03.08.2013 Views

Dipl. Ing. Matthias Mayerhofer Technische Universität München ...

Dipl. Ing. Matthias Mayerhofer Technische Universität München ...

Dipl. Ing. Matthias Mayerhofer Technische Universität München ...

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

Iron Based Catalysts 33<br />

The percentage of the metallic iron that is available after reduction can be determined from the<br />

hydrogen consumption given from the TPR profiles and compared to that of the support (Virginie,2010a).<br />

Ellingham Lines:<br />

Ellingham Lines, as presented in Figure 15, is a graph showing the temperature dependence of the<br />

stability for compounds. They are used to determine the different iron oxides in relation to the oxygen<br />

potential and temperature in the product gas. The diagrams are useful in predicting the conditions<br />

under which a metal ore will be reduced to metal. The Ellingham lines indicate the temperature<br />

range at which the carbon monoxide will act as a reducing agent. The logarithmic quotient of<br />

the partial pressure of CO2 and CO is referred to as the oxygen potential. According to this diagram,<br />

there is only a small window at which the iron is kept to its metallic state (Nordgreen,2012).<br />

The oxygen potential in the product gas varies sharply between metallic iron and its oxides<br />

(Nordgreen,2006).<br />

The standard Gibbs reactions of formation of various oxides of iron are:<br />

2Fe + O2 → 2FeO (wüstite) (42)<br />

6FeO + O2 →2 Fe3O4 (magnetite) (43)<br />

4 Fe3O4 + O2 → 6 Fe2O3 (hematite) (44)<br />

Every point in an Ellingham diagram represents a unique thermodynamic state (combination of<br />

temperature and partial pressure of oxygen). Any point is a pair of values of T and RT ln p(O2) and<br />

substitution of the value of T into the value of RT ln p(O2) gives the corresponding value of the partial<br />

pressure of oxygen.<br />

A gaseous atmosphere containing oxygen gas in equilibrium with carbon thus contains both CO<br />

and CO2, but the different thermodynamic stabilities of two gases causes the ratio p(CO)/p(CO2) in<br />

the gas in equilibrium with carbon to be a significant function of temperature. At lower temperatures<br />

CO2 is more stable than CO and hence the gas in equilibrium with carbon is predominantly CO2.<br />

The composition of the gas mixture in equilibrium with pure carbon (at unit activity) is determined<br />

by the equilibrium C+CO2 →2CO.<br />

Figure 15: Ellingham lines (Nordgreen,2012)

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!