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Texture microporosity

The BET surface area values are also reported with the distribution of porosity between microporosity (pore diameter <1.8 nm) deduced from N2 adsorption isotherms (t-curves) and mesoporosity (pore diameter > 1.8 nm). The following trend is observed for high atomic M/HPA ratio used for the precipitation, the precipitates exhibited high surface area mainly due to microporosity. However, depending on the nature of the coxmter cation and also of the previous ratio values, the textural characteristics were not similar. In particular, it is interesting to note the presence of mesopores for (NH4)2.4P, CS2.9P, CS2.7P and Cs2.4Si samples. [Pg.593]

Temperature of the sol-gel processing. Only in cases of the xerogels 40, 73 and 74 has a systematic study demonstrated how much the texture is temperature-dependent. From data in Table 4, an increase in the temperature of the perforation of the gel leads to a decrease in microporosity, an increase in mesoporosity and an increase in specific surface area155. It also appears that the texture of the material is not directly correlated to the degree of polycondensation (see Table 3)151,152. The same effect was also found for the xerogel P(C6H4SiOi.5)3 (30 m2g-x at 20 °C and 340 m2g 1 at 60 °C)109. [Pg.595]

The results of the textural characterisation are collected in Table 1. Although the methods used to determine the surface areas have limited value when applied to microporous solids, here they have been used as convenient methods to compare the different samples. The results show that samples have large surface areas and a well developed microporosity. [Pg.240]

The objective of the present work was to study and compare by scanning tunneling microscopy (STM) the microporosity and mesoporosity of several different carbon materials with various types and amounts of pores highly oriented pyrolytic graphite with artificially-generated model pores, activated carbon fibers, nonporous thermally treated carbon black and nonactivated carbon fibers with an ultramicroporous texture. [Pg.530]

In this study, we have prepared and characterized montmorillonite pillared with Al and La in different proportions. The structural and textural parameters of the materials were compared with those of montmorillonite pillared only with Al. We have applied classical and new models to low pressure nitrogen adsorption data to obtain a quantitative evaluation of the microporosity of the synthesized materials and their evolution under thermal treatments. [Pg.617]

In addition to the design of the solid-gas contactor device, the yield of a desulfurization process directly depends on the physicochemical properties of the used adsorbent crystallite size of the active phase, specific surface area, and porous texture. In the case of a microporous membrane, if the gas flow is forced across the microporosity, it can be expected that the retention will be highly efficient. In return, the low amount of adsorbent restricts the potential applications to the elimination of traces in high-purity gas or to the design of integrated filters for miniaturized devices like micro fuel cells. [Pg.463]

Because of their narrow microporosity, the textural characterisation of CMS is not easy. Gas and vapours adsorption, especially nitrogen adsorption at 77 K, may be kinetically hindered, and large equilibrium times are needed to obtain the adsorption isotherms. In this way, immersion calorimetry emerges as a powerful technique for the characterisation of pore size distributions in CMS. By choosing hquids with different molecular sizes, the micropore volumes can be obtained as a function of their size by applying the relationship obtained by Stoeckli and Kraehenbuehl [5] ... [Pg.303]

Porous texture characterisation of LTA, FAU and MFI type zeolites has been carried out by N2 adsorption at 77K and CO2 adsorption at 273K. These results have been compared to the data obtained from crystallographic estimations. In this way, the micropore volumes obtained by CO2 adsorption at 273K are, in all the cases, similar to the expected from the crystal framework of the zeolite. However, the micropore volumes obtained by N2 adsorption at 77K are significantly smaller. These results confirm the limitations of the N2 adsorption at 77K in measuring narrow microporosity and make evident the usefulness of CO2 adsorption at 273K to characterise porous solids with narrow microporosity. [Pg.485]

To avoid the above problem and to achieve a correct assessment of the porosity, the use of other adsorptives and experimental conditions have been proposed, such as He adsorption at 4.2K[5,6] and CO2 adsorption at 273K or 298K [4,8-12]. He adsorption at 4.2 K also covers the whole range of partial pressures and accurately estimates the microporosity [6]. However, the experimental conditions required do not allow us to propose this technique as a routine procedure for the characterisation of the porous texture of solids. [Pg.485]

Finally it should be noted that the characterisation of membranes is more demanding than most other porous materials. Firstly, the membranes separation layer is generally thin and supported, which requires a sensitive technique capable of analysing a sample in such a form. The characterisation of a powder "equivalent" to the membrane carmot in all cases be considered as representative of the membrane texture. Secondly, the structure is frequently anisotropic and moreover often microporous. Assessment of the microporosity is much less advanced compared to meso- and macro-porosity, despite emphasis given to this in the recent lUPAC symposia [6-8]. The current and widespread interest in the characterisation of microporous matericds is well illustrated by the numerous and varied publications found in these symposia proceedings. These highlight recent developments in characterisation techniques, their applications and limitations. The particular features of importance in membrane studies will be considered in the light of the characterisation techniques to be described. [Pg.69]

In the following, the usefulness of CO2 adsorption at 273 K to achieve a rather complete characterization of the porous texture of microporous carbons will be discussed. We will base our study on the results already published [33-35, 37] in which samples with different characteristics were used and CO2 adsorption experiments at high pressures (up to 4 MPa) were performed. In this study, the ACFs with different contents of microporosity have been very useful. The use... [Pg.439]

Medium surface area silicon carbide (grains 0.4-1 mm) used as support was synthesized at the CRV-Pechiney, according to the Shape Memory Synthesis developed by Ledoux and co-workers, involving the gas-solid reaetion between SiO vapours and solid carbon under dynamic vacuum around 1200-1300°C [11-13]. A calcination was then performed at 700°C for 3 h to stabilize the textural eharacteristics and to bum of the remaining unreaeted carbon. No microporosity was present in the SiC. [Pg.984]

The XRD patterns of zirconium sulfate pillared clays obtained after 90 hours of intercalation with different zirconium acetate concentrations using 0.5 as sulfate to Zr ratio and the same clay concentration as used earlier are presented in Fig. 5. The diffraction data show the appearance of two first order reflections. The first one is at 23.4 A for the lowest zirconium concentration and appears as a shoulder at the same distance for 0.05 mol/L concentration. The second reflection is observed at approximately 12.3 A for the lowest concentration and at 13.7 A for 0.1 mol/L zirconium acetate. The first one results from the intercalation of sulfated zirconium species. Those species are more voluminous than the non sulfated one which gives a distance spacing at only 19.6 A. The better intercalation of sulfated zirconium species at low Zr concentration is probably due to the slow progress of polycondensation reactions. This process reduces the number of different zirconium species and gives a better cristallinity of the solid. Table 2 summarizes the textural properties of samples prepared with different zirconium concentrations. The decrease of the surface area with the decrease of the Zr concentration is probably due to the increase of the sodium clay layers by comparison with the intercalated layers. The microporous volume increases when the Zr concentration decreases. The higher microporosity is due to the important basal distance of this sample. [Pg.1058]

In this part the effect of zirconium concentration on the textural thermal stability is investigated. Fig. 11 shows the variation of the microporous volume as a function of temperature for two Zr concentrations (0.1 mol/L and 0.025 mol/L). As shown, the Zr concentration seems to be important to the thermal stability of the microporosity. In fact, the microporosity of the sample prepared with 0.025 mol/L develops a higher thermal stability than that prepared with 0.1 mol/L zirconium. The polymeric phase deposited on the clay layers appears to be responsible for this loss of microporosity. An insignificant increase in the surface area between 120 °C and 400 °C is observed for the sample prepared with Zr concentration of 0.025 mol/L,... [Pg.1061]

Wenzel s relation has been confirmed in terms of the first two laws of thermodynamics. Huh and Mason, in 1976, used a perturbation method for solving the Young-Laplace equation while applying Wenzel s equation to the surface texture. Their results can be reduced to Wenzel s equation for random roughness of small amplitude. They assume that hysteresis was caused by nonisotropic equilibrium positions of the three-phase contact line, and its movement was predicted to occur in jumps. On the other hand, in 1966, Timmons and Zisman attributed hysteresis to microporosity of solids, because they found that hysteresis was dependent on the size of the liquid molecules or associated cluster of molecules (like water behaves as an associated cluster of six molecules). [Pg.326]

Films from the same research group were subsequently characterized with regards to their porosity, showing both zeolite microporosity and textural mesoporosity.[102] The above concept can be extended towards films with different binders, including organic polymers. Thus, two-component films comprised of nanoscale silicalite-1 and acrylic latex were deposited on silicon wafers via spin-coating.[103] In this case, a purified suspension of colloidal zeolites with sizes of 30 or 60 nm were first deposited followed by calcination. In a second step, a layer of acrylic latex was deposited, resulting in layers with dielectric constants between 2.0 and 2.5. [Pg.279]

Regarding the use of TiOj-SiOj gels as supports of metal catalysts the textural properties of the aerogels are particularly favorable. The lack of microporosity joints to the very high values of specific surface areas and, as pointed out in the results, their porous structure can resist a conventional impregnation treatment without severe changes in texture. [Pg.469]


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Microporosity

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