This invention relates to a method and an apparatus for conditioning the charge on aerosol particles for size distribution measurement by differential mobility spectrometry. Specifically, this disclosure relates to an electrical ionizer for generating positive and negative ions by corona discharge in a gas in order to condition the aerosol particle charge to a desired degree needed for the measurement. In comparison with other electrical ionizers developed in the past, the present method and apparatus offer the simplicity, reliability, ease of use, and accuracy approaching that of traditional radioactive ionizers used for such purposes. In addition to aerosol measurement by differential mobility spectrometry, the electrical ionizer can also be used for a variety of other applications where charging or charge conditioning of particles in a gas is an important consideration and requirement.
Solid and/or liquid particles suspended in a gas are referred to as aerosols, which are present naturally in the ambient atmosphere or as a result of man-made activities. Method and apparatus for measuring particles suspended in a gas are important for atmospheric aerosol research and in other scientific and technical disciplines where small particles suspended in a gas play a significant role.
An important method to measure the concentration and size distribution of aerosol particles is differential mobility spectrometry. For such a measurement the aerosol particles, i.e. particles suspended in a gas, must be conditioned in order to create a specific charge distribution on the particles. Particles not properly charge conditioned will give rise to erroneous results. The Wide-Range Particle Spectrometer (WPS™) manufactured by MSP Corporation (Product Information Bulletin, Model 1000XP, Wide Range Particle Spectrometer, MSP Corporation (2008)) is one such instrument capable of measuring aerosol size distributions from 0.01 μm to 10 μm in diameter. In this instrument, a sub-range of aerosol particle size from 0.01 to 0.5 μm is measured by differential mobility or scanning mobility spectrometry. For the purpose of this disclosure we will refer to both measurement approaches as differential mobility spectrometry, or DMS, since both are based on the differential mobility measuring principle. Instruments based on differential mobility spectrometry are available from several manufacturers. The electrical ionizer described in this disclosure can in principle be used with any one of these aerosol measuring instruments.
Traditionally, aerosol charge conditioning for DMS is accomplished by means of a radioactive ionizer. Two commonly used radioactive ionizers are Krypton 85 and Polonium 210 (B. Y. H. Liu and D. Y. H. Pui, “Electrical Neutralization of Aerosols, ” J. Aerosol Sci. 5:465-472 (1974) and B. Y. H. Liu, D. Y. H. Pui and B. Y. Lin, “Aerosol Charge Neutralization by Radioactive Alpha Source,” Particle Characterization, 3:111-116 (1986)). These radioactive ionizers make use of high-energy subatomic particles produced by radioactive decay to ionize the gas to form positive and negative ions needed for charge conditioning. Krypton 85 is a beta emitter, producing high-energy beta particles, i.e. electrons, by radioactive decay. Polonium 210 is an alpha emitter producing energetic subatomic alpha particles, which are the nuclei of helium atoms. These energetic sub-atomic particles then collide with gas molecules to form positive and negative ions for charge conditioning. These sub-atomic particles are much smaller than the size of a single atom, which is approximately 1.0 Å in the case of hydrogen. Alpha and beta particles are considerably smaller than 1.0 Å in size.
In comparison, aerosol particles are considerably larger. An aerosol particle with a diameter of 1.0 nm, which is 10 Å, is considered very small in aerosol studies and is near the lower size limit of particle measurement by DMS. Aerosol of such a small size is therefore much larger than particles of nuclear physics. Particles of nuclear physics are very different from the particles of interest in aerosol studies. These two types of particles are not the same and should be clearly distinguished. For the purpose of this disclosure, unless otherwise noted, the particles of interest are aerosol particles rather than sub-atomic particles of nuclear physics.
When gas containing suspended aerosol particles is exposed to energetic sub-atomic particles produced by radioactive decay, the gas becomes ionized to form positive and negative ions. The gaseous ions then collide with the suspended aerosol particles to produce a characteristic charge distribution referred to as a Boltzmann distribution (W. C. Hinds, Aerosol Technology, p. 303, Wiley (1982)),
where e is the elementary unit of charge, d is the particle diameter, k is Boltzamann's constant, T is the absolute temperature, n is the number of elementary units of charge on the particles and fn is the fraction of particles in the aerosol carrying n elementary units of charge. Table 1 shows the particle charge distribution according to the Boltzmann's law.
An aerosol in Boltzmann charge equilibrium will develop a charge distribution with substantially equal concentration of positively and negatively charged particles. The total charge on the particles, i.e. the sum of all positive and negative charges carried by the particles, is equal to zero. As a result, an aerosol in Boltzmann charge equilibrium has no overall net charge. Overall the aerosol is electrically neutral while the individual particles in the aerosol may carry a charge, although not all particles are charged. The conditions needed to produce Boltzmann charge distribution are discussed in B. Y. H. Liu and D. Y. H. Pui, “Electrical Neutralization of Aerosols,” 5. Aerosol Sei. 5:465-472 (1974) and B. Y. H. Liu, D. Y. H. Pui and B. Y. Lin, “Aerosol Charge Neutralization by Radioactive Alpha Source,” Particle Characterization, 3:111-116 (1986).
When an aerosol carrying suspended particles are charge-conditioned by flowing the aerosol through a radioactive ionizer under suitable operating conditions, it will emerge from the ionizer carrying the charge distribution shown in Table 1. This specific charge distribution is then used for size distribution analysis by DMS.
An electrical ionizer for aerosol charge conditioning and measurement by DMS, therefore, must generate a charge distribution similar to the Boltzmann charge distribution generated by a radioactive ionizer in order to achieve accurate measurement results. One difference between radioactive ionizer and electric ionizer is that ionization by sub-atomic particles produced by radioactive decay occurs in the absence of an external electric field, whereas charge conditioning by ions generated by corona discharge frequently occurs when there is a significant electric field present. Not all electrical ionizers are thus capable of charge conditioning an aerosol to a sufficient degree to produce a Boltzmann distribution. As a result, an electrical ionizer capable of generating a charge distribution similar to the Boltzmann distribution is needed for high accuracy aerosol measurement by DMS. Such an ionizer is now needed because of the increased regulation on the use of radioactive material, which makes the use of radioactive ionizers less attractive or convenient for scientific research and technical applications.
Other developments in electrical ionizers include those described in F. J. Romay, B Y. H. Liu and D. Y. H. Pui, “A Sonic Jet Corona Ionizer for Electrostatic Discharge and Aerosol Neutralization” Aerosol Sci. Technol, 20: 31-41 (1994) and in U.S. Pat. No. 6,544,484. Both use a DC corona discharge to generate separate streams of positive and negative ions in clean air, which are then mixed with an aerosol to provide positive and negative ions for charge conditioning. The aerosol is thus diluted, which is a disadvantage in some applications. Both devices have failed to achieve wide spread acceptance, perhaps as a result of complexity, reliability, and/or cost. Another approach to aerosol charge neutralization is by means of an AC corona discharge as described by Riebel et al in U.S. Pat. No. 7,031,133.
This disclosure includes an apparatus for exposing particles in a gas in order to cause the charge on the particles to change, the apparatus comprising a chamber with an inlet for the gas to enter and an outlet for the gas to exit. The chamber is surrounded by an enclosure with a conductive wall, the wall being held at a ground potential. An electrode with an exposed tip is in contact with the gas in the chamber, the electrode being held at a different potential from the ground potential. The inlet and outlet define a gas flow path from the inlet to the outlet such that the gas flow path passes mainly through a region of space with a low electric field intensity. The electrode is connected to a source of voltage sufficient to cause a corona discharge to occur forming ions in the chamber.
A method is also disclosed for conditioning a charge on particles in the gas to produce substantially equal concentrations of positively and negatively charged particles and a substantially zero total particle charge in said gas for aerosol measurement by differential mobility spectrometry, said method comprising causing said gas to flow thorough a chamber, the chamber having an inlet for the gas to enter and an outlet for the gas to exit and includes the gas to flow through a chamber along a gas flow path that extends from an inlet of the chamber to an outlet of the chamber, and creating an AC corona discharge within the chamber having a high electric field intensity region and a lower electric field intensity region with the gas flow from the inlet to the outlet occurring mainly in the lower intensity region thereby creating substantially equal concentrations of positively and negatively charged particles, and a substantially zero total particle charge in the gas.
Aerosol for charge conditioning and measurement by DMS comes from source 150, which can be an aerosol in the ambient atmosphere for measurement by DMS for concentration and size distribution analysis. It can be an aerosol generated for laboratory research in which the aerosol size distribution is to be measured by DMS. The aerosol can also be generated by a specific process or for a specific purpose, in an industrial setting, where knowledge about the aerosol size distribution is important. In all cases, aerosol size distribution analysis by DMS can be made with the system shown in
Aerosol from source 150 in
The operating principle of the electrical ionizer 100 is explained with the aid of
When gaseous ions are generated by a corona discharge in the region of space adjacent to the electrode tip 15, the ions will flow along the electric field lines at a velocity in proportion to the electric field intensity. The velocity of ions, which is referred to as the drift velocity, will thus be higher along the electric field lines with a high electric field intensity, and lower along the longer electric field lines with a lower electric field intensity. By creating two separate streams of ions, one flowing at a high velocity toward the near wall, i.e. wall near the high voltage electrode, and another flowing at a lower velocity toward the far wall, we have created two separate regions of space in the ionization chamber, in which one region on the average has a lower electric field intensity than the other. The region with a high electric field, i.e. electric field intensity, is the region of space below the boundary electric field lines 54 and 64, while the low electric field region is the region above these boundary field lines 54 and 64.
When using the ionization chamber depicted in
The ionization chamber depicted in
The corona current flow from the high voltage electrode to the grounded electrode nearby also has an effect on the performance of the electrical ionizer. A high ionization current will generally lead to more rapid charge conditioning, and a low ionization current will require keeping the aerosol flow through the ionizer at a sufficiently low flow rate to insure the desired charge distribution similar to that of a Boltzmann distribution will indeed develop. This, however, can lead to greater undesired particle loss by electrostatic deposition in the ionization chamber. Such a loss is undesirable because it would lead to reduced measurement accuracy for DMS measurement. The most appropriate range of corona ion flow is in the range between 0.1 and 5 mA in rms AC current flow for proper charge conditioning for DMS aerosol measurement. In the case where a DC corona discharge is needed for creating a unipolar charge, i.e. charge of the same electrical polarity, either a positive or a negative polarity, the required DC current is also generally in the same 0.1 to 5 mA range.
In practical applications, it is also important to design the electrical ionizer suitable for different rate of aerosol flow needed by different applications. Too high of an aerosol flow rate or too small an ionization chamber volume will lead to incomplete charging or charge conditioning of the aerosol. Too large an ionization chamber or too low an aerosol flow rate through the ionization chamber will lead to greater losses of particles in the chamber, which is also undesirable. For the purpose of this disclosure, the most appropriate range is a range where the nominal residence time of the aerosol flow in the chamber, which is the ratio of chamber volume to the volumetric aerosol flow rate is within an appropriate range. An aerosol flow rate of 20 cubic centimeter per second through an ionization chamber having a 40 cubic centimeter volume will result in a nominal residence time of 40/20=2 seconds. The most appropriate residence time for designing ionization chambers is between 0.2 and 20 seconds.
Different application also requires different ionization chamber sizes. For charging and charge conditioning purposes for DMS, the ionization chamber is generally in the range between 6 to 600 cubic centimeters in total volume.
The above approach to designing electrical ionizers for aerosol charging and charge conditioning for laboratory aerosol studies and aerosol size analysis by DMS is generally adequate for most applications. A similar approach can be used to design electrical ionizers for other applications where accuracy of charging and charge conditioning are important, and where the loss of particles in flowing through the ionizer is also an important consideration. For those skilled in the art of aerosol measurement, it will become clear that the specific approach described in this disclosure can also be used to design electrical ionizers for those applications where the end applications may be different, but the factors affecting the acceptance of the electrical ionizer are similar or substantially the same. Further discussion of the application of the approach described in this disclosure for other applications, therefore, will not be made further.
Results in
These and other laboratory studies we have made show that the specific approach described in this disclosure to designing electrical ionizer for aerosol charge conditioning and measurement by DMS will lead to accurate measurement results. The approach can also be used for other applications where charging or charge-conditioning of aerosols are important.
Although the present invention has been described with reference to preferred embodiments, workers skilled in the art will recognize that changes may be made in form and detail without departing from the spirit and scope of the invention.
The present application is based on and claims the benefit of U.S. provisional patent application Ser. No. 61/312,455, filed Mar. 10, 2010, the content of which is hereby incorporated by reference in its entirety.
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B. Y. H. Liu, D. Y. H. Pui and B. Y. Lin, “Aerosol Charge Neutralization by Radioactive Alpha Source,” Particle Characterization, 3:111-116 (1986). |
F. J. Romay., B. Y. H. Liu and D.Y.H. Pui, “A Sonice Jet Corona Ionzer for Electrostatic Discharge and Aerosol Neutralization,” Aerosol Sci. and Technol. 20:31-34 (1994). |
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Number | Date | Country | |
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Number | Date | Country | |
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