Reaktionen monovalenter Münzmetalle in flüssigem Ammoniak

Im Rahmen dieser Arbeit konnten erstmals eine Reihe von Ammoniakaten von Münzmetallhalogeniden (M(I)Hal) und Pseudohalogeniden aus flüssigem Ammoniak in einkristalliner Form isoliert und strukturell charakterisiert werden. Mit dem Ammoniakat des Gold(I)-iodids wurden Metathesen in flüssigem Ammoniak durchgeführt, die die Isolierung einiger sehr thermolabiler, teilweise explosiver Alkoholate des Golds ermöglichten. Die Bestimmung der Kristallstruktur eines Gold(I)-phenolates erlaubte erste Einblicke in deren Aufbau.rnIn der Reihe der Ammoniakate der M(I)Hal mit Ausnahme von Silberiodid, werden keine direkten Metall-Halogen-Kontakte ausgebildet. Die Ammoniakate der Chloride und Bromide des Kupfers und Silbers sowie des Kupferiodids besitzen isotype Strukturen. Sie liegen als Trisammoniakate [M(NH3)3]Hal vor. Im Ammoniakat von Silberiodid besitzen die Silberionen durchgängig die Koordinationszahl 4. Neben Ag•••NH3- findet man auch direkte Kationen-rnAnionen-Kontakte und sehr kurze Ag(I)-Ag(I)-Abstände. Das Goldkation im Ammoniakat von Goldiodid besitzt die Koordinationszahl 2 und wird ausschließlich durch Ammoniakmoleküle koordiniert. Die gebildeten H3N-NH3-Hanteln werden über aurophile Wechselwirkungen verknüpft.rn rnDie Ammoniakate der Cyanide von Silber und Gold, enthalten molekulare Baueinheiten des Typs:(H3N)nMCN [(n= 1 für M= Au und n= 2 für M= Ag].rnrnAnders als bei den solvatfreien Homologen wird eine Ausbildung von Polymerketten nicht beobachtet. Das linear aufgebaute Ammoniakat von Goldcyanid ermöglicht die Ausbildung von aurophilen Wechselwirkungen. Metallophile Wechselwirkungen zwischen dem als Dimer vorliegenden Ammoniakat von AgCN scheinen nicht ausgebildet zu werden.rnrnMetatheseversuche von Goldiodid mit einem Amid und diversen Alkanolaten lieferten teilweise explosive Produkte. Es ist davon auszugehen, dass mit zunehmender Basizität der eingesetzten Anionen, die an das Gold(I)-ion koordinierten Ammoniakmoleküle deprotoniert werden und explosives Goldamid gebildet wird. Der als zweites Produkt entstehende Alkohol kann ebenfalls ein Ammoniakat bilden. Im Fall von Li-Fencholat wird ein solches in Form sehr tiefschmelzender Einkristalle erhalten.rnrnDa die Deprotonierung der an Gold koordinierten Ammoniakmoleküle unweigerlich zu explosiven oder sehr instabilen Produkten führt, wurde die geringere Basizität der Phenolate ausgenutzt, um dies zu umgehen. Im Falle der Umsetzung von AuI mit Li-2,6-di-tert.-butylphenolat gelang tatsächlich die Isolierung eines kristallinen Gold(I)-phenolats.rn

THERMORESPONSIVE PROPERTIES OF GOLD HYBRID NANOPARTICLES OF POLY(DI(ETHYLENE GLYCOL) METHYL ETHER METHACRYLATE) (PDEGMA) AND ITS BLOCK COPOLYMERS WITH DIFFERENT ANCHORING REGIMES

Thermo-responsive materials have been of interest for many years, and have been studied mostly as thermally stimulated drug delivery vehicles. Recently acrylate and methacrylates with pendant ethylene glycol methyl ethers been studied as thermo responsive materials. This work explores thermo response properties of hybrid nanoparticles of one of these methacrylates (DEGMA) and a block copolymer with one of the acrylates (OEGA), with gold nanoparticle cores of different sizes. We were interested in the effects of gold core size, number and type of end groups that anchored the chains to the gold cores, and location of bonding sites on the thermo-response of the polymer. To control the number and location of anchoring groups we using a type of controlled radical polymerization called Reversible Addition Fragmentation Transfer (RAFT) Polymerization. Smaller gold cores did not show the thermo responsive behavior of the polymer but the gold cores did seem to self-assemble. Polymer anchored to larger gold cores did show thermo responsivity. The anchoring end group did not alter the thermoresponsivity but thiol-modified polymers stabilized gold cores less well than chains anchored by dithioester groups, allowing gold cores to grow larger. Use of multiple bonding groups stabilized the gold core. Using block copolymers we tested the effects of number of thiol groups and the distance between them. We observed that the use of multiple anchoring groups on the block copolymer with a sufficiently large gold core did not prevent thermo responsive behavior of the polymer to be detected which allows a new type of thermo-responsive hybrid nanoparticle to be used and studied for new applications.

A Study of the Effect of Oxygen on the Rate of Dissolution of Gold in Cyanide Solutions.

The accepted chemical reactions in the dissolution of gold by cyanide solutions require the presence of gold, cyanide, water, and oxygen. The importance of dissolved oxygen in cyanide solutions as a factor is recognized by those familiar with cyanidation. Manufacturers of cyanidation equipment realize the necessity of oxygen, as shown by the appliances they have developed which are attached to the agitators in order to saturate the cyanide solutions with air.

The Effect of Temperature on the Rate of Dissolution of Gold in Cyanide Solutions which have a Constant Oxygen Content.

Since the development of cyanidation into a highly efficient process for treating gold ores, many papers have been written on its various aspects. Although, there has been much work done on it, the chemistry of the reaction is not yet completely understood.

The Crystal Chemistry of Holtite

Holtite, approximately (Al,Ta,square)Al(6)(BO(3))(Si,Sb(3+),As(3+))(Sigma 3)O(12)(O,OH,square)(Sigma 3), is a member of the dumortierite group that has been found in pegmatite, or alluvial deposits derived from pegmatite, at three localities: Greenbushes, Western Australia; Voron'i Tundry, Kola Peninsula, Russia; and Szklary, Lower Silesia, Poland. Holtite can contain >30 wt.% Sb(2)O(3), As(2)O(3), Ta(2)O(5), Nb(2)O(5), and TiO(2) (taken together), but none of these constituents is dominant at a crystallographic site, which raises the question whether this mineral is distinct from dumortierite. The crystal structures of four samples from the three localities have been refined to R(1) = 0.02-0.05. The results show dominantly: Al, Ta, and vacancies at the Al(1) position; Al and vacancies at the Al(2), (3) and (4) sites; Si and vacancies at the Si positions; and Sb, As and vacancies at the Sb sites for both Sb-poor (holtite I) and Sb-rich (holtite II) specimens. Although charge-balance calculations based on our single-crystal structure refinements suggest that essentially no water is present, Fourier transform infrared spectra confirm that some OH is present in the three samples that could be measured. By analogy with dumortierite, the largest peak at 3505-3490 cm(-1) is identified with OH at the O(2) and O(7) positions. The single-crystal X-ray refinements and FTIR results suggest the following general formula for holtite: Al(7-[5x+y+z]/3)(Ta,Nb)(x)square([2x+y+z]/3)BSi(3-y)(Sb,As)(y)O(18-y-z)(OH)(z), where x is the total number of pentavalent cations, y is the total amount of Sb + As, and z <= y is the total amount of OH. Comparison with the electron microprobe compositions suggests the following approximate general formulae Al(5.83)(Ta,Nb)(0.50)square(0.67)BSi(2.50)(Sb,As)(0.50)O(17.00)(OH)(0.50) and Al(5.92)(Ta,Nb)(0.25)square(0.83)BSi(2.00)(Sb,As)(1.00) O(16.00)(OH)(1.00) for holtite I and holtite II respectively. However, the crystal structure refinements do not indicate a fundamental difference in cation ordering that might serve as a criterion for recognizing the two holtites as distinct species, and anion compositions are also not sufficiently different. Moreover, available analyses suggest the possibility of a continuum in the Si/(Sb + As) ratio between holtite I and dumortierite, and at least a partial continuum between holtite I and holtite II. We recommend that use of the terms holtite I and holtite II be discontinued.

Carbon chemistry of ODP Leg 105 sites

The quantity and quality of organic carbon of Eocene to Holocene sediments from ODP Sites 645, 646, and 647 were investigated to reconstruct depositional environments. Results were based on organic-carbon and nitrogen determinations, Rock-Eval pyrolysis, and kerogen microscopy. The sediments at Site 645 in Baffin Bay are characterized by relatively high organic-carbon values, most of which range from 0.5% to almost 3%, with maximum values in the middle Miocene. Distinct maxima of organic-carbon accumulation rates occur between 18 and 12.5 Ma and between 3.4 and 0 Ma. At Sites 646 and 647 in the Labrador Sea, organic-carbon contents vary between 0.1% and 0.75%. Cyclic 'Milankovitch-type' changes in organic-carbon deposition imply climate-controlled mechanisms that cause these fluctuations. The composition of organic matter at Site 645 is dominated by terrigenous components throughout the entire sediment sequence. An increased content of marine organic carbon was recorded only in the late-middle Miocene. At Sites 646 and 647, the origin of the organic matter most probably is marine. Oceanic paleoproductivity values were estimated, based on the amount of marine organic carbon. During most of the Neogene time interval at Site 645, productivity was low, i.e., similar or less than that measured in Baffin Bay today. Higher values of up to 150 (200) gC/m**2/y may have occurred only in the Miocene. At Sites 646 and 647, mean paleoproductivity values vary between 90 and 170 gC/m**2/y; i.e., these are also similar to those measured in the Labrador Sea today. Lower values of 40 to 70 gC/m**2/y were estimated for the early Eocene and (middle) Miocene.