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Zhang et al. Chem Synth 2023;3:10  https://dx.doi.org/10.20517/cs.2022.40        Page 5 of 35



































                Figure 3. Development history of psaAWH. Silica  gel [31] . Porous  carbon [32] . Zeolite [33] . Metal-organic frameworks. Reproduced with
                permission [34] . Copyright The American Association for the Advancement of Science. Composite bead. Reproduced with permission [35] .
                Copyright Springer Nature. PAM-CNT-CaCl . Reproduced with  permission [36] . Copyright American Chemical Society. PNIPAAm/Alg
                                              2
                IPN gel. Reproduced with  permission [37] . Copyright Springer Nature. Covalent organic frameworks. Reproduced with  permission [27] .
                Copyright American Chemical Society. Crystalline organic porous salts. Reproduced with permission [29] . Copyright John Wiley and Sons.












                                        Figure 4. Water adsorption process of mainly classic materials.

               on the surface of the silica gel channel by forming hydrogen bonds with the hydroxyl groups. However, the
               water uptake of silica gel is generally low, particularly at low RH, which limits its application in
               psaAWH  [39,40] .


               Zeolites are crystalline porous materials that are typically composed of aluminum oxide, silicon dioxide, and
               counterions. They feature crystal channels with high polarity and electrostatic charge that facilitate good
               water adsorption [41-44] . Because of the existence of framework anions and counterions in molecular sieves,
               they usually possess multiple water adsorption sites, including Lewis acid sites (framework anions),
               Brønsted acid sites (bridging hydroxyls), counterions, and defect sites . Although these sites endow
                                                                              [41]
               molecular sieves with good hydrophilicity, their attraction to water molecules is too strong, leading to
               zeolites usually displaying type I water vapor adsorption isotherms, which are unfavorable for psaAWH
               because they represent energy-intensive regeneration processes [23,45,46] . For example, Wynnyk et al. measured
               the water adsorption isotherms of zeolite 13X at temperatures ranging from 25 °C to 150 °C  and found
                                                                                              [45]
               them to be type I. This implies that even if the regeneration temperature is as high as 150 °C, several water
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