Ruth Dary Mojica-Sepulveda, Luís Joaquín Mendoza-Herrera, Eduardo Grumel, Delia Beatriz Soria, Carmen Inés Cabello, Marcelo Trivi.Synthesis and characterization of Sr1-xLaxMnO3/SiOC nanocomposites decorated with 1D nanostructures for high temperature CO2 splitting. Eva Casado, Beatriz García, Aitana Tamayo.Modification of poly (styrene-co-divinyl benzene) porous materials for peptides enrichment and separation. Yi Liu, Hao Wang, Yongfeng Liu, Meng Shi, Duolong Di.Microporous and Mesoporous Materials 2020, 292, 109735. Benford's law, Zipf's law and the pore properties in solids. Synthesis and characterization of Ce/SiOC nanocomposites through the polymer derived ceramic method and evaluation of their catalytic activity. Beatriz García, Eva Casado, Aitana Tamayo.Highly modulated supported triazolium-based ionic liquids: direct control of the electronic environment on Cu nanoparticles. Cristián Valdebenito, Jose Pinto, Michael Nazarkovsky, Gustavo Chacón, Oriol Martínez-Ferraté, Kerry Wrighton-Araneda, Diego Cortés-Arriagada, María Belén Camarada, Jesum Alves Fernandes, Gabriel Abarca.International Journal of Molecular Sciences 2020, 21 Hybrid Materials Based on Silica Matrices Impregnated with Pt-Porphyrin or PtNPs Destined for CO2 Gas Detection or for Wastewaters Color Removal. Diana Anghel, Anca Lascu, Camelia Epuran, Ion Fratilescu, Catalin Ianasi, Mihaela Birdeanu, Eugenia Fagadar-Cosma.
Synthesis, structure and thermal properties of montmorillonite/ionic liquid ionogels. Construction and Building Materials 2020, 262, 120863. Quantitative characterization and comparsion of bentonite microstructure by small angle X-ray scattering and nitrogen adsorption.
Journal of Nanoscience and Nanotechnology 2021, 21 Pore Size Distribution and Fractal Characteristics of the Nanopore Structure in Organic-Rich Shales Using the Neimark-Kiselev Fractal Approach. Mingming Wei, Li Zhang, Yongqiang Xiong, Ping’an Peng, Yiwen Ju.Microporous and Mesoporous Materials 2021, 310, 110675. Insights into the structural and surface characteristics of microporous carbide derived carbons obtained through single and double halogen etching. Berta Perez-Roman, Rama Layek, MaAngeles Rodriguez, Fausto Rubio, Juan Rubio, Aitana Tamayo.Construction and Building Materials 2021, 269, 121331. Evaluation and comparison of bentonite surface fractal dimension and prediction of swelling deformation: Synchrotron radiation SAXS and N2-adsorption isotherms method. Russian Journal of Inorganic Chemistry 2021, 66 Synthesis of CaCu3Ti4O12: How Heat Treatment Influences Morphology and Dielectric Properties. The influences of composition and pore structure on the adsorption behavior of CH4 and CO2 on shale. Xiangzeng Wang, Junping Zhou, Xiao Sun, Shifeng Tian, Jiren Tang, Feng Shen, Jinqiao Wu.Characteristics of Pore Structure and Gas Content of the Lower Paleozoic Shale from the Upper Yangtze Plate, South China.
Xiaoyan Zou, Xianqing Li, Jizhen Zhang, Huantong Li, Man Guo, Pei Zhao.Adsorption Species Distribution and Multicomponent Adsorption Mechanism of SO2, NO, and CO2 on Commercial Adsorbents. Lei Luo, Yangyang Guo, Tingyu Zhu, and Yang Zheng.This article is cited by 24 publications. These observations lead to the physicogeometrical conjunction that, during capillary condensation in cylindrical pores, usually assumed in nitrogen porosimetry, the scaling dimension of pore anisotropy b, scaled in units of radius r, is related to the dimensionality D of the process. In the present study it is shown that, for pores of cylindrical geometry and at a specific range of pressure where those pores are filled-up during the process of capillary condensation, the local slopes d log V/dloglog or dlog S/d log r, of plots similar to the above, may be used to estimate the pore anisotropy b of the adsorbing space from the relationships log b = − 3] log(0.5 r) or log b = − 2] log(0.5 r). It has been suggested in the past that plots of the form log V = constant − ( D − 3), or its equivalent log S = const − ( D − 2) log r, can be used for the estimation of the dimensionality D of the adsorbing surface from those parts of the slopes at low pressure corresponding to straight lines. The Frenkel−Halsey−Hill (FHH) equation V/ V m ≈ −1/s is revisited in relation to the meaning of its exponent in a specific intermediate range of pressure where capillary condensation occurs.