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laws for pore size distributions . Soil Science . 117 . 311 – 314 . C alzolari , C. , U ngaro , F. , F ilippi , N. , G uermandi , M. , M alucelli , F. , M archi , N

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Agrokémia és Talajtan
Authors: András Makó, Tamás Varga, Hilda Hernádi, Viktória Labancz, and Gyöngyi Barna

. Complete characterization of pore size distribution of tilled and orchard soil using water retention curve, mercury porosimetry, nitrogen adsorption, and water desorption methods . Geoderma . 135 . 307 – 314

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total pore volume; and its shape is related to the actual pore size distribution [ 2 , 9 ]. On the other side, the Rb peak proceeds always at the same temperatures as in the case of the pure cetane (also shown in Figs. 7 , 8 ), however, it is small

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Journal of Thermal Analysis and Calorimetry
Authors: Ana C. R. Melo, Edjane F. B. Silva, Larissa C. L. F. Araujo, Mirna F. Farias, and Antonio S. Araujo

–desorption isotherms provides a powerful technique to determine the surface area, pore volume, and pore size distribution. The surface area was obtained correlating the data of P / P 0 in the range of 0.03–0.5 by the Brunauer–Emmett–Teller method (BET) [ 20 , 21

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Journal of Thermal Analysis and Calorimetry
Authors: N. Ivashchenko, V. Tertykh, V. Yanishpolskii, J. Skubiszewska-Zięba, R. Leboda, and S. Khainakov

use of an analyser of porosity and specific surface area (Micromeritics ASAP 2020, USA) at −196 °C. The total surface area was calculated by the BET method; the volume of pores and the pore-size distribution were obtained with the use of the BJH method

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microscope with EDS analyzer. The measurements of particle size distribution were carried out with Mastersizer 2000 from Malvern Instruments. The measurements of open pore size distribution were performed with PoreMaster 60 from Quantachrome

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. 5. Jiao , F , Hill , AH , Harrison , A , Berko , A , Chadwick , AV , Bruce , PG . Synthesis of ordered mesoporous NiO with crystalline walls and a bimodal pore size distribution . J Amer Chem Soc . 2008 ; 130

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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-size distribution as presented in Fig

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water and the soluble salt content in the leachate was measured using ion chromatography (Dionex IC-2000). The pore size distribution was measured by mercury intrusion porosimetry using a Quantachrome Pore Master 33. Mortar

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containing initially 10% of pitch-polymer compositions [ 18 , 19 ]. Based on earlier determined adsorption of benzene isotherms [ 19 ] it was calculated in this study pore size distributions via effective radii for investigated sorbents ( Fig. 5

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