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Timescales limitations

Sulphur dioxide takes part in chemical reactions with substances naturally present in the atmosphere and with other pollutants, some of them driven by sunlight and others by the presence of cloud droplets. The end product of the oxidation of sulphur dioxide is sulphuric acid, together with ammonium sulphate, in the form of suspended particles. These sulphur particles, known collectively as sulphate aerosol, tend not to be removed particularly efficiently by dry deposition and have timescales limited only by the scavenging during rain events. Sulphate aerosols may have lifetimes up to 10 days and may travel hundreds and thousands of kilometres before encountering rain. The capture of sulphate aerosol by rain leads to the process of wet deposition and this process accounts for the remaining one third of the total removal of sulphur species. [Pg.223]

Both MD and MC teclmiques evolve a finite-sized molecular configuration forward in time, in a step-by-step fashion. (In this context, MC simulation time has to be interpreted liberally, but there is a broad coimection between real time and simulation time (see [1, chapter 2]).) Connnon features of MD and MC simulation teclmiques are that there are limits on the typical timescales and length scales that can be investigated. The consequences of finite size must be considered both in specifying the molecular mteractions, and in analysing the results. [Pg.2241]

Molecular dynamics (MD) metliods can be used to simulate tribological phenomena at a molecular level. These have been used primarily to simulate behaviour observed in AFM and SFA measurements. Such simulations are limited to short-timescale events, but provide a weaitli of infonnation and insight into tribological phenomena at a level of detail tliat cannot be realized by any experimental metliod. One of tire most interesting contributions of molecular dynamics... [Pg.2746]

II of the actual atoms (or at least the non-hydrogen atoms) in the core system are lented explicitly. Atomistic simulations can provide very detailed information about haviour of the system, but as we have discussed this typically limits a simulation to nosecond timescale. Many processes of interest occur over a longer timescale. In the if processes which occur on a macroscopic timescale (i.e. of the order of seconds) rather simple models may often be applicable. Between these two extremes are imena that occur on an intermediate scale (of the order of microseconds). This is the... [Pg.418]

The surface consists of terraces of a height of 330 30 pm. Within error limits, this is the value that would be expected for Ge(lll) bilayers. Furthermore, we were able to observe that the electrodeposition gave rise to a less ordered surface structure with nanoclusters, transforming over a timescale of about 1 hour into a layered structure. With GeBr4 a transformation of clusters into such a layered surface was only partly seen with GeGl4 this transformation could not be observed. [Pg.315]

In presence of molecular motion the NMR line shape will change. A particularly simple situation arises, if the motion is rapid on timescale defined by the inverse width of the spectrum in absence of motion 6 1. In this fast exchange limit, which in 2H NMR is reached for correlation times tc < 1CT7 s, the motion leads to a partially averaged quadrupole coupling and valuable information about the type of motion can directly be obtained from analysis of the resulting line shapes. The NMR frequency is then given by... [Pg.28]

Mass transfer in a gas-liquid or a liquid-liquid reactor is mainly determined by the size of the fluid particles and the interfacial area. The diffusivity in gas phase is high, and usually no concentration gradients are observed in a bubble, whereas large concentration gradients are observed in drops. An internal circulation enhances the mass transfer in a drop, but it is still the molecular diffusion in the drop that limits the mass transfer. An estimation, from the time constant, of the time it wiU take to empty a 5-mm drop is given by Td = d /4D = (10 ) /4 x 10 = 6000s. The diffusion timescale varies with the square of the diameter of the drop, so... [Pg.346]

Figure 4.1. TRIR difference spectra averaged over the timescales indicated following 355 nm laser photolysis of diazirine 8 (15.7mM) in C02-satnrated dichloromethane. Reprinted with permission from B. M. Showalter and J. P. Toscano, J. Phys. Org. Chem. 2004, 14, 743. Copyright 2004, John Wiley Sons Limited. Figure 4.1. TRIR difference spectra averaged over the timescales indicated following 355 nm laser photolysis of diazirine 8 (15.7mM) in C02-satnrated dichloromethane. Reprinted with permission from B. M. Showalter and J. P. Toscano, J. Phys. Org. Chem. 2004, 14, 743. Copyright 2004, John Wiley Sons Limited.
Principles and Characteristics Supercritical fluid extraction uses the principles of traditional LSE. Recently SFE has become a much studied means of analytical sample preparation, particularly for the removal of analytes of interest from solid matrices prior to chromatography. SFE has also been evaluated for its potential for extraction of in-polymer additives. In SFE three interrelated factors, solubility, diffusion and matrix, influence recovery. For successful extraction, the solute must be sufficiently soluble in the SCF. The timescale for diffusion/transport depends on the shape and dimensions of the matrix particles. Mass transfer from the polymer surface to the SCF extractant is very fast because of the high diffusivity in SCFs and the layer of stagnant SCF around the solid particles is very thin. Therefore, the rate-limiting step in SFE is either... [Pg.85]


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See also in sourсe #XX -- [ Pg.221 ]




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