1952
DOI: 10.1139/v52-026
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Charcoal Sorption Studies: I. The Pore Distribution in Activated Charcoals

Abstract: The pore distributions of three activated charcoals have been calculated from the low temperature nitrogen and water isotherms. The method of Barrett, Joyner, and Halenda has been used with the nitrogen data, while the Kelvin equation has been applied to the water isotherm. The two curves coincide if cos 0 = 0.65 is used in the Kelvin equation, where 8 is the wetting angle. This figure is in general agreement with a published figwe obtained by an independent method.

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Cited by 19 publications
(8 citation statements)
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“…This value is slightly lower than the total pore volume obtained from SO 2 adsorption and 0.55 cm 3 g –1 from CO 2 adsorption. This difference in total pore volumes has been observed previously for adsorption on activated carbons and was attributed to the lower density of the adsorbed water phase in hydrophobic activated carbons compared with liquid water. The water vapor adsorption isotherms were analyzed by using the Dubinin–Serpinsky equation . The results calculated for the p / p 0 range 0.2–0.5 showed that the primary surface site concentration from the isotherms averaged 2.12 ± 0.05 mmol g –1 .…”
Section: Resultsmentioning
confidence: 59%
“…This value is slightly lower than the total pore volume obtained from SO 2 adsorption and 0.55 cm 3 g –1 from CO 2 adsorption. This difference in total pore volumes has been observed previously for adsorption on activated carbons and was attributed to the lower density of the adsorbed water phase in hydrophobic activated carbons compared with liquid water. The water vapor adsorption isotherms were analyzed by using the Dubinin–Serpinsky equation . The results calculated for the p / p 0 range 0.2–0.5 showed that the primary surface site concentration from the isotherms averaged 2.12 ± 0.05 mmol g –1 .…”
Section: Resultsmentioning
confidence: 59%
“…0.6 mL/g) accessible to SFe only at higher temperatures (see Table I). The truly carbonaceous nature (nonoxidized) is noted in the hydrophobic character of the water isotherm (Figure 5) (12). These results also show that sorption of sulfur hexafluoride will not be markedly hindered by sorbed water as long as the relative humidity is kept appreciably below ~50%.…”
Section: Resultsmentioning
confidence: 64%
“…5 Pore volume filling occurs at high relative pressure but the density of the adsorbed water is usually lower than that of the liquid. [6][7][8][9] This has been ascribed to the inability of adsorbed water to form a full threedimensional structure in microporosity. [6][7][8][9] Competitive adsorption is difficult to study because of problems associated with quantifying the uptakes and adsorption dynamics of the various adsorbed species in multicomponent adsorption systems.…”
Section: Introductionmentioning
confidence: 99%
“…[6][7][8][9] This has been ascribed to the inability of adsorbed water to form a full threedimensional structure in microporosity. [6][7][8][9] Competitive adsorption is difficult to study because of problems associated with quantifying the uptakes and adsorption dynamics of the various adsorbed species in multicomponent adsorption systems. The amounts adsorbed may be calculated indirectly from a complete set of adsorption isotherms for the total adsorption of the multicomponent system, using various models based on thermodynamic principles, or determined by direct measurement of the amounts of each component adsorbed.…”
Section: Introductionmentioning
confidence: 99%