Abstract
Chemical analysis shows the partition of the magnesium addition between the metal and the graphite is independent of whether the graphite is in the form of nodules or flakes. The bright central spot observed in nodular graphite polished sections is shown to be due to the structure of the nodules.
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Discussion on this paper, TP 3271E, may be sent, 2 copies, to AIME by Dec. 1, 1952. Manuscript, Oct. 2, 1951. Philadelphia Meeting, October 1952.
Published by permission of the Director-General of Scientific Services, Department of Mines and Technical Surveys, Ottawa.
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Weld, H.M., Cunningham, R.L. & Boswell, F.W.C. Observations on Nodular Graphite. JOM 4, 738–742 (1952). https://doi.org/10.1007/BF03398134
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DOI: https://doi.org/10.1007/BF03398134