<p>Hydrogen bonds’ flexible distances and moderate strength entitle compounds to dynamic properties under external stimuli. Here we report multiple phase transitions and counter-intuitive CO<sub>2</sub> adsorption behavior of dynamic guanidinium sulfate (GS) salt assembled via hydrogen-bonds. Exploration based on the energy landscape generated by crystal structure prediction (CSP) reveals three porous GS phases with stability of α &gt; β &gt; γ and the inverse order of porosity, agreeing with experimental results. Transformations among polymorphs via heating or compressing involve ion rearrangement. Adsorption isotherms of β-GS indicate that CO<sub>2</sub> firstly enters the isolated cavities at a low gating pressure, and further increasing CO<sub>2</sub> pressure leads to the continuous gas uptake but reduced pressure at a critical point and thus an unexpected negative pressure inflexion (NPI), followed by the final adsorption saturation. Theoretical calculations demonstrate that the NPI behavior stemmed from the GS structural transition from β to more porous γ-phase, with the γ-GS phase becoming more energy-favorable as CO<sub>2</sub> uptake increases. Specific supramolecular interactions ensure CO<sub>2</sub> selectivity and easy regeneration. With a CO<sub>2</sub> uptake of 4.2 mmol g<sup>-1</sup> (273 K, 100 kPa), GS salt exhibits great promise for CO<sub>2</sub> capture and transport, demonstrating the potential of simple hydrogen-bonded salts as adaptive materials.</p>

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Dynamic guanidinium sulfate salt for selective carbon dioxide adsorption with negative pressure inflexion

  • Li Zhao,
  • Chengxi Zhao,
  • Congyan Liu,
  • Zhilin Xiang,
  • Chiran Wang,
  • Songlin Cui,
  • Linjiang Chen,
  • Bo Liu

摘要

Hydrogen bonds’ flexible distances and moderate strength entitle compounds to dynamic properties under external stimuli. Here we report multiple phase transitions and counter-intuitive CO2 adsorption behavior of dynamic guanidinium sulfate (GS) salt assembled via hydrogen-bonds. Exploration based on the energy landscape generated by crystal structure prediction (CSP) reveals three porous GS phases with stability of α > β > γ and the inverse order of porosity, agreeing with experimental results. Transformations among polymorphs via heating or compressing involve ion rearrangement. Adsorption isotherms of β-GS indicate that CO2 firstly enters the isolated cavities at a low gating pressure, and further increasing CO2 pressure leads to the continuous gas uptake but reduced pressure at a critical point and thus an unexpected negative pressure inflexion (NPI), followed by the final adsorption saturation. Theoretical calculations demonstrate that the NPI behavior stemmed from the GS structural transition from β to more porous γ-phase, with the γ-GS phase becoming more energy-favorable as CO2 uptake increases. Specific supramolecular interactions ensure CO2 selectivity and easy regeneration. With a CO2 uptake of 4.2 mmol g-1 (273 K, 100 kPa), GS salt exhibits great promise for CO2 capture and transport, demonstrating the potential of simple hydrogen-bonded salts as adaptive materials.