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Journal of Thermal Analysis and Calorimetry
Authors: Dmitar Zorić, Dušan Lazar, Ognjen Rudić, Miroslava Radeka, Jonjaua Ranogajec, and Helena Hiršenberger

interval. Based on the SEM results, Fig. 2 , a very loose morphology is recognized in the case of the FA particles. The results of water absorption and apparent particle density, Table 4 , and pore-size distribution, Fig. 5 , confirm that LWA

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TM 1500 (Setaram) calorimeter under flowing argon (scanning rate 10 K min −1 , platinum crucibles, sample weight 0.001–0.020 g) up to 1200 °C. The surface area value and pore size distribution were determined by multipoint BET method by

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in oxidation reactions [ 4 , 9 , 20 ]. Recently, many nanostructured mesoporous oxides with high surface area and uniform pore size distribution have been used as supports for multiple catalyst applications. For example, nanostructured mesoporous

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. The surface area and pore volume of catalysts were measured by the BET method, and the pore size distributions were detected using the BJH method, both of which was performed by a surface area analyzer (TriStar II 3020, Micromeritics, USA). XPS was

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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. Hajnos M

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Journal of Thermal Analysis and Calorimetry
Authors: A. V. Ursu, G. Jinescu, F. Gros, I. D. Nistor, N. D. Miron, G. Lisa, M. Silion, G. Djelveh, and A. Azzouz

instrument, CuKα), thermogravimetric analysis in the temperature range 25–700 °C (Mettler Toledo TGA/SDTA 851 balance, nitrogen flow of 20 mL/min, heating rate of 10 °C/min, 3–5 mg samples). The specific surface area and pore size distributions were

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activated carbon was characterized with a Micromeritics ASAP 2020 System. The pore size distribution was determined by a low pressure nitrogen adsorption isotherm at 77 K (from 5 × 10 −7 to 0.99 p / p 0 in relative pressure range) evaluated by the Horvath

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compressive strength and Young’s modulus in gypsum from Sivas (Turkey) . – Engineering Geology , 66 , pp. 211 – 219 . Yu , S. , C.T. Oguchi 2010 : Role of pore size

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and a tetragonal flake-like shape. Figure 8 shows the N 2 adsorpotion/desorpotion isotherm and the corresponding pore size distribution of the PbTiO 3 samples. The measurement shows that the BJH (Barrett–Joyner–Halenda) desorpotion gives a main

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Journal of Thermal Analysis and Calorimetry
Authors: Hou-yin Zhao, Yan Cao, Zhi-zhong Kang, Yau-bang Wang, and Wei-ping Pan

surface area of the carriers was evaluated from the N 2 adsorption isotherms by applying the BET equation in the relative pressure range of 0.05–0.35. The mesopore size was determined using BJH method and the pore size distribution was determined by DFT

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