. Transactions. Fig. 2.—The Course of the Molten during Solidification,approximately after kuff. To A To .4. Fig. 3.—The Course of the Molten and of the Solid duringSolidification, approximately after Ruff. dissolved carbon content of the molten from which that austen-ite is depositing should be represented by the point horizontallyopposite on BB^ or B. (The conception that in undercool-ing the course of the depositing layers is along EE neednot here disturb us. For instance if, in undercooling, the ruffs carbox-irox equilibrium diagram. 435 course of the molten down to the trough of the recal
. Transactions. Fig. 2.—The Course of the Molten during Solidification,approximately after kuff. To A To .4. Fig. 3.—The Course of the Molten and of the Solid duringSolidification, approximately after Ruff. dissolved carbon content of the molten from which that austen-ite is depositing should be represented by the point horizontallyopposite on BB^ or B. (The conception that in undercool-ing the course of the depositing layers is along EE neednot here disturb us. For instance if, in undercooling, the ruffs carbox-irox equilibrium diagram. 435 course of the molten down to the trough of the recaleseeuceis PQ Q (Fig. 3), and if the course of the solidifying layers iscorrespondingly EEE^^ then for instance at E^, when themolten reaches SK (see (5)) at Q, the dissolved carbon contentof the austenite is E^^ the point horizontally opposite on SE^and the difference, E^E^, is represented by free cementite, whichgraphitizes rapidly at this temperature. And in general whilethe molten is crossing from Q on GK to Q on SK, the aus-tenite of the depositing layers is crossing from E.^ to E^ on SE.) (5) GK
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Keywords: ., bo, bookcentury1800, bookdecade1870, booksubjectmineralindustries
