Kevin R. Franklin
University of Edinburgh
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Featured researches published by Kevin R. Franklin.
Acta Crystallographica Section B-structural Science | 1988
S.J. Andrews; Miroslav Z. Papiz; R. McMeeking; Alexander J. Blake; Barrie M. Lowe; Kevin R. Franklin; John R. Helliwell; M. M. Harding
Single-crystal diffraction data have been recorded for a very small crystal of dimensions 8 x 18 × 175 ~rn 3. From these data the structure of piperazine silicate (EU 19) has been determined and refined to R = 0.094 for 490 observed reflections. Data collection for such a crystal has been made practicable by the high intensity of the Daresbury Synchrotron Radiation Source and the Enraf-Nonius FAST area detector diffractometer. The potential of this synchrotron radiation method for other small crystals including proteins is discussed. Crystal data: 2+ • 2
Zeolites | 1988
Kevin R. Franklin; Barrie M. Lowe
The hydrothermal crystallization of HEXDM-silicalite and HEXDM-ZSM-48 (HEXDM = hexane-1,6-diamine) from the reaction mixtures xHEXDM /Na 2 O zTPABr 20 SiO 2 w H 2 0 ( x = 20, 50; y = 0; z = 0; w = 250, 1000; TPA = tetrapropylammonium) has been carried out at 95°, 120°, 150°, 180°C. The crystallization of HEXDM-silicalite is favored by low temperatures and high HEXDM/SiO 2 mole ratios, whereas HEXDM-ZSM-48 is the only product at 150° and 180°C. The reaction rates are increased by the addition of alkali ( y = 0.25, 0.5), and the temperature range for the formation of silicalite is extended by the addition of TPA ions ( z = 0.1, 0.5).
Zeolites | 1987
Kevin R. Franklin; Barrie M. Lowe
Abstract A procedure for the pseudomorphic transformation of particles of silica gel to silicalite-1 is described. Examination of the product by scanning electron microscopy reveals that the particles are composed of large (∼5 μm) loosely packed crystals surrounded by a dense crust of smaller (∼1 μm) crystals. X-ray powder diffraction and thermal analysis suggest that the particles also contain a small proportion of amorphous material.
Studies in Surface Science and Catalysis | 1997
Christopher J. Adams; Abraham Araya; Stuart W. Carr; Andrew Paul Chapple; Kevin R. Franklin; Peter Graham; Alan R. Minihan; Theo Jan Osinga; John A. Stuart
This paper describes the physical and chemical properties of a new zeolite, MAP, which have led to its commercialisation for use as a detergent builder. Its advantageous calcium exchange selectivity and water sorption properties are the result of unusual flexibility of the Zeolite P framework; these are delivered through engineering the framework composition and the size and porosity of the finished particles.
Zeolites | 1988
Kevin R. Franklin; Barrie M. Lowe
Crystallization from reaction mixtures containing piperazine, silica, water, and each of 11 quaternary ammonium salts at 120°, 150°, and 180°C has been investigated. In many cases, especially at 180°C, no crystalline material was obtained even though the corresponding quaternary-free reaction mixtures gave ZSM-39 or EU-19. Silicalite precursors were formed with tetrapropylammonium, tetrabutylammonium, tetrapentylammonium, tributylpentylammonium, and tributylheptylammonium bromide at 120° and 150°C. These precursors were characterized by X-ray powder diffraction, scanning electron microscopy, and thermal analysis.
Zeolites | 1988
Kevin R. Franklin; Rebecca R. Hunt; Craig D. Williams
The sorption of butan-1-ol from dilute aqueous solution by Nu-10, ZSM-48, and three different silicalites has been investigated. All materials show a strong affinity for the alcohol; however, Nu-10 and ZSM-48 have much lower maximum capacities. A form of the Langmuir equation has been used to represent the sorption of butan-1-ol by ZSM-48 and Nu-10. The separation of water and butan-1-ol by thermal desorption is satisfactorily achieved only with ZSM-48 and the silicalite samples.
Zeolites | 1988
Kevin R. Franklin; Barrie M. Lowe
The synthesis of DEA-silica-Nu-10 and DEA-silicalite-1 (DEA = diethylamine) from the reaction mixture /DEA xNaOH 20 SiO2wH2O (w = 250, 1000; x = 0, 1, 3, 5; y = 20, 50, 100) is described. The formation of DEA-silicalite-1 is favored by static conditions, high DEA concentrations, and low temperature (120°C), whereas DEA-silica-Nu-10 requires lower DEA concentrations and is the only molecular sieve to form at 150° and 180°C, DEA-silica-Nu-10 is obtained as lath-shaped crystals that aggregate in a variety of ways, and DEA-silicalite-1 is crystallized as hexagonal blocks. Thermal analysis shows that the amount of DEA present in both materials varies markedly between samples.
Journal of The Chemical Society-dalton Transactions | 1988
Alexander J. Blake; Kevin R. Franklin; Barrie M. Lowe
The hydrothermal crystallisation of a piperazine (pipz) silicate (EU-19) from the reaction mixture (p– 2y)pipz–yM2CO3–20SiO2–wH2O (p= 15, 20, or 25; y= 0–2.5; w= 250 or 1 000; M = Na, K, or Cs) at 120 and 150 °C is described. Dependent on w, plate-like or lath-like morphologies are observed. The chemical and physical properties of EU-19 are those of a layer structured material. On calcination the EU-19 crystals are pseudomorphically converted into a thermally stable silica polymorph (EU-20).
Zeolites | 1987
Kevin R. Franklin; Barrie M. Lowe
The crystallization of PIP-ZSM-39 from the reaction mixtures (15−x)PIP xNaA 20SiO2 250H2O at 180°C is reported for x=0, 0.5, 1, 2, 5, and A=OH−, SO42− or CO32−. For x=0 large (200 μm) octahedral crystals are formed in 16 days; for x≠0 crystallization is faster but the crystals are smaller and less well-formed. At higher pH values the reactions overrun to quartz.
Studies in Surface Science and Catalysis | 1989
Kevin R. Franklin; Barrie M. Lowe
Abstract The results of an investigation into the crystallisation of silica molecular sieves and clathrasils from the amine-SiO 2 –H 2 O and amine-Na 2 O–SiO 2 –H 2 O systems are summarised. The most commonly obtained products were silica-ZSM-48 (13 amines), silica-ZSM-39 (10 amines), and EU-4 (7 amines). The formation of silicalite-1, silica-Nu-10, and silica-ZSM-23 was favoured by low temperatures, static conditions, and high amine concentrations.