4.6 Article

Experimental and Theoretical Assessment of Water Sorbent Kinetics

期刊

LANGMUIR
卷 38, 期 8, 页码 2651-2659

出版社

AMER CHEMICAL SOC
DOI: 10.1021/acs.langmuir.1c03364

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资金

  1. Natural Sciences and Engineering Research Council of Canada (NSERC) [CRD-522391]
  2. Prima [R16-46-003]
  3. Mitacs [IT16469]
  4. Awn Nanotech Inc.

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Study finds that open porosity has the greatest influence on improving sorbent kinetics. Converting sorbent kinetics data into daily water capture yields shows that there is an optimal open porosity for each sorbent, and thinner layers with moderate open porosity outperform thicker layers with high open porosity, indicating that high maximum water uptake and fast single-particle kinetics are not necessarily predictive of high daily water yield.
The kinetics of water adsorption in powder sorbent layers are important to design a scaled-up atmospheric water capture device. Herein, the adsorption kinetics of three sorbents, a chromium (Cr)-based metal-organic framework (Cr-MIL-101), a carbon-based material (nanoporous sponges/NPS), and silica gel, have been tested experimentally, using powder layers ranging from similar to 0 to 7.5 mm in thickness, in a custom-made calibrated environmental chamber cycling from 5 to 95% RH at 30 degrees C. A mass and energy transfer model was applied onto the experimental curves to better understand the contribution of key parameters (maximum water uptake, kinetics of single particles, layer open porosity, and particle size distribution). Open porosity (i.e., the void-to-particle ratio in the sorbent layer) shows the highest influence to improve the kinetics. Converting the sorbent kinetics data into a daily yield of captured water demonstrated (i) the existence of an optimal open porosity for each sorbent, (ii) that thinner layers with moderate open porosity performed respectively better than thicker layers with high open porosity, and (iii) that high maximum water uptake and fast single-particle kinetics are not necessarily predictive of high daily water yield.

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