Isotope exchange with

Caraculacu et al. [48] also quantitatively determined allylic chlorines in PVC by isotopic exchange with SO Cl2. The selective exchange of chlorine in the polymer was verified by experiments with model compounds. The number of allylic chlorines in PVC was found to be between 0.12 and 0.16 for 100 monomer units. 

Disulfane is usually made from a sulfane mixture known as crude sulfane oil while various methods are available for the preparation of the higher sulfanes. Deuterated sulfanes may be prepared by isotopic exchange with DCl [17]. 

We have previously assumed that the principle diagenetic process is attributable to exchange or interaction of (depleted) browser apatite values with (enriched) sedimentary matrix values (Lee-Thorp and van der Merwe 1987). Another possibility is ionic or isotopic exchange with soil CO2 however in most cases soil CO2 values will be closely related to matrix carbonate values. If the former is the case, one would expect enriched grazer values (near 0%o)... 

Anderson, TE. 1969 Self-diffusion of carhon and oxygen in calcite hy isotope exchange with carhon dioxide. Journal of Geophysical Research 74 3918-3932. 

Haul, RA.W. and Stein, L.H. 1955 Diffusion in calcite crystals on the basis of isotope exchange with carbon dioxide. Faraday Society Transactions 51 1280-1290. 

Figure 1.29. Calculated changes in the S 0 values of volcanic rocks (5 0 = +7.0%c) as a result of equilibrium oxygen isotope exchange with waters of different initial compositions. The dotted areas represent the ranges of rocks in the zeolite and the sericite-chlorite zones (Green et al., 1983).

It has been shown in Section 2.1.4 that methanol adsorbate formed from dilute solutions on a porous Pt surface, consists of COad and COHad in a ratio CO COH of ca. 20-30% [14]. The results of isotopic exchange with bulk CO seem to indicate that only the fraction present as COad can be desorbed and replaced by bulk CO. Probably the same arguments as in the case of pure COad can apply. COHad seems to be more strongly bound to the Pt surface and cannot be desorbed. 

Tetralin. Therefore, either trans-Decalin was formed on the surface of the coal with deuterium from the solvent or gas, or it was formed by isomerization from cis-Decalin with accompanying isotopic exchange with a deuterium source. Because the protium content of the cis-Decalins is much greater than the trans-Decalins, cis-trans isomerization is not very important. 

Synthesis of tritium-labelled brefeldin-A by catalytic isotope exchange with tritium gas... 

On these numerical arguments and on the necessity to avoid isotope exchange with liquids, we based our decision to measure stable isotope ratios in whole wood. 

An Aside Monothermal Isotope Exchange with Chemical Reflux 15 N Enrichment... 

The products of Rayleigh fractionation are effectively isolated from isotopic exchange with the rest of the system immediately upon formation. If the process occurs slowly, such that each increment of product B forms in isotopic equilibrium with the reactant A prior to isolation of B from the system, then would be an equilibrium isotope fractionation factor. However, if the process of formation of B is rapid, incremental formation of B may be out of isotopic equilibrium withH. In this case, would be a kinetic isotope fractionation factor, which may be a function of reaction rates or other system-specihc conditions. 

An important consequence of such a model is that the effect of such sedimentary systems on the ocean Mo isotope budget is not represented by a, but rather by the relative fluxes of the isotopes across the sediment-water interface. This effective fractionation factor, is likely to be smaller than a (Bender 1990 Braudes and Devol 1997) because the diffusive zone acts as a barrier to isotope exchange with overlying waters, approximating a closed system. 

Most hot spring waters have deuterium contents similar to those of local precipitation, but are usually emiched in as a result of isotopic exchange with the country rock at elevated temperatures. The magnitude of the oxygen isotope shift depends on the O-isotope composition of both water and rock, the mineralogy of the rock, temperature, water/rock ratio, and the time of interaction. 

Chemical studies also support the indicated mechanism. For example, the P-oxoacid intermediate formed in step b of Eq. 13-48 or Fig. 13-12 has been identified as a product released from the enzyme by acid denaturation during steady-state turnover.273 274 Isotopic exchange with 3H in the solvent275 and measurement of 13C isotope effects277 have provided additional verification of the mechanism. The catalytic activity of the enzyme is determined by ionizable groups with pKa values of 7.1 and 8.3 in the ES complex.278... 

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