“…An extended version of LTM (ELTM) allows the same sample to be reused for later observation or analysis by EDS in a different SEM or ESEM (Tihlaříková et al, 2019). Furthermore, several subzero temperature ESEM studies were performed including mainly dynamic observations such as nucleation processes (Zimmermann et al, 2007(Zimmermann et al, , 2008Varanasi et al, 2010;Wang et al, 2016Wang et al, , 2019, observation of liquid water droplets under triple-point pressure (Chen et al, 2017), observation of uranyl salt brine on the ice surface (Krausko et al, 2014), sublimation of frozen aqueous systems (Yang et al, 2017;Vetráková et al, 2020), ice crystal growth (Pedersen et al, 2011), morphology of ice and liquid brine at various freezing conditions (Vetráková et al, 2019), morphology of nitric acid and water ice films (Keyser & Leu, 1993), control of ice formation (Lo et al, 2017), and sublimation-induced morphology of ice (Nair et al, 2018). Although dynamic experiments of ice-containing samples in ESEM are very appealing, even more challenging is static observation at thermodynamic equilibrium, which would enable the observation of the constant intact morphology of a frozen aqueous sample, and considerably broaden the ESEM observation possibilities.…”