Texture and surface energetic heterogeneity of solids from modeling of low pressure gas adsorption isotherms

Langmuir ◽  
1992 ◽  
Vol 8 (7) ◽  
pp. 1789-1795 ◽  
Author(s):  
F. Villieras ◽  
J. M. Cases ◽  
M. Francois ◽  
L. J. Michot ◽  
F. Thomas
2018 ◽  
Vol 36 (9-10) ◽  
pp. 1629-1647
Author(s):  
A von Wedelstedt ◽  
S Arnrich ◽  
T Haehnel ◽  
G Kalies

Adsorption energy distributions from experimental gas adsorption isotherms are capable to characterize the energetic heterogeneity of a solid surface. Unfortunately, they can only be computed by the adsorption integral equation, which represents an ill-posed problem, i.e., the solution is highly sensitive to errors in the input data. Ill-posed problems are usually solved by means of regularization, but general regularization schemata do not provide useful criteria to estimate the approximation quality. In this paper, a former presented solution strategy tailor-made for the Langmuir kernel of the adsorption integral equation is extended to Fourier transform. This yields a simple and effective cut-off criterion for the Fourier cosine transform of the adsorption energy distribution. The cut-off criterion is applied to calculate adsorption energy distributions from synthetic and experimental adsorption isotherms.


Clay Minerals ◽  
2002 ◽  
Vol 37 (1) ◽  
pp. 39-57 ◽  
Author(s):  
L. J. Michot ◽  
F. Villiéras

AbstractHigh-resolution gas adsorption techniques were used to analyse the evolution of the aspect ratio and adsorption energy distribution on synthetic saponite samples with increasing layer charge. Using Ar as a gaseous probe, the aspect ratio of the saponite particles can be determined easily by decomposing the derivative adsorption isotherms and taking into account high-energy sites which can be assigned to talc-like ditrigonal cavities. Changes in the shape of the elementary particles are observed for layer charges above 1.30, i.e. when all the ditrigonal cavities contain at least one Al atom substituting for Si. When N2 is used as a probe, high-energy sites that could be wrongly interpreted as micropores on the basis of classical t-plot treatments are observed whatever the layer charge. Using the information obtained from both Ar and N2, schemes for describing adsorption can be proposed for all layer charges and suggest complex adsorption mechanisms for charged clay minerals.


2019 ◽  
Vol 251 ◽  
pp. 113368 ◽  
Author(s):  
Jing Li ◽  
Keliu Wu ◽  
Zhangxin Chen ◽  
Wenyang Wang ◽  
Bin Yang ◽  
...  

Langmuir ◽  
2020 ◽  
Vol 36 (29) ◽  
pp. 8444-8450
Author(s):  
Elvia P. Valadez Sánchez ◽  
Alexander Knebel ◽  
Luis Izquierdo Sánchez ◽  
Michael Klumpp ◽  
Christof Wöll ◽  
...  

2019 ◽  
Vol 33 (6) ◽  
pp. 4835-4848 ◽  
Author(s):  
Vikram Vishal ◽  
Debanjan Chandra ◽  
Jitendra Bahadur ◽  
Debasis Sen ◽  
Bodhisatwa Hazra ◽  
...  

Langmuir ◽  
1987 ◽  
Vol 3 (2) ◽  
pp. 300-302 ◽  
Author(s):  
P. S. Northrop ◽  
R. C. Flagan ◽  
G. R. Gavalas

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