Extended Data Fig. 3: Iron and nickel carbonyl sublimation properties.
From: Iron and nickel atoms in cometary atmospheres even far from the Sun

a, Sublimation rates (Z; in molecules cm−2 s−1) of Fe and Ni carbonyls as a function of temperature, compared to those of the main ices in comets. The carbonyl rates are intermediate between those of H2O and CO2. b, The ratio of the sublimation rate of Ni(CO)4 over that of Fe(CO)5 shows that the former is considerably higher than the latter. These quantities were computed as follows. As in refs. 53,54, we estimate the condensation or sublimation temperature Ts of these compounds by solving the equation fxnkTs = Pv,x(Ts) where fx is the relative abundance of species x, n is the number density of the gas, k is the Boltzmann constant, and Pv,x is the vapour pressure, given by the relation log[Pv,x(T)] = −(A/T) + B. The constants A and B for Fe(CO)5 and Ni(CO)4 are obtained from refs. 55,56: A = 2,097 K and B = 11.62 for Fe(CO)5, A = 1,534 K and B = 10.87 for Ni(CO)4, with Pv,x in dyn cm−2. We consider relative abundances fx of 10−3–10−5 × fx(H2O) for both Fe(CO)5 and Ni(CO)4, and we adopt n = 1013 cm−3 as in ref. 54. The resulting sublimation temperatures of the iron and nickel carbonyls (97–108 K and 74–82 K, respectively, depending on fx) are between the sublimation temperatures of H2O and CO2 (152 K and 72 K), whereas CO sublimates at 25 K (ref. 54). The sublimation rate (in molecules cm−2 s−1) from the surface of a pure ice into vacuum can be expressed as57: Zx(T) = Pv,x(T)(2πmxkT)−1/2, where T is the ice temperature and mx the mass of species x.