Auflistung nach Autor:in "Hüglin, Christoph"

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  • Vorschaubild
    Publikation
    Mobility particle size spectrometers. harmonization of technical standards and data structure to facilitate high quality long-term observations of atmospheric particle number size distributions
    (Copernicus, 29.03.2012) Wiedensohler, Alfred; Birmili, Wolfram; Nowak, Marta; Sonntag, André; Weinhold, Kay; Merkel, Maik; Wehner, Birgit; Tuch, Thomas; Pfeifer, Sascha; Fiebig, Markus; Fjäraa, Ann Mari; Asmi, Eija; Sellegri, Karine; Depuy, R.; Venzac, Hervé; Villani, Paolo; Laj, Paolo; Aalto, Pasi Pekka; Ogren, John A.; Swietlicki, Erik; Williams, Paul I.; Roldin, Pontus; Quincey, Paul; Hüglin, Christoph; Fierz-Schmidhauser, Rahel; Gysel, Martin; Weingartner, Ernest; Riccobono, Francesco; Santos, S.; Gruening, Carsten; Faloon, K.; Beddows, D.; Harrison, Roy; Monahan, C.; Jennings, Stephen G.; O'Dowd, Colin D.; Marinoni, Angela; Horn, H.-G.; Keck, L.; Jiang, Jingkun; Scheckman, Jakob; McMurry, Peter H.; Deng, Zhaoze; Zhao, Chunsheng; Moerman, Marcel; Henzing, Bas; de Leeuw, Gerrit; Löschau, G.; Bastian, S. [in: Atmospheric Measurement Techniques]
    Abstract. Mobility particle size spectrometers often referred to as DMPS (Differential Mobility Particle Sizers) or SMPS (Scanning Mobility Particle Sizers) have found a wide range of applications in atmospheric aerosol research. However, comparability of measurements conducted world-wide is hampered by lack of generally accepted technical standards and guidelines with respect to the instrumental set-up, measurement mode, data evaluation as well as quality control. Technical standards were developed for a minimum requirement of mobility size spectrometry to perform long-term atmospheric aerosol measurements. Technical recommendations include continuous monitoring of flow rates, temperature, pressure, and relative humidity for the sheath and sample air in the differential mobility analyzer. We compared commercial and custom-made inversion routines to calculate the particle number size distributions from the measured electrical mobility distribution. All inversion routines are comparable within few per cent uncertainty for a given set of raw data. Furthermore, this work summarizes the results from several instrument intercomparison workshops conducted within the European infrastructure project EUSAAR (European Supersites for Atmospheric Aerosol Research) and ACTRIS (Aerosols, Clouds, and Trace gases Research InfraStructure Network) to determine present uncertainties especially of custom-built mobility particle size spectrometers. Under controlled laboratory conditions, the particle number size distributions from 20 to 200 nm determined by mobility particle size spectrometers of different design are within an uncertainty range of around ±10% after correcting internal particle losses, while below and above this size range the discrepancies increased. For particles larger than 200 nm, the uncertainty range increased to 30%, which could not be explained. The network reference mobility spectrometers with identical design agreed within ±4% in the peak particle number concentration when all settings were done carefully. The consistency of these reference instruments to the total particle number concentration was demonstrated to be less than 5%. Additionally, a new data structure for particle number size distributions was introduced to store and disseminate the data at EMEP (European Monitoring and Evaluation Program). This structure contains three levels: raw data, processed data, and final particle size distributions. Importantly, we recommend reporting raw measurements including all relevant instrument parameters as well as a complete documentation on all data transformation and correction steps. These technical and data structure standards aim to enhance the quality of long-term size distribution measurements, their comparability between different networks and sites, and their transparency and traceability back to raw data.
    01A - Beitrag in wissenschaftlicher Zeitschrift
  • Vorschaubild nicht verfügbar
    Publikation
    Separation of volatile and non-volatile aerosol fractions by thermodesorption. instrumental development and applications
    (Elsevier, 04/2001) Burtscher, Heinz; Baltensperger, Urs; Bukowiecki, Nicolas; Cohn, P.; Hüglin, Christoph; Mohr, Martin; Matter, Urs; Nyeki, Stephan; Schmatloch, Volker; Streit, Niklaus; Weingartner, Ernest [in: Journal of Aerosol Science]
    An instrument to remove volatile material from aerosol particles by thermal desorption is presented. The thermodesorber consists of a heated tube, where volatile material is desorbed from the particles, and a water- or air-cooled tube, consisting of activated charcoal. This last tube removes desorbed material and thus prevents it from re-adsorbing onto particles. Although designed for measuring particulate emissions from combustion processes it can also be applied to atmospheric aerosols. After theoretical and experimental determination of thermodesorber operating characteristics (temperature profile, losses, removal of desorbed material), examples of applications in several fields are given. Examples of atmospheric measurements at several remote and urban sites are presented. In combustion technology, the thermodesorber is applied to remove all volatile materials, allowing separation of volatile species and the non-volatile core (mainly elemental carbon) of combustion particles. Finally, the thermodesorber is used to study adsorption and desorption processes of polycyclic aromatic hydrocarbons on particles.
    01A - Beitrag in wissenschaftlicher Zeitschrift
  • Vorschaubild
    Publikation
    Single particle characterization of black carbon aerosols at a tropospheric alpine site in Switzerland
    (Copernicus, 09.08.2010) Liu, D.; Flynn, Michael; Gysel, Martin; Targino, Admir Créso; Crawford, Ian; Bower, Keith; Choularton, Thomas; Jurányi, Zsófia; Steinbacher, Martin; Hüglin, Christoph; Curtius, Joachim; Kampus, M.; Petzold, Andreas; Weingartner, Ernest; Baltensperger, Urs; Coe, Hugh [in: Atmospheric Chemistry and Physics]
    The refractory black carbon (rBC) mass, size distribution (190–720 nm) and mixing state in sub-micron aerosols were characterized from late February to March 2007 using a single particle incandescence method at the high alpine research station Jungfraujoch (JFJ), Switzerland (46.33° N, 7.59° E, 3580 m a.s.l.). JFJ is a ground based location, which is at times exposed to continental free tropospheric air. A median mass absorption coefficient (MAC) of 10.2±3.2 m2 g−1 at λ=630 nm was derived by comparing single particle incandescence measurements of black carbon mass with continuous measurements of absorption coefficient. This value is comparable with other estimates at this location. The aerosols measured at the site were mostly well mixed and aged during transportation via the free troposphere. Pollutant sources were traced by air mass back trajectories, trace gases concentrations and the mass loading of rBC. In southeasterly wind directions, mixed or convective weather types provided the potential to vent polluted boundary layer air from the southern Alpine area and industrial northern Italy, delivering enhanced rBC mass loading and CN concentrations to the JFJ. The aerosol loadings at this site were also significantly influenced by precipitation, which led to the removal of rBC from the atmosphere. Precipitation events were shown to remove about 65% of the rBC mass from the free tropospheric background reducing the mean loading from 13±5 ng m−3 to 6±2 ng m−3(corrected to standard temperature and pressure). Overall, 40±15% of the observed rBC particles within the detectable size range were mixed with large amounts of non-refractory materials present as a thick coating. The growth of particle size into the accumulation mode was positively linked with the degree of rBC mixing, suggesting the important role of condensable materials in increasing particle size and leading to enhanced internal mixing of these materials with rBC. It is the first time that BC mass, size distribution and mixing state are reported in the free troposphere over Europe. These ground based measurements also provide the first temporal study of rBC in the European free troposphere quantitatively measured by single particle methods. At the present time there is only limited information of BC and its mixing state in the free troposphere, especially above Europe. The results reported in this paper provide an important constraint on modelled representation of BC.
    01A - Beitrag in wissenschaftlicher Zeitschrift