The Nature of the Low-Temperature Crossover of Water in Hard Confinement.

The dynamics of water confined in mesoporous MIP (2-3 nm pores in size) with silica gel (secondary silica; further, the abbreviation SG will be used) and MAP (10-35 nm pores in size) without SG borosilicate glasses have been studied by broadband dielectric spectroscopy (BDS), nuclear magnetic resonance (NMR), and differential scanning calorimetry (DSC). MIP samples contain secondary silica inside the pores and provide a confinement size of about 2-3 nm, whereas MAP samples are free of secondary silica and provide a confinement size of about 10-35 nm. It is shown by BDS and NMR techniques that water exhibits a dynamic crossover of around 180 K when it is confined in MIP samples. By contrast, water confined in larger pores (MAP) does not exhibit any changes in its relaxation behavior. It is also shown that the crossover temperature depends on the hydration level (the higher the hydration level, the lower the crossover temperature). Below the crossover temperature, we find that water reorientation is isotropic (NMR) and that the temperature-dependent dielectric relaxation strength (BDS) follows the tendency expected for a solid-like material. In contrast, water reorientation is related to long-range diffusion above the crossover temperature, and the dielectric relaxation strength follows the tendency expected for a liquid-like material. Furthermore, the calorimetric results are compatible with crossing a glass transition near 180 K. Finally, the results are discussed within the Gibbs-Thomson model. In this framework, the crossover could be related to ice crystals melting.

The dielectric response of hydrated water as a structural signature of nanoconfined lichen melanins.

Lichens are unique symbiotic organisms from a mutually beneficial alliance of fungi and algae/cyanobacteria that successfully survive extreme temperatures and drought conditions. Most probably such extraordinary vitality of lichens is underlain by melanins, one of the main structural and chemical lichen components, and their mutual relationship with residual water. In this paper, we propose mechanisms, which allow lichens to store up the extra water in their structure. Melanins that are constituents of the cortical lichen layer and presumably contribute to unique water-lichen interactions are chosen for physical experiments in a wide temperature domain. Two melanin pigments extracted from different lichens are studied here - eumelanin from Lobaria pulmonaria and allomelanin from Cetraria islandica. To investigate the inner melanin structure and water-melanin interactions, FTIR and BDS techniques are applied. The BDS technique was used in a wide temperature region of 123-293 K for melanins with various hydration levels. The relaxation processes related to the confinement of supercooled water - in melanins are observed and discussed in details. At medium and high hydration levels, the relaxation process in two melanins of different chemical compositions and supramolecular structures exhibits a well-known crossover that was already observed in many types of confinements. The analysis of FTIR and BDS results helps to clarify the lichen-water interaction processes.