𝔖 Bobbio Scriptorium
✦   LIBER   ✦

Water Adsorption on Pyrogenic Silica Followed by1H MAS NMR

✍ Scribed by Jean-Baptiste d'espinose de la Caillerie; Mohamed Raouf Aimeur; Youssef El Kortobi; André Pierre Legrand


Book ID
102581454
Publisher
Elsevier Science
Year
1997
Tongue
English
Weight
130 KB
Volume
194
Category
Article
ISSN
0021-9797

No coin nor oath required. For personal study only.

✦ Synopsis


physisorbed water), and their accessibility to water (internal On the surface of two commercial pyrogenic silicas (Degussa or external silanols). Study of the state of physisorbed water and Cabot), five resonances were identified on the basis of the itself led to the distinction between structured monolayers, chemical shift, homonuclear coupling ( T 2 ), and spin-lattice relaxclusters, and weakly bound liquid-like water molecules (14).

ation behavior (T 1 ). In accordance with previous studies we ob-Nevertheless, several difficulties remain when studying served three different types of silanol groups: (i) weakly coupled silica surfaces. First, the surface is not structured. Therefore, (long T 2 ), water inaccessible, isolated ''internal'' silanols at 1.8 although models based on small crystalline domains have ppm; (ii) weakly coupled, external ''free'' silanols revealed upon been proposed 10,, surface irregularity leads to a dehydration at 2.5 ppm; and (iii) strongly coupled external hydrogen bound silanols with an unresolved broad resonance between dispersion of the physicochemical properties of the hydroxyl 3 and 7 ppm. The resonance of water, whose position between 2.6 sites. Second, thermogravimetric dosing of structural and and 4.6 ppm depended on water content, corresponded to two adsorbed water is difficult as (de)hydration overlaps with unresolved species of slightly different T 1 . By equating this reso-(de)hydroxylation. Third, amorphous silica is a metastable nance to the weighted average of two distinct populations of water, phase, and its surface is heavily reconstructed during the we were able to distinguish the first layer of strongly hydrogen conditioning of the samples. bound water at 2.7 ppm from liquid-like water at 5 ppm. The first Among the different techniques mobilized to scrutinize layer is complete for water relative humidity as low as 3.6% and protons on the surface of silica in particular, and oxides in corresponds to a surface coverage of 4.75 H 2 O/nm 2 . If we assumed general, 1 H NMR is certainly among the most promising a cristobalite-based surface structure, this meant a 1:1 ratio between surface hydroxyls and the first layer of physisorbed water. because of its great sensitivity and dependency on hydrogen This ratio was the same for the two silicas regardless of surface bonds. Despite severe line broadening due to a combination area. ᭧ 1997 Academic Press of strong homodipolar coupling and chemical shift disper-Key Words: 1 H MAS-NMR; silica.

sion, study of precipitated and sol-gel silicas allowed identification of the resonances of water, bound silanols, and isolated silanols at circa 5, 2.5, and 1.7 ppm from tetramethylsi-


📜 SIMILAR VOLUMES


1H NMR studies of the adsorption of wate
✍ V.V. Turov; V.V. Brei; K.N. Khomenko; R. Leboda 📂 Article 📅 1998 🏛 Elsevier Science 🌐 English ⚖ 217 KB

A study has been made of silicalite samples with a specific surface area (by the BET method ) of S=350 m2 g-1 which were synthesized on the basis of fumed silica and did not contain aluminum. 1H NMR spectroscopy is used to determine the value of the chemical shift of the adsorbed water molecules and

Dissociative adsorption of water in CaNa
✍ Ilir A. Beta; Bernd Hunger; Winfried Böhlmann; Herve Jobic 📂 Article 📅 2005 🏛 Elsevier Science 🌐 English ⚖ 509 KB

Three CaNaA zeolites, in which, respectively, 49%, 65% and 83% of the Na + cations were exchanged with Ca 2+ ions, along with a NaA sample were studied by thermogravimetry, temperature-programmed DRIFT spectroscopy and MAS NMR. Thermogravimetric desorption profiles of the Ca 2+ exchanged zeolites sh