P091-0001
Vega X-Ray Fluorescence Spectroscopy: Chemical Composition of Venus Clouds
Abstract:
The abundance of Fe is low and corresponds to ≈1% of FeCl3 in the cloud mass loading. (Recently Perez-Hoyos et al. (2018, JGRE 123, 145-162) calculated the NUV absorption using erroneously the FeCl3 spectrum in ethyl acetate instead of that in H2SO4.)
If phosphorus exists in the atmosphere, then thermochemistry predicts dimer P4O6 as its major component. It can react with H2SO4 and form phosphoric acid H3PO4 that precipitates and gradually loses water converting into phosphoric anhydride P2O5. It exists as aerosol down to 25 km and then evaporates. There are two facts in favor of this explanation: the observed aerosol extended down to 33 km where the nephelometer was switched off, and the similar aerosol altitude distributions was observed by Venera 8.
The significant excess of Cl over Fe requires another chlorine aerosol species, in addition to FeCl3. AlCl3 is the best candidate that could condense in the middle cloud layer with the densities close to those measured. Composition of the clouds based on the Vega XRF data is given in the table.
According to Greaves et al. (2020), the observed absorption line at 266.94 GHz originates near 56 km and is a sum of PH3 (90%) and SO2 (10%). Expected contributions of the species must be proportional to products of their mixing ratio and line strength, that is, 2×10-8 and 1.23×10-22 cm for PH3 and 10-5 and 3.15×10-23 cm for SO2. (Line strengths are from HITRAN.) Hence the expected effect of SO2 exceeds that of PH3 by two orders of magnitude.