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Instrumentation for atmospheric ion measurements

2005/01/19 by Karen Aplin, Aplin, K. L.
Earth and Planetary Sciences · Environmental Science · #Atmospheric Ozone and Climate #Atmospheric aerosols and clouds #Atmospheric and Oceanic Physics (physics.ao-ph) #Atmospheric chemistry and aerosols #FOS: Physical sciences #Geophysics (physics.geo-ph)

paper · pdf · doi:10.48550/arxiv.physics/0501106

openalex publication_date 2005/01/19 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/28

Abstract

Small ions are part of the atmospheric aerosol spectrum, and study of ion-aerosol interactions is fundamental in atmospheric physics. Air ion physics and instrumentation are reviewed, including the historical context. A miniaturised Gerdien condenser for ion measurement, operating in situ to minimise inlet errors, is described. Two operating modes using independent current and voltage decay measurements are employed. A more sophisticated self-calibrating and fully programmable ion mobility spectrometer (PIMS) based on the same principles, is also discussed. Detailed analysis of error terms and application of new technology is demonstrated to greatly improve its capability. Self-consistent experimental approaches, including ionisation and ion concentration instruments, are used for calibration. In developing and characterising the individual components of the PIMS, favourable and unfavourable operating regimes are identified: this approach can also be applied to other aspiration ion counting techniques. Use of a sophisticated programmable electrometer permits compensation for leakage terms. Electrically-charged aerosol particles have been found to complicate the ion measurements. Consequently, conventional ion-aerosol theory, which neglects the particulate concentration, is thought to be incomplete. The polymodal ion mobility spectrum is also found to influence the instrument's operation. Development of the novel programmable ion instrumentation, in conjunction with consideration of the ion mobility spectrum yields an improved and flexible approach to in situ atmospheric ion measurements.

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