Neutron scattering quantification of unfrozen pore water in frozen mud.

The Earth's polar regions are experiencing a greater frequency of freeze-thaw events throughout the polar summer, contributing to atmospheric methane and destabilising clay-rich sediments. Clays in soils tightly bind pore water and thus substantially modify freeze-thaw events. While temperatures of phase transitions for confined pore water may be precisely assessed using calorimetric or thermal analyses to −30 or −40 °C, neutron scattering directly probes how pores in clay minerals control ice formation and melting to lower temperatures. We apply elastic neutron scattering to accurately quantify the unfrozen water content of clay gels and unambiguously identify different pore-water environments by their freezing temperatures. Using this approach, we conclude that cryosuction controls water mobility in frozen soils in the absence of soluble salts to much lower temperatures than observed by other techniques. Dyanmics determined from neutron scattering indicates that water in clay gel pores thaws at much lower temperatures than currently considered, and thus pose potential risks for contaminant migration at sub freezing temperatures. The general poor strength of wet clays can significantly impact infrastructure in cold regions undergoing an increased frequency of freeze-thaw events. Different pore water environments in clay gels can be identified and quantified by inelastic neutron scattering. [Display omitted] • Cryosuction removes interlayer water from clay gels hydrated to near saturation. • Cryosuction requires capillary connectivity to operate in clay gels. • Considerable interlayer water remains unfrozen in clay gels to below −80C. • Freezing characteristic curves can be used to identify pore environments. [ABSTRACT FROM AUTHOR]