Titlebook: Natural Microporous Materials in Environmental Technology; P. Misaelides,F. Macá?ek,C. Colella Book 1999 Springer Science+Business Media D

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Catheter

四溢

Interaction of Actinides with Natural Microporous Materials disposal of nuclear industry wastes. The contribution also includes some new data on the interaction of U and Th with granitic biotite and todorokite as well as on the sorption of Pu and Am by Greek and Slovak zeolites and clays.

Anthrp

Experimental Study on the Formation of Heavy Metal Sulphides Using Layer Silicates: Environmental Asfound in the reaction products. Mercury reacted very quickly with S. ions and in the heavy fraction of the reaction products the metacinnabar (HgS) was determined. Several thallium sulphides were obtained: T1S, T1.S (carlinite), T1.S., T1.S. and TlFeS. (raquinite), Cu.Tl.S., Cu.TlS., AgTlS, Ag.Tl.S. and AgTlS..

整理

Pillared Clays: Chemistry and Prospectscesses. Smectites with Al in the tetrahedral layer are the preferred materials for pillaring. Thus, pillared saponite is an excellent acid catalyst. In other catalytic applications and in selective adsorption pillared clays perform well, but cannot yet compete successfully with the available microporous and mesoporous materials.

Generic-Drug

Hg2+ Trapping by Thiol – Functionalised Mesoporous Silica Molecular Sievespared by electrostatic supramolecular assembly, and an uncalcined wormhole -like silica obtained through neutral surfactant assembly. Owing to the presence of a higher concentration of surface hydroxyl groups, the wormhole silica was far more effective for thiol fuctionalisation and heavy metal ion trapping.

agonist

Atomistic Computer Modelling of Chiral Pillared Claysrs, favourable π-stackings lead to clustering of pillars even with homogeneously charged smectites. Long range and/or short range ordering of the isomorphous substitution within the silicate layer strongly influences the interlayer structure, since host-guest interactions are dominated by electrostatics.

燈絲

Distribution of Industrial Minerals in Sardinia (Italy): Clinoptilolite Bearing Rocks of the Logudoroptilolite was the most widespread zeolite, whereas mordenite and chabazite rarely occured. A quantitative evaluation performed by the Reference Intensity Ratio (RIR) and Rietveld methods indicated that about 30% and 44% of samples from pyroclastic flows and epiclastic deposits, respectively, have a zeolite content higher than 50%.

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