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Calcium carbonate illustration

Both prototypal questions related illustrate the need for a successhil technical service professional to have a strong understanding of the customer s apphcations and processes, within proper intellectual property considerations. This need for a thorough understanding is not always straightforward. A common example of the complications that can arise is provided from the paint (qv) industry (11). If, for instance, a calcium carbonate suppHer would like a paint manufacturer to use their material versus a competitive one, the onus is on the suppHer to show that the material can be successfully used in the paint formula of interest. However, many such formulas are held as proprietary. The technical service professional therefore does not know the components of the paint. This would lead to an unworkable situation from an evaluation standpoint save for the fact that the paint company may supply a miHbase or other intermediate form of the paint to allow a proper comparison of carbonates to be carried out. Thus mutual benefits can result and no loss of proprietary information occur. [Pg.378]

An illustration of the difference in reactivity of a-and / -halides is provided by the ready elimination of 1,4a-dibromo-5a-cholestan-3-one to 4a-bromo-5a-cholest-l-en-3-one in collidine at room temperature. Calcium carbonate in refluxing DMA is necessary to complete the dehydrobromination to the l,4-dien-3-one. ... [Pg.304]

Rules are provided to aid decision making at each step. The procedure is illustrated with examples including separation of amino acids, p- and / -cresols, chorobenzoic acids, calcium carbonate and magnesium oxide from dolomite, and the production of salt. [Pg.277]

Calcium carbonate solubility is also temperature and pressure dependent. Pressure is a 6r more important fector than temperature in influencing solubility. As illustrated in Table 15.1, a 20°C drop in temperature boosts solubility 4%, whereas the pressure increase associated with a 4-km increase in water depth increases solubility 200-fold. The large pressure effect arises from the susceptibility of the fully hydrated divalent Ca and CO ions to electrostriction. Calcite and aragonite are examples of minerals whose solubility increases with decreasing temperature. This unusual behavior is referred to as retrograde solubility. Because of the pressure and temperature effects, calcium carbonate is fer more soluble in the deep sea than in the surfece waters (See the online appendix on the companion website). [Pg.382]

The environmental impact of acid rain depends on local geology, as Figure 10.15 illustrates. In certain regions, such as the midwestern United States, the ground contains significant quantities of the alkaline compound calcium carbonate (limestone), deposited when these lands were submerged under oceans... [Pg.347]

The effects of initial amelioration are most readily discernible in the alcohol and acid content of the new wine. Instead of alcohol concentrations of 7-10%, the new wines contain 12-13%. The effect of partial amelioration on acid content is illustrated in Table VIII. The total acid values of the new wines are the result both of partial amelioration and deposition of tartrates during the alcoholic fermentation. Even so, most of the acid values remain high, and additional techniques must be employed to reduce the acid content to an acceptable level. Processes currently used include further amelioration, blending several native varieties and hybrids of the same or different vintages, blending a small proportion of low-acid vinifera wine, and encouraging the malo-lactic fermentation. Treatment with calcium carbonate is permitted by federal regulations and occasionally is used to reduce natural acidity in the absence of a malo-lactic fermentation. [Pg.114]

The existence of alkyl- or aryl calcium amides has not as yet been unambiguously demonstrated. One reason for this seems to be because calcium— carbon bonds are much less stable than calcium—nitrogen bonds, as is illustrated by the following reaction [Eq. (2)] (12). [Pg.271]

The concept of a reversible chemical reaction may be illustrated by the decomposition of calcium carbonate, which when heated forms calcium oxide and carbon dioxide gas. At equilibrium, this system exerts a definite decomposition pressure of C02 for a given temperature. When the pressure falls below this value, CaCOj decomposes. Assume now that a cylinder is fitted with a frictionless piston and contains CaC03, CaO, and C02 in equilibrium. It is immersed in a constant-temperature bath, as shown in Fig. 2.5, with the temperature adjusted to a value such that the decomposition pressure is just sufficient to balance the weight on the piston. The system is in mechanical equilibrium, the temperature of the system is equal to that of the bath, and the chemical reaction is held in balance by the pressure of the COj. Any change of conditions, however slight,... [Pg.391]

Equations (1.3a) and (1.3b) illustrate the overall reactions of CO2 generation in aerobic and anaerobic respiration, respectively. Although not shown here, some types of bacterial fermentations can also be a source of CO2 for carbonate generation. Equation (1.5) explains the origin of C03 . This reaction is forced in the direction of C03 by loss of CO2 to the atmosphere in an open system, and by precipitation of calcium carbonate (CaC03), illustrated in Eq. (1.6), or by the formation of other carbonates not shown here. [Pg.14]

Increasing the US intensity and diameter of the horn tip increases the crystallization rate. Figure 5.14 illustrates the individual and combined effects of these variables in the crystallization of calcium carbonate at different US intensities and horn tip diameters of 3, 14 and 22 mm. As can be seen in Fig. 5.14A, increasing the US intensity decreased the Ca + concentration in the medium and increased the amount of crystallized matter formed. A similar effect was observed by increasing the diameter of the horn tip or the product of the US intensity and the square root of the horn tip area, which additionally increased the crystallization rate (see Figs. 5.14B and 5.14C). These two effects physically contribute to... [Pg.180]

The conch shell, which is 99% calcium carbonate, is therefore really a composite material in which proteins provide the toughness that makes the shell so resistant to shattering. Although the conch shell itself is not useful (except to the conch), it illustrates how composites may offer much greater strength than the individual substances involved. Lessons learned from the conch... [Pg.775]

Figure 2(C) is the result of a calculation that illustrates which cations might fit into sixfold coordination position in the calcite group structures. It is an interesting insight as both light and heavy rare earth elements are possible substitutes for calcium in the calcium carbonate structure, i.e., they plot within 15% of the calcium ionic size. However, some of the end-members incorporate elements into this crystal structure and are outside this deviation but within 30%, an expression of the potential physical expansion for this layered crystal structure. These are ionic charge differences important in whether a stable crystalline structure can be produced. Trace amounts of all these ions can be incorporated in calcite and may dictate the morphology of the crystallites. Therefore, the presence and amount of any ions in the environment in which carbonate crystallization occurs may possibly be recorded. However, in spite of the predominance of sodium and potassium in the solutions where... Figure 2(C) is the result of a calculation that illustrates which cations might fit into sixfold coordination position in the calcite group structures. It is an interesting insight as both light and heavy rare earth elements are possible substitutes for calcium in the calcium carbonate structure, i.e., they plot within 15% of the calcium ionic size. However, some of the end-members incorporate elements into this crystal structure and are outside this deviation but within 30%, an expression of the potential physical expansion for this layered crystal structure. These are ionic charge differences important in whether a stable crystalline structure can be produced. Trace amounts of all these ions can be incorporated in calcite and may dictate the morphology of the crystallites. Therefore, the presence and amount of any ions in the environment in which carbonate crystallization occurs may possibly be recorded. However, in spite of the predominance of sodium and potassium in the solutions where...

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