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Acid-base strength distribution

As seen in Fig. 2.11, the acid - base strength distribution curves intersect at a point on the abscissa where acidity = basicity - 0. Hence, the strongest Ho value of the acid sites is equal to the strongest Ho value of the basic sites. Ho.max is defined as the Ho value at a point of intersection, which expresses the equal strongest Ho value of both acidic and basic sites. Each Ho.max value, which was determined from a point of intersection of each acid-base strength distribution curve and the abscissa, is given in Table 2.4. A unique Ho.max is found for every solid. The Ho.vax value changes on calcination. [Pg.20]

The product distribution in the t-butylation of phenol with isobutanol may be explained based on the nature of acid-base strengths and the mode of adsorption of phenol. It has been reported in the literature that phenol is adsorbed horizontally on acid-catalysts like AI2O3 and a vertical mode of adsorption is proved on basic catalysts like MgO [16,17], The horizontal adsorption of phenol results in O-alkylation and also C-alkylation at ortho and para positions which are close to the surface of the catalyst whereas in the vertical adosrption mode, only the ortho selectivity is observed. The extent of C-alkylation depends on the strength of the acid site. However, a combined participation of acid-base properties is also reported in the methylation of phenol over hydrotalcites [18]. Hence, a scheme depicting the correlation between the acid-base properties of the catalysts with the product distribution in the t-butylation of phenol is shown below as. [Pg.569]

Microcdlorimetry. Differential heats of adsorption of probe molecules can be measured with high accuracy by heat-flow calorimetry and DSC. These data provide information on the acid (or base) strength distribution. Ammonia and other amines have been used as probes for acid sites on oxides (75) and in H forms of zeolite (76), and carbon dioxide and sulfur dioxide were adsorbed as acidic probes on several oxides (75). [Pg.622]

Many years ago, geochemists recognized that whereas some metallic elements are found as sulfides in the Earth s crust, others are usually encountered as oxides, chlorides, or carbonates. Copper, lead, and mercury are most often found as sulfide ores Na and K are found as their chloride salts Mg and Ca exist as carbonates and Al, Ti, and Fe are all found as oxides. Today chemists understand the causes of this differentiation among metal compounds. The underlying principle is how tightly an atom binds its valence electrons. The strength with which an atom holds its valence electrons also determines the ability of that atom to act as a Lewis base, so we can use the Lewis acid-base model to describe many affinities that exist among elements. This notion not only explains the natural distribution of minerals, but also can be used to predict patterns of chemical reactivity. [Pg.1505]

Ammonia TPD is very simple and versatile. The use of propylamine as a probe molecule is starting to gain some popularity since it decomposes at the acid site to form ammonia and propene directly. This eliminates issues with surface adsorption observed with ammonia. The conversion of the TPD data into acid strength distribution can be influenced by the heating rate and can be subjective based on the selection of desorption temperatures for categorizing acid strength. Since basic molecules can adsorb on both Bronsted and Lewis acid sites, the TPD data may not necessarily be relevant for the specific catalytic reaction of interest because of the inability to distinguish between Bronsted and Lewis acid sites. [Pg.158]

When two immiscible solvents are placed in contact with each other and a non-ionizable compound is dissolved in one of the solvents, the compound distributes itself between the two solvents. This distribution is referred to as partitioning. The ratio of the concentrations of the compound in each phase is a constant for a specific set of solvents, pH, buffers, buffer concentrations, ionic strength and temperature. This ratio is referred to as a partition coefficient or distribution coefficient and is equal to the ratio of the solubilities in the two solvents. When the compound is a weak acid or base, the distribution of the compound can be shown to be given by the following equation for a monoprotic compound ... [Pg.87]


See other pages where Acid-base strength distribution is mentioned: [Pg.313]    [Pg.19]    [Pg.20]    [Pg.20]    [Pg.49]    [Pg.313]    [Pg.19]    [Pg.20]    [Pg.20]    [Pg.49]    [Pg.211]    [Pg.540]    [Pg.409]    [Pg.220]    [Pg.219]    [Pg.982]    [Pg.1007]    [Pg.1012]    [Pg.309]    [Pg.309]    [Pg.95]    [Pg.186]    [Pg.19]    [Pg.84]    [Pg.319]    [Pg.327]    [Pg.242]    [Pg.311]    [Pg.181]    [Pg.281]    [Pg.95]    [Pg.157]    [Pg.225]    [Pg.122]    [Pg.236]    [Pg.95]    [Pg.61]    [Pg.156]    [Pg.172]    [Pg.173]    [Pg.50]    [Pg.229]    [Pg.186]    [Pg.22]    [Pg.1498]    [Pg.392]    [Pg.436]    [Pg.820]   
See also in sourсe #XX -- [ Pg.20 ]




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Acid strength

Acid-base strength

Acidizing strength

Acids acid-base strengths

Acids, acid strength

Base strength

Bases acid-base strengths

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