19 results on '"formation reaction"'
Search Results
2. Spectrophotometric determination of Sulphamethoxazole Via Charge Transfer Complex Formation Reaction
- Author
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Theiaa Najm Al-Sabha, Thabit S. Al-Ghabsha, and Mohammed S. Al-Enizzi
- Subjects
sulphamethoxazole ,formation reaction ,limits of detection (lod) ,Education ,Science (General) ,Q1-390 - Abstract
Abstract A simple and sensitive spectrophotometric method for the determination of sulphamethoxazole in pure as well as in dosage form is described. The method is based on the reaction of sulphamethoxazole as electron donor with o-chloranil as electron acceptor to form violet colored charge transfer complex having maximum absorption band at 539 nm. Under the optimized reaction conditions, Beer’s law was obeyed in the range of 2-60 μg ml-1 with molar absorptivity 3.675×103 L mol−1cm−1. The limits of detection (LOD) and limit of quantitation (LOQ) were 0.371 and 1.236 μg ml-1 respectively. The accuracy and precision of the method were satisfactory; the average recovery % was 100.95 % and values of relative standard deviations ≤1.06 %. The stoichiometry of the reaction was studied, and the reaction mechanism was postulated. The proposed method was successfully applied to the determination of sulphamethoxazole in its pharmaceutical tablets and syrup with good accuracy and precisions. Keywords: Charge transfer; Spectrophotometry; o-chloranil; sulphamethoxazole
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- 2013
- Full Text
- View/download PDF
3. Finite rate simulations and analyses of wet/distributed flame structure in swirl-stabilized combustion
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Zhang, Kai, Shen, Yazhou, Duwig, Christophe, Zhang, Kai, Shen, Yazhou, and Duwig, Christophe
- Abstract
Towards developing humidified gas turbines (HGT) capable of running at high electrical efficiencies and low emissions, wet/steam-diluted combustion in a premixed swirl burner is investigated using large eddy simulation and a partially stirred reactor method. Chemical explosive mode and extended combustion mode analyses are performed to promote the understanding of wet flame structures. The former identifies the key features of the wet methane oxidation processes, and the latter extends the flame regime classification method to describing the combustion status of fluid parcels using local properties. Three combustion regimes are extensively discussed: the swirl stabilized (SS), colorless distributed (CDC) and non-combustible. Using the combined analyses of the two approaches, it is found that compared to dry flames, wet flames present more fluid parcels defined in the practical CDC regime where local heat release is low and Damköhler number is smaller than unity. The wet fluid parcels are capable of self-igniting via radical explosion, while dry fluid parcels self-ignite via thermal runaway. The species CH2O and temperature are the first and second highest contributors towards the explosivity of dry flames, while temperature is insignificant to that of wet flames. The species C2H6 is found an important source to the self-ignitability of wet fluid parcels in the practical CDC regime due to the activation of the three-body ethane formation reaction R148: 2CH3 + M = C2H6 + M in the low O2% wet combustion environment. Proper use of proposed methods to quantify wet flame behavior guides stable and low emission operation of practical HGT., QC 20210309
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- 2021
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4. La lawsonite dans les métasédiments en base de zone sismogénique : géochimie, échelles de migration des fluides et rôle de la déformation dans les Schistes Lustrés
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LEFEUVRE, Benjamin, Institut des Sciences de la Terre de Paris (iSTeP), Centre National de la Recherche Scientifique (CNRS)-Sorbonne Université (SU)-Institut national des sciences de l'Univers (INSU - CNRS), Sorbonne Université, Philippe Agard, Anne Verlaguet, Benoit Dubacq, and Benoît Dubacq
- Subjects
Zonation en éléments traces ,[SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/Petrography ,[SDU.STU]Sciences of the Universe [physics]/Earth Sciences ,Lawsonite ,Alpine Schistes Lustrés ,Trace elements and major elements ,Zones de subduction ,Lawsonite blueschist ,Séismes lents ,Slow earthquakes ,Réaction de formation ,[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry ,Fluid circulation ,Subduction zones ,Circulation des fluides ,Formation reaction ,[SDU.STU.AG]Sciences of the Universe [physics]/Earth Sciences/Applied geology ,Trace elements zoning ,[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics ,Metasediments ,Slow seisms ,Métasédiments ,Subduction zone ,Fluid/Rock interaction ,Schistes Lustrés Alpins ,Lawsonite-forming reaction ,[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy - Abstract
In subduction zones, the migration of fluids derived from the dehydration of metasediments has important consequences on the mechanic properties of rocks, hence on seismicity. Geophysical imaging of the velocity of pressure and shear waves shows that fluids are present in large quantities and migrating in the 30-40 km depth range. This range corresponds to the depth at which slow slip events are supposed to take place, and it is currently assumed that fluids play a large part in the onset of these slow slip events. Deformation mechanisms accompanying slow slip events are still debated, as well as the exact role of fluids which remain enigmatic in their source, origin, volumetric importance together with the scale and the mode of their migration.To better understand how such fluids migrate in subducted metasediments and refine the budget of fluids in this context (from ~150°C-0.3 GPa to 350°C-1.2 GPa), we have studied subunits of the Schistes Lustrés Complex of the Western Alps.Lawsonite (ideally CaAl2Si2O7(OH)4.H2O) is ubiquitous in these rocks, in the schistose matrix as well as in metamorphic veins, attesting to fluid-rock interactions at depth. Lawsonite, a highly hydrated mineral (~12wt.% H2O) is of particular interest as it is known to play a key role in recycling fluids to mantle depths for it is stable up tu ultra-high pressures.Yet the formation of large amounts of lawsonite in subducted pelagic sediments – where pelitic and carbonated horizons alternate – is unexplained and lawsonite-forming reactions are poorly documented. In particular, the need for large amounts of calcium sourced from carbonated horizons led some authors to suggest ample decarbonation, allowing for export of carbon, a major constituent of these rocks.This study aims first at defining which reactions allowed lawsonite crystallization to shed light on element transfer at depth. The petrologic study allowed distinguishing several types of lawsonite based on textural, micro-structural and morphologic criteria. The vast majority of the lawsonite crystals show textural equilibrium with ankerite, and the following reaction is proposed: chlorite + kaolinite + aragonite = lawsonite + ankerite + quartz + H2O. This reaction shows zero net export of carbon during lawsonite crystallization. Thermodynamic modelling suggests lawsonite crystallization initiates early during the metamorphic history of the Schistes Lustrés (~13 km depth) and is on-going the metamorphic peak, due to sluggish kinetics and the apparition of additional yet subordinate reactions.A detailed geochemical study of the lawsonite types has been carried out in this study. Results highlight the differences in fluid-rock interactions and their time evolution. The earliest, most abundant lawsonite type shows closed-system crystallization with small equilibrium length-scales (micro- to millimetres) whereas later lawsonite types indicate system opening with increased fluid mobility and element transfer via advection.Observations concur to showing progressive system opening in the Schistes Lustrés via increased fluid mobility. This took place increment by increment as shown by textural and compositional analysis, such as strontium-rich lawsonite overgrowths. Scales of fluid mobilization remain uncertain and analysis of strontium isotopic ratios will help further constraining the source of fluids and their interactions with the host rock.; La circulation des fluides issus des réactions de déshydratation, intenses dans les métasédiments, a des conséquences majeures sur les propriétés rhéologiques des roches, tout particulièrement dans les zones de subduction, à l'interface entre les plaques. Les méthodes géophysiques y suggèrent la présence, au travers des vitesses des ondes sismiques (Vp/Vs) notamment, de fortes concentrations de fluides entre 30 et 40 km sous la surface. C’est également dans cette gamme de profondeur que de nouveaux types de séismes ont été décrits au début des années 2000 : les séismes lents, pour lesquels il est admis que les fluides jouent un rôle important mais dont le déclenchement, les mécanismes de déformations associés, de même que la source des fluides, leur origine, leur volume et l’échelle et le mode de leur circulation demeurent débattus. Pour améliorer les bilans de production de fluides dans ces gammes de pression – température (de 150 à 350 °C, de 0.3 à 1.2 GPa) et affiner la compréhension de la migration des fluides dans ces roches, nous avons recours à un analogue de terrain maintenant à l’affleurement : le complexe des Schistes Lustrés alpins. La présence ubiquiste de lawsonite dans ces métasédiments, dans la matrice et dans différentes générations de veines, localement en grande abondance, y témoigne d’intenses interactions fluides-roches en profondeur. La lawsonite est d'autant plus importante que ce minéral hydraté (~12 % poids de H2O; de formule théorique CaAl2Si2O7(OH)4.H2O) est aussi connu pour jouer un rôle important dans le recyclage des fluides en contexte de subduction, jusqu’aux conditions de ultra-haute pression (>300 km). La formation d'une telle quantité de lawsonite dans les sédiments pélagiques (alternances de bancs pélitiques et de bancs carbonatés) est toutefois difficile à expliquer et les réactions permettant sa formation sont encore peu documentées. En particulier, la nécessité d’un apport en Ca pour sa cristallisation amène certains auteurs à suggérer la décarbonatation des horizons calcaires, ce qui semble en désaccord avec les observations de terrain et a des implications fortes pour la dynamique du carbone présent en quantités importantes dans ces roches. Dans un premier temps, cette thèse vise à mieux contraindre les réactions de formation de la lawsonite afin de clarifier les échanges de matières effectifs en profondeur. L’étude pétrologique révèle la présence de plusieurs types de lawsonite sur des critères texturaux, micro-structuraux et morphologiques. La majorité des lawsonites observées sur le terrain montre des textures de co-cristallisation avec l’ankérite, et la réaction de formation suivante a été identifiée : chlorite + kaolinite + aragonite = lawsonite + ankérite + quartz + H2O. Cette réaction indique que la formation de lawsonite ne constitue pas une source de carbone, son bilan net étant nul. La modélisation thermodynamique de cette réaction l’identifie comme précoce dans l’enfouissement des Schistes Lustrés (s’initiant vers environ 13 km de profondeur). La cristallisation de lawsonite dans ces roches apparaît toutefois étendue dans le temps et se prolongeant jusqu’au pic métamorphique, du fait du délai cinétique de cette réaction et de l’apparition de réactions additionnelles. Dans un deuxième temps, une étude géochimique fine des éléments traces réalisée sur les différents types de lawsonite rencontrés sur le terrain permet de mettre en évidence deux comportements très différents en terme d’interactions fluides-roches. Si la première génération (LwsA) témoigne d’une cristallisation en système fermé (échelle micro- à millimétrique), la deuxième génération (LwsB) atteste au contraire de la remobilisation de fluides dans un système plus ouvert (échelle métrique à hectométrique). Les observations faites dans cette étude mettent en évidence une ouverture progressive du système que représente les Schistes Lustrés, en terme de circulation de fluides. Cette ouverture se fait de manière incrémentale comme en témoignent les textures et les surcroissances des lawsonites, enrichies en Sr. Les échelles sur lesquelles sont remobilisés les fluides sont encore incertaines et l'étude en cours sur les rapports isotopiques du strontium apportera des éléments de réponses pour mieux contraindre la migration de ces fluides.
- Published
- 2020
5. Real-time investigations on the formation of Cu(In,Ga)(S,Se)2 while annealing Cu–In–Ga precursors with different sulphur–selenium mixtures
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Hölzing, A., Schurr, R., Yoo, H., Wibowo, R.A., Lechner, R., Palm, J., Jost, S., and Hock, R.
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COPPER compounds , *RING formation (Chemistry) , *SELENIDES , *ANNEALING of metals , *CHEMICAL precursors , *SULFUR compounds , *MIXTURES , *CHALCOPYRITE , *PHOTOVOLTAIC cells , *THIN films - Abstract
Abstract: To enhance the conversion efficiency of thin film photovoltaics, chalcopyrite based absorber materials are usually substituted in the cation and anion lattice to yield an absorber with a graded bandgap composed of mixed pentanary crystals Cu(In,Ga)(Se,S)2. Applying in-situ investigations during the crystallisation of the chalcopyrite is a prerequisite to understand the formation of inhomogeneities and elemental gradients caused by the growth process. The variation of anions yields a combined crystallisation path due to metal sulphoselenides with chalcogen exchange reactions upon heating, i.e. copper sulphoselenides act as a chalcogen buffer and afford substitution of S with Se during annealing. The extended chalcogen substitutions occur due to the complete solid solution of S and Se in Cu(S,Se) and Cu2−x(S,Se). On the contrary, different reaction paths are found for the cations. Although the metals show a good intermixture within the intermetallic alloys featuring In–Ga substitutions, no formation of a mixed or ternary (In,Ga)-chalcogenide is observed. This can be attributed to a narrow solid solution range of the (In,Ga)-chalcogenides. As a consequence the preceding formation of an In-rich and the delayed crystallisation of a Ga-rich chalcopyrite cause a vertical elemental gradient with Ga-accumulation near the back electrode. An interdiffusion of the In- and Ga-rich chalcopyrites is observed for increasing annealing time and temperature. The presented study is focused on quantification of the phase evolution, variation of lattice parameter and diffusion of elements as obtained by Rietveld refinements. [Copyright &y& Elsevier]
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- 2013
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6. Investigation of the solid state reactions by time-resolved X-ray diffraction while crystallizing kesterite Cu2ZnSnSe4 thin films
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Yoo, H., Wibowo, R.A., Hölzing, A., Lechner, R., Palm, J., Jost, S., Gowtham, M., Sorin, F., Louis, B., and Hock, R.
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SOLID state chemistry , *CHEMICAL reactions , *CHALCOGENIDES , *KESTERITE , *SOLAR cells , *THIN films , *X-ray diffraction , *CRYSTALLIZATION kinetics - Abstract
Abstract: The pentanary chalcogenide Cu2ZnSn(S,Se)4 (CZTSSe) compound is attracting considerable attention as a low-cost and high-efficient solar cell. The band gap can be tuned by adding Se to pure kesterite Cu2ZnSnS4, which influences the crystallization kinetics. The investigation of the crystallization of the pure selenium (Se) compound Cu2ZnSnSe4 can be helpful in understanding the reaction path between the elements of CZTSSe. Sputtered Cu-poor intermetallic Cu–Zn–Sn precursors were deposited on Mo-coated polyimide foil and sequentially capped by a thermally evaporated Se layer. Two different amounts of Se were deposited: amount that exactly matches the composition of Cu2ZnSnSe4; and that corresponding to twofold excess of the compound''s element ratio. These two compositions were chosen to investigate influences of the amount of Se on the reaction path and kinetics. Also, the reaction of pure metallic Sn with Se was studied by stacking Sn layers on Mo-coated foils for observing a Sn-loss phenomenon. It was also deposited with two different amounts of Se matching approximately the compositions of SnSe and SnSe2. Time-resolved X-ray diffraction was employed to measure the solid state reactions while increasing the sample temperature up to 550°C at a rate of 0.5K/s in an evacuated reaction chamber. After the experiment, sample is analyzed by Raman spectroscopy to distinguish the CZTSe from secondary phases. [Copyright &y& Elsevier]
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- 2013
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7. The influence of gallium on phase transitions during the crystallisation of thin film absorber materials Cu(In,Ga)(S,Se)2 investigated by in-situ X-ray diffraction
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Hölzing, A., Schurr, R., Jost, S., Palm, J., Deseler, K., Wellmann, P., and Hock, R.
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GALLIUM , *PHASE transitions , *CRYSTALLIZATION , *THIN films , *X-ray diffraction , *CHALCOPYRITE crystals , *PHOTOVOLTAIC cells , *WIDE gap semiconductors , *SOLAR spectra - Abstract
Abstract: Chalcopyrite based photovoltaic materials Cu(InxGa1−x)(SySe1−y)2 (CIGSSe) are substituted in the cation and anion lattice to adopt the semiconductor bandgap to the terrestrial solar spectrum. In-situ X-ray diffraction (XRD) investigations on the crystallisation of thin film absorber materials Cu(In,Ga)(S,Se)2 while annealing stacked elemental layers (SEL) show phase transitions proceeding during the chalcopyrite synthesis. Thin layers of metals with elemental ratio Cu:In:Ga=3:2:1 are deposited onto Mo-coated polyimide foil by DC-magnetron sputtering. The metal precursor is covered with S and subsequently Se by thermal evaporation of the elements in chalcogen excess (S+Se)/(Cu+In+Ga)=2.3. Investigated chalcogen ratios reach from pure Se to pure S. Crystalline phases formed during the annealing of SEL are qualitatively determined. The results are compared to conclusions drawn from previous experiments on Ga-free CuIn(S,Se)2 absorbers. The presence of Ga and S influences significantly the time-scale and the temperatures of phase transitions, i.e. the sulfoselenisation of precursor phases Cu16(In,Ga)9 and Cu9(Ga,In)4 proceeds faster with increasing S and is shifted to higher temperatures as compared to Ga-free Cu11In9/Cu16In9. [Copyright &y& Elsevier]
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- 2011
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8. Real-time investigations on the formation reactions during annealing of sulfurized Cu–Sn precursors
- Author
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Schurr, R., Hölzing, A., and Hock, R.
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ANNEALING of metals , *THIN films , *SOLAR cells , *INTERMETALLIC compounds , *TERNARY alloys , *CRYSTALLIZATION , *COPPER compounds , *CHEMICAL reactions , *BINARY metallic systems - Abstract
Abstract: The quaternary compound kesterite Cu2ZnSnS4 (CZTS) is a promising candidate for the production of low-cost thin film solar cells. Depending on the precursor composition and deposition technique several intermetallic precursor phases may appear, affecting the formation reactions during the crystallization process of the thin film absorber. A better understanding of these formation reactions in the system Cu–Zn–Sn–S is required for the optimization of CZTS absorbers and future development of solar modules. The crystallization of CZTS is completed by the reaction of Cu2SnS3 and ZnS. The formation of Cu2SnS3 itself depends on the different available precursor compounds after sulfur evaporation. Incomplete conversion of binary sulfides during annealing may lead to the formation of undesirable compounds, i.e. the transformation of Cu2SnS3 into Cu4SnS4 via reaction with Cu2-x S, which affect or even inhibit the crystallization of CZTS. Therefore a precise knowledge about formation reactions of binary and ternary Cu–Sn sulfides during annealing at low temperatures is important to crystallize a monophase CZTS absorber. Real-time investigations on the formation reactions in the quaternary and also the ternary subsystems of Cu–Zn–Sn–S while annealing stacked elemental layers elucidate the reaction paths of binary and ternary sulfides. We report on results of time-resolved and angle-dispersive XRD experiments during annealing comparing the formation reactions in sulfurized Cu–Sn precursors prepared by different deposition techniques. [Copyright &y& Elsevier]
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- 2011
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9. Potential formation of PCDD/Fs and related bromine-substituted compounds from heating processes for ashes
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Kawamoto, Katsuya
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POLYCHLORINATED dibenzodioxins , *POLYCHLORINATED dibenzofurans , *FLY ash , *INCINERATION , *WASTE management , *SOLID waste , *COPPER catalysts , *BROMINE compounds , *SUBSTITUTION reactions , *REACTION mechanisms (Chemistry) - Abstract
Abstract: Thermal experiments were conducted using real boiler ash and fly ash samples from three types of municipal or industrial solid waste incineration plants to understand the formation reactions of polychlorinated dibenzo-p-dioxin and furans (PCDD/Fs) and related bromine compounds that were chlorinated–brominated dibenzodioxins and furans (PXDD/Fs) and polybrominated dibenzo-p-dioxin and furans (PBDD/Fs). The results obtained were as follows: The formation of PCDD/Fs was clearly shown, and fly ash containing abundant carbon matter had a significant potential for de novo synthesis. The homologous distribution change apparently showed that the formation of PXDD/Fs occurred from the substitution of a bromine atom with a chlorine atom in the PCDD/F molecules. This suggests that PXDD/Fs are usually formed with PCDD/Fs on the ash. PBDD/Fs might be formed from any reaction mechanism different from that of PXDD/Fs. The existence of carbonaceous matters always does not mean the potential formation of PCDD/Fs. However, any addition of catalytic copper may influence the nature of ash to increase the formation potential. The findings suggest that there are many instances that result in the unintended production of trace hazardous pollutants in the incineration process and show that careful and sophisticated control is required to prevent the formation of pollutants. [Copyright &y& Elsevier]
- Published
- 2009
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10. Study on Coordination Behaviour of Manganese Chloride with L-a-Histidine.
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G. Shengli, C. Sanping, L. Huanyong, H. Rongzu, and S. Qizhen
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ENTHALPY , *THERMODYNAMICS , *MANGANESE , *CALORIMETRY , *TEMPERATURE measurements , *THERMOGRAVIMETRY - Abstract
The reaction thermodynamic and kinetic equations for the non-reversible reactions are established. The enthalpy change of formation reaction of manganese(II) histidine (His) complex in water has been determined by microcalorimetry, using manganese chloride with L-a-histidine at 298.15-323.15 K. The standard enthalpy of formation of Mn(His)22+(aq) has been calculated. On the basis of experimental and calculated results, three thermodynamics parameters (the activation enthalpy, the activation entropy and the activation free energy), the rate constants, along with three kinetic parameters (the apparent activation energies, the pre-exponential constant and the reaction order) are obtained. The results show that the reaction easily takes place over the studied temperature range. The solid complex Mn(His)2Cl2·4H2O was prepared and characterized by IR and TG-DTG. [ABSTRACT FROM AUTHOR]
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- 2004
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11. The Thermokinetics of the Formation Reaction of Cobalt Histidine Complex.
- Author
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Shengli, G., Mian, J., Sanping, C., Rongzu, H., and Qizhen, S.
- Abstract
The enthalpy change of formation reaction of cobalt(II) histidine (His) complex in water has been determined by a microcalorimeter, using cobalt chloride with L-α-histidinein the temperature range of 25~50°C. On the basis of experimental and calculated results, three thermodynamics parameters (the activation enthalpies, the activation entropies, the activation free energies), the rate constant, three kinetic parameters (the activation energies, the pre-exponential constant and the reaction order) are obtained. The results show that the titled reaction easily took place in the studied temperature. [ABSTRACT FROM AUTHOR]
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- 2001
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12. Buchwald-Hartwig C-N bond and C-O bond formation reactions
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Li, Jie Jack and Li, Jie Jack
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- 2003
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13. Buchwald-Hartwig C-N bond and C-O bond formation reactions
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Li, Jie Jack and Li, Jie Jack
- Published
- 2002
- Full Text
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14. Diastereoselective synthesis of the C29–C41 fragment of karlotoxin 2.
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Reddy, D. Srinivas, Gaddam, Janardhan, Devunuri, Nagaraju, and Mohapatra, Debendra K.
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STEREOSELECTIVE reactions , *CHEMICAL synthesis , *TOXINS , *ISOMERIZATION , *GRIGNARD reagents , *REGIOSELECTIVITY (Chemistry) - Abstract
A highly diastereoselective synthesis of the C29–C41 fragment of karlotoxin 2 (KmTx2) is described by employing regio-selective epoxide opening, our own developed domino isomerization followed by C–O and C–C bond formation reaction and chelation-controlled Grignard reaction as key steps. The synthesis involves installation of seven stereocenters present in the C29–C41 fragment of karlotoxin 2. [ABSTRACT FROM AUTHOR]
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- 2015
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15. Prediction of thermodynamic properties of formation of HCl at temperatures 200–1000 K.
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Hesam, A., Nikoofard, H., and Sargolzaei, M.
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HARMONIC oscillators , *PARTITION functions , *HYDROGEN chloride , *MOLECULAR vibration , *THERMODYNAMIC functions - Abstract
• The standard molar thermodynamic properties of formation of HCl was studied. • A closed-form expression for the vibration part of the molecular partition function is used. • The internal interaction was modeled by an improved Manning-Rosen oscilator. • Results were compared with the harmonic and an-harmonic oscillator models. In this work, the thermodynamic properties of the formation reaction of hydrogen chloride from the reactants chlorine and hydrogen are studied by employing the developed Manning-Rosen potential. A closed-form expression for the vibration part of the molecular partition function is used to calculate the vibrational contribution of the thermodynamic properties. The results obtained are used to investigate the change in the thermodynamic functions for the formation reaction of HCl at a high temperature range. The predicted results are compared with the ones obtained from the other theoretical approaches based on the harmonic and an-harmonic oscillator models. [ABSTRACT FROM AUTHOR]
- Published
- 2021
- Full Text
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16. Spectrophotometric determination of Sulphamethoxazole Via Charge Transfer Complex Formation Reaction
- Author
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Mohammed S. Al-Enizzi, Thabit S. Al-Ghabsha, and N. Al-Sabha
- Subjects
Reaction conditions ,chemistry.chemical_classification ,Chemistry ,Reaction formation ,Analytical chemistry ,Electron donor ,Electron acceptor ,Charge-transfer complex ,Dosage form ,chemistry.chemical_compound ,Absorption band ,limits of detection (lod) ,formation reaction ,sulphamethoxazole ,lcsh:L ,lcsh:Science (General) ,lcsh:Education ,lcsh:Q1-390 - Abstract
A simple and sensitive spectrophotometric method for the determination of sulphamethoxazole in pure as well as in dosage form is described. The method is based on the reaction of sulphamethoxazole as electron donor with o-chloranil as electron acceptor to form violet colored charge transfer complex having maximum absorption band at 539 nm. Under the optimized reaction conditions, Beer’s law was obeyed in the range of 2-60 μg ml-1 with molar absorptivity 3.675×103 L mol−1cm−1. The limits of detection (LOD) and limit of quantitation (LOQ) were 0.371 and 1.236 μg ml-1 respectively. The accuracy and precision of the method were satisfactory; the average recovery % was 100.95 % and values of relative standard deviations ≤1.06 %. The stoichiometry of the reaction was studied, and the reaction mechanism was postulated. The proposed method was successfully applied to the determination of sulphamethoxazole in its pharmaceutical tablets and syrup with good accuracy and precisions. Keywords: Charge transfer; Spectrophotometry; o-chloranil; sulphamethoxazole
- Published
- 2013
17. Enhancement of Hydrolysis through the Formation of Mixed Heterometal Species: Al3+/CH3Sn3+ Mixtures
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Concetta De Stefano, Alba Giacalone, Rosalia Maria Cigala, Antonio Gianguzza, Silvio Sammartano, Cigala,RM, De Stefano C, Giacalone, A, Gianguzza, A, and Sammartano S
- Subjects
equilibrium analysi ,equilibrium analysis ,mixed hydrolysis of metal ions ,aluminium(III) ,monomethyltin(IV) ,Aqueous solution ,Chemistry ,Stereochemistry ,General Chemical Engineering ,Potentiometric titration ,Empirical relationships, Formation reaction, Mixed species, Mixed systems, Potentiometric technique ,General Chemistry ,Potentiometric technique ,Medicinal chemistry ,Turn (biochemistry) ,Hydrolysis ,Mixed systems ,Mixed species ,Empirical relationships ,Settore CHIM/01 - Chimica Analitica ,Solubility ,mixed hydrolysis of metal ion ,Formation reaction ,Equilibrium constant - Abstract
The hydrolysis of mixed-metal cations (Al3+/CH3Sn3+) was studied in aqueous solutions of NaNO3, at I = 1.00 ± 0.05 mol·dm−3 and T = 298.15 K, by potentiometric technique. Several hydrolytic mixed species are formed in this mixed system, namely, Alp(CH3Sn)q(OH)r with (p, q, r) = (1, 1, 4), (1, 1, 5), (1, 1, 6), (2, 1, 4), (1, 2, 5), (1, 4, 11), (1, 3, 8), and (7, 6, 32). The stability of these species, expressed by the equilibrium: pAl3+ + qCH3Sn3+ + rOH− = Alp(CH3Sn)q(OH)r 3(p+q)−r, βpqr OH, can be modeled by the empirical relationship: log βpqr OH = −3.34 + 2.67p + 9.23(q + r). By using the equilibrium constant Xpqr relative to the formation reaction: pAl(p+q)(OH)r + q(CH3Sn)(p+q)(OH)r = (p + q)Alp(CH3Sn)q(OH)r, it was found that the formation of heterometal mixed species is thermodynamically favored, and the extra stability can be expressed as a function of the difference in the stability of parent homometal species. This leads, in turn, to a significant enhancement of hydrolysis and solubility.
- Published
- 2013
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18. Thermochemistry of the ternary solid complex Gd(C5H8NS2)3(C12H8N2)
- Author
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Chen, S., Meng, X., Xie, G., Gao, S., and Shi, Q.
- Published
- 2006
- Full Text
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19. Study on Coordination Behaviour of Manganese Chloride with L-a-Histidine
- Author
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Shengli, G., Sanping, C., Huanyong, L., Rongzu, H., and Qizhen, S.
- Published
- 2004
- Full Text
- View/download PDF
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