The Phase Rule and Its ApplicationsFindlay, Alexander
Science
The Phase Rule and Its Applications
Findlay, Alexander
Chemistry, Physical and theoretical; Phase rule and equilibrium; Solution (Chemistry)
In another series of equilibria which can be obtained, carbon is one of the
solid phases. In Fig. 121 the equilibria between carbon, carbon monoxide,
and carbon dioxide under pressures of one and of a quarter atmosphere, are
represented by dotted lines.[379]
If we consider only the dotted line on the right, representing the
equilibria under atmospheric pressure, we see that the points in which the
dotted line cuts the other two curves must represent systems in which
carbon monoxide and carbon dioxide are in equilibrium with FeO +
Fe_{3}O_{4} + C, on the one hand, and with Fe + FeO + C on the other. These
systems can only exist at one definite temperature, if we make the
restriction that the pressure is maintained constant (atmospheric
pressure). Starting, therefore, with the equilibrium FeO + Fe_{3}O_{4} + CO
+ CO_{2} at a temperature of about 670°, and then add carbon to the system,
the reaction
C + CO_{2} = 2CO
will occur, because the concentration of CO_{2} is greater than what
corresponds with the system FeO + Fe_{3}O_{4} + C in equilibrium with
carbon monoxide and dioxide. In consequence of this reaction, the
equilibrium between FeO + Fe_{3}O_{4} and the gas phase is disturbed, and
the change in the composition of the gas phase is opposed by the reaction
Fe_{3}O_{4} + CO = 3FeO + CO_{2}, which continues until either all the
carbon {309} or all the ferric oxide is used up. If the ferric oxide first
disappears, the equilibrium corresponds with a point on the dotted line in
the middle area of Fig. 121, which represents equilibria between FeO + C as
solid phases, and a mixture of carbon monoxide and dioxide as gas phase. If
the temperature is higher than 685°, at which temperature the curve for
C--CO--CO_{2} cuts that for Fe--FeO--CO--CO_{2}; then, when all the ferric
oxide has disappeared, the concentration of CO_{2} is still too great for
the coexistence of FeO and C. Consequently, there occurs the reaction C +
CO_{2} = 2CO, and the composition of the gas phase alters until a point on
the upper curve is reached. A further increase in the concentration of CO
is opposed by the reaction FeO + CO = Fe + CO_{2}, and the pressure remains
constant until all the ferrous oxide is reduced and only iron and carbon
remain in equilibrium with gas. If the quantities of the substances have
been rightly chosen, we ultimately reach a point on the dotted curve in the
upper part of Fig. 121.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account