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Particles yields

With the exception of the scanning probe microscopies, most surface analysis teclmiques involve scattering of one type or another, as illustrated in figure A1.7.11. A particle is incident onto a surface, and its interaction with the surface either causes a change to the particles energy and/or trajectory, or the interaction induces the emission of a secondary particle(s). The particles that interact with the surface can be electrons, ions, photons or even heat. An analysis of the mass, energy and/or trajectory of the emitted particles, or the dependence of the emitted particle yield on a property of the incident particles, is used to infer infomiation about the surface. Although these probes are indirect, they do provide reliable infomiation about the surface composition and structure. [Pg.304]

The PLM can be used in a reflection or a transmission mode. With either mode, light of various wavelengths from ultraviolet to infrared, polarized or unpolarized, is used to yield a wide variety of physical measurements. With just ordinary white light, a particle or any object detail down to about 0.5 p.m (500 nm) in diameter can be observed to detect shape, size, color, refractive index, melting point, and solubiUty in a group of solvents, all nondestmetively. Somewhat larger particles yield UV, visible, or IR absorption spectra. [Pg.333]

Fig. 12. Micromechanics of ductile reinforcement particles yielding within process 2one and particles bridging in crack wake. Fig. 12. Micromechanics of ductile reinforcement particles yielding within process 2one and particles bridging in crack wake.
A beam of charged particles (an ion beam) with an energy from a few hundred keV to several MeV is produced in an accelerator and bombards a sample. Nuclear reactions with low-Z nuclei in the sample are induced by this ion beam. Products of these reactions (typically p, d, t, He, a particles, and y rays) are detected, producing a spectrum of particle yield versus energy. Many (p, a) reactions have energies that are too low for efficient detection. In these cases, the associated y rays are detected instead. Important examples are ... [Pg.681]

As with conventional Cl, this is a very mild form of ionization leading to molecular species with little or no fragmentation, i.e. (M + H)+ and (M — H) . This is not, however, always the case. The use of chromatographic modifiers may change the composition of the Cl plasma to such a state that, as in Cl and thermospray, other ions may be formed, e.g. the presence of ammonium acetate may lead to (M - - NH4)+ and (M - - CHsCOO)" ions in the positive- and negative-ion modes, respectively. The chemistry of the analyte may also have an effect, as has been discussed for ESI, with, for example, the spectra of fullerenes extracted from soot particles yielding an M+ molecular species [16],... [Pg.182]

Fig. 3 Effects of pH on the particle yield, size. Fig. 4 Effects of temperature on the particle yield, and number density. (30°C isothermal) size, SDod number density. Fig. 3 Effects of pH on the particle yield, size. Fig. 4 Effects of temperature on the particle yield, and number density. (30°C isothermal) size, SDod number density.
By investigating the effects of pH, it was shown that H2P04 was the actual precursor of lanthanum phosphate precipitation. The particle yield was proportional to the H2P04 concentratian. The number density was proportional to the square of the H2p04 concentration. A maximum particle size was obtained at an optimum precursor concentiation as a result of the tradeoff of the nuclealion and growth. [Pg.836]

Table 1. Characteristics of the supports used for deposition of metallic Au particles, yields of the metallic Au and Au hydroxide, and the size of metallic Au particles on the different supports. Table 1. Characteristics of the supports used for deposition of metallic Au particles, yields of the metallic Au and Au hydroxide, and the size of metallic Au particles on the different supports.
It should be emphasized that in the above presentation of permutation operations, they were carried out on symbols, rather than physical objects. One 1 was exchanged for another as a result of a paper operation . The ication of this principle in physical systems must be made with cate. When it is said that the "exchange of two identical particles yields the following results , it must be understood that it is the exchange of identity of the par-tides, stich as labels or coordinate s that has been made. [Pg.308]

Following Barry, James et al (1972), and Thomas and Hinchliffe (1972) investigated the use of wire screens for collecting 218Po atoms or ions. Experiments were done in the absense of aerosol particles, yielding collection efficiency as a function of screen dimensions and face velocity. Information was developed on the fraction of deposited o-activity that could be counted from the front and back sides of the screens. [Pg.345]

Lee et a/.88 used the results of their investigation of the effects of chlorine on the radiolysis of HC1 to correct Vandame s a-particle data86. As shown in Table 6, his corrected yields agree reasonably well with those for the X- and y-radiolysis. However, the true initial a-particle yields may still be slightly higher than those given in Table 6, since no allowance was made for the effects of reaction (21)... [Pg.161]

An energy balance on the particle yields heat generated by reaction = heat lost by conduction + heat lost by radiation... [Pg.429]

Infrared spectra suggested that a sulfate ion coordinates to two titanium atoms as a bidentate in particles. The maximum particle size was found at Aerosol OT mole fraction of 0.35 in the mixtures. The particle size increased linearly with increasing the concentration of sulfuric acid at any Wo, but with increasing Wo the effect was the opposite at any sulfuric acid concentration. These effects on the particle size can be explained qualitatively in relation with the extent of number of sulfate ions per micelle droplet. These precursor particles yield amorphous and nanosized TiO particles, reduced by 15% in volume by washing of ammonia water. The Ti02 particles transformed from amorphous to anatase form at 400°C and from anatase form to rutile form about at 800°C. In Triton X-100-n-hexanol-cyclohexane systems, however, spherical and amorphous titanium hydroxide precursor were precipitated by hydrolysis of TiCl4 (30). When the precursor particles were calcinated,... [Pg.94]

The integration of this equation over the entire projected area of the particle yields the buoyancy force ... [Pg.239]

Integrating Eqn.(5.41) and averaging over many particles yields, if tZ = kT/m and... [Pg.105]

Fig. 38 Transmission electron micrographs of gold nanoparticles organized in 2D arrays through binding of two types of three-branched DNA motifs, (a) Array where only one tile contains 5 nm particles. The resulting arrangement has two different characteristic length scales, (b) Array where both tiles contain 5-nm particles, yielding an equally spaced pattern, (c) Array where one tile contains a 5-nm particle and the other tile contains a 10-nm particle. The pattern of alternating smaller and bigger spheres mimics the rhombic pattern of the tile array. Adapted with permission from [164]... Fig. 38 Transmission electron micrographs of gold nanoparticles organized in 2D arrays through binding of two types of three-branched DNA motifs, (a) Array where only one tile contains 5 nm particles. The resulting arrangement has two different characteristic length scales, (b) Array where both tiles contain 5-nm particles, yielding an equally spaced pattern, (c) Array where one tile contains a 5-nm particle and the other tile contains a 10-nm particle. The pattern of alternating smaller and bigger spheres mimics the rhombic pattern of the tile array. Adapted with permission from [164]...
Kilauea volcano, Hawaii, USA, erupted in January, 1983. During a two-week period including the eruption, atmospheric particulate matter (PM) around the volcano was collected on 0.4 pm air filters (Zoller, Parrington and Phelan Kotra, 1983). Measurements of the atmospheric particles yielded 0.0045-1.600 ng m-3 (nanograms of arsenic per cubic meter of air). Before the eruption, the average arsenic concentrations were 0.013-0.039 ng m-3 (Zoller, Parrington and Phelan Kotra, 1983). [Pg.96]


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See also in sourсe #XX -- [ Pg.406 ]




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