The influence of solvents on the redox behaviour of bistriphenylphosphinomercury perchlorate has been investigated by polarographic, voltammetric and potentiometric methods. The electrode process was found to be reversible in acetonitrile, propylene carbonate, N,N-dimethylformamide and dimethyl sulfoxide. An irreversible process was observed in nitromethane employing the dropping mercury electrode as well as in N,N-dimethylthioformamide and N-methyl-2-thiopyrrolidinone employing the rotating platinum electrode. Half wave potentials and diffusion coefficients have been measured. A linear relationship between theE1/2 and the donor number (DN) of the solvent has been found for the reversible electrode reactions. Ligand replacement occurs in N,N-dimethylthioformamide and N-methyl-2-thiopyrrolidinone.Mit 1 Abbildung 相似文献
The 18-methylene-1,2-dehydroaspidospermidine (III) was stereospecifically transformed into the schizozygane alkaloid strempeliopine (II) in 16,6 % overall yield. 相似文献
Water-soluble and insoluble, organic and inorganic, natural and man-made aerosol particles participate in vapor-liquid, vapor-solid (ice), and liquid-solid phase transitions in the atmosphere. Hydrosol particles (aerosol particles that have been transferred into water droplets) nucleate ice through freezing. A small without scavenging or being scavenged by another aerosol particle. It is also difficult to imagine that pure mineral particles can be lifted from soil surfaces. In view of this, an ice-nucleating site may be a much smaller particle attached to a larger clay particle. To this category belong, e.g., silver iodide-clay mixed particles. Limited studies indicate that decaying leaves and forest litter under the surface of soils are a potential source of biogenic ice-forming nuclei but that their contribution to the atmosphere is very limited. Research should be directed to study possible relations between cloud condensation nuclei and ice-forming nuclei derived from natural organic compounds (terpenes, leaf-derived nuclei, bacteria, etc.).
A balance must be maintained between large cloud chambers, in which duplication of in-cloud processes is possible, and the special instrumentation which provides information about the modes of ice nucleation on aerosol particles. The two modes of instrumentation should supplement each other.
The greatest difficulty in attempting to make a comparison between the number of ice-forming nuclei estimated in the laboratory and the number in a cloud is the lack of knowledge of the time-temperature-humidity history of the aerosol particles. In nature, the ability of an aerosol particle to nucleate ice may be destroyed or“poisoned“ in the presence of pollutants. An aerosol particle may, on the other hand, become an activated or warmer ice-forming nucleus, e.g.,after the sublimation of ice once formed on it. The temperature of ice nucleation is not a singular property of a particle; the warmest temperatures of ice nucleation of, e.g., particles of a certain soil 10cm in diameter are-15°C,-10°C, and-8°C for nucleation through freezing, condensation followed by freezing and contact, respectively (ref.26). The progress made in instrumentation permits studies of the modes of ice nucleation. Understanding the physical and chemical processes taking place in clouds makes estimates of the rates of ice particle formation more realistic (Young [ref.157]).
The reader should examine two previous reviews written by Mossop (1963) and Montefinale . (1971) for a more complete list of references. 相似文献
Zusammenfassung Zwecks Kristallisation von Carbonat-Apatiten wurden Hydrothermalreaktionen sowie Schmelzvorgänge bei Gemischen von Calciumphosphaten und Calcit untersucht. Die vorliegenden Produkte konnten mit analytischen, kristallchemischen und elektronenmikroskopischen Beobachtungen und Messungen als Einkristalle von Hydroxyl- bzw. Fluorapatit identifiziert werden mit einem Carbonatgehalt, der in der Kristallstruktur eingelagert ist.Mit 4 AbbildungenUnter Mitarbeit vonHelga Schmidt. Vortrag auf der Jahrestagung des Vereins Österreichischer Chemiker, Wien 1962. 相似文献
The conceptual basis and main results of a new model of the dissociative electrical double layer augmented with Lubetkin-Middleton-Ottewill (LMO) dissociative law are summarized. The main results are: the derivation of fundamental limiting laws of planar repulsions in the limit of surface contact, and their transition to the Debye-Hückel limiting laws at infinite separation; the prediction of stronger and longer-range electrostatic forces, quantitatively and consistently accounting for repulsions in colloidal montmorillonites; the discovery of the classical Debye-Hückel interionic effect being operative in increasing double-layer dissociation by lowering the activities of diffuse ions via the LMO law; the prediction of maxima of Stern potentials in spherical symmetry without any further assumptions, and the prediction of no maxima for platelike montmorillonites. In the light of these new insights, the concepts of "hydration forces" and other close-range "non-DLVO" forces may need to be revised, as well as the origin of the maxima of electrophoretic mobilities (Stern potentials) for spherical colloids. 相似文献
Résumé On a préparé des monocristaux de copolymères biséquencés polyoxyéthylène-polystyrène (POE-PS) à partir de leurs solutions diluées, qui peuvent contenir jusqu'à 55% de PS. Les principales formes de ces cristaux et leurs variantes morphologiques, observées sous microscope optique, sont décrites et rattachées à la maille cristallographique du POE. On présente aussi quelques exemples de monocristaux obtenus par ensemencement, dans lesquels les différentes formes se succèdent par filiation; on discute les transitions des formes et leur dépendance vis à vis des conditions de cristallisation.La cristallisation de ces copolymères provoque généralement un fractionnement en composition, car la proportion de PS dans les cristaux est limitée. On propose deux modèles de structure différents, dans lesquels une ou deux couches cristallines de POE en configuration repliée sont recouvertes par le PS amorphe. Le processus de fractionnement est interprété à partir de ces deux structures en admettant une extension critique pour les séquences de PS, dont l'une des extrémités est ancrée sur la surface des repliements du POE.
Summary Single crystals of copolymers, composed of one Poly(ethylene-oxide), (POE), and one Polystyrene (PS) block, (which may contain 55% of PS, by weight), have been prepared from dilute solutions. The principal crystal habits and their morphological variations, as observed with an optical microscope, are described and related to the unit cell of POE. Single crystals grown from various types of seeds, in which different external habits succeed one another, are also shown. Transitions of crystal habits and their dependence on crystallisation conditions are discussed in some detail.Generally, crystallisation of these copolymers produces some fractionation with respect to composition, for only a limited fraction of the initial PS can enter into the crystal. Two different crystal structures are proposed in which a single, or a double crystalline layer of folded POE is covered by amorphous PS. The fractionation process is interpreted on the basis of these two structural models, assuming a critical extension of the PS blocks anchored at one end to the fold surface of PEO.
Zusammenfassung Einkristalle von Copolymeren aus einem Polyäthylenoxyd (PEO) und Polystyrol (PS)-Block, die gewichtsmäßig 55% PS enthalten können, wurden aus verdünnten Lösungen präpariert. Der grundsätzliche Charakter der Kristalle und ihre morphologischen Variationen, wie es in einem optischen Mikroskop beobachtet wird, ist beschrieben und mit der Elementarzelle PEO in Beziehung gebracht. Einkristalle, entstanden aus verschiedenen Typen von Kristallkeimen, in welchen verschiedene äußere Formen auftreten, die aufeinanderfolgen, werden gezeigt. Die übrigen Kristallformen und ihre Abhängigkeit von den Kristallisationsbedingungen werden im einzelnen diskutiert.Im allgemeinen verursacht die Kristallisation dieser Copolymeren gewisse Fraktionierung hinsichtlich der Zusammensetzung, da nur eine begrenzte Menge des ursprünglichen Polystyrols in den Kristall eintreten kann. Zwei verschiedene Kristall-Strukturen werden vorgeschlagen, in denen bzw. eine oder zwei Schichten von gefaltetem PEO mit amorphem Polystyrol bedeckt ist. Der Fraktionierungsprozeß wird auf Grund dieser zwei Struktur-Modelle interpretiert, die eine kritische Größe der PS-Blöcke, verankert an einem Ende der gefalteten Oberfläche von PEO, annehmen.
The condensation of 3.4-dimethyl-3-pyrrolin-2-one with p-methyl-, p-chloro-benzaldehyde and ferrocenealdehyde yields theZ-andE-isomers of the corresponding condensates. Due to kinetic control theZ-isomers are obtained almost exclusively in this reaction. TheE-isomers of the two firstmentioned products can be produced by photochemical isomerization. The structures (tautomeric forms) and configurations of the isomers were established by the Lanthanide-induced-shift-technique and by evaluating the Nuclear-Overhauser-Effect. 相似文献
Herein, we report a stereospecific E-olefin dipeptide isostere synthesis that can be used to make gram quantities of the Phe-Phe isostere desired for eliminating a specific backbone H-bond donor and acceptor in the Alzheimer's disease related Abeta peptide. The Phe19-Phe20 E-olefin analogue of Abeta(1-40) was prepared by solid-phase peptide synthesis and was subjected to amyloidogenesis conditions. This analogue can aggregate into spherical morphologies but does not progress on to form protofibrils or fibrils as is the case for the all-amide sequence, providing insight into the structural requirements for amyloidogenesis. 相似文献
Zusammenfassung Es werden Messungen des dielektrischen Verlustes tan im Temperaturbereich von 1 bis 80 °K und bei verschiedenen Frequenzen zwischen 10 Hz und 10 kHz an einer Reihe von Polymeren mitgeteilt.Der dielektrische Verlust sinkt im allgemeinen mit Annäherung an den absoluten Nullpunkt monoton ab. Es scheint dies anzudeuten, daß immer ein dielektrischer Untergrund, beruhend auf allgemeinen thermischen Fluktuationen, existiert, der im übrigen für Polymere mit polaren Gruppen höher liegt als für unpolar gebaute. Zu tiefsten Temperaturen hin überlagert sich diesem allgemeinen Trend oft noch ein Maximum, wenngleich bei Temperaturen bis 1 °K herab zuweilen nur erst in einer Konstanz der Verlustwinkel-Werte angedeutet. Es sieht also so aus, als ob auch noch bei tiefsten Temperaturen singuläre Relaxationsmechanismen eine Rolle spielen können. In einer Reihe von Fällen findet man weitere Relaxationsprozesse zwischen 15 und 40 °K.Soweit sich Aktivierungsgrößen aus der Auftragung der Maximallage in der Temperatur mit der Frequenz nach Abtrennung des allgemeinen Untergrundes abschätzen lassen, werden diese mit sinkender Temperaturlage immer kleiner.Die dielektrischen Verluste sind in allen Fällenextrem abhängig von der Vorgeschichte der Proben und zwar insofern, daß offensichtlich Verspannungen im Material infolge von Deformationsprozessen und anderen Behandlungen zu einer erheblichen Erhöhung der Verluste führen, sowohl des Untergrundes als der singulären Mechanismen.
Summary Investigations of dielectric loss in the temperature range 1–80 °K and with frequencies between 10 c/sec and 10 kc/sec for diverse polymers a presented. For all polymers the dielectric loss decreases in principle monotonely with the approximation of the absolute Zero-point.Thus we suppose the existence of a common dielectric background loss depending from the thermal fluctuations in the material. Moreover this background losses are higher for substances with polar groups.At the lowest temperatures in most cases there seems to appear a loss peak. For temperatures down to 1 °K often this can be only suggested from the constancy of losses. But it seems to be a quite normal fact, that for extremely deep temperatures something as a singular relaxation mechanism may exist.Further discrete mechanisms exist for the range between 15 and 40 °K. Activation energy evaluated formally from the experimental dates in the normal manner after separation of the peaks from the background becomes smaller and smaller with decreasing temperatures.In all investigated cases the dielectric losses are very sensible to prehistory of the samples. It seems, that expecially stress, by deformation and other treatments, gives rise for an increase of loss for the background as for discrete mechanisms.