نتایج جستجو برای: atmospheric oxidation

تعداد نتایج: 192737  

Journal: :The Journal of chemical physics 2013
V Seshan D Ullien A Castellanos-Gomez S Sachdeva D H K Murthy T J Savenije H A Ahmad T S Nunney S D Janssens K Haenen M Nesládek H S J van der Zant E J R Sudhölter L C P M de Smet

A high-temperature procedure to hydrogenate diamond films using molecular hydrogen at atmospheric pressure was explored. Undoped and doped chemical vapour deposited (CVD) polycrystalline diamond films were treated according to our annealing method using a H2 gas flow down to ~50 ml∕min (STP) at ~850 °C. The films were extensively evaluated by surface wettability, electron affinity, elemental co...

2006
T. M. VanReken J. P. Greenberg P. C. Harley A. B. Guenther J. N. Smith

Direct measurement of particle formation and growth from the oxidation of biogenic emissions T. M. VanReken, J. P. Greenberg, P. C. Harley, A. B. Guenther, and J. N. Smith Advanced Study Program, National Center for Atmospheric Research, Boulder, CO, USA Atmospheric Chemistry Division, National Center for Atmospheric Research, Boulder, CO, USA Received: 23 May 2006 – Accepted: 27 May 2006 – Pub...

Journal: :Nature communications 2011
Yasuhito Sekine Katsuhiko Suzuki Ryoko Senda Kosuke T Goto Eiichi Tajika Ryuji Tada Kazuhisa Goto Shinji Yamamoto Naohiko Ohkouchi Nanako O Ogawa Teruyuki Maruoka

Early Palaeoproterozoic (2.5-2.0 billion years ago) was a critical phase in Earth's history, characterized by multiple severe glaciations and a rise in atmospheric O(2) (the Great Oxidation Event). Although glaciations occurred at the time of O(2) increase, the relationship between climatic and atmospheric transitions remains poorly understood. Here we report high concentrations of the redox-se...

2015
Philip A. E. Pogge von Strandmann Eva E. Stüeken Tim Elliott Simon W. Poulton Carol M. Dehler Don E. Canfield David C. Catling

Neoproterozoic (1,000-542 Myr ago) Earth experienced profound environmental change, including 'snowball' glaciations, oxygenation and the appearance of animals. However, an integrated understanding of these events remains elusive, partly because proxies that track subtle oceanic or atmospheric redox trends are lacking. Here we utilize selenium (Se) isotopes as a tracer of Earth redox conditions...

Journal: :Journal of the Atmospheric Sciences 2016

Journal: :Proceedings of the National Academy of Sciences 2017

2017

This manuscript describes a laboratory study on the photo-oxidation of indole under low-NOx conditions. Secondary organic aerosols (SOA) were chemically characterize to determine the importance of indole chemistry in the formation of brown carbon (BrC) constituents. State of art analytical techniques (high-resolution mass spectrometers) used is this study, provide novel and important insights i...

Journal: :The journal of physical chemistry. A 2010
Adam W Birdsall John F Andreoni Matthew J Elrod

The products of the primary OH-initiated oxidation of toluene were investigated using the turbulent flow chemical ionization mass spectrometry technique under different oxygen, NO, and initial OH radical concentrations as well as a range of total pressures. The bicyclic peroxy radical intermediate, a key proposed intermediate species in the Master Chemical Mechanism (MCM) for the atmospheric ox...

2016
Xuxing Chen Yunpeng Li Xiaoyang Pan David Cortie Xintang Huang Zhiguo Yi

The search for active catalysts that efficiently oxidize methane under ambient conditions remains a challenging task for both C1 utilization and atmospheric cleansing. Here, we show that when the particle size of zinc oxide is reduced down to the nanoscale, it exhibits high activity for methane oxidation under simulated sunlight illumination, and nano silver decoration further enhances the phot...

2017
Stuart J. Daines Benjamin J. W. Mills Timothy M. Lenton

It is unclear why atmospheric oxygen remained trapped at low levels for more than 1.5 billion years following the Paleoproterozoic Great Oxidation Event. Here, we use models for erosion, weathering and biogeochemical cycling to show that this can be explained by the tectonic recycling of previously accumulated sedimentary organic carbon, combined with the oxygen sensitivity of oxidative weather...

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