Measurement of light scattering in an urban area with a nephelometer and PM2.5 FDMS TEOM monitor: Accounting for the effect of water
| Autor: | Delbert J. Eatough, Jaron C. Hansen, Paul M. Cropper |
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| Rok vydání: | 2013 |
| Předmět: |
Light
Nephelometer Spectrometer business.industry Scattering Water Humidity Management Monitoring Policy and Law Aethalometer Light scattering Aerosol Optics Nephelometry and Turbidimetry Extinction (optical mineralogy) Environmental science Particle Particulate Matter Cities business Waste Management and Disposal Remote sensing |
| Zdroj: | Journal of the Air & Waste Management Association. 63:1004-1011 |
| ISSN: | 2162-2906 1096-2247 |
| DOI: | 10.1080/10962247.2013.770421 |
| Popis: | The US. Environmental Protection Agency (EPA) has proposed a new secondary standard based on visibility in urban areas. The proposed standard will be based on light extinction, calculated from 24-hr averaged measurements. It would be desirable to base the standard on a shorter averaging time to better represent human perception of visibility This could be accomplished by either an estimation of extinction from semicontinuous particulate matter (PM) data or direct measurement of scattering and absorption. To this end we have compared 1-hr measurements of fine plus coarse particulate scattering using a nephelometer along with an estimate of absorption from aethalometer measurements. The study took place in Lindon, UT, during February and March 2012. The nephelometer measurements were corrected for coarse particle scattering and compared to the Filter Dynamic Measurement System (FDMS) tapered element oscillating microbalance monitor (TEOM) PM2.5 measurements. The two measurements agreed with a mass scattering coefficient of 3.3 +/- 0.3 m2/g at relative humidity below 80%. However at higher humidity, the nephelometer gave higher scattering results due to water absorbed by ammonium nitrate and ammonium sulfate in the particles. This particle-associated water is not measured by the FDMS TEOM. The FDMS TEOM data could be corrected for this difference using appropriate IMPROVE protocols if the particle composition is known. However a better approach may be to use a particle measurement system that allows for semicontinuous measurements but also measures particle bound water Data are presented from a 2003 study in Rubidoux, CA, showing how this could be accomplished using a Grimm model 1100 aerosol spectrometer or comparable instrument. |
| Databáze: | OpenAIRE |
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