scholarly journals Estimation of Specific Surface Area for Zeolites by Pressure Swing Adsorption Method.

1991 ◽  
Vol 40 (459) ◽  
pp. 1573-1576
Author(s):  
Ayao TAKASAKA ◽  
Yoshihiro MATSUDA
2015 ◽  
Vol 36 (4) ◽  
pp. 3-6 ◽  
Author(s):  
Ewa Koszela-Marek

Abstract The paper presents the results of laboratory studies of the 200 MPa pressure effect on specific surface area of clay. The original high-pressure investigation stand was used for the pressure tests. Determination of the specific surface area was performed by the methylene blue adsorption method. The results of the specific surface area test were compared for non-pressurized clays and for clays pressured in a high-pressure chamber. It was found that the specific surface area of pressurized soil clearly increased. This shows that some microstructural changes take place in the soil skeleton of clays.


BioResources ◽  
2021 ◽  
Vol 16 (3) ◽  
pp. 6074-6082
Author(s):  
Weikai Wang ◽  
Minghan Li ◽  
Jiabin Cai

In order to study the effects of a messmate heartwood extraction process on its cell wall pore structure and its drying ability, its nanopore structure was explored after via gas adsorption technology. Specifically, the messmate heartwood particles were extracted with methanol, and then the cell wall pore structure of the original and extracted samples were evaluated by N2 and CO2 sorption and pycnometer methods, respectively. Overall, compared with the original samples, the cell wall porosity, micropore volume, mesopore volume, BET specific surface area, and specific surface area of the micropores of the extracted messmate heartwoods increased by 2.55%, 0.007 cm3/g, 0.0014 cm3/g, 0.24 m2·g-1, and 21.9 m2·g-1, respectively. The cell wall pore volume measured via the gas adsorption method was smaller than the measurement from the pycnometer method. The results indicated that the presence of extractives made the messmate cell wall have a decreased pore volume and porosity, which may be one of the reasons messmate wood is difficult to dry. Messmate extractives primarily were present in the micropores of the cell wall in the range of 0.4 nm to 0.7 nm. However, gas sorption technology could not detect all the pores in the cell wall of the messmate heartwood sample.


2013 ◽  
Vol 785-786 ◽  
pp. 749-752
Author(s):  
Ya Jun Luo ◽  
Qian Yan ◽  
Yong Chao Zhou ◽  
Deng Liang He ◽  
Xiao Li Hu

Activated carbon was modified with silica aerogel by the Sol-Gel. The surface characteristics and structure of activated carbon modified by the silica aerogel were characterized with N2 adsorption method, Scanning Electron Microscope and Thermal Analysis. The experiment results show that the silica aerogel can be used to modify activated carbon for the preparation of composite. SiO2 aerogel can effectively cover holes in the activated carbon, specific surface area of activated carbon composite modified by SiO2 aerogel was between activated carbon and silica aerogel. When MSiO2: MC is 1:3, specific surface area of the composite was 758.638 m2/g; When MSiO2:MC is 1:2, specific surface area of the composite was 760.38 m2/g; When MSiO2:MC is 1:1, specific surface area of the composite was 862.755 m2/g.


2007 ◽  
Vol 336-338 ◽  
pp. 1886-1888
Author(s):  
Yan Yu ◽  
Yu Zhong Ruan

Alumina adsorbent was synthesized from waste aluminum sludge in this research. The nitrogen isothermal adsorption method (77K) is applied to measure the BET specific surface area and pore structure of activated alumina at different activation temperatures. The research results indicate that, thermal treatment has huge influences on the test sample’s specific surface area and pore structure. Its specific surface area and pore volume expand and then diminish, whereas the holding time rises, getting its peak of 348 m² /g and 0.55 (cm³ /g) respectively at the activation temperature of 600°C and holding time for 1 hour. The average pore diameter value increases along with the lengthening of activation temperature and holding time, reaching the maximum of 11nm at activation temperature of 750°C and holding time for 4 hours. After comprehensive analysis, the activation temperature of 600°C and holding time for 1 hour are determined as ideal conditions for activated alumina respectively.


1996 ◽  
Vol 465 ◽  
Author(s):  
P. Hölttä ◽  
M. Siitari-Kauppi ◽  
P. Huihuri ◽  
A. Lindberg ◽  
A. Hautojärvt

ABSTRACTThe sorption of sodium (22Na), calcium (45Ca) and strontium (85Sr) was studied on mica gneiss, unaltered, moderately altered and strongly altered tonalite samples taken from hole SY-KR7 drilled in the Syyry area in Sievi, Western Finland. The crushed rock samples were sieved into six fractions from 71 μm to 1250 μm. A proportional mineral composition for the different fractions were estimated by X-ray diffraction. The specific fraction surface areas were determined by the BET nitrogen adsorption method. The fractal method was applied to characterize rocks and to describe quantitatively surface irregularity. The mass distribution ratio values for each fraction were determined using the static batch method. The sorption of tracers onto different minerals was observed using rock thin sections. Kd-values calculated from thin section Ka-values and Kd revalues obtained from batch experiments were in good agreement. Mass distribution ratios for different size fractions are given, and the effect of the specific surface area is discussed. Owing to larger specific surface areas considerably higher sorption on smaller fractions was found for altered tonalites.


2008 ◽  
Vol 8 (5) ◽  
pp. 1261-1275 ◽  
Author(s):  
M. Kerbrat ◽  
B. Pinzer ◽  
T. Huthwelker ◽  
H. W. Gäggeler ◽  
M. Ammann ◽  
...  

Abstract. Chemical and physical processes, such as heterogeneous chemical reactions, light scattering, and metamorphism occur in the natural snowpack. To model these processes in the snowpack, the specific surface area (SSA) is a key parameter. In this study, two methods, computed tomography and methane adsorption, which have intrinsically different effective resolutions – molecular and 30 μm, respectively – were used to determine the SSA of similar natural snow samples. Except for very fresh snow, the two methods give identical results, with an uncertainty of 3%. This implies that the surface of aged natural snow is smooth up to a scale of about 30 μm and that if smaller structures are present they do not contribute significantly to the overall SSA. It furthermore implies that for optical methods a voxel size of 10 μm is sufficient to capture all structural features of this type of snow; however, fresh precipitation appears to contain small features that cause an under-estimation of SSA with tomography at this resolution. The methane adsorption method is therefore superior to computed tomography for very fresh snow having high SSA. Nonetheless, in addition to SSA determination, tomography provides full geometric information about the ice matrix. It can also be advantageously used to investigate layered snow packs, as it allows measuring SSA in layers of less than 1 mm.


2007 ◽  
Vol 7 (4) ◽  
pp. 10287-10322 ◽  
Author(s):  
M. Kerbrat ◽  
B. Pinzer ◽  
T. Huthwelker ◽  
H. W. Gäggeler ◽  
M. Ammann ◽  
...  

Abstract. Chemical and physical processes, such as heterogeneous chemical reactions, light scattering, and metamorphism occur in the natural snowpack. To model these processes in the snowpack, the specific surface area (SSA) is a key parameter. In this study, two methods, computed tomography and methane adsorption, which have intrinsically different spatial resolutions –molecular and 30 μm, respectively – were used to determine the SSA of identical natural snow samples. The two methods give identical results, with an uncertainty of 3%. This implies that the surface of natural snow is smooth up to a scale of about 30 μm and that for optical methods a voxel size of 10 μm is sufficient to capture all structural features of natural snow. This smoothness can be physically explained by calculating sublimation and surface diffusion on the snow particles. The methane adsorption method is superior to computed tomography for very fresh snow, but thin layers typical for natural snowpacks can not be resolved. Computed tomography can measure SSA in layers of less than 1 mm thickness, and is therefore advantageous in layered snowpacks.


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