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I Carbonate Chemistry

Since the successful exploration of silver(i) oxide usage as a multifunctional precursor for the synthesis of silver(i) A-heterocyclic carbene complexes, there has been an increasing number of reports related to silver(i) A-heterocyclic carbene chemistry. Silver(i) oxide can act as a weak base to deprotonate imidazolium salts, generating the free A-heterocyclic carbene ligands in situ, which then forms the silver(i) carbene complexes readily. This reaction can take place in the presence of air and moisture, and as a result, no special treatment in regard to the solvents has to be undertaken. More importantly, its basicity is rather specific toward the deprotonation at the G2 position of the imidazole moiety. Exploration of using silver(i) carbonate as a milder precursor in place of silver(i) oxide has also been pursued, but longer reaction times are usually required. [Pg.206]

The carbon-rich stars losing a large amount of mass are a fascinating laboratory for studying carbon chemistry in space. Below, I describe what is known about these stars, and how we can hope to use them to understand the nature of celestial carbon-chemistry. [Pg.64]

The behavior of Rh(I) dpm-bridged complexes offers an interesting counterpoint to the Pd(I) based chemistry. For example carbon monoxide addition to the A-frame Rh2(dpm)2(y-Cl)(C0)2 (15, 25,26) and to the face-to-face dimer Rh2(dpm)2(C0)2Cl2 (27) results in shortening the Rh-Rh separations as shown in reactions (12) and (13). Structural characterization of the common product... [Pg.175]

Of all of the elements of the Periodic Table, only neighboring carbon and boron share the properties of self-bonding (catenation) and the support of electron-delocalized structures based upon these catenated frameworks. Carbon catenation, of course, leads to the immense field of organic chemistry. Boron catenation provides the nido-, arachno-, and /i p/io-boranes, which may be considered as the borane equivalents of aliphatic hydrocarbons, and the discrete families of c/oso-borane derivatives which bear a for nal resemblance to the aromatic hydrocarbons, heterocycles, and metallocenes. Aside from these analogies, boron and carbon chemistries are also important to each other through their extravagant ability to mix m ways not available to other element-pairs. Thus, the conflux of boron and carbon chemistries effectively provides an element-pair for exploitation in a variety of novel ways. [Pg.197]

Figure 9 Comparison of silicate mass fractions. Two assumptions for interior strueture are shown (i) differentiated—rock core, ice mantle, and (ii) homogeneous—uniformly mixed ice and roek. Also shown are silicate mass fractions for the Jupiter and Saturn systems and expected values for two models of the early solar nebula carbon chemistry (see text) (after Johnson et aL, 1987) (reproduced by permission of Ameriean Geophysieal Union from /. Geophys. Res. Space Phys. 1987, 92, 14884-14894). Figure 9 Comparison of silicate mass fractions. Two assumptions for interior strueture are shown (i) differentiated—rock core, ice mantle, and (ii) homogeneous—uniformly mixed ice and roek. Also shown are silicate mass fractions for the Jupiter and Saturn systems and expected values for two models of the early solar nebula carbon chemistry (see text) (after Johnson et aL, 1987) (reproduced by permission of Ameriean Geophysieal Union from /. Geophys. Res. Space Phys. 1987, 92, 14884-14894).
While the Wessling-Zimmermann route is a typical method of polymer synthesis, both PPVs and their corresponding oligomers can be synthesized by the extension of methods used for the synthesis of the easiest building block, stilbene 70 (scheme 13). Conceptionally, this is possible by (i) carbon-carbon double bond formation, for whieh synthetic organic chemistry provides a great number of methods [116], and (ii) by aryl-vinyl coupling [117] some examples of both methods are outlined in scheme 13. [Pg.32]

This book is concerned with an important area of organic (i.e., carbon) chemistry that has developed enormously over the past half-century, yet is still neglected in many organic textbooks. This is the chemistry of compounds in which carbon atoms are covalently bonded to more neighboring atoms than can be explained in terms of classical two-center, electron-pair bonds. Such carbon atoms are referred to as hypercarbon atoms (short for hypercoordi-nated carbon atoms ) because when first discovered, their coordination numbers seemed unexpectedly high. [Pg.2]

Pitman, J.I., 1978. Carbonate chemistry of groundwater from Chalk, Givendale, East Yorkshire. Geochim. Cosmochim. Acta, 42 1885—1897. [Pg.208]

Polysilanes are important as photoresists. I.M.T.Davidson et.al. have identified three pathways in the photodegradation of these species. Sekiguchi et al. have described a potentially valuable new photochemical synthesis of tetramethyldisilene (44) based on irradiation of its 1,4-adduct with benzene. An interesting contrast between silicon and carbon chemistry is provided by the photoisomerisation of the trisilacycloheptene (45) to the corresponding trans isomer (46) (Shimizu et al.). [Pg.575]

I inorganic chemistry I inorganic chemistry is the j chemistry of all other sub- stances other than organic com-I pounds, although it is conve-I nient to include in it such com- mon carbon compounds as are frequentiy encountered e.g. car-t bon dioxide, carbonates or arc essential to placing the element carbon in its correa relationship in the periodic system of classi-i ficadon. [Pg.119]


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