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Phase correction, overview

Fig. 2. Overview of pulse shaping results, (a) and (b) depict measured SHG FROG traces before and after adaptive phase correction, respectively. Corresponding retrieved traces are displayed in (c) and (d). (e) Shows fundamental spectrum (shaded contour) measured at the crystal location in the FROG apparatus and the spectrum recovered by the FROG retrieval algorithm (open circles). Dash-dotted curve represents spectral phase prior to adaptive shaping, whereas dashed curve shows the optimized phase, (f) Initial (solid curve) and optimized (shaded contour) temporal intensity profiles. Dashed curve depicts temporal phase of the optimized pulse. Fig. 2. Overview of pulse shaping results, (a) and (b) depict measured SHG FROG traces before and after adaptive phase correction, respectively. Corresponding retrieved traces are displayed in (c) and (d). (e) Shows fundamental spectrum (shaded contour) measured at the crystal location in the FROG apparatus and the spectrum recovered by the FROG retrieval algorithm (open circles). Dash-dotted curve represents spectral phase prior to adaptive shaping, whereas dashed curve shows the optimized phase, (f) Initial (solid curve) and optimized (shaded contour) temporal intensity profiles. Dashed curve depicts temporal phase of the optimized pulse.
In a recent paper by Alam and Alam,4 a good overview of the different two-way multivariate methods and their application to NMR data is given. Also some of the important issues such as phase correction, alignment, line shape and resolution that should be kept in mind when using multivariate methods for the analysis of NMR data are discussed (see also ref.5). [Pg.211]

Practical details of data acquisition and reduction (e.g., phase correction, choice of excitation waveform and response apodization, etc.) have been left to the remaining Chapters. The intent here has been to present an overview from which it should be possible to better understand the motives for the specific transform procedures presented in the remaining Chapters. [Pg.42]

Surface diffusion has been extensively studied in literature. An overview of experimental data is given in Table 6.1. Okazaki, Tamon and Toei (1981), for example, measured the transport of propane through Vycor glass with a pore radius of 3.5 nm at 303 K and variable pressure (see Table 6.1). The corrected gas phase permeability was 0.69 m -m/m -h-bar, while the surface permeability was 0.55 m -m/m -h-bar, and so almost as large as the gas phase permeability (Table 6.1). It is clear from Table 6.1, that the effects of surface diffusion, especially at moderate temperatures, can be pronounced. At higher temperatures, adsorption decreases and it can be expected that surface diffusion will become less pronounced. [Pg.102]

We present an overview of variational transition state theory from the perspective of the dynamical formulation of the theory. This formulation provides a firm classical mechanical foundation for a quantitative theory of reaction rate constants, and it provides a sturdy framework for the consistent inclusion of corrections for quantum mechanical effects and the effects of condensed phases. A central construct of the theory is the dividing surface separating reaction and product regions of phase space. We focus on the robust nature of the method offered by the flexibility of the dividing surface, which allows the accurate treatment of a variety of systems from activated and barrierless reactions in the gas phase, reactions in rigid environments, and reactions in liquids and enzymes. [Pg.67]

Phosphate accessory phases contain a wealth of petrologic and chronological information, but each possesses particular properties that make accurate quantitative microanalysis difficult. This chapter provides an overview of the literature concerned with the main problems of electron microprobe (BMP) phosphate analysis. These include the volatility of fluorine in F-bearing apatite, and the mutual interference of L- and M-line X-rays from the major and trace elements in monazite and xenotime, along with consideration of standards, detection limits, absorption edges, and ZAF corrections in REE phosphates. [Pg.337]

A comprehensive overview of frequency-domain DOT techniques is given in [88]. Particular instraments are described in [166, 347, 410]. It is commonly believed that modulation techniques are less expensive and achieve shorter acquisition times, whereas TCSPC delivers a better absolute accuracy of optical tissue properties. It must be doubted that this general statement is correct for any particular instrument. Certainly, relatively inexpensive frequency-domain instruments can be built by using sine-wave-modulated LEDs, standard avalanche photodiodes, and radio or cellphone receiver chips. Instruments of this type usually have a considerable amplitude-phase crosstalk". Amplitude-phase crosstalk is a dependence of the measured phase on the amplitude of the signal. It results from nonlinearity in the detectors, amplifiers, and mixers, and from synchronous signal pickup [6]. This makes it difficult to obtain absolute optical tissue properties. A carefully designed system [382] reached a systematic phase error of 0.5° at 100 MHz. A system that compensates the amplitude-phase crosstalk via a reference channel reached an RMS phase error of 0.2° at 100 MHz [370]. These phase errors correspond to a time shift of 14 ps and 5.5 ps RMS, respectively. [Pg.101]

In [43, 47, 48] the corrections are applied to a deterministic or stochastic molecular dynamics method with the goal of improving numerical stability at large timestep and/or enhancing phase space exploration. A practical overview of these methods, with a molecular dynamics test example, may be found in [43]. [Pg.417]

See also Atomic Absorption Spectrometry Interferences and Background Correction. Atomic Emission Spectrometry Principles and Instrumentation Interferences and Background Correction Flame Photometry Inductively Coupled Plasma Microwave-Induced Plasma. Atomic Mass Spectrometry Inductively Coupled Plasma Laser Microprobe. Countercurrent Chromatography Solvent Extraction with a Helical Column. Derivatization of Analytes. Elemental Speciation Overview Practicalities and Instrumentation. Extraction Solvent Extraction Principles Solvent Extraction Multistage Countercurrent Distribution Microwave-Assisted Solvent Extraction Pressurized Fluid Extraction Solid-Phase Extraction Solid-Phase Microextraction. Gas Chromatography Ovenriew. Isotope Dilution Analysis. Liquid Chromatography Ovenriew. [Pg.4847]

This study provides a preliminary overview of possible accident risks for deep geothermal systems. Future research should analyze other sources of accident risks, e.g., the chemical composition of the geofluids in the operational phase. Furthermore, exposure and toxicity analyses need to be carried out for hazardous substances in order to correctly assess the risk of chemicals. [Pg.1529]


See other pages where Phase correction, overview is mentioned: [Pg.173]    [Pg.2]    [Pg.99]    [Pg.39]    [Pg.157]    [Pg.118]    [Pg.389]    [Pg.28]    [Pg.527]    [Pg.185]    [Pg.152]    [Pg.99]    [Pg.630]    [Pg.393]    [Pg.451]    [Pg.2132]    [Pg.183]    [Pg.40]    [Pg.2]   
See also in sourсe #XX -- [ Pg.67 , Pg.68 , Pg.69 ]




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Phase correction

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