Dh

-ft = kinpwpc - kout(1 + h)pc h = hRa + (kf-t pahsrh - 1^(1 - e-k°wpc (V+m-W^ (1-5)

This equation was used to calculate the nonlinear best-fit line shown in Fig. 1.6 and shows that water binding to collagen during atmospheric rehydration can be simply described by the dynamic mass action relationship. The value of hRa is accurately extracted («2%) from these measurements as the hydration level where the zone 0 and zone I relationships intersect, as shown in Fig. 1.6 by the large X.

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