Chain Conformation, Crystal Structures, and Structural Disorder in Stereoregular Polymers

Author(s):  
Claudio De Rosa
1966 ◽  
Vol 39 (1) ◽  
pp. 14-35 ◽  
Author(s):  
Paolo Corradini

Abstract The first synthetic polymer from a diene for which stereoregularity was proved was poly(2-chloro-butadiene). Two stereoregular polymers of isoprene, synthesized by living organisms, were known before: gutta-percha and natural rubber. The crystal structure of all these polymers was established in 1942 by Bunn. After the discovery of Ziegler-Natta catalysts, many stereoregular polymers of dienes were prepared. The first, polybutadiene with 1,1-trans enchainment, was described originally in 1955. Subsequently, between 1955 and 1957, the crystal structures of all the stereoregular isomers of polybutadiene were elucidated. It is now possible to make a sufficiently comprehensive picture of the chain constitution, configuration, and conformation of a great number of stereoregular polymers of dienes.


2019 ◽  
Vol 7 (42) ◽  
pp. 13104-13110 ◽  
Author(s):  
Jayabalan Pandidurai ◽  
Jayachandran Jayakumar ◽  
Natarajan Senthilkumar ◽  
Chien-Hong Cheng

The crystal structures show a U shape for 26DAcBPy and 26DPXZBPy and a linear chain conformation for 25DAcBPy; for the first time, we reveal that the conformations are the result of intramolecular hydrogen bonding of these molecules.


Author(s):  
Gerard E. Spinnler ◽  
Max T. Otten

Antigorite is one of the serpentine minerals, a group of 1:1 layer silicates with the approximate composition of Mg3Si2O5(OH)4. These minerals display an unusual variety of crystal structures even though they are almost identical in composition; chrysotile has an elongated-tube structure, lizardite occurs as flat plates, and antigorite has corrugates layers.The details of the crystal structures of the serpentine minerals are not completely known. Threedimensional structure refinements only exist for one- and two- layer lizardite. For antigorite, the only direct structural information consists of a two-dimensional Fourier synthesis of hOI diffractions. The lack of detailed structural data on these minerals arises from the complexity of the structures as well as the paucity of sufficiently large, well-formed single crystals. In addition, structural disorder is common in these minerals, making structure refinement difficult.High resolution transmission electron microscopy (HRTEM) has been used to study antigorite in order to discriminate among various structural models of antigorite and to characterize its microstructures


Author(s):  
Sivaprasad Ghanta ◽  
Nilanjan Roy ◽  
Partha Pratim Jana

A binary phase Ir8Cd41 in the Ir–Cd binary system and novel ternary phases in the Ir–Cd–Cu system have been synthesized from the constituent elements using high-temperature solid-state synthesis. The structure of previously reported Ir8Cd41 and newly found ternary phases in the Ir–Cd–Cu system have been characterized by single crystal X-ray diffraction and EDS analysis. The structural analysis reveals that Ir8Cd41 adopts V8Ga41-type structure and ternary Ir–Cd–Cu phases adopt two 2 × 2 × 2-superstructures of the γ-brass-related phase. The structures of ternary Ir–Cd–Cu phases are associated with structural disorder (vacancies as well as mixed site occupancies). The crystal structures of the ternary phases are viewed using layer description and cluster concept. The 2 × 2 × 2-superstructure of γ-brass-related phases in the Cu-poor region are not isostructural with the phases in the Cu-rich region, and they are consistent with the absence of a continuous phase region between two 2 × 2 × 2-superstructures of γ-brass-related phases. In the Cu-poor region, the structures contain ∼404 atoms per unit cell, whereas in the Cu-rich phases the structures contain ∼411 atoms in their respective unit cells. The crystal structures in the Cu-poor region represent a new type in the 2 × 2 × 2-superstructure of γ-brass-related phases in view of the combination of constituent cluster types, whereas the structures in the Cu-rich region adopt the Rh7Mg44 structure type.


2007 ◽  
Vol 22 (1) ◽  
pp. 27-34 ◽  
Author(s):  
A. Gómez ◽  
J. Rodríguez-Hernández ◽  
E. Reguera

A new structural model is proposed for cubic nitroprussides and the crystal structure for the complex salts of Fe(2+), Co(2+), and Ni(2+) refined in that model. In cubic nitroprussides the building unit, [Fe(CN)5NO]2−, and the assembling metal (M=Fe2+, Co2+, Ni2+), have ¾ occupancy with three formula units per cell (Z=3). This leads to certain structural disorder and to different local environments for the outer metal. The crystallographic results are supported by the Mössbauer and infrared data. The XRD powder patterns, index in a cubic cell (Fm3m space group), show a sinuous background because of diffuse scattering from positional disorder of the metal centers. Because of this, the crystal structures were refined allowing the metal centers to move from the (0,0,0) and (0,0,1/2) positions (away from positional symmetry restrictions). The refinement under these conditions leads to excellent agreement factors (Rwp, Rp, S), good pattern background fitting, and produced a refined structural model consistent with the crystal chemistry of nitroprussides. The studied materials are obtained as hydrates. On heating, the crystal water evolves, and below 100°C an anhydrous phase is obtained, preserving the framework of the original hydrates. The loss of the crystal water leads to cell contraction that represents around 2% of cell volume reduction. On cooling down from room temperature to 77 and 12 K, a slight expansion for the -M-N≡C-Fe-C≡N-M- chain length is observed, suggesting that at low temperature and reduction in the metals charge delocalization on the CN bridges takes place. For M=Fe and Co the crystal structure was also refined for the anhydrous phase at 12, 77, and 300 K.


Author(s):  
R. E. Ferrell ◽  
G. G. Paulson ◽  
C. W. Walker

Selected area electron diffraction (SAD) has been used successfully to determine crystal structures, identify traces of minerals in rocks, and characterize the phases formed during thermal treatment of micron-sized particles. There is an increased interest in the method because it has the potential capability of identifying micron-sized pollutants in air and water samples. This paper is a short review of the theory behind SAD and a discussion of the sample preparation employed for the analysis of multiple component environmental samples.


Author(s):  
J.M. Cowley

The problem of "understandinq" electron microscope imaqes becomes more acute as the resolution is improved. The naive interpretation of an imaqe as representinq the projection of an atom density becomes less and less appropriate. We are increasinqly forced to face the complexities of coherent imaqinq of what are essentially phase objects. Most electron microscopists are now aware that, for very thin weakly scatterinq objects such as thin unstained bioloqical specimens, hiqh resolution imaqes are best obtained near the optimum defocus, as prescribed by Scherzer, where the phase contrast imaqe qives a qood representation of the projected potential, apart from a lack of information on the lower spatial frequencies. But phase contrast imaqinq is never simple except in idealized limitinq cases.


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