2022
DOI: 10.1002/aic.17684
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Responses to the comments on “Monte Carlo simulations for water adsorption in porous materials: Best practices and new insights”

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Cited by 3 publications
(5 citation statements)
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“…By further assuming that MOFs studied herein all feature a perfect step isotherm such that a C -ratio of >1 or <1 respectively predicts that the MOF possesses a zero uptake or saturation loading. To mimic the environment of arid climates, the adsorption condition is set to a relative humidity (RH) of 20% at 298 K, and the desorption condition is set to 15% RH at 338 K. , Following the recommendation by Datar et al., , the saturation pressure in this study has been set to be 986 Pa at 298 K, the saturation pressure computed per the adopted TIP4P-Ew model. At 338 K, a pressure of 9765 Pa is used, which is determined through the Antoine equation, with parameters provided by Vega et al The result of the equation at 298 K closely matches the value obtained by Datar et al It has been shown that it is critical to use the saturation pressure of the adopted model; with this, simulations of different water models can still yield comparable results.…”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…By further assuming that MOFs studied herein all feature a perfect step isotherm such that a C -ratio of >1 or <1 respectively predicts that the MOF possesses a zero uptake or saturation loading. To mimic the environment of arid climates, the adsorption condition is set to a relative humidity (RH) of 20% at 298 K, and the desorption condition is set to 15% RH at 338 K. , Following the recommendation by Datar et al., , the saturation pressure in this study has been set to be 986 Pa at 298 K, the saturation pressure computed per the adopted TIP4P-Ew model. At 338 K, a pressure of 9765 Pa is used, which is determined through the Antoine equation, with parameters provided by Vega et al The result of the equation at 298 K closely matches the value obtained by Datar et al It has been shown that it is critical to use the saturation pressure of the adopted model; with this, simulations of different water models can still yield comparable results.…”
Section: Methodsmentioning
confidence: 99%
“…Such methods biasedly sample all accessible loading macrostates, and their relative probability is then computed. As demonstrated by Datar et al, a particular approach of flat histogram methodsthe so-called NVT+W method developed by Witman et alcan overcome the drawback of the GCMC method to effectively compute water adsorption in MOFs. ,, This method is, however, computationally expensive to study a large number of material candidates, as it requires hundreds of canonical simulations for each structure. To this end, an approach denoted as the C-map method with a much-reduced calculation cost was further proposed by Datar et al The key idea behind this method is to sample adsorption systems only at a few selected loading macrostates to determine their range of adsorption loadings at a given condition.…”
Section: Introductionmentioning
confidence: 99%
“…Subsequently, with the C-matrix and the detailed balance between macrostates, the MPD can be calculated, followed by its reweighting to determine adsorption uptakes at desired conditions (i.e., at varying pressures and temperatures, resulting in adsorption isotherms at different temperatures). This method has been demonstrated to compute pure component adsorption for porous materials, including those structures with internal flexibility and the adsorption of molecules with bimodal MPD distributions such as water as noted above. …”
Section: Methodsmentioning
confidence: 99%
“…To obtain the MPD, the NVT+W (canonical plus Widom) method first reported by Smit and co-workers, , a special class of the flat histogram methods that resembles the transition-matrix Monte Carlo (TMMC) , simulations with a bin size of 1, can be employed. This approach has been demonstrated to compute pure component adsorption isotherms for nanoporous materials, including challenging molecules such as water in MOFs. This approach uniformly samples each macrostate; that is, it involves calculations for each possible molecular number N . During the canonical simulation for each N , ghost Widom insertion and deletion moves, which will never be accepted are carried out to sample the transition probability from one macrostate to another macrostate (i.e., N to N + 1 or N – 1, respectively).…”
Section: Introductionmentioning
confidence: 99%
“…Specifically, the so-called NVT+W approach is adopted, which has been recently applied to study water adsorption in MOFs. The readers are referred to recent studies by Datar et al ,, However, the application of NVT+W requires sampling each possible macrostate for a structure of interest to determine its adsorption properties (i.e., adsorption isotherms), leading to a huge computational demand. To this end, in this study, we attempt to classify only each studied MOF in a binary manner to be hydrophilic or hydrophobic under the adsorption condition.…”
Section: Methodsmentioning
confidence: 99%