Big Chemical Encyclopedia

Chemical substances, components, reactions, process design ...

Articles Figures Tables About

Simple cations

VEs do not readily enter into copolymerization by simple cationic polymerization techniques instead, they can be mixed randomly or in blocks with the aid of living polymerization methods. This is on account of the differences in reactivity, resulting in significant rate differentials. Consequendy, reactivity ratios must be taken into account if random copolymers, instead of mixtures of homopolymers, are to be obtained by standard cationic polymeriza tion (50,51). Table 5 illustrates this situation for butyl vinyl ether (BVE) copolymerized with other VEs. The rate constants of polymerization (kp) can differ by one or two orders of magnitude, resulting in homopolymerization of each monomer or incorporation of the faster monomer, followed by the slower (assuming no chain transfer). [Pg.517]

Modes of Operation There is a close analogy between sedimentation of particles or macromolecules in a gravitational field and their elec trophoretic movement in an electric field. Both types of separation have proved valuable not only for analysis of colloids but also for preparative work, at least in the laboratoiy. Electrophoresis is applicable also for separating mixtures of simple cations or anions in certain cases in which other separating methods are ineffectual. [Pg.2007]

As diphosphoric acid is tetrabasic, four series of salts are possible though not all are always known, even for simple cations. The most studied are those of Na, K, NH4 and Ca, e.g. ... [Pg.527]

It was noted that, on going from tetrabutylammonium to tetrabutylphosphoni-um, salts with a common anion displayed identical solvation properties. FLence, with these simple cations, the solvent properties are dominated by the choice of anion. It is possible that, had cations with acidic protons, such as triallcylammoni-um and trialkylphosphonium, been included in the study, these may then have also had an influence. [Pg.95]

Some metals are amphoteric. That is, they form simple cations (in acid solutions) and soluble oxyanions (in alkaline solution) only in the mid-pH range is a protective film stable. Since cathodic protection produces alkali at the structure s surface, it is important to restrict the polarisation, and thereby the amount of hydroxyl ion produced, in these cases. Thus both lead and aluminium will suffer cathodic corrosion under cathodic protection if the potential is made excessively electro negative. [Pg.122]

In previous chapters we have referred from time to time to compounds of the transition metals. Many of these have relatively simple formulas such as CuSO CrCI3, and FetNO These compounds are ionic The transition metal is present as a simple cation (Cu2+, Cr3+, Fe3+). In that sense, they resemble the ionic compounds formed by the main-group metals, such as CaS04 and AKNOJ ... [Pg.409]

When a complex ion is formed from a simple cation, the electron pairs required for bond formation come solely from the ligands. Reactions such as these, in which one species donates an electron pair to another, are referred to as Lewis acid-base reactions. In particular—... [Pg.410]

When A0 is small, the electron distribution is the same as in the simple cation if A is large, Hund s rule is not strictly followed. [Pg.419]

In the Brpnsted picture, the acid is a proton donor, but in the Lewis picture the proton itself is the acid since it has a vacant orbital. A Brpnsted acid becomes, in the Lewis picture, the compound that gives up the actual acid. The advantage of Lewis theory is that it correlates the behavior of many more processes. For example, AICI3 and BF3 are Lewis acids because they have only 6 electrons in the outer shell and have room for 8. Both SnCU and SO3 have eight, but their central elements, not being in the first row of the periodic table, have room for 10 or 12. Other Lewis acids are simple cations, like Ag. The simple reaction A + B- A—B is not very common in organic chemistry, but the scope of the Lewis picture is much larger because reactions of the types... [Pg.339]

The ionic model describes a number of metal halides, oxides, and sulfides, but it does not describe most other chemical substances adequately. Whereas substances such as CaO, NaCl, and M 2 behave like simple cations and anions held together by electrical attraction, substances such as CO, CI2, and HE do not. In a crystal of Mgp2, electrons have been transferred from magnesium atoms to fluorine atoms, but the stability of HE molecules arises from the sharing of electrons between hydrogen atoms and fluorine atoms. We describe electron sharing, which is central to molecular stability, in Chapters 9 and 10. [Pg.552]

Simple cations are unknown within Group 16 (besides Po), but several highly colored polyatomic cations (cationic clusters), like S " ", Sg, Se, SCg, Te, and Teg" ", have been isolated in non-aqueous media [15]. Some mixed chalcogen cationic clusters have also been reported. These are all unstable in water. [Pg.15]

Yet the view that the rates of electron transfer in simple reactions are principally independent of the electrode metal (which for some time had been current in the electrochemical literature) cannot be maintained in this strict form. Many experimental data relating to the exchange current densities of reactions involving simple cations (such as Fe and Fe ) provide evidence that the electrode metal does exert a rather strong influence on the reaction rates. [Pg.262]

The various types of Lewis acids are protons, simple cations, electron-deficient molecules, compounds in which the central atom can expand its octet, and elements with an electron sextet. [Pg.592]

In many other situations of donor-acceptor solutes in aprotic solvents, such as quaternary alkylammonium salts (R4NX), a UV absorption shift to higher wavelength has proved the occurrence of simple cation-anion ion... [Pg.271]

An essential requirement for such stabilisation is that the carbocation should be planar, for it is only in this configuration that effective delocalisation can occur. Quantum mechanical calculations for simple alkyl cations do indeed suggest that the planar (sp2) configuration is more stable than the pyramidal (sp3) by = 84 kJ (20 kcal) mol-1. As planarity is departed from, or its attainment inhibited, instability of the cation and consequent difficulty in its formation increases very rapidly. This has already been seen in the extreme inertness of 1-bromotriptycene (p. 87) to SN1 attack, due to inability to assume the planar configuration preventing formation of the carbocation. The expected planar structure of even simple cations has been confirmed by analysis of the n.m.r. and i.r. spectra of species such as Me3C SbF6e they thus parallel the trialkyl borons, R3B, with which they are isoelectronic. [Pg.104]

A major factor influencing the stability of less simple cations is again the possibility of delocalising the charge, particularly where this... [Pg.104]

Our work on the bifunctional activation of CO insertion was prompted by the thought that strong molecular Lewis acids should be more effective and more general than simple cations. It already had been observed that molecular Lewis acids would promote a molecular Fischer-Tropsch type reaction (5), and that iron diene complexes can be converted to polycyclic ketones by the action of aluminum halides, equation 7,(18), but information on the course of these reactions was sketchy. [Pg.12]

The most common simple cations in the soil solution are calcium (Ca2+), magnesium (Mg2+), potassium (K+), and sodium (Na+). Other alkali and alkaline-earth elements, when present, will be as simple cations also. Iron, aluminum, copper, zinc, cobalt, manganese, and nickel are also common in soil. Iron is present in both the ferrous (Fe2+) and ferric (Fe3+) states, while aluminum will be present as Al3+. Copper, zinc, cobalt, and nickel can all be present in one or both of their oxidations states simultaneously. Manganese presents a completely different situation in that it can exist in several oxidation states simultaneously. [Pg.120]

Simple cations are those that exist only in one oxidation state in soil and are mostly associated with water, although they may also be chelated and form other associations with inorganic and organic components. [Pg.136]

Another simple cation occurring commonly in soil is ammonium (NFLC). Because of the unique role and chemistry of nitrogen and nitrogen species in soil, it is discussed separately in Section 6.3 [5,6],... [Pg.136]

Examples of cations that are present in significantly lower concentrations than the simple cations are iron, manganese, zinc, copper, nickel, and cobalt. Except for cobalt, these have multiple oxidations states in soil as shown in Table 6.1. Because of their multiple oxidation states, they may be present as many more species than the simple cations. Typically, the higher oxidation states predominate under oxidizing conditions, while the lower oxidation states predominate under reducing conditions. However, it is common to find both or all oxidation states existing at the same time in either aerobic or anaerobic soil [7,8],... [Pg.137]

Many important soil components are not present as simple cations or anions but as oxyanions that include both important metals and nonmetals. The most common and important metal oxyanion is molybdate (Mo042 ). The most common and important nonmetal oxyanions are those of carbon (e.g., bicarbonate [HC03 ] and carbonate [C032-]), nitrogen (e.g., nitrate [N03 ] and nitrite [NQ2 ]), and phosphorus (e.g., monobasic phosphate [H2P04 ], dibasic... [Pg.140]

The next generalization, number 3 above, has to do with the notion that two simple cations will react with one another less rapidly than a cation and an anion of corresponding size would. Table I presents examples from the literature, where, in every case, a proton reacts with species of different charge types, and there is a steady decrease in the rate of reaction as one proceeds from top to bottom in that table. [Pg.71]

Simonetta and Heilbronner (1964) recently carried out calculations by the valence bond (VB) method for some simple cations, and compared the results obtained by this method, inter alia, with the results of Colpa and collaborators (1963) and of Koutecky and Paldus (1963). In the case of the proton addition complexes of mesitylene and cyclohepta-triene, the electron excitation energies calculated by the VB method agree very well with experiments, and also agree to a good approximation with the results of Cl calculations. The calculations also successfully reproduce the electron density of the cycloheptatriene cation. In this, a perturbation calculation allowed for the AO s adjoining the —CHg—CH2-lihkage. [Pg.297]

The addition of a cryptand to some polyelectrolytes leads to significant increases in conductivity and in some cases IR and Raman spectroscopy demonstrate that the cryptand breaks up the ion-ion interactions (Chen, Doan, Ganapathiappan, Ratner and Shriver, 1991 Doan, Ratner and Shriver, 1991). Apparently the reduction of ion association more than offsets the reduction in mobility of the cation-crypt complex, which has a larger effective radius than the simple cation. It is also possible that the cryptand-ion complex is rendered more mobile by the reduction of polymer-cation complex formation, but this point has not been investigated in any detail. [Pg.115]


See other pages where Simple cations is mentioned: [Pg.68]    [Pg.506]    [Pg.290]    [Pg.91]    [Pg.80]    [Pg.1088]    [Pg.480]    [Pg.161]    [Pg.409]    [Pg.107]    [Pg.339]    [Pg.17]    [Pg.303]    [Pg.46]    [Pg.459]    [Pg.213]    [Pg.419]    [Pg.132]    [Pg.136]    [Pg.478]    [Pg.157]    [Pg.328]    [Pg.468]   
See also in sourсe #XX -- [ Pg.119 ]




SEARCH



Cations naming simple

Hydration of Simple Cations and Anions

Reactions Catalysed by Simple Cationic Micelles

Simple Cation Adsorption from Solution

Simple Cationic Exchange

Simple cations extraction

© 2024 chempedia.info