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Generation of elements

From a C element we can generate other elements by raising it to the powers 1,2, 3. (n — 1). For example, if there is a C3 element there must also be C, where [Pg.78]


The sample environment was filled with He gas to prevent the argon X-ray emission from air. Beam scanning, data acquisition, evaluation and the generation of elemental maps were controlled by a computer. Micro-PIXE measurements were performed with a scanning 2.5MeVH+ microbeam accelerated by the 3 MV single-end accelerator. The beam diameter was 1-2 pm, so that individual particles could be analysed. The beam current was < 100 pA and the irradiation time was about 3(M0 min. [Pg.103]

The system is easier to handle due to the in situ generation of elemental bromine. [Pg.137]

If a process gas is supplied to the cathode with an H,S level of 2000 ppm, a CO, level of 1%, and an H,0 level of 12% (a saturated natural gas composition), it is assumed that 99% of the H,S is removed by reaction (5), and if the process and sweep gas flowrates are equal, then there exist an activity ratio of a oJa of 665 in the anolyte before significant (e.g. 1%) of the carbonate is oxidized. This assiunes equivalent electrode kinetics for the cathodic and anodic reactions. When compared to the activity ratio of Ocos a of 26.9, this shows the thermodynamic preference for the oxidation of to elemental sulfur by equation (8) when there is an absence of reductant at the anode. This mode of operation is preferable for commercial application, with direct production of elemental sulfur vapor, eliminating this need for a Claus reactor for sulfur production. The net effect, under these conditions, is continuous removal of H,S from the process gas accompanied by enrichment of the process gas with H, and direct generation of elemental sulfrur. ITie only reagent required is electric power at a potentially attractive rate, which will be shown. [Pg.537]

Hydride generation AAS (HGAAS) and cold vapour AAS (CVAAS) are special combinations of chemical separation and enrichment with AAS. In HGAAS the analyte is transformed to a volatile hydride, stripped off by an inert gas and atomized in a quartz tube, flame-in tube etc. About ten elements (As, Se, Bi, Sb etc.) can be determined by this technique. The accuracy and detection limits depend on the proper isolation of the hydride. CVAAS is the universally acknowledged most sensitive method for determination of Hg. The generation of elemental mercury vapour is similar to the hydride generation however the quartz cell may not be heated and this gives the name of the method. [Pg.160]

Partial fluorination is achieved by electrolysis in molten KF-2HF in the Phillips process at porous carbon electrodes. The process is thought to involve the electrochemical generation of elemental fluorine and its radical reaction with the substrate within the pores of the anode. Hydrocarbons, acid fluorides and esters are partially fluorinated with a statistical distribution of the fluoride in the alkyl chain and in current efficiencies between 80-100%. [Pg.785]

Most recently, amineboranes of the type L-BH3 (where L = NH3 tert-BuNHz MezNH Me3N) and sodium cyanotrihydroborate(III) (NaBH3CN) have been tested for efficacy of generation of elemental mercury and volatile hydrides of As(III), As(V), Sb(III), Sb(V), Bi(ni), Se(IV), Se(VI), Te(IV), and Te(VI). All of the reductants are suitable for efficient generation of cold-vapor mercury but only some of the amineboranes are suitable for hydride generation,... [Pg.191]

It might be expected that lanthanides which exhibit divalent states, like Eu and Yb, would be most likely to have their sesquioxides vaporize via the generation of monoxide vapor species. Instead these sesquioxides tend to form atomic vapor (e.g., R) species and oxygen due to the greater stability of R versus RO. Thus, for the sesquioxides of actinides with a greater tendency towards divalency or that are divalent metals (e.g., Cf, Es and Fm), the more likely it is that the vaporization mode of their sesquioxides is via generation of elemental vapor plus oxygen. [Pg.492]

A new generation of element selective detectors has become available based on chemiluminescence and plasma emission spectroscopy that have excellent sensitivity, uniformity of response, and selectivity over carbon. [Pg.25]

Element 120 is located in a region of the neutron versus proton map known as the island of stability. Write a nuclear equation for the generation of element 120 by bombarding iron isotopes on a plutonium target. [Pg.1202]

D Mello M, Duneczky C and Wyatt R E 1988 Recursive generation of individual S-matrix elements application to the collinear H + H2 reaction Chem. Phys. Lett. 148 169... [Pg.2325]

We can now proceed to the generation of conformations. First, random values are assigne to all the interatomic distances between the upper and lower bounds to give a trial distam matrix. This distance matrix is now subjected to a process called embedding, in which tl distance space representation of the conformation is converted to a set of atomic Cartesic coordinates by performing a series of matrix operations. We calculate the metric matrix, each of whose elements (i, j) is equal to the scalar product of the vectors from the orig to atoms i and j ... [Pg.485]

The described method can generate a first-order backward or a first-order forward difference scheme depending whether 0 = 0 or 0 = 1 is used. For 9 = 0.5, the method yields a second order accurate central difference scheme, however, other considerations such as the stability of numerical calculations should be taken into account. Stability analysis for this class of time stepping methods can only be carried out for simple cases where the coefficient matrix in Equation (2.106) is symmetric and positive-definite (i.e. self-adjoint problems Zienkiewicz and Taylor, 1994). Obviously, this will not be the case in most types of engineering flow problems. In practice, therefore, selection of appropriate values of 6 and time increment At is usually based on trial and error. Factors such as the nature of non-linearity of physical parameters and the type of elements used in the spatial discretization usually influence the selection of the values of 0 and At in a problem. [Pg.66]

In this section the discretization of upper-convected Maxwell and Oldroyd-B models by a modified version of the Luo and Tanner scheme is outlined. This scheme uses the subdivision of elements suggested by Marchal and Crochet (1987) to generate smooth stress fields (Swarbrick and Nassehi, 1992a). [Pg.81]

A major advantage of this hydride approach lies in the separation of the remaining elements of the analyte solution from the element to be determined. Because the volatile hydrides are swept out of the analyte solution, the latter can be simply diverted to waste and not sent through the plasma flame Itself. Consequently potential interference from. sample-preparation constituents and by-products is reduced to very low levels. For example, a major interference for arsenic analysis arises from ions ArCE having m/z 75,77, which have the same integral m/z value as that of As+ ions themselves. Thus, any chlorides in the analyte solution (for example, from sea water) could produce serious interference in the accurate analysis of arsenic. The option of diverting the used analyte solution away from the plasma flame facilitates accurate, sensitive analysis of isotope concentrations. Inlet systems for generation of volatile hydrides can operate continuously or batchwise. [Pg.99]

Chemical ingenuity in using the properties of the elements and their compounds has allowed analyses to be carried out by processes analogous to the generation of hydrides. Osmium tetroxide is very volatile and can be formed easily by oxidation of osmium compounds. Some metals form volatile acetylacetonates (acac), such as iron, zinc, cobalt, chromium, and manganese (Figure 15.4). Iodides can be oxidized easily to iodine (another volatile element in itself), and carbonates or bicarbonates can be examined as COj after reaction with acid. [Pg.100]

Salt was first electrochemicaHy decomposed by Cmickshank ia 1800, and ia 1808 Davy confirmed chlorine to be an element. In the 1830s Michael Faraday, Davy s laboratory assistant, produced definitive work on both the electrolytic generation of chlorine and its ease of Hquefaction. And ia 1851 Watt obtained the first Fnglish patent for an electrolytic chlorine production cell (11). [Pg.486]


See other pages where Generation of elements is mentioned: [Pg.77]    [Pg.274]    [Pg.67]    [Pg.516]    [Pg.77]    [Pg.34]    [Pg.551]    [Pg.49]    [Pg.325]    [Pg.297]    [Pg.68]    [Pg.483]    [Pg.320]    [Pg.275]    [Pg.77]    [Pg.274]    [Pg.67]    [Pg.516]    [Pg.77]    [Pg.34]    [Pg.551]    [Pg.49]    [Pg.325]    [Pg.297]    [Pg.68]    [Pg.483]    [Pg.320]    [Pg.275]    [Pg.1631]    [Pg.2065]    [Pg.2658]    [Pg.26]    [Pg.29]    [Pg.35]    [Pg.36]    [Pg.39]    [Pg.79]    [Pg.192]    [Pg.82]    [Pg.167]    [Pg.209]    [Pg.98]    [Pg.122]    [Pg.194]    [Pg.356]   


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Generating Elements

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