Figure 4.
Strain isotherm from in situ GISAXS derived from the shift of the out-of-plane 02 reflection in Figure 3a. Only the adsorption branch could be measured reliably with the humidity setup used.
Strain isotherm from in situ GISAXS derived from the shift of the out-of-plane 02 reflection in Figure 3a. Only the adsorption branch could be measured reliably with the humidity setup used.