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               296                                                                                        Aerosols


                         TABLE III Remote Sensing Methods for Atmospheric Aerosol Characterization
                                   Method                    Measurable light           Light source
                         Ground-based, passive
                          Photometry and radiometry     Optical thickness; sky brightness  Sun
                          Polarimetry                   Polarization of skylight   Sun; diffuse sky
                          Polar nephelometry            Extinction coefficient      Sun; skylight
                          Teleradiometry                Horizon brightness; relative contrast  Reflected and scattered light
                         Airborne, passive
                          Spectrophotometry             Albedo; optical thickness  Reflected sunlight
                          Limb occultation (satellite) radiometry  Optical thickness; polarization  Sunlight
                         Active sensing
                          Transmission/backscatter      Optical thickness          Searchlight; LIDAR a
                           a
                            LIDAR denotes light detection and ranging.
               spectroscopists, meteorologists, and space engineers for  a matrix of many different, often unknown components.
               many years. The publications listed in the bibliography  New methods have been introduced that involve spectro-
               contain the details of the methodology and the intercom-  scopic examination by a variety of techniques including
               parisons between remote sensors of different kinds and  X-ray fluorescence, plasma emission spectroscopy, neu-
               direct aerosol observations.                      tron activation analysis, photoelectron spectroscopy, and
                 In general, the methods are difficult to interpret quan-  mass spectroscopy.
               titatively in terms of aerosol properties because of am-  The wet chemical methods are summarized in Table IV.
               biguities in the size distribution–concentration–distance  Basically this approach centers on the water-soluble ex-
               profiles and variations in chemical properties contributing  tract obtained from filter substrates, impactor plates, or
               to the index of refraction. Nevertheless, remote sensing  other collection surfaces. The extraction process has to
               continues to be important for the surveillance of aerosol  be done with some care to ensure that all of the water-
               behavior in planetary atmospheres.                soluble material is removed. Standard extraction methods
                                                                 now involve the use of ultrasonic devices to maximize
                                                                 extraction efficiency. Once the extract is obtained, it can
               B. Methods for Chemical Characterization          be  subjected  to  a  number  of  the  methods  listed  in  Ta-

               After the collection of particles, it is useful to determine  ble IV, such that a detailed elemental breakdown by inor-
               the chemical characteristics of the material. This can be  ganic and (water-soluble) organic carbon is accomplished.
               accomplishedintermsofanalysisofawholesamplecorre-
               sponding to the total mass concentration, or it can be done
               on a size-fractionated basis. In some cases, individual par-  TABLE IV Wet Chemical Methods for Particle Analysis
               ticles can also be examined. Chemical characterization is  Particle                Method
               very important when one is considering a heterogeneous
               collection of aerosol particles such as those found in the  Cations
               ambient air or in the workplace. These include whole sam-  Ammonium        Indol phenol blue colorimetry,
                                                                                            ion chromatography
               ple microscopic analysis by collected batch, as well as
                                                                 Anions
               continuous measurement.
                                                                   Sulfate                Methylthymol blue colorimetry,
                                                                                            ion chromatography
                 1. Macroscopic Techniques                         Nitrate                Cadmium reduction, ion
                                                                                            chromatography
               Macroscopic methods for chemical analysis essentially  Chloride            Ferric thiocyanate, ion
               take either all of the particulate matter sampled or a sig-                  chromatography
               nificant protion of it for bulk analysis. Traditionally, this  Elements
               has been approached by the application of standard mi-  Pb, Fe, Na, K, Ca, Cr,  Atomic absorption spectroscopy,
               crochemical techniques of wet chemistry. The unique an-  Ni, As, Mn, Si      plasma emission spectroscopy
               alytical requirement for aerosol particle samples is the  Carbonaceous material
               microgram quantities collected. The analytical methods  Solvent-soluble organics  Extraction and carbon detection;
                                                                                            differential thermal analysis
               adopted must be capable of detecting these quantities in
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