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Naneum instruments

Nano-ID NPS 500


The Nano-ID NPS500 sets a new standard for high sensitivity and selectivity aerosol measurements. It provides the ability to measure particle size distributions over a range of 5 nm to 500 nm with 128 user-selectable channels. Read More

Nano-ID Select

The Nano-ID Select is a wide-range sampler and is unique in that it spans the entire aerosol range from 2 nm up to 20 μm. Read More

 

 


What is in your air

The Nano-ID Select was employed to sample aerosol particles in the air at a semi-rural site in the USA, and SEM images of particles in the aerosol samples were subsequently obtained by the RJ-Lee Group. The images show the complex morphology and chemical composition of particles in the air that we breathe every day (see figures 2.1-2.5).

Figure 2.1 shows a crystalline particle formed mainly from iron oxide. It is interesting that on the surface of the particle many small nanoparticles can be seen. These nanoparticles most likely became attached to the surface of the big crystal while the particle was airborne. The origin of the iron oxide particle is not known but it was most likely formed by nucleation from a gas phase.

Figure 2.2 shows a completely different spherical particle also with many smaller irregular shaped particles attached.   Analysis of the chemical composition reveals the presence of iron oxide and other constituents including Ca, Cu and Si. The small nanoparticles seen on the surface of the carrier particle also most likely became attached to the surface whilst the particles were airborne.

Figure 2.3 shows the completely different morphology of a cluster of perfect spherical particles.   The chemical composition of the particles is mostly S and O, and is a signature of engineered nanoparticles such as SiO2 (Aerosil).

Figure 2.4 shows an agglomerate of many spherical particles containing mainly carbon. The chemical composition confirms that the particles originated from a combustion process, for example they might have been generated by a diesel engine.  

Figure 2.5 is an example of the complexity of real atmospheric aerosol particles. The particle shown here is an agglomerate of many smaller spherical or compacted particles. The image shows the results of gas-to-particle interactions that have caused the shape of constituent particles to be smoothed, or possibly covered with some kind of film formed by adsorption or by chemical reactions.  The chemical composition is mainly C, S and O.  Images were taken in narrow energy bands corresponding to emissions of the separate elements C and S.  It was found that both elements are present in various particles but in different proportions, indicating that particles are internally mixed. These particles are most likely the result of burning biomass.

Figure 2.1: An SEM image accompanied by an XRF element spectrum below.

Figure 2.4: An SEM image accompanied by an XRF element spectrum below.

Figure 2.5: An SEM image obtained in the energy band corresponding to a single element: C (top- left) and S (bottom-left) accompanied by an XRF element spectrum bottom-right.

 
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