Abstract
Phase change materials (PCMs) which melt in the
temperature range of 100-230 °C, are a promising alternative for the storage of
thermal energy. In this range, large amounts of energy available from
solar-thermal, or other forms of renewable heat, can be stored and applied to domestic
or industrial processes, or to an Organic Rankine Cycle (ORC) engine to
generate electricity. The amount of energy absorbed is related to the latent heat
of fusion (ΔHf) and is often connected to the extent of hydrogen
bonding in the PCM. Herein, we report fundamental studies, including crystal
structure and Hirshfeld surface analysis, of a family of guanidinium organic
salts that exhibit high values of ΔHf, demonstrating that the
presence and strength of H-bonds between ions plays a key role in this property.
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MX42 18 3
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