Answers are grounded in this paper and cite their sources.
Intercalated water in graphite oxide (GO) was investigated by using different techniques: broadband dielectric spectroscopy (BDS) (10 −2 −10 9 Hz; 140−300 K), differential scanning calorimetry, X-ray diffraction, and attenuated total reflection geometry in Fourier transform infrared spectroscopy (ATR-FTIR). We have studied the water concentration ( c w ) region from 0 wt % (anhydrous GO) up to 25 wt % since in this range the water crystallization is avoidable. The interlayer distance during hydration increases from 5.67 to 8 Å which corresponds to the uptake of a water monolayer in the interlayer space of GO. A clear relaxation due to water molecule reorientation is seen by BDS. The rotational water dynamics is dependent on the hydration level. At high water concentration ( c w > 15 wt %), water−water interactions seem to dominate the dielectric response. This result is also compatible with those from FTIR and X-ray measurements. In this water concentration region, a slight dynamical crossover in the temperature dependence of the relaxation times is observed. We show that the crossover temperature on this system ( T cross ) depends on the confinement size.
No takes yet. Share an insight, caveat, or question.
Cerveny et al. (2010) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: