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Isotope interaction

In a discussion of permeability it is important to recognize that we deal with operational definitions, since the act of measurement influences the state of the system. In your case, applying an electrical potential gradient and performing electrodialysis alter the distribution of ionophore within the membrane. I wonder whether you have attempted to measure permeability by isotopic tracer techniques In this method the distribution of ionophore would not be influenced. Furthermore, information can be obtained on the question of carriers versus channels or pores. It should not be difficult to determine the extent of possible isotope interaction between tracer species and abundant species in the membrane as discussed by Kedem and Essig [J. Gen. Physiol., 48, 1047 (1965)]. Positive isotope interaction would tend to suggest the presence of channels or pores, negative isotope interaction the presence of carriers. [Pg.326]

Explain how mass-dependent and mass-independent isotopic fractionation of oxygen isotopes interact to produce the range of compositions that we observe in cosmochemical materials. [Pg.226]

Bonn, Metselaar and Van der Elsken 17S> discussed the spectra of NOj in various alkali-halide lattices in terms of rotatory motions of the nitrate groups, but Kato and Rolfe 176> have questioned this approach, and prefer isotopic interaction instead. [Pg.72]

The full relation for the chemical potential of the copolymers in the bulk Pbmsh can be obtained from the Flory-Huggins energy of mixing between diblock copolymers A-N and homopolymers P [259, 260], when interaction parameters %AP> %AN, and % (% =%np) are specified. In most experiments brush N-mers and homopolymer P-mers are microstructurally identical and differ only in the isotopic status. Related isotopic interaction parameter % is usually much smaller than parameters yAP and %AN. Assuming [254] Xan=X,m<+X, and neglecting volume fraction of the anchor moieties in the bulk, the expression for pbulk is obtained in the form... [Pg.84]

By regarding the H- and D- molecules as different species with volume fractions and (pj, the random phase approximation [Eq. (23.19)] may be fitted to the data with Xhd as the only adjustable parameter [56-58]. Complementary experiments on polystyrene [61] and poly (dimethyl silox-ane) [62] confirm the existence of a universal isotope effect, arising from the small differences in volume and polarizability between C-H and C-D bonds [63]. Table (23.7) lists typical values of the isotopic interaction parameter for various polymers in the concentration range 0.2 < < 0.8,... [Pg.418]

TABLE 23.7. Isotopic interaction parameter for various polymers. [Pg.418]

The above results raise the important question of how SANS studies are influenced by isotope effects. As explained earlier, initial SANS experiments on polymers relied on analogies with LS, where the limit of zero concentration was required to eliminate inter-chain scattering. Under such conditions, the isotope effect contributes almost insignificantly to the intensity, and this may be illustrated by calculating dX/dfl(0) via Eqs. (23.24) and (23.25) for the sample of 5.0 wt% PSD in PSH as in Section 23.3.1. The inclusion of an isotopic interaction parameter Zhd = 1.8 X 10 " changes dX/d/2(0) to 17.5 cm compared to 17.4 cm calculated from Eq. (23.11) in the absence of isotope effects. Upon recognizing that information on chain statistics could equally weU be obtained from concentrated isotopic mixtures, many experiments were conducted under such conditions in order to enhance the intensity. It is under these conditions that isotope-induced segregation effects are manifested. [Pg.419]

Table 7.4. Typical isotopic interaction parameters for various polymers... Table 7.4. Typical isotopic interaction parameters for various polymers...
This result is strictly valid in the limit of infinite polyion dilutions, a situation for which polyion-polyion interactions are vanishing. For more concentrated solutions one has to take into account isotopic interactions fss when flux equations for both labelled and unlabelled particles are developed. For this point see References [3] and [4]. [Pg.267]

The simplest system exliibiting a nuclear hyperfme interaction is the hydrogen atom with a coupling constant of 1420 MHz. If different isotopes of the same element exhibit hyperfme couplings, their ratio is detemiined by the ratio of the nuclear g-values. Small deviations from this ratio may occur for the Femii contact interaction, since the electron spin probes the inner stmcture of the nucleus if it is in an s orbital. However, this so-called hyperfme anomaly is usually smaller than 1 %. [Pg.1556]

We further make the following tentative conjecture (probably valid only under restricted circumstances, e.g., minimal coupling between degrees of freedom) In quantum field theories, too, the YM residual fields, A and F, arise because the particle states are truncated (e.g., the proton-neutron multiplet is an isotopic doublet, without consideration of excited states). Then, it is within the truncated set that the residual fields reinstate the neglected part of the interaction. If all states were considered, then eigenstates of the form shown in Eq. (90) would be exact and there would be no need for the residual interaction negotiated by A and F. [Pg.158]

Gas-flow counting is a method for detecting and quantitating radioisotopes on paper chromatography strips and thin-layer plates. Emissions are measured by interaction with an electrified wire in an inert gas atmosphere. AH isotopes are detectable however, tritium is detected at very low (- 1%) efficiency. [Pg.439]

At low temperatures unstable adsorption products or reaction intermediates could be trapped. Thus, carbonite CO, ions arise on CO interaction with basic oxygen ions which account for catalytic reaction of isotopic scrambling of CO or thiophene on activated CaO. [Pg.431]

During the operation of nuclear power reactors, which are fuelled with ceramic UO2 fuel rods, the fission of the nuclei leads to die formation of fission products which are isotopes of elements in all of tire Groups of the Periodic Table. The major fission products, present in 1-10% abundance, fall into five groups divided according to the chemical interaction of each product with the fuel ... [Pg.249]

NAA involves the bombardment of the sample with neutrons, which interact with the sample to form different isotopes of the elements in the sample (14). Many of these isotopes are radioactive and may be identified by comparing their radioactivity with standards. This technique is not quite as versatile as XRF and requires a neutron source. [Pg.205]

A typical SSIMS spectrum of an organic molecule adsorbed on a surface is that of thiophene on ruthenium at 95 K, shown in Eig. 3.14 (from the study of Cocco and Tatarchuk [3.28]). Exposure was 0.5 Langmuir only (i.e. 5 x 10 torr s = 37 Pa s), and the principal positive ion peaks are those from ruthenium, consisting of a series of seven isotopic peaks around 102 amu. Ruthenium-thiophene complex fragments are, however, found at ca. 186 and 160 amu each has the same complicated isotopic pattern, indicating that interaction between the metal and the thiophene occurred even at 95 K. In addition, thiophene and protonated thiophene peaks are observed at 84 and 85 amu, respectively, with the implication that no dissociation of the thiophene had occurred. The smaller masses are those of hydrocarbon fragments of different chain length. [Pg.103]

From this expression, it is obvious that the rate is proportional to the concentration of A, and k is the proportionality constant, or rate constant, k has the units of (time) usually sec is a function of [A] to the first power, or, in the terminology of kinetics, v is first-order with respect to A. For an elementary reaction, the order for any reactant is given by its exponent in the rate equation. The number of molecules that must simultaneously interact is defined as the molecularity of the reaction. Thus, the simple elementary reaction of A P is a first-order reaction. Figure 14.4 portrays the course of a first-order reaction as a function of time. The rate of decay of a radioactive isotope, like or is a first-order reaction, as is an intramolecular rearrangement, such as A P. Both are unimolecular reactions (the molecularity equals 1). [Pg.432]

Deuterium occurs naturally, mixed m with plain hydrogen in the tiny proportion of 0.015 percent in other words, plain hydrogen is the more common isotope by a factor of 6,600. Tritium for fusion energy can be created from another nuclear process involving the interaction of the neutron (in the equation above) with lithium ... [Pg.874]


See other pages where Isotope interaction is mentioned: [Pg.134]    [Pg.2096]    [Pg.2772]    [Pg.26]    [Pg.30]    [Pg.92]    [Pg.459]    [Pg.217]    [Pg.134]    [Pg.2096]    [Pg.2772]    [Pg.26]    [Pg.30]    [Pg.92]    [Pg.459]    [Pg.217]    [Pg.1170]    [Pg.1363]    [Pg.1379]    [Pg.1438]    [Pg.1466]    [Pg.1475]    [Pg.2317]    [Pg.181]    [Pg.982]    [Pg.94]    [Pg.418]    [Pg.477]    [Pg.481]    [Pg.360]    [Pg.245]    [Pg.550]    [Pg.238]    [Pg.982]    [Pg.305]    [Pg.1107]    [Pg.177]   
See also in sourсe #XX -- [ Pg.326 ]




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