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Published on: February 27, 2021
Halite particles injected into the stratosphere by the 1982 el chichon eruption
Summary
Halite particles from the El Chichón eruption likely influenced stratospheric chemistry. These particles may have released hydrogen chloride, potentially impacting ozone depletion.
Area of Science:
- Stratospheric chemistry
- Volcanic aerosol science
- Atmospheric chemistry
Background:
- The 1982 El Chichón eruption injected significant material into the stratosphere.
- Understanding the composition and evolution of volcanic aerosols is crucial for atmospheric studies.
Purpose of the Study:
- To identify and characterize halite particles from the El Chichón eruption cloud.
- To investigate the potential role of these particles in stratospheric chemical processes.
Main Methods:
- Collection of stratospheric particles using a quartz crystal microbalance cascade impactor.
- Analysis of particle size and composition.
- Correlation with lidar measurements of hydrogen chloride and optical depolarization.
Main Results:
- Identified halite particles approximately 2 micrometers in size.
- Observed enrichments in hydrogen chloride and increased optical depolarization, potentially linked to halite.
- Evidence suggests halite reacted with sulfuric acid, releasing hydrogen chloride.
Conclusions:
- Halite particles from the El Chichón eruption were present in the lower stratosphere.
- These particles may have influenced observed atmospheric phenomena, including hydrogen chloride concentrations.
- The release of hydrogen chloride from halite could contribute to catalytic ozone destruction in the stratosphere.
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