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Level levels, typical

Gas-phase reactions play a fundamental role in nature, for example atmospheric chemistry [1, 2, 3, 4 and 5] and interstellar chemistry [6], as well as in many teclmical processes, for example combustion and exliaust fiime cleansing [7, 8 and 9], Apart from such practical aspects the study of gas-phase reactions has provided the basis for our understanding of chemical reaction mechanisms on a microscopic level. The typically small particle densities in the gas phase mean that reactions occur in well defined elementary steps, usually not involving more than three particles. [Pg.759]

All teclmologically important properties of semiconductors are detennined by defect-associated energy levels in the gap. The conductivity of pure semiconductors varies as g expf-A CgT), where is the gap. In most semiconductors with practical applications, the size of the gap, E 1-2 eV, makes the thennal excitation of electrons across the gap a relatively unimportant process. The introduction of shallow states into the gap through doping, with either donors or acceptors, allows for large changes in conductivity (figure C2.16.1). The donor and acceptor levels are typically a few meV below the CB and a few tens of meV above the VB, respectively. The depth of these levels usually scales with the size of the gap (see below). [Pg.2882]

Sensitivity levels more typical of kinetic studies are of the order of lO molecules cm . A schematic diagram of an apparatus for kinetic LIF measurements is shown in figure C3.I.8. A limitation of this approach is that only relative concentrations are easily measured, in contrast to absorjDtion measurements, which yield absolute concentrations. Another important limitation is that not all molecules have measurable fluorescence, as radiationless transitions can be the dominant decay route for electronic excitation in polyatomic molecules. However, the latter situation can also be an advantage in complex molecules, such as proteins, where a lack of background fluorescence allow s the selective introduction of fluorescent chromophores as probes for kinetic studies. (Tryptophan is the only strongly fluorescent amino acid naturally present in proteins, for instance.)... [Pg.2958]

Immersion Gleaning. The simplest method for using an alkaline cleaner is by immersion. A part is placed on a hook or rack and immersed ia the cleaner solution so that all of the part is below the Hquid level. A typical concentration, temperature, and process time for an immersion cleaner would be ca 75 g/L at 77°C for 5 min. In addition to being the simplest method, immersion is also among the least expensive in terms of equipment. Only a vessel to contain the cleaning solution and a means of heating the solution are needed. [Pg.220]

The resistance of the polymer to oils and organic solvents can be direcdy attributed to the hydroxyl fiinctionahty and the fihn-forrning properties of the polymer. Treated paper substrates display a significant amount of oil resistance, which make them valuable for packing papers and food-grade paperboard containers. This performance improvement is achieved despite the fact that the 1—3 wt % add-on level, typical of size press appHcations, is too low to provide a continuous poly(vinyl alcohol) film. [Pg.489]

For a total condenser, accumulator level is typically set by varying distillate draw. For a partial condenser, it can be controlled with a condenser hot gas bypass. [Pg.68]

Filter life Measure of the duration of a filter s useful service. This is based on the amount of standard contaminant required to cause differential pressure to increase to an unacceptable level-typically 2-4 times the initial differential pressure, a 50-80% drop in initial flow, or a downstream measure of unacceptable particulate. Filter media A porous material for separating suspended particulate matter from fluid. [Pg.614]

A device commonly used to measure atmospheric pressure is the mercury barometer (Figure 5.1), first constructed by Evangelista Torricelli in the seventeenth century. This consists of a closed gas tube filled with mercury inverted over a pool of mercury. The pressure exerted by the mercury column exactly equals that of the atmosphere. Hence the height of the column is a measure of the atmospheric pressure. At or near sea level, it typically varies from 740 to 760 mm, depending on weather conditions. [Pg.104]

We will now add random noise to each concentration value in Cl through C5. The noise will follow a gaussian distribution with a mean of 0 and a standard deviation of. 02 concentration units. This represents an average relative noise level of approximately 5% of the mean concentration values — a level typically encountered when working with industrial samples. Figure 15 contains multivariate plots of the noise-free and the noisy concentration values for Cl through C5. We will not make any use of the noise-free concentrations since we never have these when working with actual data. [Pg.46]

PAC is faster-acting than alum, even in cold water. It produces a compact, fast-settling floe and is effective over a wide range of pH levels (typically 4-9.5). It provides good color removal. [Pg.316]

The BX converts all cations to sodium and the desilicizer exchanges all anions, including silica, for hydroxyl ions, thus effectively changing the treated water into a dilute caustic solution. This is normally a suitable proposition for boiler MU because the FW pH level typically required at these presssures is 8.5 to 9.5. A schematic layout of this type of plant is shown in Figure 9.3b. [Pg.358]

The actual pressure exerted by the atmosphere varies with altitude and weather. The pressure of the atmosphere at the cruising height of a commercial jetliner (10 km) is only about 200 Torr (about 0.3 atm), and so airplane cabins must be pressurized. A very low pressure atmospheric region, such as an area of low pressure on the weather chart in Fig. 4.6, typically has a pressure of about 0.98 atm at sea level. A typical region of high pressure is about 1.03 atm. [Pg.266]

Similar results were reported in deforested Amazonian rainforests (66). Within three years following forest clearing and burning, nutrient concentrations of soil leachates had returned to levels typical of primary forests of the area. A combination of high rates of immobilization and storage by successional vegetation, coupled with a decline in easily decomposable substrates, was attributed to the reduction in leaching losses. [Pg.443]

On plant surfaces, as in soils, numerous studies have demonstrated that endosulfan is oxidized to endosulfan sulfate. Initial residues of endosulfan on treated vegetables generally range from 1 to 100 mg/kg. However, residue levels typically decrease to less than 20% of initial levels within 1 week after treatment (NRCC 1975). Residues of endosulfan isomers are generally negligible after 2-3 weeks the a-isomer is much less persistent than the P-isomer. In most plant residue studies, endosulfan sulfate residue levels tend to increase relative to the parent isomers and other metabolites and appear to be very persistent (Coleman and Dolinger 1982). [Pg.230]

For undoped a-Si H the (Tauc) energy gap is around 1.6-1.7 eV, and the density of states at the Fermi level is typically lO eV cm , less than one dangling bond defect per 10 Si atoms. The Fermi level in n-type doped a-Si H moves from midgap to approximately 0.15 eV from the conduction band edge, and in / -type material to approximately 0.3 eV from the valence band edge [32, 86]. [Pg.10]


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See also in sourсe #XX -- [ Pg.102 , Pg.103 , Pg.104 , Pg.105 ]




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