Effect of Relative Humidity on Bipolar Electrostatic Charge Profiles of dry Powder Aerosols.

PURPOSE: This work investigated the effect of relative humidity (RH) on bipolar electrostatic charge profiles of dry powder inhaler aerosols using the Bipolar Charge Analyzer (BOLAR). METHODS: Two commercial products, Pulmicort® (400 µg, budesonide) and Bricanyl® (500 µg, terbutaline sulfate) Turbuhaler®, were used as model dry powder inhalers (DPIs) in this study. Three individual doses from each Turbuhaler® were sampled at 15, 40, 65 and 90% RH. Subsequently, charge and mass profiles were determined for each dispersion. RESULTS: The aerosols from these two Turbuhaler® DPI were bipolarly charged, with larger particles carrying negative charge and smaller particles positive charge. Particles changed polarity around 2.60-4.17 µm and 0.95-2.60 µm for Pulmicort® and Bricanyl®, respectively. The effect of RH on particles differed between DPIs even though the mass output was not significantly affected. The net charge profiles of Pulmicort® were relatively independent of RH, whereas those of Bricanyl® showed a reduction in the charge magnitude with increasing RH. Both positive and negative charge profiles followed a similar trend with the change in RH and individually they had higher magnitudes than the measured net charge. CONCLUSIONS: This study showed drug-specific bipolar charging of the Turbuhaler® DPI aerosols at varied RHs. Bricanyl® was more susceptible to RH and showed decreased bipolar and net charge levels with increasing RH, in comparison to Pulmicort®.

An amorphous solid state of biogenic secondary organic aerosol particles.

Secondary organic aerosol (SOA) particles are formed in the atmosphere from condensable oxidation products of anthropogenic and biogenic volatile organic compounds (VOCs). On a global scale, biogenic VOCs account for about 90% of VOC emissions and of SOA formation (90 billion kilograms of carbon per year). SOA particles can scatter radiation and act as cloud condensation or ice nuclei, and thereby influence the Earth's radiation balance and climate. They consist of a myriad of different compounds with varying physicochemical properties, and little information is available on the phase state of SOA particles. Gas-particle partitioning models usually assume that SOA particles are liquid, but here we present experimental evidence that they can be solid under ambient conditions. We investigated biogenic SOA particles formed from oxidation products of VOCs in plant chamber experiments and in boreal forests within a few hours after atmospheric nucleation events. On the basis of observed particle bouncing in an aerosol impactor and of electron microscopy we conclude that biogenic SOA particles can adopt an amorphous solid-most probably glassy-state. This amorphous solid state should provoke a rethinking of SOA processes because it may influence the partitioning of semi-volatile compounds, reduce the rate of heterogeneous chemical reactions, affect the particles' ability to accommodate water and act as cloud condensation or ice nuclei, and change the atmospheric lifetime of the particles. Thus, the results of this study challenge traditional views of the kinetics and thermodynamics of SOA formation and transformation in the atmosphere and their implications for air quality and climate.

Nucleation mode particles with a nonvolatile core in the exhaust of a heavy duty diesel vehicle.

The characteristics of the nucleation mode particles of a Euro IV heavy-duty diesel vehicle exhaust were studied. The NOx and PM emissions of the vehicle were controlled through the use of cooled EGR and high-pressure fuel injection techniques; no exhaust gas after-treatment was used. Particle measurements were performed in vehicle laboratory and on road. Nucleation mode dominated the particle number size distribution in all the tested driving conditions. According to the on-road measurements, the nucleation mode was already formed after 0.7 s residence time in the atmosphere and no significant changes were observed for longer residence times. The nucleation mode was insensitive to the fuel sulfur content, dilution air temperature, and relative humidity. An increase in the dilution ratio decreased the size of the nucleation mode particles. This behavior was observed to be linked to the total hydrocarbon concentration in the diluted sample. In volatility measurements, the nucleation mode particles were observed to have a nonvolatile core with volatile species condensed on it. The results indicate that the nucleation mode particles have a nonvolatile core formed before the dilution process. The core particles have grown because of the condensation of semivolatile material, mainly hydrocarbons, during the dilution.