Authors:G. W. Chądzyński, P. Staszczuk, D. Sternik, and M. Błachnio
surface area S BET was calculated using BET method and was found equal to 6.6 m 2 g −1 with the corresponding total porosity varying from 0.0203 to 0.0228 cm 3 g −1 ( Table 1 ). The total pore volume and the pore-sizedistribution as presented in Fig
Authors:Faezeh Farzaneh, Zeinab Sharif, Zahra Mehraban, and Mehdi Ghandi
common average pore size of ≈2.71 nm as calculated by the BJH method. BET surface area, pore volume and poresizedistribution (BJH method) data for MASM are reported in Table 1 . The BET surface area, BJH pore volumes and pore diameter are 1212.37 m 2
Authors:C. Amairia, S. Fessi, A. Ghorbel, and A. Rîves
sizedistributions were determined by the BJH method, using the desorption branches of isotherms. The total pore volume was estimated by means of the total amount of adsorbed gas at relative pressure p/p 0 = 0.98.
The crystal phases of the
Brutsaert, W., 1966. Probability laws for poresizedistributions. Soil Sci. 117. 311–314.
Comegna, V., Damiani, P. & Somella, A., 1998. Use of a fractal model for determining soil water retention curves. Geoderma
Authors:C. Munteanu, M. Caldararu, V. Bratan, P. Yetisemiyen, G. Karakas, and N. I. Ionescu
The samples were analyzed for surface area and poresizedistribution by a Micromeritics ASAP 2020 physisorption analyzer using N 2 -BET adsorption technique. The XRD analysis were carried out by a Philips PW 1840 instrument with Cu target and Ni
Authors:Denis A. Brosnan, John P. Sanders, and Stephanie A. Hart
water and the soluble salt content in the leachate was measured using ion chromatography (Dionex IC-2000). The poresizedistribution was measured by mercury intrusion porosimetry using a Quantachrome Pore Master 33.
Authors:Susana Pinto-Castilla, Santiago Marrero, Yraida Díaz, Joaquín L. Brito, Pedro Silva, and Paulino Betancourt
volume and poresizedistribution were obtained from N 2 adsorption–desorption isotherms which were collected with a Micromeritics ASAP 2010C system at −196 °C using the conventional BET and BJH methods. The samples were degassed at 250 °C for 2 h before
Authors:Hou-Yin Zhao, Yan Cao, Quentin Lineberry, and Wei-Ping Pan
min. The apparent surface area of the samples was evaluated from the N 2 adsorption isotherms by applying the BET equation in the relative pressure range of 0.05–0.35. The poresizedistribution and the micropore volume were determined by t -plot