976 resultados para 2-mercaptoimidazole silica gel for Hg-II separation


Relevância:

100.00% 100.00%

Publicador:

Resumo:

Sais de diazônio são um classe de compostos amplamente usados em química orgânica. Sua aplicação abrange uma gama de sínteses desde corantes até reações de hetero-acoplamento para produção de fármacos, mas pouco é conhecido de sua redução eletroquímica para fins sintéticos. As metodologias empregadas na redução de sais de diazônio geralmente envolvem o uso de metais ou compostos capazes de transferir elétrons como Pd, Cu ou tetratiafulvaleno. Neste trabalho é descrita a redução eletroquímica de dois sais de diazônio: tetrafluoroborato de 2-(2-propen-1-ilóxi)benzenodiazônio (1) e tetrafluoroborato de 2-(2-propen-1-iltio)benzenodiazônio (2) usando três eletrodos: Pt, Hg e pó de grafite. Quando foi feita a eletrólise de (1) utilizando cátodo de Hg vários produtos foram formados envolvendo uma reação de ciclização intramolecular, porém não conseguimos separá-los pelos métodos cromatográficos. A eletrólise de (2) em condições experimentais similares conduziu a uma mistura complexa de produtos provavelmente devido a uma interação do Hg com o átomo de enxofre do substrato e seus produtos de redução. Usando o cátodo de Pt e sal (1) a reação não foi eficiente pois ocorria uma queda brusca da corrente, provavelmente devido ao bloqueio da superfície do eletrodo. Concernente ao eletrodo de pó de grafite, apenas alguns experimentos preliminares foram feitos, portanto uma análise de seu desemprenho é prematura.

Relevância:

100.00% 100.00%

Publicador:

Resumo:

Resorcinol-Formaldehyde xerogels are organic polymers that can be easily tailored to have specific properties. These materials are composed of carbon, hydrogen and oxygen, and have a surface that is very rich in oxygen functionalities, and is therefore very hydrophilic. Their most interesting feature is that they may have the same chemical composition but a different porous texture. Consequently, the influence of porous characteristics, such as pore volume, surface area or pore size can be easily assessed. In this work, a commonly used desiccant, silica gel, is compared with organic xerogels to determine their rate and capacity of water adsorption, and to evaluate the role of surface chemistry versus porous texture. It was found that organic xerogels showed a higher rate of moisture adsorption than silica gel. Pore structure also seems to play an important role in water adsorption capacity. The OX-10 sample, whose porosity was mainly composed of micro-mesoporosity displayed a water adsorption capacity two times greater than that of the silica gel, and three times higher than that of the totally macroporous xerogel OX-2100. The presence of feeder pores (mesopores) that facilitate the access to the hydrophilic surface was observed to be the key factor for a good desiccant behaviour. Neither the total pore volume nor the high surface area (i.e. high microporosity) of the desiccant sample, is as important as the mesopore structure.

Relevância:

100.00% 100.00%

Publicador:

Resumo:

In the present study, two low generation triazine-based dendrimers, G1.0(Cl)4 dendrimer and G1.5(OH)8 dendrimer, were synthesized and their cytotoxicity were tested by using the NIH 3T3 and the A2780 cell lines. In the synthesis process of the G1.0(Cl)4 dendrimer, cyanuric chloride (CAC) which has high reactivity chlorine atom was connected to the terminal of triethylene glycol (TEG) via nucleophilic substitution by controlling temperature. The prepared G1.0(Cl)4 dendrimer was purified by silica gel column chromatography. Then the four chlorine atoms in the G1.0(Cl)4 dendrimer were substituted by diethanolamine (DEA) to give dendrimer with the hydroxyl terminal group G1.5(OH)8. The starting materials, CAC, G1.0(Cl)4 dendrimer and G1.5(OH)8 dendrimer were analyzed by one-dimensional NMR, FTIR and MS techniques. The two dendrimers, G1.0(Cl)4 and G1.5(OH)8, showed perfect stability in the air environment at room temperature. However, G1.0(Cl)4 is not soluble in water while the G1.5(OH)8 dendrimer is a water soluble compound. Furthermore, cell biological evaluation at the studied concentrations showed that the CAC, as well as the prepared G1.0(Cl)4 and G1.5(OH)8 dendrimers, have no cytotoxicity towards the NIH 3T3 and A2780 cell lines.

Relevância:

100.00% 100.00%

Publicador:

Resumo:

The basement at Ocean Drilling Program (ODP) Sites 677 and 678 originated from the Galapagos spreading center of the Costa Rica Rift and has moved about 200 km over the last 6 m.y. (Fig. 1) (Shipboard Scientific Party, 1987, 1988; Scientific Drilling Party, 1987). Sediments about 300 m thick cover basement so young that basal sediments at Sites 677 and 678 have been reheated up to 60?-70?C at Site 677 and altered to limestone and/or chert (Shipboard Scientific Party, 1988). Sediments from both sites indicate (1) a high sedimentation rate (about 48 m/m.y.) and (2) biogenic silica and carbonate as the main constituents of sediments (Table 1) (Shipboard Scientific Party, 1988). Heatflow observations and measurements of interstitial water chemistry around the sites show that Site 677 is in a lower heatflow zone (166 mW/m**2; 1°12.14'N, 83°44.22'W) whereas Site 678 is located in a zone of higher heat flow (250 mW/m**2; 1°13.01'N, 83°43.39'W) (Langseth et al., 1988; Shipboard Scientific Party, 1988). In the flank hydrothermal systems, circulating solution is moving upward through the sedimentary column in zones of higher heat flow while it is moving downward in zones of lower heat flow (Anderson and Skilbeck, 1981). The chemistry of the interstitial waters is modified by several processes such as (1) diagenetic reactions and (2) advective and (3) diffusive transports of dissolved constituents. Analyses of Ca2+ and Mg2+ in interstitial waters from Sites 677 and 678 show that their profiles are mainly controlled by advective transport (Shipboard Scientific Party, 1988). In contrast, the interstitial-water profiles for NH4+, Si, and PO4[3-] are highly affected by reactions in the sediments. Site 677 offers a good opportunity to investigate amino acids in the interstitial waters because sediments of similar compositions have been deposited at constant rates of sedimentation. There are few previous works on amino acid distributions in interstitial waters (Henrichs and Parrington, 1979; Michaelis et al., 1982; Henrichs et al., 1984; Henrichs and Farrington, 1987; Ishizuka et al., 1988). In this chapter, we report (1) Rock-Eval analysis and (2) the composition of total hydrolyzable and dissolved free amino acids (THAA and DFAA, respectively) in the interstitial waters. Our objectives are to discuss (1) the possible origin of organic materials, (2) the characteristics of THAA and DFAA, and (3) their relationships in interstitial waters.

Relevância:

100.00% 100.00%

Publicador:

Resumo:

Issued Apr. 1922-1945 in 2 parts with separate numbering; Teil II contains treaties and other special materials.

Relevância:

100.00% 100.00%

Publicador:

Resumo:

Atlas to accompany pt. 1, v. 1, has also special t.-p.: Lethaea Palaeozoica, oder Beschreibung und Abbildung der für die einzelnen Abtheilungen der palaeozoischen formation bezeichnendsten Versteinerungen. Von Ferd. Roemer.

Relevância:

100.00% 100.00%

Publicador:

Resumo:

Contiene: T. 1 (1805), T. 2 (1809), T. 3 (1819), T. 4 (1819)

Relevância:

100.00% 100.00%

Publicador:

Resumo:

Contiene: T. I -- T. II.

Relevância:

100.00% 100.00%

Publicador:

Resumo:

Contiene: Tomo I - Tomo II.

Relevância:

100.00% 100.00%

Publicador:

Resumo:

Contiene: T. I: 1e partie. Idéologie proprement dite (An XIII [1804] ; 2 ?ed. ; XXXII, 456 p.) -- T. II: 2e partie. Grammaire (An XI [1803] ; XII, 454 p.) -- T. III: 3e partie. Logique (An XII [1805] ; VIII, 671 p.) -- T. IV: 4e et 5e parties. Traité de la volanté et de ses effects (Vve. Cournier, 1815 ; VI, 578 p.)

Relevância:

100.00% 100.00%

Publicador:

Resumo:

También enc. en 2 v.

Relevância:

100.00% 100.00%

Publicador:

Resumo:

1. sér., I. 1552-1565.--II. 1566.--III. 1567-1572.--IV. 1572-1574.--V. 1574-1577.--VI. 1577-1579.--VII. 1579-1581.--VIII. 1581-1584.--[IX] Supplément. 2. sér., I. 1584-1599.--II. 1600-1625.--III. 1625-1642.--IV. 1642-1650.--V. 1650-1688.

Relevância:

100.00% 100.00%

Publicador:

Resumo:

Available on demand as hard copy or computer file from Cornell University Library.

Relevância:

100.00% 100.00%

Publicador:

Resumo:

8 portraits of the author (clipped from advertisement) mounted on p. [5] of v.1.