Abstract

The thermal expansion coefficient of polycrystalline graphite was formulated in terms of the single crystal values and the preferred orientation of individual crystallites on the assumption that a part of lattice expansion can be accommodated by the micro-cracks in sample. This model was checked for 10 brands of nuclear graphites, and an improved formula was proposed for the thermal expansion coefficient of bulk graphite.The previous formula included a temperature indenpendent factor named “accommodation coefficient” which is defined as amount of contribution of lattice expansion coefficient to bulk sample. But a temperature dependency was observed for this factor measured between 20°C and 900°C. Instead of the relief rate, we have assumed a temperature independency on the relief quantity of littice expansion coefficient.This new formula was found to be in better agreement with the experimental results obtained over a range of temperature up to 900°C

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