Rubidium salts

The collector contains an electrically-heated rubidium salt used as the thermionic source. During the elution of a molecule of a nitrogen compound, the nitrogen is ionized and the collection of these ions produces the signal. The detector is very sensitive but Its efficiency is variable subject to the type of nitrogen molecule, making quantification somewhat delicate. 

Since, in both these reactions (i.e. KI or Rbl and Agl), product formation occurs on both sides of the original contact interface, it is believed that there is migration of both alkali metal and silver ions across the barrier layer. Alkali metal movement is identified as rate limiting and the relatively slower reaction of the rubidium salt is ascribed to the larger size and correspondingly slower movement of Rb+. The measured values of E are not those for cation diffusion alone, but include a contribution from... 

It is a pyrophoric and treacherously shock-sensitive explosive, especially as the dry black form. It will deflagrate under nitrogen or argon when scratched with a spatula, and ignites in contact with poly(chlorotrifluoroethylene), (Fluorolube). The caesium and rubidium salts are not shock-sensitive but will deflagrate on friction and are... 

Yamaguchi and coworkers have found that proline rubidium salts catalyze the asymmetric Michael addition of nitroalkanes to prochiral acceptors. When (25)-L-prolines are used, acyclic ( )-enones give (S)-adducts. Cyclic (Z)-enones give (R)-adducts predominantly (Eq. 4.139).203 Recently, Hanessianhas reported that L-proline (3 7% mol equiv) and 2,5-dimethylpiperazine are more effective to induce catalytic asymmetric conjugate addition of nitroalkanes to cycloal-kanones.204... 

The trimolybdates in the solid state are polymeric in nature (119, 120). Two different structure types are obtained as the potassium and rubidium salts K2[Mo3Oi0] and Rb2[Mo3Oi0] H20 shown in Fig. 14. The rubidium compound consists of a chain of Mo06 octahedra, whereas the potassium compound comprises edge-shared distorted Mo05 poly-hedra and Mo06 octahedra (121). 

The metal fulminates are all powerfully explosive. Of several salts examined, those of cadmium, copper and silver were more powerful detonators than mercury fulminate, while thallium fulminate was much more sensitive to heating and impact. Formally related salts are also explosive [1]. Sodium, potassium, rubidium and caesium fulminates are all easily detonated by feeble friction or heat. They all form double salts with mercury(II) fulminate which also explode readily, that of the rubidium salt at 45 °C [2],... 

Only a few group 1 and 2 metal derivatives of selenolates have been structurally characterized. They are prepared with the same methods used for the thiolates.155,158 At present there are no crystal structures of lithium terphenyl selenolates. However, the potassium and rubidium salts, which are dimeric, have been structurally characterized.155 They are isomorphous, both to each other and to the closely related thiolate analogues.1533 Currently, there are no reported terphenylselenolates reported for the alkaline-earth metals. 

In a series of reports between 1991 and 1997 Yamaguchi showed that rubidium salts of L-proline (9) catalysed the conjugate addition of both nitroalkanes [29, 30] andmalonates [31-33] to prochiral a,p-unsaturated carbonyl compounds in up to 88% ee (Scheme 1). Rationalisation of the selectivities observed involved initial formation of an iminium ion between the secondary amine of the catalyst and the a,p-unsaturated carbonyl substrate. Subsequent deprotonation of the nucleophile by the carboxylate and selective delivery using ion pair... 

A quite new type of antibiotic and one of the few naturally-occurring boron compounds is boromycin (86). Hydrolytic cleavage of D-valine with the M(7) hydroxides gave caesium and rubidium salts of this antibiotic, and crystal structure analysis established the formula as (XIIT). The rubidium ion is irregularly coordinated by eight oxygen atoms. Experiments with models showed that the cation site would be the natural place for the—NH3+ end of the D-valine residue, and the whole structure raises the possibility that transport of larger alkali metals is related to the N-ends of peptides and proteins. 

Rubidium metal and its salts bave very few commercial apphcations. They are used in research involving magnetohydrodynamics and thermoionic experiments. Rubidium is used in pbotocells. The metal also is a getter of oxygen in vacuum tubes. The beta-emitter rubidium -87 is used to determine age of some rocks and minerals. Radioisotopes of rubidium have been used as radioactive tracers to trace the flow of blood in the body. The iodide salt treats goiters. Rubidium salts are in pharmaceuticals as soporifics, sedatives, and for treating epilepsy. 

Cesium chlorostannate, Cs2SnCl6, more insoluble than the rubidium salt, precipitates before any rubidium starts to precipitate. Under such controlled addition of stannic chloride, potassium chloride remains in solution in chloride form. Rubidium chlorostannate complex, on thermal decomposition, forms rubidium chloride, RbCl. 

Rubidium carbonate is used in special glass and in fiber optics. It enhances stability and durability of glass, reducing its conductivity. It also is used in the preparation of Rb metal and other rubidium salts. 

Rubidium chloride is used in preparing rubidium metal and many rubidium salts. Also, it is used in pharmaceuticals as an antidepressant and as a density-gradient medium for centrifugal separation of viruses, DNA, and large particles. Other applications are as an additive to gasoline to improve its octane number and as a catalyst. 

The preparation of this substance from silver 0-alumina is similar to the preparation of lithium 0-alumina. The melt consists of 10 g of rubidium chloride. The exchange temperature is 800°. For crystals 2 mm in diameter it takes about 16 hours to reach 99% of equilibrium. The rubidium salts used should contain less than 0.02% potassium and less than 0.1% sodium. After decantation of the melt the crystals are washed with water containing 2% propylamine or ethylenediamine to remove residual potassium salts and silver chloride. They are dried at 200°. The rubidium 0-alumina crystals contain less than 0.05 wt % silver. 

Precipitate with aq. ammonia. Evaporate the soln. down to about 100 c.c., and filter the ot liquid so as to remove calcium sulphate. The cone. soln. is sat. with ammonium alum and allowed to stand for some time. The mixed crystals of potassium, rubidium, and oeesium alums and of lithium salt are dissolved in 100 c.c. of distilled water and recrystal-lized. The recrystallization is repeated until the crystals show no spectroscopic reaction for potassium or lithium. The yield naturally depends on the variety of lepidolite employed. 100. grms of an average sample gives about 10 grms. of crude crystals and about 3 grms. of the purified caesium and rubidium alums. For the purification of caesium and rubidium salts, see the chlorides. The mother-liquors are treated with an excess of barium carbonate, boiled, and filtered. The filtrate is acidified with hydrochloric acid, and evaporated to dryness. The residue is extracted with absolute alcohol in which lithium chloride is soluble, and the other alkali chlorides are sparingly soluble. 

R. Bunsen, H. Erdmann, and others 15 have made rubidium hydrosulphate, RbHS04. It is obtained by heating the rubidium salt of a volatile acid with sulphuric acid to about 250°-257° the oily liquid, on cooling, forms a crystalline mass of this salt. R. Bunsen made caesium hydrosulphate, CsHS04, by treating caesium carbonate with sulphuric acid under similar conditions. Both salts crystallize from water in rhombic, crystals. 

The principal rubidium salts which would probably have been present in the sediment (chloride, sulfate, bicarbonate, etc.) are all soluble in water. As discussed later, the red clay was thoroughly dialyzed prior to use (including prior to analysis by emission spectroscopy). Any rubidium salts initially present in the clay samples would, therefore, have been removed by the dialyzing solution. Hence, it was assumed that the rubidium concentration given in Table I represented sorbed rubidium which had been in equilibrium with the rubidium in the original interstitial seawater. Then when calculating distribution coefficients from experimental data, the concentration given in Table I was used as the initial clay-phase rubidium concentration, rather than zero as used with most of the other species studied. 

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