Big Chemical Encyclopedia

Chemical substances, components, reactions, process design ...

Articles Figures Tables About

Water appearance

As is commonly the case with crystalline polymers the glass transition temperature is of only secondary significance with the aliphatic polyamide homopolymers. There is even considerable uncertainty as to the numerical values. Rigorously dried polymers appear to have TgS of about 50°C, these figures dropping towards 0°C as water is absorbed. At room temperature nylon 66 containing the usual amounts of absorbed water appears to be slightly above the T ... [Pg.489]

Similar questions are raised if we consider the effect of cooling the gases produced from the candle. Cooling these gases results in condensation—drops of liquid water appear. If the water vapor contains molecules, made up of atoms, what happens to these molecules (and atoms) when the gas condenses Are they still present in the liquid ... [Pg.27]

Figure 2.40 shows the unsteady flow upstream of the ONE in one of the parallel micro-channels of d = 130 pm at = 228kW/m, m = 0.044 g/s (Hetsroni et al. 2001b). In this part of the micro-channel single-phase water flow was mainly observed. Clusters of water appeared as a jet, penetrating the bulk of the water (Fig. 2.40a). The vapor jet moved in the upstream direction, and the space that it occupied increased (Fig. 2.40b). In Fig. 2.40a,b the flow moved from bottom to top. These pictures were obtained at the same part of the micro-channel but not simultaneously. The time interval between events shown in Fig. 2.40a and Fig. 2.40b is 0.055 s. As a result, the vapor accumulated in the inlet plenum and led to increased inlet temperature and to increased temperature and pressure fluctuations. Figure 2.40 shows the unsteady flow upstream of the ONE in one of the parallel micro-channels of d = 130 pm at = 228kW/m, m = 0.044 g/s (Hetsroni et al. 2001b). In this part of the micro-channel single-phase water flow was mainly observed. Clusters of water appeared as a jet, penetrating the bulk of the water (Fig. 2.40a). The vapor jet moved in the upstream direction, and the space that it occupied increased (Fig. 2.40b). In Fig. 2.40a,b the flow moved from bottom to top. These pictures were obtained at the same part of the micro-channel but not simultaneously. The time interval between events shown in Fig. 2.40a and Fig. 2.40b is 0.055 s. As a result, the vapor accumulated in the inlet plenum and led to increased inlet temperature and to increased temperature and pressure fluctuations.
Besides water, the most common weak base is ammonia, NH3, whose proton transfer equilibrium with water appears in Section 16-. Many other weak bases are derivatives of ammonia called amines, hi these organic compounds, one, two, or three of the N—H bonds in ammonia have been replaced with N—C bonds. The nitrogen atom in an amine, like its counterpart in ammonia, has a lone pair of electrons that can form a bond to a proton. Water does not protonate an amine to an appreciable extent, so all amines are weak bases. Table 17-4 lists several examples of bases derived from ammonia. [Pg.1233]

At first sight the concept of a structure for liquid water appears strange. In the solid state atoms are relatively fixed in space, albeit with some vibrational motion about equilibrium positions, and no difficulty is associated with the idea of locating these equilibrium positions by some appropriate physical technique, and thereby assigning a structure to the solid. [Pg.34]

As a increases, the average distance between ionized groups decreases so that these neighbouring groups begin to have an effect. When a exceeds 0-3, individual water spheres begin to overlap and eventually coalesce into a cylindrical form. With further increases in a, a second outer cylindrical sheath of water appears in which water molecules are oriented by the cooperative effect of two or more carboxyl groups. [Pg.74]

Occasionally, departures from these considerations have been made where such action appeared advantageous in bringing out a relationship between formally unrelated compounds or hazards. In all multi-component cases, however, the secondary reactants (except air and water) appear as formula entries back-referred to the main entry text, so that the latter is accessible from either primary or secondary reactants. See Dimethyl sulfoxide Acyl halides (main entry)... [Pg.2118]

A number of natural waters, from in and around the area of Tampa Bay, Florida, were analysed for tin content. All samples were analysed without pretreatment. Samples that were not analysed immediately were frozen until analysis was possible. Polyethylene bottles, 500 ml volume, were used for sample acquisition and storage. The results of the analyses appear in Table 10.1. The average total tin content of fresh, saline, and estuarine waters are 9.1,4.2, and 12 ng/1, respectively. Approximately 17-60% of the total tin present was found to be in the methylated forms. The saline waters appear to have the highest percentage of methylated tin compounds 60% of the total tin present... [Pg.470]

The infrared spectrum of erythromycin is commonly used for its identification. Figure 2 shows the spectrum of a 75 mg./ml. chloroform solution. The bands at 1685 and 1730 cm- are due to the ketone carbonyl and the lactone carbonyl, respectively. The absorption peaks between 1000 and 1200 cm-1 are due to the ethers and amine functions. The CH2 bending is evidenced by peaks between 1340 and 1460 cm-, and alkane stretching peaks appear between 2780 and 3020 cm-. Hydrogen bonded OH and water appear as bands between 3400 and 3700 cm-1. [Pg.163]

HydrophiIic versus hydrophobic coadsorption. The contrast between the hydrophilic and hydrophobic coadsorption seen on Rh(111) and Pt(lll), if confirmed under normal electrochemical conditions, might be of electrocatalytic importance. On Rh(lll), where net attractive CO-HgO interactions produce a mixed phase in which CO is displaced to a three-fold binding site which is not occupied in the absence of water, CO and water appear to occupy adjacent binding sites. Such thorough mixing of the oxygen source (water) and the intermediate [or poison] (CO) should improve electrooxidation rates for C 0 H fuels (11). On Pt(lll), where net repulsions cause condensation of CO and water into separate patches, reaction between the adsorbed species could occur only at the boundaries between patches, and one would expect slower kinetics. [Pg.70]

Femtosecond solvation dynamics experiments in water [147] clearly hint at the existence of a bimodal response of the solvent to a change in solute charge density that is produced by photon absorption for instance. Water appears to show an ultrafast component in the fl/ kT timescale and a slow component due to diffusive motions whose timescale would be in the 1/y range. [Pg.311]

The dog s requirement for water appears to be self-regulated and depends on factors such as the type of feed consumed, ambient temperature, amount of exercise, and physiological state therefore, in most cases, dogs should have free access to water. [Pg.598]

What happens if we replace our reactant, KF(1), with KF(aq) This apparently minor change makes a big difference in the results. The potassium ions and the fluoride ions are still present, so they are still under consideration, but we also need to consider water. Water appears in many places in a table of reduction potentials. We must examine every place it appears alone on a side or with one of the ions we know to be present, K+ and I. The potassium and fluorine halfreactions, with their reduction potentials are ... [Pg.275]

An influential textbook in physical organic chemistry by Lapworth s student, William Waters, appeared in 1935 with an introduction by Lowry giving an account of recent developments as Lapworth saw them. 132 But, as Robinson knew, the history of a theory and the history of a discipline in large measure is created by historical introductions and the systems of citations in the most-cited articles and books in a field. [Pg.211]

In summary, water appears as an extremely unsuitable solvent for coordination of hard Lewis acids to hard Lewis bases, as it strongly solvates both species and hinders their interaction. Hence, catalysis of Diels-Alder reactions in water is expected to be difficult due to the relative inefficiency of the interactions between the Diels-Alder reactants and the Lewis acid catalyst. On the other hand, the high stereoselectivities and yields observed in biosyntheses, with water as the solvent, indicate that these rationalizations cannot entirely be true. As a matter of fact, we will demonstrate in the following that Lewis acid catalysis in water is not only possible, but also allows for effective as well as environmentally friendly reaction conditions. [Pg.1070]

Reduction of propellant size by grinding under water appears to be feasible with the current concept. However, it is noted that this feasibility depends very much on successful propellant grain extraction using the untested RDM concept. [Pg.88]

The potential impacts of organic leachates from complex mixtures on surface and ground waters appear to be of environmental concern, thus the testing methodology provides a systematic approach for such evaluations. [Pg.232]

Ruthenium on platinum was found to facilitate the oxidation of oCOad but noteoCOad interacting water, appeared to play a role of the oxygen source, replacing Pt-OH. Contrarily, tin and molybdates on platinum showed promoting effects for the oxidation of eoCOad but not AoCOad Redox couples of tin or molybdenum oxides appeared to play a role of a mediator as well as the ox en source. The active potentials were the bwest for molybdates and the second for tin. [Pg.244]

Figure 7. A Mg vs. 5 Mg plot of calcite speleothems and their drip waters from the Soreq cave site, Israel (data from Galy et al. 2002) compared with seawater. The horizontal trend of the data suggests that Mg in carbonates is related to aqueous Mg by equilibrium fractionation processes. Results of a three-isotope regression, shown on the figure and in Table 3, confirm that the (3 value defined by the data is similar to the predicted equilibrium value of 0.521 and distinct from kinetic values. The positive A Mg characteristic of the speleothem carbonates is apparently inherited from the waters. The positive A Mg values of the waters appear to be produced by kinetic fractionation relative to primitive terrestrial Mg reservoirs (the origin). Figure 7. A Mg vs. 5 Mg plot of calcite speleothems and their drip waters from the Soreq cave site, Israel (data from Galy et al. 2002) compared with seawater. The horizontal trend of the data suggests that Mg in carbonates is related to aqueous Mg by equilibrium fractionation processes. Results of a three-isotope regression, shown on the figure and in Table 3, confirm that the (3 value defined by the data is similar to the predicted equilibrium value of 0.521 and distinct from kinetic values. The positive A Mg characteristic of the speleothem carbonates is apparently inherited from the waters. The positive A Mg values of the waters appear to be produced by kinetic fractionation relative to primitive terrestrial Mg reservoirs (the origin).

See other pages where Water appearance is mentioned: [Pg.272]    [Pg.280]    [Pg.132]    [Pg.77]    [Pg.5]    [Pg.12]    [Pg.105]    [Pg.11]    [Pg.119]    [Pg.154]    [Pg.413]    [Pg.459]    [Pg.289]    [Pg.431]    [Pg.7]    [Pg.183]    [Pg.295]    [Pg.204]    [Pg.225]    [Pg.348]    [Pg.1376]    [Pg.1548]    [Pg.371]    [Pg.192]    [Pg.320]    [Pg.428]    [Pg.754]    [Pg.272]    [Pg.182]   
See also in sourсe #XX -- [ Pg.55 ]




SEARCH



Appearance

Liquid water, first appearance

Liquid water, first appearance Earth

Water, first appearance on Earth

© 2024 chempedia.info