Capillary-Orifice Model for High-Speed Flow through Porous Media

Tex., Feb. 11, 1965. (2) Ahner, W. D., Feinman, J., A.I.Ch.E. J. 10, 652 (1964). (3) Ezz, S. Y., Trans. A.I.M.E. 218, 709 (1960). (4) Feinman, J., Ind...
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G K Q

= gas flow rate: lb. mole/hr. sq. ft. = equilibrium constant, Hz-FeO-HgO system

R V y

= = = =

R

= =

as defined by Feinman (4) radius of oxide particle, ft. fraction of oxygen removed mass of Fe per unit hearth area, lb. mole Fe/sq. ft. mole fraction of water in exit gas total pressure of hydrogen, atm.

literature Cited

(1) Agarwal, J . C., Davis, W. L., A.1.Ch.E. Meeting, Houston, Tex., Feb. 11, 1965. (2) Ahner, W. D., Feinman, J., A.Z.Ch.E. J . 10, 652 (1964). (3) Ezz, S. Y . , Trans. A . I . M . E . 218, 709 (1960). (4) Feinman, J., IND. ENG. CHEM.PROCESS DESIGNDEVELOP. 3, 241 (1964). (5) Feinman, J., Drexler, I. D., A.Z.Ch.E. J . 7, 584 (1961).

(6) Ishii, Tadao, Osberg, G. L.: Ibid., 11, 279 (1965). (7) Langston, B. C.. Stephens, F. M., J . ;Metals 12, No. 4. 312 (1960); “Iron Ore Reduction.” p. 120. Pergarnon Press, New York, 1962. (8) Lubker, R. A,: Bruland. K. LV., Chem. En