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Penglin Ye

Bio: Penglin Ye is an academic researcher from Carnegie Mellon University. The author has contributed to research in topics: Nucleation & Cloud condensation nuclei. The author has an hindex of 21, co-authored 27 publications receiving 2629 citations.

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Journal ArticleDOI
Joao Almeida1, Joao Almeida2, Siegfried Schobesberger3, Andreas Kürten1, Ismael K. Ortega3, Oona Kupiainen-Määttä3, Arnaud P. Praplan4, Alexey Adamov3, António Amorim5, F. Bianchi4, Martin Breitenlechner6, A. David2, Josef Dommen4, Neil M. Donahue7, Andrew J. Downard8, Eimear M. Dunne9, Jonathan Duplissy3, Sebastian Ehrhart1, Richard C. Flagan8, Alessandro Franchin3, Roberto Guida2, Jani Hakala3, Armin Hansel6, Martin Heinritzi6, Henning Henschel3, Tuija Jokinen3, Heikki Junninen3, Maija Kajos3, Juha Kangasluoma3, Helmi Keskinen10, Agnieszka Kupc11, Theo Kurtén3, Alexander N. Kvashin12, Ari Laaksonen10, Ari Laaksonen13, Katrianne Lehtipalo3, Markus Leiminger1, Johannes Leppä13, Ville Loukonen3, Vladimir Makhmutov12, Serge Mathot2, Matthew J. McGrath14, Tuomo Nieminen15, Tuomo Nieminen3, Tinja Olenius3, Antti Onnela2, Tuukka Petäjä3, Francesco Riccobono4, Ilona Riipinen16, Matti P. Rissanen3, Linda Rondo1, Taina Ruuskanen3, Filipe Duarte Santos5, Nina Sarnela3, Simon Schallhart3, R. Schnitzhofer6, John H. Seinfeld8, Mario Simon1, Mikko Sipilä3, Mikko Sipilä15, Yuri Stozhkov12, Frank Stratmann17, António Tomé5, Jasmin Tröstl4, Georgios Tsagkogeorgas17, Petri Vaattovaara10, Yrjö Viisanen13, Annele Virtanen10, Aron Vrtala11, Paul E. Wagner11, Ernest Weingartner4, Heike Wex17, Christina Williamson1, Daniela Wimmer1, Daniela Wimmer3, Penglin Ye7, Taina Yli-Juuti3, Kenneth S. Carslaw9, Markku Kulmala3, Markku Kulmala15, Joachim Curtius1, Urs Baltensperger4, Douglas R. Worsnop, Hanna Vehkamäki3, Jasper Kirkby1, Jasper Kirkby2 
17 Oct 2013-Nature
TL;DR: The results show that, in regions of the atmosphere near amine sources, both amines and sulphur dioxide should be considered when assessing the impact of anthropogenic activities on particle formation.
Abstract: Nucleation of aerosol particles from trace atmospheric vapours is thought to provide up to half of global cloud condensation nuclei(1). Aerosols can cause a net cooling of climate by scattering sun ...

738 citations

Journal ArticleDOI
Jasmin Tröstl1, Wayne Chuang2, Hamish Gordon3, Martin Heinritzi4, Chao Yan5, Ugo Molteni1, Lars Ahlm6, Carla Frege1, F. Bianchi5, F. Bianchi1, F. Bianchi7, Robert Wagner5, Mario Simon4, Katrianne Lehtipalo1, Katrianne Lehtipalo5, Christina Williamson8, Christina Williamson4, Christina Williamson9, J. S. Craven10, Jonathan Duplissy5, Jonathan Duplissy11, Alexey Adamov5, Joao Almeida3, Anne-Kathrin Bernhammer12, Martin Breitenlechner12, Sophia Brilke4, Antonio Dias3, Sebastian Ehrhart3, Richard C. Flagan10, Alessandro Franchin5, Claudia Fuchs1, Roberto Guida3, Martin Gysel1, Armin Hansel12, Christopher R. Hoyle1, Tuija Jokinen5, Heikki Junninen5, Juha Kangasluoma5, Helmi Keskinen9, Helmi Keskinen13, Helmi Keskinen5, Jaeseok Kim13, Jaeseok Kim9, Manuel Krapf1, Andreas Kürten4, Ari Laaksonen14, Ari Laaksonen13, Michael J. Lawler13, Michael J. Lawler15, Markus Leiminger4, Serge Mathot3, Ottmar Möhler16, Tuomo Nieminen11, Tuomo Nieminen5, Antti Onnela3, Tuukka Petäjä5, Felix Piel4, Pasi Miettinen13, Matti P. Rissanen5, Linda Rondo4, Nina Sarnela5, Siegfried Schobesberger5, Siegfried Schobesberger9, Kamalika Sengupta17, Mikko Sipilä5, James N. Smith18, James N. Smith13, Gerhard Steiner12, Gerhard Steiner19, Gerhard Steiner5, António Tomé20, Annele Virtanen13, Andrea Christine Wagner4, Ernest Weingartner1, Ernest Weingartner9, Daniela Wimmer4, Daniela Wimmer5, Paul M. Winkler19, Penglin Ye2, Kenneth S. Carslaw17, Joachim Curtius4, Josef Dommen1, Jasper Kirkby3, Jasper Kirkby4, Markku Kulmala5, Ilona Riipinen6, Douglas R. Worsnop5, Douglas R. Worsnop11, Neil M. Donahue2, Neil M. Donahue5, Urs Baltensperger1 
26 May 2016-Nature
TL;DR: It is shown that organic vapours alone can drive nucleation, and a particle growth model is presented that quantitatively reproduces the measurements and implements a parameterization of the first steps of growth in a global aerosol model that can change substantially in response to concentrations of atmospheric cloud concentration nuclei.
Abstract: About half of present-day cloud condensation nuclei originate from atmospheric nucleation, frequently appearing as a burst of new particles near midday. Atmospheric observations show that the growth rate of new particles often accelerates when the diameter of the particles is between one and ten nanometres. In this critical size range, new particles are most likely to be lost by coagulation with pre-existing particles, thereby failing to form new cloud condensation nuclei that are typically 50 to 100 nanometres across. Sulfuric acid vapour is often involved in nucleation but is too scarce to explain most subsequent growth, leaving organic vapours as the most plausible alternative, at least in the planetary boundary layer. Although recent studies predict that low-volatility organic vapours contribute during initial growth, direct evidence has been lacking. The accelerating growth may result from increased photolytic production of condensable organic species in the afternoon, and the presence of a possible Kelvin (curvature) effect, which inhibits organic vapour condensation on the smallest particles (the nano-Kohler theory), has so far remained ambiguous. Here we present experiments performed in a large chamber under atmospheric conditions that investigate the role of organic vapours in the initial growth of nucleated organic particles in the absence of inorganic acids and bases such as sulfuric acid or ammonia and amines, respectively. Using data from the same set of experiments, it has been shown that organic vapours alone can drive nucleation. We focus on the growth of nucleated particles and find that the organic vapours that drive initial growth have extremely low volatilities (saturation concentration less than 10(-4.5) micrograms per cubic metre). As the particles increase in size and the Kelvin barrier falls, subsequent growth is primarily due to more abundant organic vapours of slightly higher volatility (saturation concentrations of 10(-4.5) to 10(-0.5) micrograms per cubic metre). We present a particle growth model that quantitatively reproduces our measurements. Furthermore, we implement a parameterization of the first steps of growth in a global aerosol model and find that concentrations of atmospheric cloud concentration nuclei can change substantially in response, that is, by up to 50 per cent in comparison with previously assumed growth rate parameterizations.

507 citations

Journal ArticleDOI
Jasper Kirkby1, Jasper Kirkby2, Jonathan Duplissy3, Jonathan Duplissy4, Kamalika Sengupta5, Carla Frege6, Hamish Gordon2, Christina Williamson7, Christina Williamson1, Martin Heinritzi8, Martin Heinritzi1, Mario Simon1, Chao Yan4, Joao Almeida2, Joao Almeida1, Jasmin Tröstl6, Tuomo Nieminen4, Tuomo Nieminen3, Ismael K. Ortega, Robert Wagner4, Alexey Adamov4, António Amorim9, Anne-Kathrin Bernhammer8, F. Bianchi10, F. Bianchi6, Martin Breitenlechner8, Sophia Brilke1, Xuemeng Chen4, J. S. Craven11, Antonio Dias2, Sebastian Ehrhart1, Sebastian Ehrhart2, Richard C. Flagan11, Alessandro Franchin4, Claudia Fuchs6, Roberto Guida2, Jani Hakala4, Christopher R. Hoyle6, Tuija Jokinen4, Heikki Junninen4, Juha Kangasluoma4, Jaeseok Kim12, Jaeseok Kim7, Manuel Krapf6, Andreas Kürten1, Ari Laaksonen12, Ari Laaksonen13, Katrianne Lehtipalo4, Katrianne Lehtipalo6, Vladimir Makhmutov14, Serge Mathot2, Ugo Molteni6, Antti Onnela2, Otso Peräkylä4, Felix Piel1, Tuukka Petäjä4, Arnaud P. Praplan4, Kirsty J. Pringle5, Alexandru Rap5, N. A. D. Richards5, Ilona Riipinen15, Matti P. Rissanen4, Linda Rondo1, Nina Sarnela4, Siegfried Schobesberger4, Siegfried Schobesberger7, Catherine E. Scott5, John H. Seinfeld11, Mikko Sipilä4, Mikko Sipilä3, Gerhard Steiner4, Gerhard Steiner16, Gerhard Steiner8, Yuri Stozhkov14, Frank Stratmann17, António Tomé18, Annele Virtanen12, Alexander L. Vogel2, Andrea Christine Wagner1, Paul E. Wagner16, Ernest Weingartner6, Daniela Wimmer4, Daniela Wimmer1, Paul M. Winkler16, Penglin Ye19, Xuan Zhang11, Armin Hansel8, Josef Dommen6, Neil M. Donahue19, Douglas R. Worsnop12, Douglas R. Worsnop4, Urs Baltensperger6, Markku Kulmala4, Markku Kulmala3, Kenneth S. Carslaw5, Joachim Curtius1 
26 May 2016-Nature
TL;DR: Ion-induced nucleation of pure organic particles constitutes a potentially widespread source of aerosol particles in terrestrial environments with low sulfuric acid pollution.
Abstract: Atmospheric aerosols and their effect on clouds are thought to be important for anthropogenic radiative forcing of the climate, yet remain poorly understood. Globally, around half of cloud condensation nuclei originate from nucleation of atmospheric vapours. It is thought that sulfuric acid is essential to initiate most particle formation in the atmosphere, and that ions have a relatively minor role. Some laboratory studies, however, have reported organic particle formation without the intentional addition of sulfuric acid, although contamination could not be excluded. Here we present evidence for the formation of aerosol particles from highly oxidized biogenic vapours in the absence of sulfuric acid in a large chamber under atmospheric conditions. The highly oxygenated molecules (HOMs) are produced by ozonolysis of α-pinene. We find that ions from Galactic cosmic rays increase the nucleation rate by one to two orders of magnitude compared with neutral nucleation. Our experimental findings are supported by quantum chemical calculations of the cluster binding energies of representative HOMs. Ion-induced nucleation of pure organic particles constitutes a potentially widespread source of aerosol particles in terrestrial environments with low sulfuric acid pollution.

502 citations

Journal ArticleDOI
TL;DR: Measurements from the Cosmics Leaving Outdoor Droplets chamber reveal the formation of neutral particles containing up to 14 SA and 16 DMA molecules, corresponding to a mobility diameter of about 2 nm, under atmospherically relevant conditions, revealing the fundamental processes involved in particle formation and growth.
Abstract: For atmospheric sulfuric acid (SA) concentrations the presence of dimethylamine (DMA) at mixing ratios of several parts per trillion by volume can explain observed boundary layer new particle formation rates. However, the concentration and molecular composition of the neutral (uncharged) clusters have not been reported so far due to the lack of suitable instrumentation. Here we report on experiments from the Cosmics Leaving Outdoor Droplets chamber at the European Organization for Nuclear Research revealing the formation of neutral particles containing up to 14 SA and 16 DMA molecules, corresponding to a mobility diameter of about 2 nm, under atmospherically relevant conditions. These measurements bridge the gap between the molecular and particle perspectives of nucleation, revealing the fundamental processes involved in particle formation and growth. The neutral clusters are found to form at or close to the kinetic limit where particle formation is limited only by the collision rate of SA molecules. Even though the neutral particles are stable against evaporation from the SA dimer onward, the formation rates of particles at 1.7-nm size, which contain about 10 SA molecules, are up to 4 orders of magnitude smaller compared with those of the dimer due to coagulation and wall loss of particles before they reach 1.7 nm in diameter. This demonstrates that neither the atmospheric particle formation rate nor its dependence on SA can simply be interpreted in terms of cluster evaporation or the molecular composition of a critical nucleus.

203 citations

Journal ArticleDOI
TL;DR: The PQA-modified magnetite nanoparticles retained 100% biocidal efficiency against E. coli during eight exposure/collect/recycle procedures without washing with any solvents or water, making the nanoparticles easy to remove from water after antibacterial tests.

181 citations


Cited by
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TL;DR: The current status and future perspectives in atom transfer radical polymerization (ATRP) are presented in this paper, with a special emphasis on mechanistic understanding of ATRP, recent synthetic and process development, and new controlled polymer architectures enabled by ATRP.
Abstract: Current status and future perspectives in atom transfer radical polymerization (ATRP) are presented. Special emphasis is placed on mechanistic understanding of ATRP, recent synthetic and process development, and new controlled polymer architectures enabled by ATRP. New hybrid materials based on organic/inorganic systems and natural/synthetic polymers are presented. Some current and forthcoming applications are described.

2,188 citations

Journal ArticleDOI
TL;DR: Design, and Applications Shutao Wang,“, Kesong Liu, Xi Yao, and Lei Jiang*,†,‡,§ †Laboratory of Bio-inspired Smart Interface Science, Technical Institute of Physics and Chemistry, and ‡Beijing National Laboratory for Molecular Science.
Abstract: Design, and Applications Shutao Wang,†,‡ Kesong Liu, Xi Yao, and Lei Jiang*,†,‡,§ †Laboratory of Bio-inspired Smart Interface Science, Technical Institute of Physics and Chemistry, and ‡Beijing National Laboratory for Molecular Science, Institute of Chemistry, Chinese Academy of Sciences, Beijing 100190, People’s Republic of China Key Laboratory of Bio-Inspired Smart Interfacial Science and Technology of Ministry of Education, School of Chemistry and Environment, BeiHang University, Beijing 100191, People’s Republic of China Department of Biomedical Sciences, City University of Hong Kong, Hong Kong P6903, People’s Republic of China

1,218 citations

Journal ArticleDOI
TL;DR: The state of the art in the field of antimicrobial polymeric systems during the last decade is described in this paper, where a classification of the different materials is carried out dividing basically those synthetic polymers that exhibit antimicrobial activity by themselves; those whose biocidal activity is conferred through their chemical modification; those that incorporate antimicrobial organic compounds with either low or high molecular weight; and those that involve the addition of active inorganic systems.

1,063 citations

Journal ArticleDOI
TL;DR: This Perspective presents recent advances in macromolecular engineering enabled by ATRP with emphasis on various catalytic/initiation systems that use parts-per-million concentrations of Cu catalysts and can be run in environmentally friendly media, e.g., water.
Abstract: This Perspective presents recent advances in macromolecular engineering enabled by ATRP. They include the fundamental mechanistic and synthetic features of ATRP with emphasis on various catalytic/initiation systems that use parts-per-million concentrations of Cu catalysts and can be run in environmentally friendly media, e.g., water. The roles of the major components of ATRP—monomers, initiators, catalysts, and various additives—are explained, and their reactivity and structure are correlated. The effects of media and external stimuli on polymerization rates and control are presented. Some examples of precisely controlled elements of macromolecular architecture, such as chain uniformity, composition, topology, and functionality, are discussed. Syntheses of polymers with complex architecture, various hybrids, and bioconjugates are illustrated. Examples of current and forthcoming applications of ATRP are covered. Future challenges and perspectives for macromolecular engineering by ATRP are discussed.

985 citations