posted on 2024-10-30, 15:07authored byStefano Pantaleone, Giulia De Gasperis, Marta Corno, Albert Rimola, Nadia Balucani, Piero Ugliengo
The prebiotic history of phosphorus is a matter of debate
in the
scientific community: its origin, how it landed on Earth, the selective
speciation of the phosphate, and its inclusion in the organic matrix
are the main unsolved issues. In this regard, Schreibersite ((Fe,Ni)3P), a mineral present in iron meteorites, can play a fundamental
role as a carrier of reactive P which, as a result of the weathering
processes, produces oxygenated phosphorus compounds, even the phosphate
among others. In the present paper, we studied the interaction of
methanol (alone and mixed with water) with the Schreibersite surfaces
throughout periodic density functional theory calculations at the
PBE level. The results indicate that Schreibersite promotes the deprotonation
of methanol and water both from thermodynamic and kinetic points of
view, thus enabling the first step toward corrosion. We have simulated
advanced stages of the corrosion process up to the formation of the
phosphate and the phosphorylated form of methanol (methyl phosphate),
showing that the formation of both products is thermodynamically favored,
as well as its solubilization, which allows other water molecules
to proceed with further corrosion of Schreibersite.