Abstract
The magnetic anisotropy of natural rubber was measured by Krishnan's oscillation method. In the first place, the anisotropy was measured by varying the time of vulcanization and was found to decrease with the time of vulcanization. In the second place, the anisotropy was measured as a function of temperature. Similar to the breadth of nuclear magnetic resonance line, an abrupt change in the slope of the anisotropy versus temperature curve was observed at the second-order transition temperature. Above and below this transition temperature, its change with temperature was not so strong.
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