Abstract
Equilibrium vapor pressures of iron from its dilute solutions in liquid uranium were measured at high temperatures (2250–2750 K). From the Fe vapor pressure data at known compositions ( x Fe), Henry’s coefficient ( K Fe= p Fe/ x Fe) of the solute was obtained as log K Fe (±0.07) (Pa)=−18975.6(±1098.1)/T+11.15(±0.44) . The behavior of K Fe( T) is shown to be marginally different from that of the equilibrium vapor pressures of pure liquid iron ( p Fe°). The partial molar excess Gibbs energy of iron at infinite dilution derived from the behavior is expressed as Δ E G ̄ Fe ∞=−1588+1.25T ( J mol −1) . The result is discussed in the light of the quasi-regular solution model and compared with data of the system available in the literature.
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