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1.
BJA Educ ; 19(3): 96, 2019 03.
Article in English | MEDLINE | ID: mdl-33465183

ABSTRACT

[This corrects the article DOI: 10.1016/j.bjae.2018.08.004.].

2.
Phys Chem Chem Phys ; 20(4): 2704-2715, 2018 Jan 24.
Article in English | MEDLINE | ID: mdl-29319702

ABSTRACT

Total neutron scattering has been used in conjunction with H/D and *N/15N isotopic substitution to determine the detailed liquid-state structures of pyridine and naphthalene. Analysis of the data via an empirical potential-based structure refinement method has allowed us to interrogate the full six-dimensional spatial and orientational correlation surfaces in these systems, and thereby to deduce the fundamental effects of a heteroatom and aromatic core-size on intermolecular π-π interactions. We find that the presence of a nitrogen heteroatom, and concomitant dipole moment, in pyridine induces surprisingly subtle departures from the structural correlations observed in liquid benzene: in both cases the most probable local motif is based on perpendicular (edge-to-face) intermolecular contacts, while parallel-displaced configurations give rise to a clear shoulder in the correlation surface. However, the effect of the heteroatom is revealed through detailed analysis of the intermolecular orientational correlations. This analysis shows a tendency for neighbouring pyridine molecules to direct one meta- and one para-hydrogen towards the neighbouring aromatic π-orbitals in edge-to-face configurations, while head-to-tail alignment of adjacent nitrogen atoms is favoured in face-to-face configurations. In contrast to this, increasing aromatic core size from one to only two rings has a clear and profound effect on the π-π interactions and liquid structure. Our experiments show that naphthalene-naphthalene contacts are dominated by parallel-displaced configurations, akin to those found in graphite. This marks a fundamental difference with the structure of liquid benzene, in which perpendicular geometries are favoured. Furthermore, it is remarkable to note that in the systems studied, the most favoured spatio-orientational configurations observed in the liquid state are not predicted from ab initio calculations and/or solid state crystallographic studies. This highlights the need for caution when extrapolating the results of crystallographic and computational studies to aromatic interactions in liquids and disordered systems.

3.
BJA Educ ; 18(10): 300-309, 2018 Oct.
Article in English | MEDLINE | ID: mdl-33456794
5.
Phys Chem Chem Phys ; 12(23): 6253-9, 2010 Jun 21.
Article in English | MEDLINE | ID: mdl-20431839

ABSTRACT

The structure and superconducting properties of ammoniated calcium-graphite intercalation compound (Ca-GIC) have been investigated using in situ time-of-flight neutron diffraction, Raman spectroscopy and magnetization studies. Ammonia absorption has been carried out by exposing preformed Ca-GIC to ammonia vapour at various pressures. Our in situ neutron diffraction data reveal a complex ammonia pressure dependent structural transformation, in which the growth of secondary ammoniated Ca-GIC phases are observed at the expense of the pristine CaC(6) and graphite. The ammonia absorption is irreversible in nature, and degassing the sample at elevated temperature leads to the formation of calcium amide and hydrogen. The Raman spectroscopy and magnetization studies show that the ammonia absorption not only leads to a large stacking disorder, but it also reduces the superconducting CaC(6) phase fraction. Finally, we propose a molecular stacking model which accounts for the observed ammonia absorption and concomitant structural phase transitions.

6.
J Phys Condens Matter ; 22(43): 436001, 2010 Nov 03.
Article in English | MEDLINE | ID: mdl-21403336

ABSTRACT

The magnetic behaviour in Dy(1-x)Mm(x)Co(2) (x = 0, 0.1, 0.2, 0.3, 0.4, and 0.5; Mm = mischmetal) compounds is reported using temperature and field dependence of magnetization (M-T and M-H respectively) measurements. A strong composition dependent irreversibility is observed in both the M-T and M-H scans below the magnetic ordering temperature (T(C)). A clear change of the first-order magnetic transition of DyCo(2) to a second-order one in Dy(0.5)Mm(0.5)Co(2) is evidenced by M-T and a series of Arrott (M(2) versus H/M) plots, obtained from the M-H isotherms around T(C). The variation in induced moments of the Co sublattice is estimated. It is found that the Mm substitution can only lead to a considerable reduction in the T(C), saturation magnetization, and Co moment. The observed behaviour of M-T and M-H plots with increasing Mm content is discussed in detail.

7.
Proc Natl Acad Sci U S A ; 96(7): 3358-64, 1999 Mar 30.
Article in English | MEDLINE | ID: mdl-10097044

ABSTRACT

Clay minerals are layer type aluminosilicates that figure in terrestrial biogeochemical cycles, in the buffering capacity of the oceans, and in the containment of toxic waste materials. They are also used as lubricants in petroleum extraction and as industrial catalysts for the synthesis of many organic compounds. These applications derive fundamentally from the colloidal size and permanent structural charge of clay mineral particles, which endow them with significant surface reactivity. Unraveling the surface geochemistry of hydrated clay minerals is an abiding, if difficult, topic in earth sciences research. Recent experimental and computational studies that take advantage of new methodologies and basic insights derived from the study of concentrated ionic solutions have begun to clarify the structure of electrical double layers formed on hydrated clay mineral surfaces, particularly those in the interlayer region of swelling 2:1 layer type clay minerals. One emerging trend is that the coordination of interlayer cations with water molecules and clay mineral surface oxygens is governed largely by cation size and charge, similarly to a concentrated ionic solution, but the location of structural charge within a clay layer and the existence of hydrophobic patches on its surface provide important modulations. The larger the interlayer cation, the greater the influence of clay mineral structure and hydrophobicity on the configurations of adsorbed water molecules. This picture extends readily to hydrophobic molecules adsorbed within an interlayer region, with important implications for clay-hydrocarbon interactions and the design of catalysts for organic synthesis.

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