Pore-Size Distribution of Porous Iron

Physics

Scientific paper

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Scientific paper

Ritter and Drake1 have proved the usefulness of measuring the penetration of mercury under pressure, in order to elucidate the pore-size distribution of various substances. From elementary theory, it follows that for the radius rp of pores filled at a pressure p: where σ is surface tension and θ is contact angle. Substitution of σ = 480 dyne/cm. and θ = 140° gives: .

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