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Large Uncertainties in the Thermodynamics of Phosphorus (III) Oxide (PO) Have Significant Implications for Phosphorus Species in Planetary Atmospheres

arXiv:2305.17405 · doi:10.1021/acsearthspacechem.3c00016

Abstract

Phosphorus (III) oxide (PO) has been suggested to be a major component of the gas phase phosphorus chemistry in the atmospheres of gas giant planets and of Venus. However, PO's proposed role is based on thermodynamic modeling, itself based on values for the free energy of formation of PO estimated from limited experimental data. Values of the standard Gibbs free energy of formation (Go(g)) of PO in the literature differ by up to ~656 kJ/mol, a huge range. Depending on which value is assumed, PO may either be the majority phosphorus species present or be completely absent from modeled atmospheres. Here, we critically review the literature thermodynamic values and compare their predictions to observed constraints on PO geochemistry. We conclude that the widely used values from the NIST/JANAF database are almost certainly too low (predicting that PO is more stable than is plausible). We show that, regardless of the value of Go(g) for PO assumed, the formation of phosphine from PO in the Venusian atmosphere is thermodynamically unfavorable. We conclude that there is a need for more robust data on both the thermodynamics of phosphorus chemistry for astronomical and geological modeling in general and for understanding the atmosphere of Venus and the gas giant planets in particular.

Article published in ACS Earth Space Chem. https://pubs.acs.org/doi/full/10.1021/acsearthspacechem.3c00016

References in corpus (2)

Large Uncertainties in the Thermodynamics of Phosphorus (III) Oxide (P$_4$O$_6$) Have Significant Implications for Phosphorus Species in Planetary Atmospheres · wovepaper