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PH carbonation

We now consider as an example an analysis (Table 15.1) of water from Mono Lake, California. The reported alkalinity of 34 818 mg kg-1 as CaC03 is equivalent to 700 meq of acid or 350 mmol of H2SO4. Since at this pH carbonate and bicarbonate species are present in roughly equal concentrations, we can quickly estimate the total carbonate concentration to be about 30 000 mg kg-1. We take this value as a first guess and model the titration with react... [Pg.221]

In addition to oxidation-reduction reactions occurring under various conditions, increased carbon dioxide will also affect soil pH. Carbon dioxide... [Pg.111]

The behavior of practically all luminescent materials is sensitive to various parameters of physical and chemical origin. The excited state lifetimes and average intensities of the fluorescence and/or phosphorescence of these materials are modulated, for example, by temperature, oxygen, pH, carbon dioxide, voltage, pressure, and ionic strength. Consequently, the luminescence of various materials could be used, in principle, to monitor parameters of interest in medicine, industry, research, and the environment. [Pg.255]

THE EFFECT OF POC AND PIC FORMATION AND DEGRADATION ON THE pH, CARBONATE ALKALINITY, AND XCO2 OF SEAWATER... [Pg.389]

Typically, buffers in the region of pH 7-9 have been used in MEEKC. At these pH values the buffers generate a high electroosmotic flow (EOF). Extreme values of pH have been used in MEECK specifically to suppress solute ionization. For example, a pH of 1.2 of the buffer has been used to prevent the ionization of acids (30,31). To eliminate the ionization of basic compounds, a buffer at pH 12 has been used. These pH values were used in MEEKC to measure the solubility of ionic compounds (30). High-pH carbonate buffers (31) were applied in place of the standard borate or phosphate buffers. [Pg.146]

Ketones and /3-diketones SDS, heptane, butane-l-ol, high-pH carbonate buffer 36... [Pg.161]

In contrast to equilibria dominated by chloride complexation, equilibria involving hydrolysis or carbonate complexation are strongly influenced by pH. A cation s tendency towards hydrolysis, and its complexation behaviour in general, can be described in terms of the ratio of its ionic charge squared (z2) to its ionic radius (r) in Angstroms (Turner et al., 1981). Cations with z2/r in the intermediate range, 7 < z/r < 25, have seawater speciation schemes that are strongly influenced by solution pH. Carbonate equilibria of the form... [Pg.326]

Aly, R. et al., Effect of prolonged occlusion on the microbial flora, pH, carbon dioxide and transepidermal water loss on human skin, J. Invest. Dermatol., 71,378, 1978. [Pg.168]

Species reported should be correct with regard to the original pH of the sample. At a neutral pH, carbonate species will be almost all HCO3 and high CO3 cannot exist. [Pg.54]

Factors that influence the release of oxygen from oxyhaemoglobin are partial pressure or demand for oxygen at the site (for metabolism), pH, carbon dioxide... [Pg.156]

Relationship between pH, carbon dioxide partial pressure, and estimated corrosion rate... [Pg.3]

Effect of Total Copper, pH, Carbonate, and Dissolved Organic Matter... [Pg.147]

Finally, models were calculated which predict the variations in chemical speciation of copper resulting from changes in the chemical parameters pH, carbonate alkalinity, concentration of dissolved organic matter, and concentration of total dissolved copper. [Pg.147]

Numerous secondary mineral-fluid reactions have been shown to occur in crystalline rock environments (Bucher and Stober, 2000). As mentioned previously, reactions in ultramaflc and maflc rocks can have considerable control on pH, carbonate precipitation, and most likely the accumulation of excess H2 gas (Barnes and O Neil, 1971 Sherwood Lollar et al., 1993b). A typical reaction (Equation (1)) (not balanced) that would involve olivine dissolution (Drever, 1988) and in closed systems would also consume water and concentrate solutes is as follows ... [Pg.2808]

Given values for Cf, AT], K2 and an. we can solve Eqs. (5.22) to (5.24) for concentrations of the carbonate species as a function of pH. Carbonate species concentrations computed for Cr- 10" ° are plotted in Fig. 5.2. Also shown are concentrations of H and OH. Important features of the diagram include (1) the pH regions of dominance of H2CO3, HCO3, and C03 with increasing pH (2) the fact that crossovers of their concentration curves occur where pH = pAf for each dissociation step (3) the pH dependence of the distribution plot is independent of C and (4) concentrations of H+ and OH" are independent of Cp We will return to this figure later in the chapter when we discuss acidity and alkalinity. [Pg.155]

Figure 7.20 Carbon dioxide and pH. Carbon dioxide in the tissues diffuses into red blood cells, Inside a red blood cell, carbon dioxide reacts with water to form carbonic acid, in a reaction catalyzed by the enzyme carbonic anhydrase. Carbonic acid dissociates to form HCOj and H , resulting in a drop in pH inside the red cell. Figure 7.20 Carbon dioxide and pH. Carbon dioxide in the tissues diffuses into red blood cells, Inside a red blood cell, carbon dioxide reacts with water to form carbonic acid, in a reaction catalyzed by the enzyme carbonic anhydrase. Carbonic acid dissociates to form HCOj and H , resulting in a drop in pH inside the red cell.
Luis Baiba has recently proposed that inexpensive spot tests, which can be done in the field, can be used as an efficient proxy for the elemental and organic analyses. He demonstrated that patterns revealed by spot test measurements of pH, carbonate, phosphate, and organic materials correspond closely to those revealed by the more sophisticated analyses. Although the data from spot tests are difficult to interpret in terms of specific activities, they are quite helpful in selecting much smaller subsets of the original samples that can then by analyzed for elements and organic molecules. [Pg.174]

All samples were analyzed at the Archaeometry Laboratory at the Universidad Nacional Autonoma de Mexico with spot tests for pH, carbonate, phosphorus, and organics including hpids and proteins. Based on the results of the spot tests and the distribution maps of the resulting patterns, 20 samples were selected for subsequent analysis by GC/MS. [Pg.179]

Zeebe, R. E. 2005b. Large effect of hydration on fractionation between H2O and CO2 Implications for the pH-carbonate-S O relationship and inferred climate changes. Geophysical Research Abstracts, 7, 1607-7962. [Pg.57]


See other pages where PH carbonation is mentioned: [Pg.223]    [Pg.804]    [Pg.912]    [Pg.378]    [Pg.742]    [Pg.546]    [Pg.742]    [Pg.122]    [Pg.496]    [Pg.602]    [Pg.107]    [Pg.244]    [Pg.348]    [Pg.390]    [Pg.539]    [Pg.191]    [Pg.4775]    [Pg.234]    [Pg.310]    [Pg.325]    [Pg.235]    [Pg.535]    [Pg.173]    [Pg.984]    [Pg.1807]    [Pg.359]    [Pg.31]    [Pg.378]    [Pg.937]    [Pg.185]    [Pg.296]   
See also in sourсe #XX -- [ Pg.79 ]




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