Equilibrium of Sulfur-Bearing Gases and Solids Relevant to the Burning of Limestone

The American Institute of Mining, Metallurgical, and Petroleum Engineers
H. A. Wriedt L. S. Darken
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
9
File Size:
739 KB
Publication Date:
Jan 1, 1974

Abstract

The equilibria at 1 atm total pressure and 600° to 1300°C (1112° to 2372°F) between gas mixtures with various partial pressures of the reactive constituents (principally sulfur dioxide, carbon dioxide, water vapor, oxygen or carbon monoxide, and hydrogen) and coexisting solid phases (groups variously including calcium oxide, calcium carbonate, calcium sulfide, calcium sulfate, iron, ferrous sulfide, and the iron oxides) are examined. Tables and charts show the combinations of temperature, oxygen activity, and carbon dioxide partial pressure under which the various groups of the solid phases coexist and the corresponding sulfur dioxide pressures. In the presence of calcium sulfide, calcium sulfate, and calcium oxide, the partial pressure of sulfur dioxide has a peak value at each temperature which increases from 101 atm at about 800°C (1472°F) to 1 atm at about 1200°C (2192°F). With water vapor present, hydrogen sulfide may predominate among gaseous sulfur compounds, particularly at low temperatures and oxygen activities; under all other circumstances considered, sulfur dioxide is the dominant gaseous sulfur-bearing species.
Citation

APA: H. A. Wriedt L. S. Darken  (1974)  Equilibrium of Sulfur-Bearing Gases and Solids Relevant to the Burning of Limestone

MLA: H. A. Wriedt L. S. Darken Equilibrium of Sulfur-Bearing Gases and Solids Relevant to the Burning of Limestone. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1974.

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