KONA Powder and Particle Journal
Online ISSN : 2187-5537
Print ISSN : 0288-4534
ISSN-L : 0288-4534
Review Papers
A PM1.0/2.5/10 Trichotomous Virtual Impactor Based Sampler: Design and Applied to Arid Southwest Aerosols Part I: Design
Virgil MarpleDale LundgrenBernard Olson
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2013 Volume 30 Pages 15-21

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Abstract

A PM1.0/2.5/10 Trichotomous sampler has been developed to determine if the particles in the saddle point between the coarse and fine particle modes (specifically the 1.0 μm to 2.5 μm size range) are primarily coarse or fine mode particles. The sampler consists of a standard high volume sampler with two high volume virtual impactors (one with a cut size of 2.5 μm and the other with a cut size of 1.0 μm) inserted between the PM10 inlet and the 8×10 inch (20×25 cm) after filter. By using nine 47 mm filters, at various locations within the trichotomous sampler, a technique has been developed for subtracting out the effects of particles smaller than the cutsize of a virtual impactor from the minor flow particle collection.

Introduction

Many types of studies require measuring the aerodynamic diameter size distribution of air-borne (aerosol) particles, where the aerodynamic diameter of a particle is the diameter of a unit density sphere that has the same falling speed as the particle in question. One type of inertial classifier is the most common method for aerodynamic particle size classification, that being the air jet impacting on a solid plate inertial impactor (Marple, 1970). Since impactors were first developed in 1860, many single stage and cascade impactors have been designed, built, tested, and sometimes made commercially available (Marple, 2004)

One shortcoming of the inertial impactor is that particles can bounce off of the impaction plate (particle bounce), or can be blown off the plate after collection (particle blow-off). This will result in particles that are intended to be collected on a certain stage being collected on subsequent stages of the cascade impactor, giving an erroneous size distribution measurement.

A variation of the inertial impactor, which solves the particle bounce problem, is the virtual impactor (Fig. 1a), which replaces the impaction plate with an open ended tube, called a collection probe, a diameter of which is about 35% larger than the nozzle diameter (Xu, 1991) The entrance to the collection probe creates a condition that can be thought of as a virtual impaction surface (thus the name) through which particles pass into a void. Large particles penetrate far into the collection probe and are carried out the opposite end with a small percentage of the total flow, known as the minor flow. Smaller particles that do not penetrate as far into the probe, reverse direction and leave at the outer circumference of the probe with the remaining flow, known as the major flow. Performance of the virtual impactor stage is characterized by a collection efficiency curve, as shown in Fig. 1b. The size of particles that are collected with 50% efficiency is called the cutsize of the virtual impactor stage. Efficiency, defined as the percentage of particles passing through the virtual impactor nozzle and collected in the minor flow (Marple and Chein, 1980), can have collection characteristics that are similar to inertial impactors.

Fig. 1

Virtual Impactor Stage and Particle Collection Efficiency curve.

a) Nozzle/collection probe virtual impactor stage

b) Particle collection efficiency curve

Although the virtual impactor configuration solves the particle bounce problem of the inertial impactor, it does create another problem unique to virtual impactors. The problem is that the minor flow contains particles smaller than the cutsize in a concentration equal to that in the major flow. These small particles in the minor flow will be referred to as “background” particles in this paper and constitute a contamination of the large particle fraction with small background particles, and is the reason that the efficiency curve does not go to zero at small particles sizes in Fig. 1b.

A number of researchers have developed designs to eliminate these background particles by providing a clean particle free core of air in the central portion of the flow passing through the nozzle (Masuda et al., 1978; Chen et al.1986). This clean core of air will then be the air that passes through the collection probe, thus eliminating small background particles in the minor flow. This clean core of air does complicate the flow system of an otherwise simple classifier and is nearly impossible to incorporate into virtual impactors that have more than one nozzle/collection probe set in one stage, or in cascade designs.

In this paper we describe another solution to the background particle problem. The solution is to collect particles smaller than the virtual impactor cut-size on a filter that is identical in size, material, and flow rate to the filter collecting the particles larger than the cutsize (minor flow collection). Identical analysis of both filters will allow for the effects of the background particles to be subtracted from the particles larger than the cutsize. This technique is the one chosen in the design of the PM1.0/2.5/10 Trichotomous sampler described in Part I of this paper. Part II, to be published in the 2013 issue of KONA, will describe the use of the PM1.0/2.5/10 Trichotomous sampler in a study of atmospheric aerosol particles in the southwestern US, specifically in Phoenix, Arizona.

Design Criteria for the PM1.0/2.5/10 Trichotomous Sampler

When the fine particle standard was established in the US in1997, there was much discussion among experts as to whether the standard should be set at 1.0 μm or 2.5 μm. The problem arose from the nature of the particle size distributions in atmospheric aerosols. Whitby (1978) discovered that atmospheric particle size distributions were trimodal in nature, with fresh combustion particles in the smallest mode, aged combustion particles in the intermediate mode (fine particle mode) and mechanically generated particles in the largest mode (coarse particle mode). An excellent discussion of this topic is presented by John (2011).

It was generally agreed that the particle size separating the fine and coarse particle modes was in the 1 μm to 2.5 μm range. Particles in this size range consist of particles from the lower tail of the coarse particle mode and particles from the upper tail of the fine particle mode (see Fig. 2). The discussion centered on the question of whether the particles in the range of 1 μm to 2.5 μm were mostly fine or mostly coarse mode particles.

Fig. 2

Fine and Coarse Particle Modes. From U.S. Environmental Protection Agency (1982).

The PM1.0/2.5/10 Trichotomous sampler was designed to answer this question by using two virtual impactors in series (cascade) with cut sizes of 2.5μm and 1.0 μm. It was decided to use the standard 40 cfm (1.13 m3/min) 10 μm classifying inlet of the PM10 sampler as the sampler’s first stage to avoid the need to develop a new sampling inlet.

PM1.0/2.5/10 Trichotomous Sampler

Major Components

The superstructure of the trichotomous sampler is the standard high volume 40 cfm (1.13 m3/min) flowrate PM10 sampler, which consists of a PM10 size selective inlet (McFarland et.al., 1984) and an 8×10 inch (20×25 cm) filter, but the heart of the PM1.0/2.5/10 Trichotomous sampler is two high volume virtual impactors (HVVIs) (Marple and Olson, 1995) with cut sizes of 2.5 μm and 1.0 μm. The HVVIs, being of small size (8.25 in.×6.75 in.×2.75 in. high ) (21cm×17cm×7cm) and yet having a flow rate of 40 cfm, were designed specifically to further size classify particles in the high volume PM10 sampler (Marple et.al., 1990). Two HVVIs are inserted in series between the PM10 inlet and the 8×10 filter. The 2.5 μm HVVI is located inside the lower cavity of the PM10 size selective inlet, with an additional chamber inserted between the inlet and the 8×10 filter to house the 1 μm HVVI, which is mounted directly above the 8×10 inch filter.

Figs. 3, 4 and 5 show schematics of the sampler and the two HVVIs and Fig. 6 shows photos of the major components. The colored filter holders in these figures will be explained in the following section.

Fig. 3

Schematic of PM1.0/2.5/10 Trichotomous Sampler.

Fig. 4

Schematic of 2.5 μm HVVI.

Fig. 5

Schematic of 1.0 μm HVVI.

Fig. 6

Photos of PM1.0/2.5/10 Trichotomous Sampler.

a) Assembled sampler; b) 2.5 μm HVVI; c) 1.0 μm HVVI

A-PM10 inlet; B-Intermediate chamber; C-Base; D-2.5 μm HVVI; E-1.0 μm HVVI; F-Afterfilter.

A schematic of the overall sampler is presented in Fig. 3. The flow path through the sampler is through: 1) the 10 um size selective inlet, 2) the 2.5 μm HVVI, 3) the 1.0 μm HVVI and then 4) the 8×10 inch after filter. Air is pulled through the sampler using two blowers in series rather than just one blower as in the standard high volume sampler. The blower system consists of a standard high volume blower with an auxiliary blower mounted at its exhaust. This modification to the standard high volume sampler is necessary due to the additional pressure drop of the HVVIs. Flow control is achieved with a mass flow controller supplied with the high volume sampler. This flow controller controls the speed of the second blower only, thus, controlling the back pressure of the first blower, which operates at full speed.

Flow paths through the two HVVIs are similar and shown schematically in Figs. 4 and 5. Flow enters the HVVIs through nozzles (12 and 80 nozzles for the 2.5μm and 1.0μm HVVIs, respectively) on either side of the HVVI housings. Particles larger than the cutsize are collected with the minor flow in the center chamber, along with 5% of the particles smaller than the cutsize (the minor flow is 5% of the total flow for both HVVIs). Particles smaller than the cut size remain with the major flow and exit through the bottom of the HVVI housings.

Fig. 6 shows photos of major components of the sampler. Fig. 6a shows the assembled sampler with the PM10 high volume inlet, the intermediate chamber and the high volume sampler stand. Sets of pressure gages and control valves, located on both sides of the stand, are for controlling the flow through the various filters in the sampler. Fig. 6b shows the 2.5 μm HVVI located inside the PM10 inlet and on top of the intermediate chamber. Fig. 6c shows the 1.0 μm HVVI inside the intermediate section and on top of the standard 8×10 inch high volume filter. Both 2.5 μm and 1.0 μm HVVIs have bases specifically designed for the trichotomous sampler to accommodate the various 47 mm filters.

Filter Sample Locations

Nine 47 mm diameter filters are in various locations in the trichotomous sampler to collect particle samples of PM10, PM2.5, PM1, PM2.5–10 and PM1–2.5. The filters are inserted into filter holders and the holders are clamped into manifolds within the trichotomous sampler. These filter holders are also used to transport the filters to and from the field test site. To ensure that the filter holders are inserted into the correct location in the sampler, filter holders, and manifolds, are color coded. In addition, the filter holders, shown in Fig. 7, are of special design so that they can only be inserted into the manifolds in one direction, insuring that the filter holders cannot be inserted backwards and the flow will always be in the correct direction through the filters. At some locations, two filters were used for the purpose of using two different particle analysis techniques.

Fig. 7

47 mm filter holder.

Placement of the nine 47 mm filters in the trichotomous sampler are shown on the schematics in Fig. 3, and in the photos in Figs. 8 and 9, where Figs. 8 and 9 shows the bases of the 2.5 μm and 1.0 μm HV-VIs, respectively. The heads of the HVVIs have been removed in these photos.

Fig. 8

Photo of 2.5 μm base showing 47 mm filter holder placements.

A-PM10 filter (grey filter holder); B-PM2.5–10 filter (gold filter holder); C-PM2.5–10 2×7 inch filter.

Fig. 9

Photo of 1.0 μm base showing 47 mm filter holder placements.

D-PM2.5 filter (blue filter holder); E-PM1–2.5 filter (red filter holders); F-PM1 filter (green filter holders); G-background control filters (black filter holders); H-PM<1 8×10 inch filter.

Filters shown in Figs. 8 and 9 are as follows:

  • Fig. 8
  • 1. One 47mm PM10 filter (A, the grey holder) located after the PM10 inlet and before the 2.5 μm HVVI.
  • 2. One 47mm PM2.5–10 filter (B, the gold holder) samples particles from the minor flow of the 2.5 μm HVVI. Also shown is the 2×7 inch (5 ×17.5 cm) minor flow filter so that the total minor flow rate can be brought to 2 cfm.

  • Fig. 9
  • 3. One 47mm PM2.5 filter (D, the blue holder) samples the 2.5 μm HVVI major flow aerosol.
  • 4. Two 47mm PM1–2.5 filters (E, the red holders), which sample the 1.0 μm HVVI minor flow aerosol.
  • 5. Two 47mm PM1 filter (F, the green holders) which samples the 1.0 μm HVVI major flow aerosol.
  • 6. Two 47mm background filters (G, the black holders) located above the 8×10 inch final filter. These filters have zero flow rate (are used as control filters).

The flow rate through each filter is controlled by a flow circuit consisting of an orifice flow meter, connected to a Magnehelic pressure gage, and followed by a manual flow control valve. Flow from each filter is routed back into the primary flow circuit downstream of the 8×10 inch filter, allowing the flow rate to be controlled, and remains constant at 40 cfm. Since a maximum of 2 cfm is passing through any 47 mm filter, normally the flow remains relatively constant over a 24 hour sampling period. Therefore, the control valve for each filter need only be set at the onset of sampling. However, for heavy particle loading conditions, an intermediate adjustment of flow rate can easily be made.

Collection Characterizes

There are three inertial classifiers in the trichotomous sampler: a PM10 high volume inlet, and two HVVIs virtual impactors. The PM10 inlet uses inertial impactor technology to remove particles larger than 10 μm, and has been the subject of many wind tunnel evaluation and calibrations.

The 2.5 μm HVVI was designed specifically to further classify particles within the standard high volume PM10 sampler. Initial application was separation of coarse mechanically generated aerosol particles from smoke particles being emitted from wood burning fireplaces (Marple, et.al., 1990). Since these mechanically generated aerosols are solid, the 2.5 μm HVVI was calibrated with solid ammonium fluoresce-in particles generated using a vibrating orifice monodisperse aerosol generator (VOMAG) (Berglund and Liu, 1973). The collection efficiency curve of the 2.5 μm HVVI is shown in Fig. 10.

Fig. 10

Particle classification curves for 1.0 and 2.5 HVVIs.

However, the 1.0 μm HVVI was designed specifically for use in the trichotomous sampler and had to be calibrated for this program. Since particles less than 1 μm in diameter are formed by condensation, liquid particles were used in its calibration. In a method commonly used in our laboratory, a VOMAG was used to generate oleic acid droplets tagged with uranine dye. By washing out various parts of the classifier with known amounts of wash solution and analyzing the wash solution with a fluorometer to determine the dye concentration, the collection efficiency of the HVVI was determined as a function of particle size. The resulting efficiency curve for the 1.0 μm HVVI is also shown in Fig. 8. Note in the efficiency curves for both 2.5 μm and 1.0 μm HVVIs that the lower efficiency asymptotically approaches the fraction of the minor flow (5%).

Analysis Techniques

The PM1.0/2.5/10 Trichotomous sampler was developed to provide a means for determining if particles in the 1.0 to 2.5 μm size range are mostly coarse or mostly fine mode particles. Since coarse and fine mode particles originate from different sources, more than one analysis method had to be employed; one for coarse particles and one for fine particles. Therefore, two filters were used in some locations within the trichotomous sampler.

Part II of this paper, to be published in the 2013 issue of KONA, describes the use of PM1.0/2.5/10 Trichotomous samplers in a study of atmospheric aerosol particles in the southwestern US, specifically in Phoenix, Arizona. Proton-induced X-ray emission (PIXE) and photon-induced x-ray fluorescence (XRF) methods were used to determine the concentration and composition of the coarse particle mode. Both of these methods are commonly used due to their nondestructive multi-element capabilities and relatively good sensitivities. A different analysis technique was used to analyze the filters for fine particles. The water-soluble portion of suspended particulate matter was quantified using ion chromatography (IC).

Filters in the grey, gold, blue, red and green filter holders were subjected to PIXI analysis and filters in the red and green filter holders were subjected to IC analysis.

Conclusion

An ambient high volume sampler has been specifically developed to answer the question of whether particulate matter in the saddle point between the coarse and fine particle modes (1.0 μm to 2.5 μm range) consist primarily of coarse or fine particles. The sampler consists of the standard 40 cfm high volume ambient air PM10 sampler with two high volume virtual impactors, one with a cut size of 2.5 μm and the other with a cut size of 1.0 μm, inserted between the PM10 inlet and the 8×10 inch after filter. Particles were collected on seven 47 mm filters at various locations within the sampler to enable analyses by different techniques to determine the fraction of the particles in the 1.0 μm to 2.5 μm range that was from the coarse mode aerosol or the fine mode aerosol.

Acknowledgements

Development and calibration of the PM1.0/2.5/10 Trichotomous sampler has been supported by the National Mining Association.

Author’s short biography

Virgil A. Marple

Virgil A. Marple is a Professor in the Mechanical Engineering Department at the University of Minnesota. He received his Ph.D. from the University of Minnesota in 1970. He is Director of the Particle Calibration Laboratory, and his research interest includes development of inertial classifiers, measurement of mining related aerosol in both the coal and taconite industries and measurement of pharmaceutical aerosols.

Dale A. Lundgren

Dale A Lundgren is Professor Emeritus - Environmental Engineering Department, University of Florida. He received his Ph.D. from the University of Minnesota in 1973. His recent research interest has been as a consultant to the National Resource Research Institute (University of Minnesota Duluth campus) studying particulate concentrations in cities and taconite mines on the Minnesota Iron range.

Bernard A. Olson

Bernard A. Olson is a Research Associate and Manager of the Particle Calibration Laboratory in the Mechanical Engineering Department at the University of Minnesota. He received his BSME, MSME, and Ph.D. from the University of Minnesota. For the past 22 years his research has been in the design, testing and numerical modeling of aerosol sampling instruments, characterization of mining aerosols related to the coal mine and taconite industries and effluents generated by cooking appliances in the commercial kitchen industry.

References
 

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