Monday, March 15, 2010

Aurora 2000 PM correlation nephelometer

The Aurora 2000 PM correlation nephelometer uses a single wavelength to measure aerosol light scattering and derive particulate concentrations.

The Aurora 2000 nephelometer is available in two configurations.

PM correlation nephelometer
  1. PM2.5 Size Selective Inlet (SSI) to sample PM2.5,
    ideal in areas with stable aerosol chemistry
  2. Communicates directly with a BAM1020,
    ideal in areas with multiple aerosol sources

More info at = www.ecotech.com


Configuration 1

The Aurora 2000 nepheleometer is available with automatic flow control and a PM2.5 Size Selective Inlet. This configuration improves the correlation between the Aurora 2000 nephelometer and Federal Equivalent PM2.5 Methods. pm 2.5 correlation nephelometer

This sampling method enables a manual correction factor to be entered in order to derive real time (1 minute) PM2.5 concentrations. In applications where the aerosol chemistry is stable this configuration provides excellent results with minimal maintenance and a high degree of correlation.

The Aurora Nephelometer employs a smart heater controlled by a relative humidity sensor, this allows the user to set the maximum relative humidity of the sampled air, eliminating the influence of water vapour on the measurement and thus performing a “dry measurement”.


Configuration 2

In applications where aerosol chemistry is subject to change, a correction factor derived from manual sampling may be unreliable. nephelometer
The Automatic correlation PM nephelometer connects directly to the Met One BAM1020 in order to monitor and log PM hourly averages generated by a BAM1020 (PMBAM). These hourly averages are compared to the Aurora nephelometer’s hourly average scattering coefficient (σscat) and a scattering to PM coefficient factor (CoefScat/PM) is calculated. This factor is then applied to the next hour of 1 min scattering coefficients measured in order to determine a 1 minute average for PM concentrations (PMaurora). This data can also be used to determine changes in aerosol source through deviations in light scattering from the expected values.

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