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shrinkage ratio

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shrinkage ratio [′shriŋ·kij ‚rā·shō]
(geology)
The ratio of a volume change to the moisture-content change above the shrinkage limit.


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Heat-induced shrinkage was determined by heating a free standing sample (nonisometric) at 270[degrees]C for 5 min and calculating the shrinkage ratio (i.
Equation 1 reveals that the self-crimp is caused by the difference in shrinkage ratios between the two sides of the fiber.
 
 
 
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