Relevant bibliographies by topics / Scandian

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Scandian'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Scandian"

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Raudsepp, Mati, Allan C. Turnock, and Frank C. Hawthorne. "Powder Diffraction Data for Synthetic Pargasite, Scandian Pargasite and Their Fluorine Analogues: NaCa2Mg4(Al,Sc)Si6Al2O22(OH,F)2." Powder Diffraction 4, no. 1 (March 1989): 36–39. http://dx.doi.org/10.1017/s0885715600016316.

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AbstractIndexed X-ray powder diffraction data and crystal data are reported for: synthetic pargasite (P: NaCa2Mg4AlSi6Al2O22(OH)2), fluor-pargasite (FP: NaCa2Mg4AlSi6Al2O22F2), scandian pargasite (SP: NaCa2Mg4.4Sc0.6Si6Al2O22(OH)2) and scandian fluor-pargasite (SFP: NaCa2Mg4.2Sc0.8Si6Al2O22F2).
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Galuskina, I. O. "A natural scandian garnet." American Mineralogist 90, no. 10 (October 1, 2005): 1688–92. http://dx.doi.org/10.2138/am.2005.1981.

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STRACHAN, R. A., and J. A. EVANS. "Structural setting and U–Pb zircon geochronology of the Glen Scaddle Metagabbro: evidence for polyphase Scandian ductile deformation in the Caledonides of northern Scotland." Geological Magazine 145, no. 3 (March 6, 2008): 361–71. http://dx.doi.org/10.1017/s0016756808004500.

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AbstractWithin the Scottish Caledonides, the Glen Scaddle Metagabbro was intruded into the Moine Supergroup of the Northern Highland Terrane after Grampian D2 folding and prior to regional D3 and D4 upright folding and amphibolite-facies metamorphism. A U–Pb zircon age of 426 ± 3 Ma obtained from the metagabbro is interpreted to date emplacement. D3–D4 folding is constrained to have occurred during the Scandian orogenic event. In contrast, polyphase folding and regional metamorphism of the Dalradian Supergroup southeast of the Great Glen Fault is entirely Grampian. These differences are consistent with published tectonic models that invoke a minimum of 700 km of post-Scandian sinistral displacements across the Great Glen Fault to juxtapose the Grampian and Northern Highland terranes.
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Gee, D. G. "The Scandinavian Caledonides - basement involvement in Scandian thrusting." Geologiska Föreningen i Stockholm Förhandlingar 113, no. 2-3 (September 10, 1991): 259–60. http://dx.doi.org/10.1080/11035899109453867.

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Clayhills, Tom. "On the occurrence of the genus Hyperaspis (Col. Coccinellidae) in Fenno-Scandian countries." Entomologica Fennica 11, no. 2 (June 1, 2000): 109–12. http://dx.doi.org/10.33338/ef.84051.

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The distribution of the species of Hyperaspis occurring in northern Europe, H. pseudopustulata and H. inexpectata is discussed and the confusion concerning H. reppensis based on old traditional determinations in our countries is straightened out. H. reppensis does not occur in northern Europe. H. concolor is reported from Sweden as new for the Fenno-Scandian countries.
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Mako, Calvin A., Richard D. Law, Mark J. Caddick, J. Ryan Thigpen, Kyle T. Ashley, John Cottle, and Andrew Kylander-Clark. "Thermal evolution of the Scandian hinterland, Naver nappe, northern Scotland." Journal of the Geological Society 176, no. 4 (April 5, 2019): 669–88. http://dx.doi.org/10.1144/jgs2018-224.

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Gee, David G. "Chapter 23 Swedish Caledonides: key components of an early–middle Paleozoic Himalaya-type collisional orogen." Geological Society, London, Memoirs 50, no. 1 (2020): 577–99. http://dx.doi.org/10.1144/m50-2019-20.

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AbstractCaledonian collision of continents Laurentia and Baltica, with at least 1000 km of lateral shortening, dominates the bedrock along the northern margins of the North Atlantic Ocean. Scandian (Silurian–Devonian) underthrusting of Laurentia by Baltica resulted in stacking of the main orogenic wedge and its migration onto the platform edge of Baltica. Complementary thrust sheets, exposed in northeastern Greenland, telescoped the Laurentian continental margin. The Swedish part of the Caledonides, comprising the foreland segment along the central half of this mountain belt, includes the key components of: (1) the Baltoscandian inner margin, including Ordovician and Silurian foreland basins; (2) the Neoproterozoic extended outer margin dominated by mafic magma and continent–ocean transition zone; (3) Iapetus oceanic terranes; and (4) evidence that substantial parts of the outermmost Baltoscandian margin experienced deep subduction and high- and ultrahigh-pressure (HP/UHP) metamorphism during late Cambrian–Ordovician accretion. This evidence, integrated with the Norwegian Caledonides, defines an orogenic pro-wedge comparable to that in the Himalaya today. Orthogonal Scandian collision, lasting for about 60 million years (c. 440–380 Ma), involved late Silurian–Early Devonian HP/UHP metamorphism of the underthrusting Baltoscandian basement. By the Middle Devonian, the hinterland was experiencing orogen-parallel folding and axial extension, accompanying exhumation, while the orogenic pro-wedge continued to migrate eastwards on to the platform.
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Gee, D. G. "Thrust tectonics in the Scandes - upper crustal extension during Scandian compression." Geologiska Föreningen i Stockholm Förhandlingar 110, no. 4 (December 1988): 390–92. http://dx.doi.org/10.1080/11035898809452682.

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Fletcher, T. P., A. K. Higgins, and J. S. Peel. "A Balto-Scandian Middle Cambrian fauna from Peary Land, North Greenland." Rapport Grønlands Geologiske Undersøgelse 137 (December 31, 1988): 118. http://dx.doi.org/10.34194/rapggu.v137.8010.

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The first record of Middle Cambrian faunas of 'Atlantic' affinity from the Franklinian basin sequence of North Greenland was made by Poulsen (1969) who noted that previously described Greenland faunas were of 'Pacific' type. Field work by the Geological Survey of Greenland during the last decade has established that 'Atlantic' faunas are widespread in more outer shelfsequences along the northern coast of North Greenland while the 'Pacific' faunas occur within inner shelfsequences more to the south, near the margin of the Inland Ice. North Greenland preserves both faunas in dose geographical juxtaposition in only slightly tectonised geological settings. Thus, alatest Middle Cambrian trilobite fauna described by Robison (in press) from the Holm Dal Formation in an area some 40 km south of the presently discussed locality (and more inner shelf) includes a mixture of polymeroids characteristic of the Cedaria Zone of North America and agnostoids characteristic of the Lejopyge laevigata Zone of the Swedish standard zonation.
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Spencer, B. M., J. R. Thigpen, R. D. Law, C. A. Mako, C. S. McDonald, K. V. Hodges, and K. T. Ashley. "Rapid cooling during late-stage orogenesis and implications for the collapse of the Scandian retrowedge, northern Scotland." Journal of the Geological Society 178, no. 1 (August 13, 2020): jgs2020–022. http://dx.doi.org/10.1144/jgs2020-022.

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New 40Ar/39Ar thermochronological and deformation temperature analyses in the Scandian (c. 435–420 Ma) orogenic retrowedge of northern Scotland demonstrate accelerated cooling during late syn- to post-orogenic exhumation of the high-grade orogenic core. Initial cooling rates of 10–30°C myr−1 immediately following peak orogenesis transitioned to rapid rates of 45–90°C myr−1 during final exhumation of the Naver thrust sheet in the orogenic core. The flanking ductile thrust sheets exhibit a similar, albeit less pronounced, acceleration of cooling, with rates increasing by c. 150–300% following peak orogenesis. Closer to the foreland, the Moine thrust sheet did not experience increased cooling rates. Calculated unroofing rates of 3.75 mm a−1 in the high-grade Naver thrust sheet suggest increasing, rapid exhumation in the orogenic core during a presumed collapse phase of orogenesis. This is contrary to the expectation of decreasing erosional efficiency as topography is diminished and is interpreted to suggest that unroofing of the Scottish Caledonides may have been partially enhanced by upper crustal extensional deformation during ductile flow of the infrastructure of the orogenic core. Similar processes have been interpreted in the East Greenland Caledonides, which form the northern extension of the Scandian retrowedge.Supplementary material:40Ar/39Ar analytical data for muscovite (Supplementary Data Table 1), 40Ar/39Ar analytical data for amphibole (Supplementary Data Table 2), and electron microprobe analytical data for amphibole samples (Supplementary Data Table 3) is available at: https://doi.org/10.6084/m9.figshare.c.5087057
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Dissertations / Theses on the topic "Scandian"

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Fleck, Andrew. "SCANDAL, INC." Miami University Honors Theses / OhioLINK, 2003. http://rave.ohiolink.edu/etdc/view?acc_num=muhonors1111086181.

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Miller, Stuart Raymond. "Scandium-bearing open framework materials /." St Andrews, 2008. http://hdl.handle.net/10023/570.

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Miller, Stuart R. "Scandium bearing open framework materials." Thesis, University of St Andrews, 2007. http://hdl.handle.net/10023/570.

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Here I report the hydrothermal chemistry of scandium, examining the behavior of the Sc³⁺ cation in various systems, including phosphates, phosphites, phosphonates and carboxylates. In total, 27 different materials, 23 of which are novel, have been synthesised and their structures solved. Seven different scandium phosphate-based materials have been successfully synthesised using amines and alkali hydroxides as structure directing agents, producing chain, layer and framework materials. Thermal analysis of these materials indicated that they were not stable upon removal of the template, because there are hydrogen bonding networks between the template and free OH groups on the phosphate groups. Certain conditions lead to the crystallization of either kolbeckite, Sc(PO₄).2H₂O, or a langbeinite-type structure, (NH₄)₂Sc₂(HPO₄)(PO₄)₂, which are dense frameworks. Investigation of scandium phosphites leads to the formation of more thermally stable frameworks. Investigation of scandium phosphite-based materials using different structure directing agents yielded three framework phosphite materials and one layered phosphite / phosphate. The use of lithium hydroxide and ethylenediamine within scandium phosphite systems resulted in the crystallization of a gainesite type framework, (LiSc(HPO₃)₂)and (H₃N(CH₂)₂NH₃)₂Sc₄(HPO₃)₈, which distorts in order to accommodate the amine, but not the lithium cation. Decreasing the potential for the formation of hydrogen bonding networks in the phosphite systems led to the formation of framework structures, however these structures did not retain their crystalline integrity upon removal of the template. In order to impart structure directing properties upon scandium-based materials but avoid the formation of hydrogen bonding networks upon which the crystalline integrity is dependent, scandium phosphonates were investigated. Seven different scandium phosphonate materials have been synthesised, two of which have been solved from powder diffraction data, and one from a combination of powder diffraction data, molecular modeling and single crystal data. Synthesis of scandium phosphonate materials yielded two thermally stable, porous materials with reversible water adsorption properties, NaSc(CH₃PO₃)₂•H₂O and Sc₂(O₃PCH₂(NHC₅H₁₀NH)₋CH₂PO₃)₃4H₂O. The success of this approach led to the examination of scandium carboxylate metal organic framework materials. The incorporation of Sc³⁺ into microporous carboxylate frameworks yielded three aliphatic scandium carboxylates and six aromatic scandium carboxylates. The scandium analogue of MIL-53 shows potential for gas adsorption studies, as well as illustrating that scandium carboxylates can be isostructural to metal carboxylate materials already published. The scandium terephthalate, Sc₂(O₂CC₆H₄CO₂)₃, is a small pore framework material with an unprecedented structure type, the adsorption properties of which have been examined using a variety of different small gas molecules and hydrocarbons, including X-ray analysis of the structures whilst adsorbing different molecules. ⁴⁵Sc MAS NMR has been performed on the materials prepared pure and characterized in this thesis, in order to establish a library of chemical shifts for scandium in different framework environments.
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Xia, Ye, and 夏晔. "High resolution spectroscopy of scandium monohalides." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2012. http://hub.hku.hk/bib/B49617886.

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This thesis reports the study of the molecular and electronic structure of scandium monohalides using the technique of laser ablation/reaction with supersonic free jet expansion used for producing the target molecules and laser induced fluorescence (LIF) spectroscopy for recording their electronic transition spectrum. The scandium diatomic molecules studied in this work were scandium monoiodide (ScI) and scandium monobromide (ScBr), which were produced by the reaction of Sc atoms with 2% CH3I and 2% C2H5Br gases seeded in Ar carrier gas, respectively. The LIF spectrum of the electronic transition of ScI and ScBr were recorded in the visible and near infrared spectral region between 613 and 854 nm. The analysis of the high resolution electronic spectra of ScI and ScBr yielded molecular constants and information of electronic structures. For all the transition bands observed, rotationally-resolved transition lines were fit to a theoretical model to retrieve molecular constants for both upper and lower electronic states. For the ScI molecule, seven vibrational bands of the D1П –X^1 Σ^+ system were recorded and analyzed. Accurate molecular constants for the v = 0 – 2 levels of the D^1П state and the v = 0 – 3 levels of the X^1 Σ^+ state were obtained. The equilibrium bond lengths, re (Å), for the electronic states of ScI were determined as follows: ScI X^1 Σ^+ D^1П r_e(Å) 2.6078 2.7146 For the ScBr molecule, three electronic transition systems were recorded and analyzed, which include six vibrational bands of the C^1 Σ^+– X^1 Σ^+ system, seven vibrational bands of the e^3Δ–a^3Δsystem and two vibrational bands of the d3Φ – a3Δ system. Rotationally resolved transition lines of both Sc79Br and Sc81Br isotopes were observed and analyzed. Least-squares fitting of the measured line positions yielded accurate molecular constants for the v = 0 – 2 levels of the X^1 Σ^+ state, the v = 0 – 3 levels of the C^1 Σ^+ state, the v = 0 and 1 levels of the d3Φ state and the v = 0 – 2 levels of both e3Δ and a3Δ states, respectively. The equilibrium bond lengths, re (Å), determined for electronic states of ScBr are given as follows: ScBr X^1 Σ^+ a^3Δ C^1 Σ^+ r_e(Å) 2.3806 2.4767 2.4776 A molecular orbital (MO) energy level diagram has been used to examine the electronic configurations giving rise to the different observed electronic states of ScI and ScBr. An attempt has been made to put the MOs of all the scandium monohalides under a single picture. A comparison of the molecular constants for the different electronic states of scandium monohalides indicates a weakening of the chemical bonding between the scandium atom and the halogen atoms down the group.
published_or_final_version
Chemistry
Doctoral
Doctor of Philosophy
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Clough, Benjamin. "New scandium and titanium borylimido chemistry." Thesis, University of Oxford, 2017. https://ora.ox.ac.uk/objects/uuid:1a9dbfb3-98c3-4fd6-96ac-5fba09f3ffcd.

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This Thesis reports the synthesis and reactivity of scandium and titanium borylimides. New, versatile synthetic routes to such complexes of these two metals were targeted, and their reactions with small, unsaturated compounds were explored, with a particular focus being the reactivity of alkynes with these systems. Chapter One provides a background on Group 4 imido and hydrazido complexes. Group 4 alkoxyimides are also reviewed, as well as the developing field of rare earth imides. The Chapter focuses on the synthesis, structure, and stoichiometric and catalytic reactions of these complexes with unsaturated substrates, and ends with a description of the handful of known transition metal borylimides. Chapter Two first describes the synthesis and structures of new titanium borylimido synthons prepared from Ti(NMe2)2Cl2. From the borylimide Ti{NB(NAr'CH)2}Cl2(py)3 are then formed five new compounds supported by a range of tridentate, nitrogen-based ligands. Chapter Three describes the synthesis of half-sandwich titanium borylimides through tertbutylimide/borylamine exchange. A sandwich compound is also described, and the electronic structures of these complexes are analysed by DFT, QTAIM and NBO studies. Reactivity with heteroallenes, and exchange reactions with amines are also explored. Chapter Four describes the reactivity of diamide-donor-supported titanium borylimides with terminal alkynes. The principal reaction outcomes are [2+2] cycloadditions and C–H bond activations, and an interesting C–F bond activation is also described. Kinetic studies of some reactions are presented, and will be supported by further DFT studies. Chapter Five explores attempts to prepare the first rare earth borylimide. Kinetic and computational evidence is presented for the existence of a transient scandium borylimide which rapidly undergoes interesting sp, sp2 and sp3 C–H bond activations. Chapter Six presents full experimental procedures and characterising data for the new complexes reported.
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Riva, Sephira. "Scandium metal processing for aerospace application." Thesis, Swansea University, 2018. https://cronfa.swan.ac.uk/Record/cronfa39867.

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The use of scandium has been conventionally restricted to minor additions in alloys for structural applications. The term ‘scandium effect’ came thus to indicate the properties improvements caused by the precipitation of scandium intermetallics in the matrix. The development of High-Entropy Alloys (HEA, multi-principal component alloys combining compositional complexity with simple crystal structures) opened the door for the development of new systems, and therefore for new applications for lightweight metals such as scandium. This work is a thorough investigation of the potential of scandium-based in- termetallics in the growing field of HEAs. The synthesis and characterisation of multi-principal component alloys contain- ing scandium as active alloying element illustrate the compound-forming ability of this element. The high mixing entropy of the studied systems (comprising alloys of scandium with first raw metals or with hcp-structured elements) cannot efficiently inhibit the precipitation of stable intermetallic compounds. Among them, of in- terest is the so-called W -phase, so-far only reported for Al-basedCu-containing commercial alloys. Small scandium additions to Al2CoCrFeNi, Al0.5CoCrCuFeNi and AlCoCr- Cu0.5FeNi cause the segregation of a secondary phase along grain boundaries. This hexagonal Laves phase, formed by scandium in combination with Al, Co, Cr, Cu, Fe and Ni, does not disrupt the HEA matrix and is extremely stable. Moreover, it deeply affects microstructure and mechanical properties – for ex-ample, by enhancing the HEA stability with the postponement of a T-dependent phase exsolution by roughly 150 °C. Furthermore, a synergistic effect in the main phase stabilisation takes place when the Sc-doped sample is pressed at 9.5 GPa: no transition occurs and the intermetallic dissolves in the matrix. Preliminary investigations performed by spark-plasma sintering of different additives (among which Sc2O3, used as a source of scandium metal) in combination with the Al CoCrFeNi alloy led to the discovery of a promising nanodiamond HEA composite.
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Kerdsongpanya, Sit. "Scandium Nitride Thin Films for Thermoelectrics." Licentiate thesis, Linköpings universitet, Tunnfilmsfysik, 2012. http://urn.kb.se/resolve?urn=urn:nbn:se:liu:diva-85917.

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Thermoelectric devices are one of the promising energy harvesting technologies, since they can convert heat (i.e. a temperature gradient) to electricity. This result leads us to use them to harvest waste heat from heat engines or in power plants to generate usable electricity. Moreover, thermoelectric devices can also perform cooling. The conversion process is clean, with no emission of greenhouse gases during the process. However, the converting efficiency of thermoelectrics is very low because of the materials limitations of the thermoelectric figure of merit (ZTm). Thus, there is high demand to maximize the ZTm. I have discovered that ScN has high power factor 2.5 mW/(mK2) at 800 K, due to low metalliclike electrical resistivity (∼3.0 μΩm) with retained relatively large Seebeck coefficient of -86 μV/K. The ScN thin films were grown by reactive dc magnetron sputtering from Sc targets. For ScN, X-ray diffraction, supported by transmission electron microscopy, show that we can obtain epitaxial ScN(111) on Al2O3(0001). We also reported effects on thermoelectric properties of ScN with small changes in the composition with the power factor changing one order of magnitude depending on e.g. oxygen, carbon and fluorine content which were determined by elastic recoil detection analysis. The presence of impurities may influence the electronic density of states or Fermi level (EF) which could yield enhancement of power factor. Therefore, the effects of defects and impurities on the electronic density of states of scandium nitride were investigated using first-principles calculations with general gradient approximation and hybrid functionals for the exchange correlation energy. Our results show that for Sc and N vacancies can introduce asymmetric peaks in the density of states close to the Fermi level. We also find that the N vacancy states are sensitive to total electron concentration of the system due to their possibility for spin polarization. Substitutional point defects shift the Fermi level in the electronic band according to their valence but do not introduce sharp features. The energetics and electronic structure of defect pairs are also studied. By using hybrid functionals, a correct description of the open band gap of scandium nitride is obtained, in contrast to regular general gradient approximation. Our results envisage ways for improving the thermoelectric figure of merit of ScN by electronic structure engineering through stoichiometry tuning and doping.
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Demir, Selvan [Verfasser]. "Scandium cluster and metallocene chemistry / Selvan Demir." Köln : Universitäts- und Stadtbibliothek Köln, 2010. http://d-nb.info/1013831799/34.

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Böhmer, Norbert. "Einwirkung von Ammoniumhalogeniden auf Scandium und Gadolinium." [S.l. : s.n.], 2001. http://deposit.ddb.de/cgi-bin/dokserv?idn=963638432.

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Scotney, Christopher C. J. "Investigations using chiral scandium (III) Lewis acids." Thesis, University of Nottingham, 2011. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.555431.

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Lewis acidic chiral scandium(III) catalysts have been developed and tested with a range of bidentate substrates in both Diels-Alder and aza-Michael reactions. Scandium(III) complexes incorporating bipybox, phenbox (a new class oftetradentate chiral ligand) and pybox ligands, have been found to give significant enantioselectivity in reactions involving 3-acyloxazolidinones and 3-formylpyrone- containing substrates. Molecular modelling has been used to understand more about the action of these catalysts and to design new ligands which can lead to higher levels of enantioselectivity in these reactions. For acyloxazolidinone-containing substrates it was found that scandium(III)/pybox catalysts gave the same sense of stereocontrol in both Diels-Alder and aza-Michael reactions. It was observed that the sense of enantiocontrol with a particular class of ligand was determined by the stereochemistry of the R -substituent on the ligand and the degree of this stereocontrol was influenced by its size. These observations have lead to a proposal of how the substrates bind to the chiral scandium(III) catalysts for each ligand type and how the enantioselectivity of the products is derived. The chiral scandium(III) Lewis acid catalysts were also used to promote an endo- selective intramolecular Diels-Alder reaction of a 3-formylpyrone-containing substrate, the key step in a synthesis of solanapyrone D. This natural product was prepared in up to 77 % ee with all four contiguous formed in this final step of the synthesis. The highest levels of enantioselectivity for this reaction were given by scandium(III)-pybox catalysts. A greater understanding of chiral scandium(III) catalysts, particularly the substrate- catalyst interactions, has been gained in this thesis and can hopefully be used in the future to aid further development of asymmetric catalysis with scandium(III). 11.
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Books on the topic "Scandian"

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Baltz, Lewis. Lewis Baltz: Scandiano. [Rubiera, Italy?]: Arcadia edizioni, 1991.

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Venturi, Giovanni Battista. Storia di Scandiano. [Sala Bolognese, BO]: A. Forni, 1997.

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Greene, Viktor A. Scandium: Compounds, productions, and applications. Hauppauge, N.Y: Nova Science Publishers, 2010.

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Quick, Amanda. Scandal. Thorndike, Me: Thorndike Press, 1991.

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Endō, Shūsaku. Scandal. London: Owen, 1988.

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Quick, Amanda. Scandal. New York: Bantam, 1991.

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Donald, Seaman, ed. Scandal! New York: Stein and Day, 1986.

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Endō, Shūsaku. Scandal. London: Peter Owen, 2006.

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Endō, Shūsaku. Scandal. Harmondsworth: Penguin, 1989.

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Rina, Onur, ed. Scandal. New York: Greenwillow Books, 2012.

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Book chapters on the topic "Scandian"

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Wain, Barry. "Scandal, What Scandal?" In Malaysian Maverick, 149–82. London: Palgrave Macmillan UK, 2009. http://dx.doi.org/10.1057/9780230251236_6.

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Samson, Iain M., and Mathieu Chassé. "Scandium." In Encyclopedia of Earth Sciences Series, 1323–26. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-39312-4_281.

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Samson, Iain M., and Mathieu Chassé. "Scandium." In Encyclopedia of Earth Sciences Series, 1–5. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-39193-9_281-1.

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Cotton, Simon. "Scandium." In Lanthanides and actinides, 1–9. London: Macmillan Education UK, 1991. http://dx.doi.org/10.1007/978-1-349-11904-2_1.

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Brookins, Douglas G. "Scandium." In Eh-pH Diagrams for Geochemistry, 120–21. Berlin, Heidelberg: Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-73093-1_49.

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Butler, Ian, and Mark Drakeford. "Scandal." In Social Policy, Social Welfare and Scandal, 1–5. London: Palgrave Macmillan UK, 2003. http://dx.doi.org/10.1057/9780230554467_1.

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Dolan, Jill. "Scandal." In The Feminist Spectator in Action, 39–45. London: Macmillan Education UK, 2013. http://dx.doi.org/10.1007/978-1-137-03291-1_7.

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Alberg, Jeremiah. "Scandal." In The Palgrave Handbook of Mimetic Theory and Religion, 485–91. New York: Palgrave Macmillan US, 2017. http://dx.doi.org/10.1057/978-1-137-53825-3_64.

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Rando, David. "Scandal." In Modernist Fiction and News, 47–72. New York: Palgrave Macmillan US, 2011. http://dx.doi.org/10.1057/9780230119666_3.

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Baker, James. "Scandal." In The Business of Satirical Prints in Late-Georgian England, 21–56. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-49989-5_2.

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Conference papers on the topic "Scandian"

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Che, Siqi, Calvin A. Mako, Mark J. Caddick, and R. D. Law. "APPLYING GARNET-MONAZITE THERMOMETRY TO SCANDIAN THRUST SHEETS IN NORTHWEST SCOTLAND." In 68th Annual GSA Southeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019se-327566.

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Spencer, Brandon M., James Thigpen, Richard D. Law, K. V. Hodges, Sean Gallen, Jason Dortch, and Calvin A. Mako. "THERMAL EVOLUTION OF THE SCANDIAN OROGENIC RETROWEDGE, NORTHERN SCOTLAND: TECTONIC IMPLICATIONS OF RAPID COLLAPSE." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-356750.

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Mako, Calvin A., Richard D. Law, J. Ryan Thigpen, Kyle T. Ashley, Michael J. Jercinovic, and Michael L. Williams. "TIMING OF GARNET GROWTH AND BREAKDOWN USING MONAZITE GEOCHRONOLOGY IN THE SCANDIAN (TACONIC) OROGENIC WEDGE, NW SCOTLAND." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272468.

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Mako, Calvin A., Richard D. Law, John M. Cottle, J. Ryan Thigpen, and Kyle T. Ashley. "MONAZITE-XENOTIME THERMOMETRY CONSTRAINTS ON THE METAMORPHIC EVOLUTION OF THE SCANDIAN NAPPE STACK, NW HIGHLANDS TERRANE, SCOTLAND." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-284730.

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Thigpen, James, Kyle T. Ashley, Calvin A. Mako, Richard D. Law, and Brandon M. Spencer. "NUMERICAL INVESTIGATIONS OF RAPID HEATING IN THRUST BELTS AND IMPLICATIONS FOR METAMORPHISM IN THE SCANDIAN OROGENIC WEDGE, NW SCOTLAND." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-359871.

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Hollocher, Kurt, Peter Robinson, and Emily O. Walsh. "PRE-SCANDIAN AMALGAMATION OF ROCKS NOW EXPOSED IN THE UPPER AND UPPERMOST ALLOCHTHONS OF THE SCANDINAVIAN CALEDONIDES: EVIDENCE AND INTERPRETATIONS IN RELATION TO LAURENTIA AND GANDERIA." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272371.

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Postava, K., L. Halagačka, D. Hrabovský, O. Životský, J. Pištora, D. A. Pawlak, S. Turczynski, and K. Kolodziejak. "Optical spectroscopy of terbium-scandium-aluminium garnet and terbium-scandium perovskite." In SPIE Europe Optics + Optoelectronics, edited by Vladimir Kuzmiak, Peter Markos, and Tomasz Szoplik. SPIE, 2009. http://dx.doi.org/10.1117/12.820789.

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Bordean, Despina-Maria. "SCANDIUM, ELEMENT OF SURPRISES." In 13th SGEM GeoConference on ECOLOGY, ECONOMICS, EDUCATION AND LEGISLATION. Stef92 Technology, 2013. http://dx.doi.org/10.5593/sgem2013/be5.v1/s20.113.

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McMillen, Colin D., Joseph W. Kolis, and John Ballato. "Growth and Properties of Doped Scandia Crystals." In LEOS 2007 - IEEE Lasers and Electro-Optics Society Annual Meeting. IEEE, 2007. http://dx.doi.org/10.1109/leos.2007.4382466.

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Mrázková, Z., D. Hrabovský, K. Postava, J. Pištora, S. Turczynski, K. Kolodziejak, and D. A. Pawlak. "Far-infrared spectroscopy of terbium-scandium-aluminium garnet and terbium-scandium perovskite." In 17th Slovak-Czech-Polish Optical Conference on Wave and Quantum Aspects of Contemporary Optics. SPIE, 2010. http://dx.doi.org/10.1117/12.881907.

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Reports on the topic "Scandian"

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Huleatt, Mike. Australian resource reviews: Scandium 2019. Geoscience Australia, 2019. http://dx.doi.org/10.11636/9781925848458.

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Boyle, Timothy J., Ryan Falcone Hess, Michael Luke Neville, and Panit Clifton Howard. Scandium separation from tungsten crucibles :. Office of Scientific and Technical Information (OSTI), February 2013. http://dx.doi.org/10.2172/1088104.

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Smith, A. B., and P. T. Guenther. Fast neutron scattering near shell closures: Scandium. Office of Scientific and Technical Information (OSTI), August 1992. http://dx.doi.org/10.2172/7012008.

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Smith, A. B., and P. T. Guenther. Fast neutron scattering near shell closures: Scandium. Office of Scientific and Technical Information (OSTI), August 1992. http://dx.doi.org/10.2172/10187759.

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De Lorenzi-Venneri, Giulia. Sesame Equation of State Number 2100 for Scandium. Office of Scientific and Technical Information (OSTI), October 2012. http://dx.doi.org/10.2172/1053531.

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Kayaoglu, Barin. Turkish military hit by food poisoning scandal. Al-Monitor: The Pulse of the Middle East, June 2017. http://dx.doi.org/10.26598/auis_ug_is_2017_06_19.

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Smith, A. B., J. W. Meadows, and R. J. Howerton. A basic evaluated neutronic data file for elemental scandium. Office of Scientific and Technical Information (OSTI), November 1992. http://dx.doi.org/10.2172/6709834.

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Smith, A. B., J. W. Meadows, and R. J. Howerton. A basic evaluated neutronic data file for elemental scandium. Office of Scientific and Technical Information (OSTI), November 1992. http://dx.doi.org/10.2172/10131914.

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Azoulay, Pierre, Alessandro Bonatti, and Joshua Krieger. The Career Effects of Scandal: Evidence from Scientific Retractions. Cambridge, MA: National Bureau of Economic Research, May 2015. http://dx.doi.org/10.3386/w21146.

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Moore, G., G. C. Nelson, and H. H. Madden. Auger analysis of scandium, Sc-Oxide, Sc-Deuteride and Sc-Nitride. Office of Scientific and Technical Information (OSTI), September 1996. http://dx.doi.org/10.2172/369715.

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