High-pressure CH4 and CO2 sorption isotherms as a function of coal maturity and the influence of moisture

2013 ◽  
Vol 118 ◽  
pp. 45-57 ◽  
Author(s):  
Yves Gensterblum ◽  
Alexej Merkel ◽  
Andreas Busch ◽  
Bernhard M. Krooss
Carbon ◽  
2009 ◽  
Vol 47 (13) ◽  
pp. 2958-2969 ◽  
Author(s):  
Y. Gensterblum ◽  
P. van Hemert ◽  
P. Billemont ◽  
A. Busch ◽  
D. Charriére ◽  
...  

2010 ◽  
Vol 84 (2) ◽  
pp. 115-124 ◽  
Author(s):  
Y. Gensterblum ◽  
P. van Hemert ◽  
P. Billemont ◽  
E. Battistutta ◽  
A. Busch ◽  
...  

2013 ◽  
Vol 118 ◽  
pp. 89-94 ◽  
Author(s):  
Vyacheslav N. Romanov ◽  
Tae-Bong Hur ◽  
James J. Fazio ◽  
Bret H. Howard ◽  
Gino A. Irdi

2019 ◽  
Vol 62 (1) ◽  
pp. 105-114
Author(s):  
Xiuping Jiang ◽  
Xiuping Jiang ◽  
Huanhuan Li ◽  
Hosahalli S. Ramaswamy ◽  
Songming Zhu ◽  
...  

Abstract. Understanding of moisture sorption isotherms (MSI) is critical for predicting the stability of wood during handling, transport, and storage. The aim of this study was to evaluate the adsorption and desorption isotherm characteristics of high-pressure (HP) treated paulownia wood and to identify the best-fitting model to describe its sorption behavior. The equilibrium moisture contents (EMCs) of HP-treated paulownia wood were obtained using a static gravimetric method under different storage conditions: three temperatures (20°C, 30°C, and 40°C) and five water activity (aw) levels (0.32 to 0.95). Results showed that HP parameters did not significantly affect the MSI trend of treated groups. Eight modified models (modified Chung-Pfost, modified Henderson, modified Oswin, modified Halsey, Chen-Clayton, Guggenheim-Anderson-de Boer (GAB), simply modified GAB, and Peleg) were fitted to the experimental data. The Chen-Clayton model (temperature-dependent) produced randomized residuals and the best prediction performance for both adsorption and desorption among all models. Net isosteric heat of adsorption and desorption decreased from 7.55 to 4.84 kJ mol-1 and from 18.1 to 12.2 kJ mol-1, respectively, with an increase in EMC from 7.5% to 10%. The isosteric temperature (Tß) was 352 K for adsorption and 335 K for desorption, between which all the adsorption and desorption reactions proceeded at the same rate. All thermodynamic functions were adequately characterized by a power law model. Keywords: Equilibrium moisture content, High-pressure treatment, Modeling, Moisture sorption isotherm, Paulownia wood, Temperature, Thermodynamic analysis.


2014 ◽  
Vol 132 ◽  
pp. 131-146 ◽  
Author(s):  
Matus Gasparik ◽  
Thomas F.T. Rexer ◽  
Andrew C. Aplin ◽  
Pierre Billemont ◽  
Guy De Weireld ◽  
...  

2017 ◽  
Vol 43 ◽  
pp. 45-53 ◽  
Author(s):  
Viridiana Tejada-Ortigoza ◽  
Luis Eduardo Garcia-Amezquita ◽  
Vinicio Serment-Moreno ◽  
J. Antonio Torres ◽  
Jorge Welti-Chanes

Materials ◽  
2020 ◽  
Vol 13 (4) ◽  
pp. 917 ◽  
Author(s):  
Anna Pajdak ◽  
Norbert Skoczylas ◽  
Arkadiusz Szymanek ◽  
Marcin Lutyński ◽  
Piotr Sakiewicz

The article presents comparative characteristics of the pore structure and sorption properties of raw halloysite (R-HAL) and after calcination (C-HAL) at the temperature of 873 K. Structural parameters were determined by optical scanning and transmission electron microscopy methods as well as by mercury porosimetry (MIP, Hg) and low-pressure nitrogen adsorption (LPNA, N2, 77 K). The surface area parameter (LPNA) of halloysite mesopores before calcination was 54–61 m2/g. Calcining caused the pore surface to develop to 70–73 m2/g. The porosity (MIP) of halloysite after calcination increased from 29% to 46%, while the surface area within macropores increased from 43 m2/g to 54 m2/g. The total pore volume within mesopores and macropores increased almost twice after calcination. The course of CH4 and CO2 sorption on the halloysite was examined and sorption isotherms (0–1.5 MPa, 313 K) were determined by gravimetric method. The values of equilibrium sorption capacities increased at higher pressures. The sorption capacity of CH4 in R-HAL was 0.18 mmol/g, while in C-HAL 0.21 mmol/g. CO2 sorption capacities were 0.54 mmol/g and 0.63 mmol/g, respectively. Halloysite had a very high rate of sorption equilibrium. The values of the effective diffusion coefficient for methane on the tested halloysite were higher than De > 4.2 × 10−7 cm2/s while for carbon dioxide De > 3.1 × 10−7 cm2/s.


Fuel ◽  
2010 ◽  
Vol 89 (3) ◽  
pp. 569-580 ◽  
Author(s):  
Dongyong Li ◽  
Qinfu Liu ◽  
Philipp Weniger ◽  
Yves Gensterblum ◽  
Andreas Busch ◽  
...  

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