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

               Table 1. Summary of characteristics of several freshwater production technologies
                Technology name  Geographic dependencies  Weather dependencies  Implementation premise
                Seawater desalination  Yes               No                    Coastal
                Rainwater collection  No                 Yes                   Rainfall
                Fog collection   No                      Yes                   Foggy
                Condensation     No                      Yes                   Difficult to implement at low RH
                psaAWH           No                      No                    Presence of atmospheric humidity

























                      Figure 1. (A) Water production process of psaAWH; (B) water release mechanism of porous materials in psaAWH.

               external atmosphere, which significantly reduces the sensible heat required for the condensation process.
               Finally, the moist air can be easily cooled and condensed into liquid water. Therefore, if psaAWH is to be
               implemented in a certain climate, the porous adsorbent must possess the ability to adsorb atmospheric
               water at the relative humidity (RH) of the climate, which can be verified using the water vapor adsorption
               isotherm. As shown in Figure 1B, the abscissa is the relative partial pressure of water vapor (RH), and the
               ordinate is the water vapor adsorption capacity of the porous materials. Under ambient RH (P ), the porous
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               material exhibited higher water uptake (W ). With external stimulation (such as increasing temperature),
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               the RH around the porous material decreased to P . At this time, the water uptake decreased to W , and
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               excess water molecules were released into a closed space to obtain liquid water through condensation.
               Therefore, the difference between W  and W  determines the working ability of a material. P  is the applied
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               RH of the adsorbent; that is, the RH of the atmosphere must be greater than P . Owing to the steep water
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               uptake of the S-type (type-IV, V) vapor adsorption isotherm, it can have a high working capacity under
               small external RH changes [Figure 2]. In contrast, other types of water vapor adsorption isotherms often
               require greater RH changes to produce a better working capacity because of the lack of steep water uptake at
               an appropriate RH, which often implies that higher energy must be provided to heat the adsorbent .
                                                                                                  [15]
               Hence, an ideal porous sorbent for psaAWH should feature: (1) an S-type water vapor adsorption isotherm
               at  the  required  RH;  (2)  high  water  uptake  to  maximize  water  production  per  cycle;  (3)  rapid
               adsorption/desorption kinetics under lower energy consumption to maximize the circulation rate; and (4)
               structural resilience to multiple water adsorption/desorption cycles. To date, much effort has been devoted
               to the development of porous adsorbents with high psaAWH performances. However, the diversity of
               adsorbent types and modification strategies makes it difficult for us to intuitively understand their
               structure-activity relationships. The summary of the structure-activity relationship of adsorbents has
               considerable guiding significance for future research. At present, some reviews have summarized this and
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