There have been volcanic eruptions in the past with a 
significant co-emission of halogens.
See for instance this recent study 
https://acp.copernicus.org/articles/21/9009/2021/acp-21-9009-2021.html
So in a similar case (unlikely but possible) this would matter.


> On 3 Aug 2021, at 18:19, Kevin Lister <kevin.lister2...@gmail.com> wrote:
> 
> 
> I would doubt that there is enough HCl in the atmosphere to make this a 
> significant contributor to the overall CO2 imbalance. 
> 
>> On Tue, Aug 3, 2021 at 12:29 AM Greg Rau <gh...@sbcglobal.net> wrote:
>> 2HCl + CaCO3 ---> CaCl2 + CO2 + H2O.   How is this a good thing for GHGs and 
>> GW?
>> Greg
>> 
>> On Monday, August 2, 2021, 03:52:35 PM PDT, Geoeng Info 
>> <infogeo...@gmail.com> wrote:
>> 
>> 
>> https://pubs.acs.org/doi/abs/10.1021/acsearthspacechem.1c00151
>> 
>> Heterogeneous Reactivity of HCl on CaCO3 Aerosols at Stratospheric 
>> Temperature
>> 
>> Han N. Huynh and V. Faye McNeill
>> 
>> 
>> Abstract
>> Recently proposed as a possible alternative to sulfate particles for 
>> stratospheric solar radiation management (SSRM), calcite (CaCO3) aerosols 
>> have been modeled to have minimal negative impact on both stratospheric 
>> ozone level, through heterogeneous chemistry, and stratospheric temperature. 
>> However, the heterogeneous chemistry of CaCO3 aerosols with relevant trace 
>> gases, such as HCl, at stratospheric conditions is still underexamined. We 
>> studied the kinetics of HCl uptake on airborne CaCO3 aerosols at 
>> stratospheric temperature, 207 ± 3 K, by performing experiments under dry 
>> conditions using an aerosol flow tube coupled with a custom-built quadrupole 
>> chemical ionization mass spectrometer (CIMS) for HCl detection. The reactive 
>> uptake coefficient for HCl was measured to be 0.076 ± 0.009. This exceeds 
>> the reactive uptake coefficient of 0.013 ± 0.001 that we previously reported 
>> for this system at 296 K, consistent with the expected negative temperature 
>> dependence of gas uptake on solid surfaces. This finding suggests an initial 
>> strong reactive uptake of HCl gas on CaCO3 aerosol surfaces in the 
>> stratosphere
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