Trajectories of particle inside cavity are dependant on the velocity and electric field distributions.Red particles = unselected particle sizesYellow Particles = selected particle sizesYe
These results were sprayed with solution of 0.05M NaCl.
Malic acid, NaCl and mixitures
Honors Research Oral Presentation
Atmospheric Aerosols: Investigating and Characterizing the Hygroscopicity of Nanoparticles<br />By: Alexander Girau<br />Advisor: Dr. Joelle S. Underwood<br />
What are atmospheric aerosols?<br />Aerosols are liquid or solid particles or combinations suspended in gas such as dust, mist, or fumes. Atmospheric aerosol nanoparticles are defined as particles with aerodynamic diameters of 100 nm (0.1mm) and less.<br />Width of human hair<br />Aerosol particle of interest<br />2.5mm <br />0.1mm <br />10mm <br />
What are atmospheric aerosols?<br />They are a complex and dynamic mixture of solid and liquid particles from biogenic and anthropogenic sources.<br />Biogenic aerosols: <br />Sea foam (blue)<br />Biological debris (dark green)<br />Volcanic dust (bright red)<br />Anthropogenic aerosols:<br />Industrial dust (grey)<br />Soot carbon (black)<br />Biomass combustion (dark red)<br />
Exosphere<br />Atmosphere<br />Thermosphere<br />Mesosphere<br />Ozone Shield<br />Stratosphere<br />Troposphere<br />Where are they found???<br />They are primarily found in the troposphere which extends 16 km above sea level. Satellites have an elevation of ~ 650 km<br />
Why to study Atmospheric Aerosols?<br />Atmospheric aerosols act as micro chemical reaction vessels. <br />They help in the transportation of non-volatile material; they play an important role in the formation of clouds and have a profound effect on the earth’s climate.<br /> Yet the ability of these particles to attract water molecules is not well understood. <br />
Water Uptake Character = Hygroscopicity<br />Water uptake studies investigate the role of chemical content and particle size on the water uptake process.<br />The hygroscopicity of a particle is defined as its water uptake characterization.<br />This study attempts to explain water uptake phenomena involving atmospheric aerosols.<br />Particles of interest then must be able to interact with water; materials with a strong affinity for absorbing moisture from the atmosphere are called deliquescent materials.<br />Deliquescent materials allow us to study a particle’s transition from the solid phase to the aqueous phase at a specific relative humidity (RH)<br />
Water Uptake by Nanoparticles<br />RH is responsible for the deposition of water molecules as a film to the surface of a crystalline particle.<br />As RH is increased, more molecules of water adsorb to the surface.<br />When RH reaches a threshold, the film of water becomes thick enough to promote a phase transition from solid to aqueous.<br />This transition is known as deliquescence and occurs at the deliquescence relative humidity (DRH)<br />Growth factor (GF) curves quantify particle hygroscopicity <br />GF is a ratio measuring the particle’s mobility diameter at a specific RH to that of a dry particle. <br />
Why do we study Deliquescence?<br />We are interested in particle deliquescence because we want to understand:<br />How this interaction changes, depending on the chemical content and the size of the nanoparticle of interest, <br />If chemical and photochemical properties of the particle change as more water is adsorbed on the surface of particle<br />Ex. Does a 50 nm NaCl particle deliquesce differently than a 50 nm KCl particle ? And if it does, what effects can we generalize that this will have on things like cloud formation???<br />The value of understanding elementary molecules serves as the basis for possibly understanding more complex molecules such as greenhouse emissions. <br />
Governing Principle of Water Uptake Studies<br />Particles having diameters <100 nm are ubiquitous and abundant precursors to the larger aerosols that influence global climate.<br />Surface energy of nanoparticles provides a significant contribution to their overall free energy. As a result, DRH and ERH can significantly change.<br />Due to the Kelvin Effect the hygroscopic growth of atmospheric nanoparticles is expected to be lower compared to that of their larger counterpart<br />Thus, the Kelvin Effect accounts for size dependence of deliquescence RH observed for particles with diameter <100 nm. <br />
Governing Principle of Water Uptake Studies<br />>100 nm particles<br />< 100 nm particle<br />Bulk Solution, virtually infinite surface<br />Flat Surface, exhibited by a larger particle<br />Curve Surface, exhibited by smaller particle<br />Physical Interpretation of Kelvin Effect: larger particles exhibit flatter surface and thus are more thermodynamically favorable to adsorb water films than smaller particles that exhibit a curves surface.<br />
Summary of Experimental Apparatus<br />1. Electrospray: polydispersed particles will be generated and then size selected depending on objective of experiment<br />2. Particle Conditioning: size selected nanoparticles will be exposed to a specified RH, promoting deliquescence.<br />3. Particle Sizing: the number size distribution of particles will be measured post conditioning. It is at this step that the growth factor can be determined to characterize the hygroscopicity of the molecule of interest.<br />
Ultrafine Particle Generation<br />The ultrafine particles required to study deliquescence are generated through an in-house electrospray. <br /><ul><li>A syringe pump, feeds a solution of particles of interest.
A positively charged high voltage (+HV) is applied to the syringe, causing highly charges particle to shoot off towards a static eliminator.
These particle are then introduced into a optional differential mobility analyzer (DMA) to promote a size selection step. </li></ul>DMA-1<br />Electrospray Setup<br />
Ultrafine Particle Generation<br />Electrospray apparatus generates particles in a polydispersed fashion. Thus a Boltzmann distribution is measured for the multifarious particles created.<br /><ul><li>Particle diameters < 50 nm and geometric standard deviations < 1.2 are readily achieved.
Use of an optional DMA narrows the distribution and provides additional stability. </li></li></ul><li>Optional: DMA-1<br />A simple description of the DMA is that the instrument is just two charged concentric cylinders with an inlet slit and a sampling slit.<br />The DMA separates particles based on their electrical mobility.<br />Aerosol particles for sizing are inserted into the annular region between the two cylinders at the inlet slit; they are carried by a constant flow of purified air to maintain a consistent laminar (non turbulent) flow. <br />(Aerosol Generated from Electrospray)<br />+HV<br />(Clean Air )<br />
Optional: DMA-1<br />Particles with mobilities in a certain narrow range are sampled at the sampling slit.<br />the sizing chosen depends on certain parameters such as the applied voltage, the sheath flow rates, etc.<br />The path of aerosol particles within the DMA is based on a stream function, thus a consistent flow is required to allow correct sizing by electrical charging. <br />(Aerosol Generated from Electrospray)<br />+HV<br />Polydispersed aerosols<br />Unselected aerosol<br />Selected aerosol<br />(Clean Air )<br />
Analysis of DMA-1 Selection<br />Figure 1. The result of a properly selective DMA. As the voltage is increased the center of the distribution is shifted towards a larger diameter. <br />Figure 2. Analysis of uncertainty associated with the effects of voltage applied size selection. As the voltage is ramped, the confidence interval is increased. This is physically depicted in the broadening of the peaks in Figure 1.<br />Figure 1. <br />Figure 2. <br />
Particle Conditioning<br />After the particle size of interest has been properly selected it then proceeds to the particle conditioning process.<br /><ul><li>Water Uptake Region: the region is kept a predetermined RH to expose the selected particle of interest.
Sheathe Air Conditioning: the sheath air required to facilitate laminar flow through out the system is kept at a minimum RH to keep air as dry as possible.</li></li></ul><li>Particle Sizing by DMA-2 and CPC<br />The particle sizing step consist of the tandem DMA-2 and condensation particle counter (CPC).<br />DMA -2 in conjunction with the CPC measures the number size distribution of the particles. <br />The DMA-2 is responsible for measuring the change in particle diameter.<br />Once monodispersed aerosols are exposed to the RH in the particle conditioning step, the number size distribution of the water uptake process was measured by the DMA-2 and the CPC.<br />(conditioned monodispersed aerosols)<br />
Particle Sizing by DMA-2 and CPC<br />Figure 3. Analysis of the number size distribution of particles at selected sizes.<br />The CPC measures the presence of particles as a Boltzmann distribution. As the voltage is ramped to select larger particles, the CPC registers a decrease in the numbers concentration. <br />Figure 3. <br />
What does all this data mean?<br />Soluble, crystalline particles deliquesce at well-defined RH.<br />Deliquescence RH and ensuing hygroscopic growth at higher RH are sensitive to both particle chemical content and particle size.<br />Kelvin effect accounts for size dependence of deliquescence RH observed for particles with diameter <100 nm<br />
Ongoing Work<br />The role of chemical content and particle size are being studied for a variety of mixed salt and carboxylic acid particles.<br /> Modeling studies are underway to develop a better understanding of the relative importance of size and content<br />