advances in chemical ionization mass spectrometry have allowed the detection of a new group o...
NO3 radical oxidation of most monoterpenes is a significant source of secondary organic aerosol (SOA...
Understanding secondary organic aerosols (SOA) is important because of their impact onclimate and hu...
Highly oxidized multifunctional organic molecules (HOMs) are a newly-found class of compounds that a...
Oxidation by hydroxyl radical (OH) and ozonolysis are the two major pathways of daytime biogenic vol...
We present a hypothesis that autoxidation (inter- and intramolecular hydrogen abstraction by peroxy ...
Aromatic hydrocarbons contribute significantly to tropospheric ozone and secondary organic aerosols ...
It has been postulated that secondary organic particulate matter plays a pivotal role in the early g...
It is generally assumed that isoprene-derived secondary organic aerosol (SOA) precursors are mainly ...
Terpenes are emitted by vegetation, and their oxidation in the atmosphere is an important source of ...
Terpenes are emitted by vegetation, and their oxidation in the atmosphere is an important source of ...
Recent advances in chemical ionization mass spectrometry have allowed the detection of a new group o...
It is generally assumed that isoprene-derived secondary organic aerosol (SOA) precursors are mainly ...
Explaining the formation of secondary organic aerosol is an intriguing question in atmospheric scien...
Highly oxygenated organic molecules (HOM) are found to play an important role in the formation and g...
Recent advances in chemical ionization mass spectrometry have allowed the detection of a new group o...
NO3 radical oxidation of most monoterpenes is a significant source of secondary organic aerosol (SOA...
Understanding secondary organic aerosols (SOA) is important because of their impact onclimate and hu...
Highly oxidized multifunctional organic molecules (HOMs) are a newly-found class of compounds that a...
Oxidation by hydroxyl radical (OH) and ozonolysis are the two major pathways of daytime biogenic vol...
We present a hypothesis that autoxidation (inter- and intramolecular hydrogen abstraction by peroxy ...
Aromatic hydrocarbons contribute significantly to tropospheric ozone and secondary organic aerosols ...