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. 2013 Jan 8;104(1):85–95. doi: 10.1016/j.bpj.2012.11.3818

Figure 3.

Figure 3

Relationship between simulated fluxes and osmotic gradients. Water fluxes (JW) were obtained at 10 s (solid dots) and at the beginning of the osmotic challenge (open dots) from simulations shown in Fig. 4. At 10 s, the relationship between JW and Δosm is nonlinear, just as experimentally observed (8). However, through simulation it is also possible to analyze initial JW values (open dots), where this relationship is linear, just as predicted by Eq. 1 (R2 > 0.96).