1957Journal of the Japan Institute of Metals and MaterialsOpen access

Study on Carbides in Iron and Steel by Electrolytic Isolation (6th Report). On the Heterogeneities of Cementite in Low Alloy Steels

Tomoo Sato, Taiji Nishizawa

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Abstract

Thermo-magnetic studies on cementite isolated from low alloy steels confirmed that the compositions of cementite are frequently heterogeneous. (1) In 0.61%, 1.08%Mn steel, tempered between 500 to 650°, the cementite particles randomly contained various amounts of Mn; 1∼3%Mn at 500°,1∼5.5%Mn at 550°,1.5∼6.2%Mn at 600°,and 4∼6.3%Mn at 650°, by 1 hr tempering. It is conceivable that the heterogeneous enrichment of Mn in cementite particles intemp tempering was caused by ununiform or structure-sensitive movement of Mn atoms in ferrite matrix. Similar appearance was recognized in cementite in tempered 1.13%C, 1.42%Cr steel. (2) Cr concentration in pro-eutectoid cementite was higher than in the pearlitic cementite. But, Mn concentration in pro-eutectoid cementite was lower than in pearlitic cementite. Generalizing these results, it is deduced that A1pt-raising elements (Cr,Mo,W,V,Ti etc) dissolve in pro-eutectoid cementite more than in pearlitic cementite. On the contrary, A1pt-lowering elements (Mn,Ni etc) dissolve in pearlitic cementite more than in pro-eutectoid cementite.

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Thermo-magnetic studies on cementite isolated from low alloy steels confirmed that the compositions of cementite are frequently heterogeneous. (1) In 0.61%, 1.08%Mn steel, tempered between 500 to 650°, the cementite particles randomly contained various amounts of Mn; 1∼3%Mn at 500°,1∼5.5%Mn at 550°,1.5∼6.2%Mn at 600°,and 4∼6.3%Mn at 650°, by 1 hr tempering. It is conceivable that the heterogeneous enrichment of Mn in cementite particles intemp tempering was caused by ununiform or structure-sensitive movement of Mn atoms in ferrite matrix. Similar appearance was recognized in cementite in tempered 1.13%C, 1.42%Cr steel. (2) Cr concentration in pro-eutectoid cementite was higher than in the pearlitic cementite. But, Mn concentration in pro-eutectoid cementite was lower than in pearlitic cementite. Generalizing these results, it is deduced that A1pt-raising elements (Cr,Mo,W,V,Ti etc) dissolve in pro-eutectoid cementite more than in pearlitic cementite. On the contrary, A1pt-lowering elements (Mn,Ni etc) dissolve in pearlitic cementite more than in pro-eutectoid cementite.

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Thermo-magnetic studies on cementite isolated from low alloy steels confirmed that the compositions of cementite are frequently heterogeneous. (1) In 0.61%, 1.08%Mn steel, tempered between 500 to 650°, the cementite particles randomly contained various amounts of Mn; 1∼3%Mn at 500°,1∼5.5%Mn at 550°,1.5∼6.2%Mn at 600°,and 4∼6.3%Mn at 650°, by 1 hr tempering. It is conceivable that the heterogeneous enrichment of Mn in cementite particles intemp tempering was caused by ununiform or structure-sensitive movement of Mn atoms in ferrite matrix. Similar appearance was recognized in cementite in tempered 1.13%C, 1.42%Cr steel. (2) Cr concentration in pro-eutectoid cementite was higher than in the pearlitic cementite. But, Mn concentration in pro-eutectoid cementite was lower than in pearlitic cementite. Generalizing these results, it is deduced that A1pt-raising elements (Cr,Mo,W,V,Ti etc) dissolve in pro-eutectoid cementite more than in pearlitic cementite. On the contrary, A1pt-lowering elements (Mn,Ni etc) dissolve in pearlitic cementite more than in pro-eutectoid cementite.

Key concepts: Cementite, Ledeburite, Eutectic system, Metallurgy, Materials science, Tempering, Carbide, Alloy

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