Carbon evolution

Muller G. and Wagner F. (1978) Holocene carbonate evolution in Lake Balaton (Hungary) a response to climate and impact of man. Spec. Publ. Int. Ass. Sedim. 2, 57-81. 

Grotzinger J. P. and James N. P. (2000) Precambrian Carbonates, Evolution and Understanding Carbonate Sedimentation and Diagenesis in the Evolving Precambrian World. SEPM Special Publication 67. 

A new element for simultaneous indirect detection of C and signals in labelled proteins was proposed by Uhrin et The CT- CHs, VT- N-HSQC sequence combines constant-time carbon evolution with variable delay nitrogen evolution. This is achieved by the variation of the position of a 90° pulse creating transverse coherence within the C constant-time period. The maximum indirect acquisition time for both nuclei is determined by constant-time period set to l/ /(C,C) = 28.6 ms. The method is best suited for detection of CH3 signals due to their slower relaxation. The proposed element was incorporated into NOESY-based experiments resulting in 3D NOESY-CH3NH and 3D HSQC-NOESY-CH3NH sequences. The experiments... 

Montaron, B., 2008. Carbonate evolution. Oil Gas Middle East (August), 26-31. 

F re 4-7. Volatile nitrogen and carbon evolution from sawdust normalized to total volatile matter evolution... 

Figure 4-8. Volatile nitn en and carbon evolution fifom urban wood waste as a function of temperature...

In addition to the abnormal properties already discussed, aqueous hydrofluoric acid has the properties of a typical acid, attacking metals with the evolution of hydrogen and dissolving most metallic hydroxides and carbonates. 

Fig. 1. Comparison of two different dynamical simulations for the Butane molecule Verlet discretization with stepsize r = O.OOSfs. Initial spatial deviation 10 A. Left Evolutions of the total length (=distance between the first and the last carbon atom) of the molecule (in A). Right Spatial deviation (in A) of the two trajectories versus time.

The top part of Fig. 1 shows the time evolution of the central dihedral angle of butane, r (defined by the four carbon atoms), for trajectories... 

Fig. 1. The time evolution (top) and average cumulative difference (bottom) associated with the central dihedral angle of butane r (defined by the four carbon atoms), for trajectories differing initially in 10 , 10 , and 10 Angstoms of the Cartesian coordinates from a reference trajectory. The leap-frog/Verlet scheme at the timestep At = 1 fs is used in all cases, with an all-atom model comprised of bond-stretch, bond-angle, dihedral-angle, van der Waals, and electrostatic components, a.s specified by the AMBER force field within the INSIGHT/Discover program.

Fig. 2. Time-evolution of the methyl/ethyl C-C distances for both the zirconocene and the corresponding titanocene catalyst. The two curves starting at around 3.2 A represent the distance between the methyl carbon atom and the nearest-by ethylene carbon atom in the zirconocene-ethylene and the titanocene-ethylene complex, respectively. The two curves starting at around 1.35 A reflect the ethylene internal C-C bond lengths in the two complexes.

Ethyl bromide soon distils over, and collects as heavy oily drops under the water in the receiving flask, evaporation of the very volatile distillate being thus prevented. If the mixture in the flask A froths badly, moderate the heating of the sand-bath. When no more oily drops of ethyl bromide come over, pour the contents of the receiving flask into a separating-funnel, and carefully run oflF the heavy lower layer of ethyl bromide. Discard the upper aqueous layer, and return the ethyl bromide to the funnel. Add an equal volume of 10% sodium carbonate solution, cork the funnel securely and shake cautiously. Owing to the presence of hydrobromic and sulphurous acids in the crude ethyl bromide, a brisk evolution of carbon dioxide occurs therefore release the... 

Add 15 g. of finely powdered ammonium carbonate gradually to 50 ml. of glacial acetic acid contained in a 150 ml. round-bottomed flask, shaking the mixture during the addition to ensure a steady evolution of carbon dioxide. When all the carbonate has... 

Prepare a mixture of 30 ml, of aniline, 8 g. of o-chloro-benzoic acid, 8 g. of anhydrous potassium carbonate and 0 4 g. of copper oxide in a 500 ml. round-bottomed flask fitted with an air-condenser, and then boil the mixture under reflux for 1 5 hours the mixture tends to foam during the earlier part of the heating owing to the evolution of carbon dioxide, and hence the large flask is used. When the heating has been completed, fit the flask with a steam-distillation head, and stcam-distil the crude product until all the excess of aniline has been removed. The residual solution now contains the potassium. V-phenylanthrani-late add ca. 2 g. of animal charcoal to this solution, boil for about 5 minutes, and filter hot. Add dilute hydrochloric acid (1 1 by volume) to the filtrate until no further precipitation occurs, and then cool in ice-water with stirring. Filter otT the. V-phcnylanthranilic acid at the pump, wash with water, drain and dry. Yield, 9-9 5 g. I he acid may be recrystallised from aqueous ethanol, or methylated spirit, with addition of charcoal if necessary, and is obtained as colourless crystals, m.p. 185-186°. 

Nitrogen. To one portion of the filtrate, add z-3 ml. of 10, aqueous sodium hydroxide solution, then add about o-2 g. of ferrous sulphate and proceed as in the Lassaigiie nitrogen test (p, 322). Note, however, that the fiUal acidification with dilute siiphiiric acid must be made with care, owing to the vigorous evolution of carbon dioxide from the carbonate present. 

Solubility in sodium carbonate solution. Note that phenols, when soluble in water, will also dissolve in NagCOg solution, but usually loithout evolution of CO, i.e., without the formation of a sodium derivative. This reaction can therefore be used to distinguish between carboxylic adds and most phenols. See Section 5, p. 330. 

Reaction with sodium carbonate. Boil about 0 5 g. of 0- and of />-nitrophenol in turn with Na2C03 solution, using the method described in Section 5, p. 336, and note the evolution of CO2. 

A solution prepared by dissolving 2 g. of biomine in 100 g. of carbon tetra. chloride is satisfactory. Carbon tetrachloride is employed because it is an excellent solvent for bromine as well as for hydrocarbons it possesses the additional advan. tage of low solubility for hydrogen bromide, the evolution of which renders possible the distinction between decolourisation of bromine due to substitution or due to addition. 

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