REALTIME OPTICAL METHOD AND SYSTEM FOR DETECTING AND CLASSIFYING BIOLOGICAL AND NON-BIOLOGICAL PARTICLES
20170315045 · 2017-11-02
Inventors
Cpc classification
G01N2021/217
PHYSICS
International classification
Abstract
Methods, apparatuses, and systems for detecting and classifying individual airborne biological and non-biological particles, in real time, based on particle size and polarized elastic scatter. Auto-fluorescence content may also be used along with particle size and polarized elastic scatter for further orthogonal classification. With polarized elastic scattering, the degree of linear or circular depolarization produced from particle morphology, refractive index, internal asymmetric structures and molecular optical activity can be used for classifying individual airborne particles. Alternatively, circular intensity differential scattering (CIDS) or linear intensity differential scattering (LIDS) can be used to discriminate individual particles.
Claims
1. A method of detecting and classifying single airborne particles, said method comprising: (a) directing an airborne sample having a plurality of airborne particles into an optical sensing zone of an optical detector, the airborne sample being taken from an environment surrounding the optical detector; (b) illuminating a single airborne particle in the optical sensing zone with a first polarized light beam; (c) detecting elastic light scatter resulting from the illumination of the single airborne particle with the first polarized light beam; (d) determining, using the detected elastic light scatter resulting from the illumination of the single airborne particle with the first polarized light beam, each of the following: (i) a size of the single airborne particle; and, (ii) a first value for the single airborne particle wherein the first value is one of a depolarization value for the single airborne particle and an intensity differential elastic scattering value for the single airborne particle; and, (e) determining at least one characteristic of the single airborne particle based on the size of the single airborne particle and the first value for the single airborne particle.
2. The method of claim 1, wherein: (a) the single airborne particle has an aerodynamic diameter of no greater than 10 microns.
3. The method of claim 1, wherein: (a) the at least one characteristic identifies the single airborne particle as biological or non-biological.
4. The method of claim 1, wherein: (a) the at least one characteristic identifies the single airborne particle as a specific type of biological particle.
5. The method of claim 1, further including the steps of: (a) illuminating the single airborne particle in the optical sensing zone with a second polarized light beam wherein the second polarized light beam is spaced a predetermined distance from the first polarized light beam, the first polarized light beam is a horizontally polarized light beam and the second polarized light beam is a vertically polarized light beam; and, (b) detecting elastic light scatter resulting from the illumination of the single airborne particle with the horizontally polarized light beam and the vertically polarized light beam.
6. The method of claim 5, further including the step of: (a) prior to detecting step of claim 5, passing elastic light scatter resulting from the illumination of the single airborne particle with the horizontally polarized light beam and the vertically polarized light beam through a horizontal polarization filter.
7. The method of claim 6, wherein: (a) the first value is a linear depolarization value.
8. The method of claim 1, further including the steps of: (a) illuminating the single airborne particle in the optical sensing zone with a second polarized light beam wherein the second polarized light beam is spaced a predetermined distance from the first polarized light beam, the first polarized light beam is a right handed circularly polarized light beam and the second polarized light beam is a left handed circularly polarized light beam.
9. The method of claim 8, wherein: (a) the first value is one of a circular depolarization value and circular intensity differential scattering value.
10. The method of claim 1, wherein: (a) if the first value is a depolarization value, determining the depolarization value by using at least one of the following equations: (i) δ.sub.N=[I.sub.V]/[I.sub.H+I.sub.V] where δ.sub.N represents normalized depolarization, I.sub.H represents the elastic scatter intensity for horizontally polarized light and is the same as the polarization state of the illumination beam and I.sub.V represents the elastic scatter intensity for vertically polarized light; (ii) δ=I.sub.HV/I.sub.HH where δ represents depolarization, I.sub.HH represents the elastic scatter intensity for horizontally polarized light and horizontally polarized incident beam, I.sub.HV represents the elastic scatter intensity for horizontally polarized light and a vertically polarized incident beam; (iii) δ.sub.+C=[I.sub.⊥]/[I.sub.∥+I.sub.⊥] where δ.sub.+C represents circular depolarization when using right handed circularly polarized light as the illumination source, I.sub.⊥ represents the elastic scatter intensity for perpendicularly polarized light and I.sub.∥ represents the elastic scatter intensity for parallel polarized light; (iv) δ.sub.−C=[I.sub.∥]/[I.sub.∥+I.sub.⊥] where δ.sub.−C represents circular depolarization when using left handed circularly polarized light as the illumination source, I.sub.⊥ represents the elastic scatter intensity for perpendicularly polarized light and I.sub.∥ represents the elastic scatter intensity for parallel polarized light; and, (b) if the first value is an intensity differential elastic scattering value, determining the intensity differential elastic scattering value by using at least one of the following equations: (i) [I.sub.L(θ)−I.sub.R(θ)]/[I.sub.L(θ)+I.sub.R(θ)] where I.sub.L(θ) is the light scattered at angle θ when the incident beam is left circularly polarized and I.sub.R(θ) is the light scattered at angle θ when the incident beam is right circularly polarized; and, (ii) [I.sub.H(θ)−I.sub.V(θ)]/[I.sub.H(θ)+I.sub.V(θ)] where I.sub.H(θ) is the light scattered at angle θ when the incident beam is horizontally polarized and I.sub.V(θ) is the light scattered at angle θ when the incident beam is vertically polarized.
11. A method of detecting and classifying single airborne particles, said method comprising: (a) using a vacuum source to pull an airborne sample having a plurality of airborne particles into an optical sensing zone of an optical detector from an environment surrounding the optical detector; (b) illuminating a single airborne particle in the optical sensing zone with a horizontally polarized light beam; (c) illuminating the single airborne particle in the optical sensing zone with a vertically polarized light beam, wherein the vertically polarized light beam illuminates the single airborne particle before or after the horizontally polarized light beam illuminates the single airborne particle; (d) detecting elastic light scatter resulting from the illumination of the single airborne particle with the horizontally polarized light beam and the vertically polarized light beam; and, (e) prior to the detecting step of paragraph (d), passing elastic light scatter resulting from the illumination of the single airborne particle with the horizontally polarized light beam through a horizontal polarization filter.
12. The method of claim 11, including the further step of: (a) a prior to the detecting step of paragraph (d) of claim 11, passing elastic light scatter resulting from the illumination of the single airborne particle with the vertically polarized light beam through a horizontal polarization filter.
13. The method of claim 11, including the further step of: (a) a prior to the detecting step of paragraph (d) of claim 11, passing elastic light scatter resulting from the illumination of the single airborne particle with the vertically polarized light beam through a vertical polarization filter.
14. The method of claim 12, including the further step of: (a) determining, using the detected elastic light scatter resulting from the illumination of the single airborne particle, each of the following: (i) a size of the single airborne particle; and, (ii) a linear depolarization value for the single airborne particle; and, (b) determining at least one characteristic of the single airborne particle based on the size of the single airborne particle and the linear depolarization value for the single airborne particle.
15. The method of claim 11, wherein: (a) the single airborne particle has an aerodynamic diameter in a range of 0.5 to 1.5 microns.
16. The method of claim 11, wherein: (a) the single airborne particle has an aerodynamic diameter no greater than 10 microns.
17. The method of claim 11, further including the step of: (a) passing elastic light scatter resulting from the illumination of the single airborne particle with the horizontal polarized light beam and the vertically polarized light beam through an orthogonal fluorescence detection channel wherein the orthogonal fluorescence detection channel is disposed on one side of the optical sensing zone and the horizontal polarization filter is disposed on an opposite side of the optical sensing zone.
18. The method of claim 12, further including the step of: (a) directing elastic light scatter passing through the horizontal polarization filter to a single light detector.
19. A single airborne particle optical analyzer for detecting and classifying single airborne particles, said single airborne particle optical analyzer comprising: (a) an optical sensing zone; (b) a vacuum source for pulling an airborne sample having a plurality of airborne particles into an optical sensing zone of an optical detector from an environment in which the optical sensing zone is located; (c) means for illuminating a single airborne particle in the optical sensing zone with at least one polarized light beam; (d) a light detector for detecting elastic light scatter resulting from the illumination of the single airborne particle; (e) a processor for determining, using the detected elastic light scatter resulting from the illumination of the single airborne particle, each of the following: (i) a size of the single airborne particle; and, (ii) a first value for the single airborne particle wherein the first value is one of a depolarization value for the single airborne particle and an intensity differential elastic scattering value for the single airborne particle; and, (f) the processor further being configured to determine at least one characteristic of the single airborne particle based on the size of the single airborne particle and the first value for the single airborne particle.
20. The single airborne particle optical analyzer of claim 19, wherein: (a) the single airborne particle has an aerodynamic diameter of no greater than 10 microns.
21. The single airborne particle optical analyzer of claim 19, wherein: (a) the at least one characteristic identifies the single airborne particle as biological or non-biological.
22. The single airborne particle optical analyzer of claim 19, wherein: (a) the at least one characteristic identifies the single airborne particle as a specific type of biological particle.
23. The single airborne particle optical analyzer of claim 19, wherein: (a) said means for illuminating includes a laser, a quarter wave retarder and a birefringent crystal, wherein the quarter water retarder circularly polarizes a beam generated by said laser and wherein said birefringent crystal produces vertically and horizontally polarized beams separated in space by a predetermined distance and said birefringent crystal is disposed relative to said optical sensing zone such that the single airborne particle is illuminated by the vertically and horizontally polarized beams as the single airborne particle passes through the optical sensing zone.
24. The single airborne particle optical analyzer of claim 23, further including: (a) a horizontal polarization filter being disposed relative to the optical sensing zone and the light detector such that elastic light scatter resulting from the illumination of the single airborne particle by the vertically and horizontally polarized beams passes through said horizontal polarization filter prior to the elastic light scatter being detected by the light detector.
25. A method of detecting and classifying single airborne particles, said method comprising: (a) directing an airborne sample having a plurality of airborne particles into an optical sensing zone of an optical detector, the airborne sample being taken from an environment surrounding the optical detector; (b) illuminating a single airborne particle in the optical sensing zone with a first polarized light beam; (c) determining from the illumination of the single airborne particle with the first polarized light beam, each of the following: (i) particle auto-fluorescence; and, (ii) a first value for the single airborne particle wherein the first value is a depolarization value for the single airborne particle; and, (d) determining at least one characteristic of the single airborne particle based on particle auto-fluorescence and the first value for the single airborne particle.
Description
BRIEF DESCRIPTION OF THE DRAWINGS
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DETAILED DESCRIPTION OF THE PREFERRED EMBODIMENTS OF THE INVENTION
[0030] The preferred forms of the presented invention will now be described with reference to
[0031] The preferred forms of the present invention relate to enhanced methods, apparatuses and systems for the detection and classification of biological and non-biological particulates in a real-time manner. The various detection schemes exploit one physical phenomena which involves the interaction of light with a single aerosol particle (i.e., polarized elastic scattering). A second physical phenomena which involves the interaction of light with a single aerosol particle may be used (i.e., fluorescence). In addition to these optical phenomena (i.e., polarized elastic scattering and fluorescence), the particle's size is preferably determined substantially simultaneously.
[0032] The preferred forms of the present invention are capable of detecting and classifying single airborne particles having an aerodynamic diameter of 10 microns or less (e.g., 0.5 to 1.5 microns).
[0033] Described herein are eight optical detectors having aerosol sensing configurations which are variations of linearly polarized and circularly polarized excitation approaches. Particle sizing using polarized elastic scatter detection is applicable to all the sensing configurations with the exception of
[0034]
[0035] In each of the of the preferred optical detectors when measuring only particle size and polarized elastics scatter, a broad range of wavelengths can be used for excitation (e.g., 200-1500 nm). When measuring particle size, polarized elastic scatter, and fluorescence, then the excitation wavelengths need to be within the absorption bands of the endogenous fluorophores of interest such as 250-300 nm and 350-450 nm. Depending on the sensing configuration, the excitation source can be an edge emitting laser diode, vertical cavity surface emitting laser diode, light emitting diode or other laser source. Additionally, one or more of the sources can be configured to produce dual circularly or linearly polarized beams separated in space (e.g., vertically separated) using birefringent optics for illumination of single particles with two or more wavelengths and two polarization states for each wavelength at a time exciting the particle.
[0036] For flow rates exceeding 1 liter per minute, laser line generating optics may be used to generate a laser line thickness of from about 5 to about 300 micron, and a depth of field and laser line width that is at least two times (2×) the diameter of the inlet (aerosol orifice). For flow rates exceeding 20 liters per minute the use of a circular inlet may become restrictive and a rectangular inlet may be preferred. In cases of a rectangular inlet used to accommodate sampling flows exceeding 20 liters per minute, a laser line generating approach is preferred with the depth of field and laser line width adjusted to illuminate, at a minimum, the entire rectangular nozzle area. The above laser line generating approaches are to ensure complete illumination of the air sampling region with the purpose of near 100% percent illumination of the aerosol particles sampled. The laser line thickness is desired to be small as permissible with the optical design to ensure the highest possible aerosol count rate without illuminating more than one aerosol particle, in the size range of interest, so as to minimize particle coincidence.
[0037] In applications that require little pressure drop during sampling and/or low audible noise during operation the configurations described in the present invention can be operated without an aerosol inlet nozzle. In these configurations, the laser line illumination geometry and collection optics are used to interrogate a predefined region of the sampling volume providing a means for individual particle detection with low pressure drop and low audible noise through the use of axial fans as the vacuum source.
[0038] Various light collection geometries can be employed with different parameters applied for the different physical phenomena being measured. For particle sizing, using polarized elastic scatter detection, there are numerous approaches that can be taken and those skilled in the art are familiar with near forward scattering collection, side scatter collection, back scatter collection and wide angle collection using parabolic collectors. For polarized elastic detection, the process is sensitive to the angular collection angle and, therefore, aerosol sensing configurations that include mainly side scatter collection are preferred. For fluorescence detection, collection of fluorescence orthogonal to the direction of the light beam is preferred to minimize effects of stray light on the fluorescence signal(s).
[0039]
[0040] The excitation source 100 is preferably a continuous source or modulated at 20 MHz or greater frequency and can be an edge emitting laser diode, vertical cavity surface emitting laser diode, light emitting diode or some other laser. The wavelength of excitation source 100 can be in the range of 200-1500 nm. Light emitted from source 100 is collimated using an aspheric lens 110. Depending on the source spatial filtering between the source 100 and the aspheric lens 110, or after lens 110 but before the aerosol cell 140 may be necessary. Collimated light is then introduced to beam shaping optics 125. The beam shaping optics 125 can be a single lens or group of lens designed to create a sheet of light at the aerosol nozzle region that is preferably from about 5 to about 300 micron in thickness and a depth of field and beam width that is preferably two times (2×) larger than the diameter of the inlet. In one embodiment, the beam shaping optics 125 can be a spherical lens and a cylinder lens designed to generate the above geometry. In another embodiment, only a cylinder lens is used for the beam shaping optics 125. In a further embodiment, the beam shaping optics 125 are comprised of top hat beam shaping optics which distributes the energy of a Guassian beam to a top hat profile. An example is a plano-convex lens that has a diffractive pattern located on its plane surface. Another example is the use of a single aspheric lens to convert the Guassian beam to a top hat profile. In another embodiment, the beam shaping optics 125 can be a single Powell lens or a spherical lens coupled with a Powell lens. When rectangular nozzles are used the beam shaping optics 125 can be comprised of the same components as listed above for circular nozzles but optical designs are preferably pursued that fulfill the depth of field requirements since the depth of field will be longer than the laser line width in these instances. The depth of field length in these instances can be greater than ten times (10×) the laser line width. To achieve near 100% illumination of sampled particles, within the desired size range, the width and depth of the sheet of light created by the beam shaping optics 125 should exceed, at a minimum, the dimensions of the rectangular nozzle.
[0041] Light from the beam optics 125 is introduced to a linear polarizer 120 with an extinction ratio preferably ranging from 100:1 to 10.sup.7:1. Certain sources such as edge emitting laser diodes and vertical cavity surface emitting laser diodes possess an inherent polarization ratio around 100:1 and depending on the accuracy requirements of the polarization measurement for a particular application the linear polarizer 120 can be omitted. After linear polarization, the collimated light is then introduced to a quarter wave retarder 130 to circularly polarize the beam before introduction to a birefringent crystal 135. Examples of birefringent crystals that can be used include yttrium vandate, barium borate, calcite and rutile. The introduction of the circularly polarized light to the birefringent crystal 135 produces vertically and horizontally polarized beams of equal intensity and separated in space (e.g., vertically separate) by a certain distance depending on the length of the crystal. In various configurations a separation of 250 micron to 1000 micron is preferred.
[0042] The light beams are then introduced into the optical viewing region 145 as seen in
[0043] In the preferred embodiment illustrated in
[0044] For linear depolarization detection and particle sizing, light that has scattered orthogonally to the laser source first passes through a horizontally polarized filter 207 and is then introduced to collection optic 170 and subsequently to light detector 210. The light detector 210 can be a silicon photodiode, gallium arsenide photodiode, avalanche photodiode, silicon photomultiplier, photomultiplier tube or arrays of these types of detectors. The type of detector will vary depending on the collection optic 170 used, the amount of scattered light excepted per aerosol event, the dynamic range of the detector, and the detector's cut-off frequency or response time. The signal produced from light detector 210 is then introduced to an amplifier circuit 220 whereby a 100 nanosecond to 10 microsecond current pulse is first converted to an analog voltage and then to a digital signal using an analog-to-digital converter 230. The signal from 230 is then introduced to the signal processor 240 for analysis. The signal processor 240 can be a microcontroller, digital signal processor, field programmable gate array or a microcomputer, as would be readily understood by one skilled in the field of signal processing.
[0045] As previously explained, for the configuration illustrated in
[0046] The amplifier circuits 220 for each channel can be configured to perform analog signal processing functions. The analog input bandwidth for the amplifier circuits 220 for each channel can be configured to capture the fastest expected current pulses. The pulse time is primarily a function of the aerosol particle's migration time through the optical viewing region 145 and is expected to be in the range of 100 nanoseconds to 10 microseconds. Additional analog signal processing functions include the triggering of a pulse detector circuit when an analog voltage level from the detection channels exceeds a preprogrammed level, integration and holding of light detector pulse for each detection event, production of a pulse height level for each detection channel, the use of one or more amplifier stages for each detection channel to capture the entire signal range for particles ranging in size from submicron in aerodynamic diameter to 25 micron or larger, and the production of an analog to digital conversion signal for each of the two detection events.
[0047] For both particle sizing and linear depolarization detection, the signal processor 240 is preferably configured to receive digital signals from the two detections events that occurred as the single particle traversed the horizontally and vertically polarized beams. For particle sizing, the first detection event is preferably used to size the particle and pulse height analysis is performed on each of the aerosol events occurring in the first and second illumination points or areas in the optical viewing region 145. For linear depolarization detection, the amplitudes of each detection per aerosol event is used for the depolarization measurement. The degree of depolarization for each aerosol event can be calculated by performing one of the calculations below:
δ.sub.N=[I.sub.V]/[I.sub.H+I.sub.V] or δ=I.sub.HV/I.sub.HH
The linear depolarization value is then preferably binned with the particle size for each aerosol event. Using particle size and linear depolarization value data for each aerosol particle, preferably a comparison can be made to a library of aerosol types from the previous measurements of known aerosols that include bacterial spores, vegetative cells, viruses, viral aggregates, protein toxin aggregates, fungal particles, pollen particles, man-made biological particles and non-biological aerosols such as salt particles, water droplets, dust particles, organic carbon particles and other relevant non-biological particles depending on the application. With the library and unknown particle data, polarized elastic scatter plots can be generated as a function of particle size permitting the detection and classification of biological and non-biological particles.
[0048]
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[0053] In the embodiment illustrated in
[0054] For particle sizing, the horizontally polarized scatter signal is used to size the particle and pulse height analysis is performed on the scatter amplitudes from vertically and horizontally polarized light. For linear depolarization detection, the amplitudes from each detection event for the two detectors is used for the depolarization measurement. The degree of depolarization for each aerosol event can be calculated by performing one of the calculations below:
δ.sub.N=[I.sub.V]/[I.sub.H+I.sub.V] or δ=I.sub.HV/I.sub.HH
The linear depolarization value is then binned with the particle size for each aerosol event. Using particle size and linear depolarization value data for each aerosol particle a comparison is preferably made to a library of aerosol types from the previous measurements of known aerosols that include bacterial spores, vegetative cells, viruses, viral aggregates, protein toxin aggregates, fungal particles, pollen particles, man-made biological particles and non-biological aerosols such as salt particles, water droplets, dust particles, organic carbon particles and other relevant non-biological particles depending on the application. With the library and unknown particle data, polarized elastic scatter plots can be generated as a function of particle size permitting the detection and classification of biological and non-biological particles.
[0055]
[0056] When measuring particle size, polarized elastic scatter, and fluorescence, the excitation wavelengths need to be within the absorption bands of the endogenous fluorophores of interest such as 250-300 nm and 350-450 nm. These excitation wavelength ranges correspond to the absorption bands to one or more endogenous fluorophores commonly encountered in biological particles, which include, but are not limited to aromatic amino acids, NADH, flavins, chlorophylls, and sideophores. For the fluorescence detection channel, similar detection electronics and detectors as that described in the above embodiments can be used with an additional fluorescence filter 208 for passing a band of light that is matched with the emission wavelengths of the desired endogenous fluorophores. In this embodiment, both the linear depolarization value obtained for each particles and the presence or absence of fluorescence and the fluorescence intensity can be used for classification of biological particles from non-biological particles and to classify biological types from one another.
[0057]
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[0059] With circular depolarization detection, the normalized depolarization of light scattered from a particle is given by the relationship:
δ.sub.+C=[I.sub.⊥]/[I.sub.∥+I.sub.⊥]
δ.sub.−C=[I.sub.∥]/[I.sub.∥+I.sub.⊥]
Where δ.sub.+C represents circular depolarization when using right handed polarized light as the illumination source, δ.sub.−C represents circular depolarization when using left handed polarized light as the illumination source, I.sub.⊥ represents the scatter intensity for perpendicularly polarized light and I.sub.∥ represents the scatter intensity for parallel polarized light. In this embodiment, circular depolarization measurements can be performed on single particles using both left handed and right handed circularly polarized excitation. The same detectors and electronics as the embodiment illustrated in
[0060] Signal processing for this embodiment involves measuring the polarized scatter intensity of parallel and perpendicularly polarized light for each illumination event per aerosol particle and then calculating the left handed and right handed circular depolarization ratios for each particle. The circular depolarization values are then binned with the particle size for each aerosol event. Particle size and circular depolarization value data for each aerosol particle is then compared to a library of aerosol types from the previous measurements of known aerosols that include bacterial spores, vegetative cells, viruses, viral aggregates, protein toxin aggregates, fungal particles, pollen particles, man-made biological particles and non-biological aerosols such as salt particles, water droplets, dust particles, organic carbon particles and other relevant non-biological particles depending on the application. With the library and unknown particle data, polarized elastic scatter plots can be generated as a function of particle size permitting the detection and classification of biological and non-biological particles.
[0061]
[I.sub.L−I.sub.R]/[I.sub.L+I.sub.R],
Where I.sub.L is the light scattered intensity when the incident beam is left circularly polarized and I.sub.R is the light scattered intensity when the incident beam is right circularly polarized. The current pulses produced from the detection events are used for measuring the CIDS value for each particle. The CIDS value is then binned with the particle size for each aerosol event. Using particle size and CIDS value data for each aerosol particle, a comparison can be made to a library of aerosol types from the previous measurements of known aerosols that include bacterial spores, vegetative cells, viruses, viral aggregates, protein toxin aggregates, fungal particles, pollen particles, man-made biological particles and non-biological aerosols such as salt particles, water droplets, dust particles, organic carbon particles and other relevant non-biological particles depending on the application. With the library and unknown particle data, polarized elastic scatter plots can be generated as a function of particle size permitting the detection and classification of biological and non-biological particles.
[0062]
[I.sub.H−I.sub.V]/[I.sub.H+I.sub.V],
Where I.sub.H is the light scattering intensity when the incident beam is horizontally polarized and I.sub.V is the light scattered when the incident beam is vertically polarized. The current pulses produced from the detection events are used for measuring the LIDS value for each particle. The LIDS value is then binned with the particle size for each aerosol event. Using particle size and LIDS value data for each aerosol particle, a comparison can be made to a library of aerosol types from the previous measurements of known aerosols that include bacterial spores, vegetative cells, viruses, viral aggregates, protein toxin aggregates, fungal particles, pollen particles, man-made biological particles and non-biological aerosols such as salt particles, water droplets, dust particles, organic carbon particles and other relevant non-biological particles depending on the application. With the library and unknown particle data, polarized elastic scatter plots can be generated as a function of particle size permitting the detection and classification of biological and non-biological particles.
[0063]
[0064] The forgoing disclosure of the preferred embodiments of the present invention has been presented for purposes of illustration and description. It is not intended to be exhaustive or to limit the invention to the precise forms disclosed. Many variations and modifications of the embodiments described herein will be apparent to one of ordinary skill in the art in light of the above disclosure. The scope of the invention is to be defined only by the claims appended hereto, and by their equivalents. The claims are not limited to the preferred embodiments and have been written to preclude such a narrow construction using the principles of claim differentiation.
[0065] Further, in describing representative embodiments of the present invention, the specification may have presented the preferred method and/or process of the present invention as a particular sequence of steps. However, to the extent that the method or process does not rely on the particular order of steps set forth herein, the method or process should not be limited to the particular sequence of steps described. As one of ordinary skill in the art would appreciate, other sequences of steps may be possible. Therefore, the particular order of steps set forth in the specification should not be construed as limitations on the claims. In addition, the claims directed to the method and/or process of the present invention should not be limited to the performance of their steps in the order presented, and one skilled in the art can readily appreciate that the sequences may be varied and still remain within the spirit and scope of the present invention.