Thermal decomposition of hydronium jarosite (H3O)Fe3(SO4)2(OH)6

Thermogravimetry combined with mass spectrometry has been used to study the thermal decomposition of a synthetic hydronium jarosite. Five mass loss steps are observed at 262, 294, 385, 557 and 619°C. The mass loss step at 557°C is sharp and marks a sharp loss of sulphate as SO₃ from the hydronium jarosite. Mass spectrometry through evolved gases confirms the first three mass loss steps to dehydroxylation, the fourth to a mass loss of the hydrated proton and a sulphate and the final step to the loss of the remaining sulphate. Changes in the molecular structure of the hydronium jarosite were followed by infrared emission spectroscopy. This technique allows the infrared spectrum at the elevated temperatures to be obtained. Infrared emission spectroscopy confirms the dehydroxylation has taken place by 400 and the sulphate loss by 650°C. Jarosites are a group of minerals formed in evaporite deposits and form a component of the efflorescence. The minerals can function as cation and heavy metal collectors. Hydronium jarosite has the potential to act as a cation collector by the replacement of the proton with a heavy metal cation.     

Thermal decomposition of ammonium fluoroferrates (NH4)xFeF2x (2≤x≤3)

Different ammonium fluoroferrates (NH₄)_xFeF_2x (2≤x≤3) have been investigated. The thermal decomposition of the compounds obtained can be interpreted by their identical crystal structures (cryolite type). The decomposition products of all ammonium fluoroferrates formed in initial stage are isostructural of NH₄FeF₄. The decomposition is accompanied by the partial reduction of Fe(III) to Fe(II) by ammonium isolated. The end product of the thermal decomposition is FeF₂ and FeF₃ mixture.     

Thermal decomposition of the layered double hydroxides of formula Cu6Al2(OH)16CO3 and Zn6Al2(OH)16CO3

Zn-Al hydrotalcites and Cu-Al hydrotalcites were synthesised by coprecipitation method and analysed by X-ray diffraction (XRD) and thermal analysis coupled with mass spectroscopy. These methods provide a measure of the thermal stability of the hydrotalcite. The XRD patterns demonstrate similar patterns to that of the reference patterns but present impurities attributed to Zn(OH)₂ and Cu(OH)₂. The analysis shows that the d003 peak for the Zn-Al hydrotalcite gives a spacing in the interlayer of 7.59 ? and the estimation of the particle size by using the Debye-Scherrer equation and the width of the d003 peak is 590 ?. In the case of the Cu-Al hydrotalcite, the d003 spacing is 7.57 ? and the size of the diffracting particles was determined to be 225 ?. The thermal decomposition steps can be broken down into 4 sections for both of these hydrotalcites. The first step decomposition below 100°C is caused by the dehydration of some water absorbed. The second stage shows two major steps attributed to the dehydroxylation of the hydrotalcite. In the next stage, the gas CO₂ is liberated over a temperature range of 150°C. The last reactions occur over 400°C and involved CO₂ evolution in the decomposition of the compounds produced during the dehydroxylation of the hydrotalcite.     

Dynamic disorder in ammonium oxofluorotungstates (NH4)2WO2F4 and (NH4)3WO3F3

Ammonium oxofluorotungstates, (NH₄)₂WO₂F₄ and (NH₄)₃WO₃F₃, are characterized by vibration spectroscopy and quantum chemistry methods with the use of NMR ¹⁹F and ¹H data. It is shown in the approximation of the density-functional theory that in isolated octahedrons [WO₂F₄]^2? and [WO₃F₃]^3? the mutual arrangement of oxygen atoms in cis-position corresponds to the energy minimum. The presence of intraspheric disorder in [WO₃F₃]^3? (unlike [WO₂F₄]^2?) explains the complex character of vibrational spectra of this anion and eliminates existent in the literature differences in their interpretation (between C _2v and C _3v structure variants). Models of intraspheric dynamics of [WO₃F₃]^3? are discussed.     

Thermal decomposition of liebigite

Summary A combination of high resolution thermogravimetric analysis coupled to a gas evolution mass spectrometer has been used to study the thermal decomposition of liebigite. Water is lost in two steps at 44 and 302°C. Two mass loss steps are observed for carbon dioxide evolution at 456 and 686°C. The product of the thermal decomposition was found to be a mixture of CaUO₄ and Ca₃UO₆. The thermal decomposition of liebigite was followed by hot-stage Raman spectroscopy. Two Raman bands are observed in the 50°C spectrum at 3504 and 3318 cm^-1 and shift to higher wavenumbers upon thermal treatment; no intensity remains in the bands above 300°C. Three bands assigned to the υ₁ symmetric stretching modes of the (CO₃)^2- units are observed at 1094, 1087 and 1075 cm^-1 in agreement with three structurally distinct (CO₃)^2- units. At 100°C, two bands are found at 1089 and 1078 cm^-1. Thermogravimetric analysis is undertaken as dynamic experiment with a constant heating rate whereas the hot-stage Raman spectroscopic experiment occurs as a staged experiment. Hot stage Raman spectroscopy supports the changes in molecular structure of liebigite during the proposed stages of thermal decomposition as observed in the TG-MS experiment.     

Thermal decomposition of struvite

Struvite (NH₄MgPO₄·6H₂O) is a mineral often found in urinary tracts and kidneys. Thermal decomposition using slow low heating shows that the 'kidney' stone can be decomposed at temperatures below 40°C. At this temperature both ammonia and water are evolved. If more rapid heating is employed the decomposition occurs at around 80°C. The implication of this work rests with the use of low slow heat for the decomposition of the kidney stones. This revised version was published online in July 2006 with corrections to the Cover Date.     

Thermal decomposition of jarosites of potassium,sodium and lead

Summary Jarosites are a group of minerals formed in evaporite deposits and form a component of efflorescence. As such the minerals can function as cation and heavy metal collectors. Thermogravimetry coupled to mass spectrometry has been used to study three Australian jarosites which are predominantly K, Na and Pb jarosites. Mass loss steps of K-jarosite occur over the 130 to 330 and 500 to 622°C temperature range and are attributed to dehydroxylation and desulphation. In contrast the behaviour of the thermal decomposition of Na-jarosite shows three mass loss steps at 215 to 230, 316 to 352 and 555 to 595°C. The first mass loss step for Na-jarosite is attributed to deprotonation. For Pb-jarosite two mass loss steps associated with dehydroxylation are observed at 390 and 418°C and a third mass loss step at 531°C is attributed to the loss of SO₃. Thermal analysis is an excellent technique for the study of jarosites. The analysis depends heavily on the actual composition of the jarosite.     

Thermal decomposition of Fe2(SO4)3: Demonstration of Fe2O3 polymorphism

The mechanism of the thermal decomposition of Fe₂(SO₄)₃ in air has been studied at different temperatures (520-700 °C) using mainly ⁵⁷Fe Mössbauer spectroscopy. Iron(III) oxides with corundum (), bixbyite (), spinel () and orthorhombic () structures were identified as solid products of this conversion. A significant influence of the heating temperature on the decomposition mechanism and on the phase composition of reaction products was found.     

Thermal decomposition of the synthetic hydrotalcite iowaite

The thermal stability and thermal decomposition pathways for synthetic iowaite have been determined using thermogravimetry in conjunction with evolved gas mass spectrometry. Chemical analysis showed the formula of the synthesised iowaite to be Mg_6.27Fe_1.73(Cl)_1.07(OH)₁₆(CO₃)_0.336.1H₂O and X-ray diffraction confirms the layered structure. Dehydration of the iowaite occurred at 35 and 79°C. Dehydroxylation occurred at 254 and 291°C. Both steps were associated with the loss of CO₂. Hydrogen chloride gas was evolved in two steps at 368 and 434°C. The products of the thermal decomposition were MgO and a spinel MgFe₂O₄. Experimentally it was found to be difficult to eliminate CO₂ from inclusion in the interlayer during the synthesis of the iowaite compound and in this way the synthesised iowaite resembled the natural mineral.     

Study of the Dehydration/Rehydration of Ammonium Tris-Oxalato Aluminate(III) (NH4)3Al(C2O4)3⋅3H2O at Controlled Atmosphere

The study of the dehydration/rehydration of ammonium tris-oxalato aluminate(III) (NH₄)₃Al(C₂O₄)₃⋅3H₂O in flowing dinitrogen saturated with water vapor at room temperature, using thermogravimetric analysis and X-ray diffraction techniques, allowed the determination of the temperature stability domains of (NH₄)₃Al(C₂O₄)₃⋅3H₂O, (NH₄)₃Al(C₂O₄)₃⋅2H₂O and the anhydrous salt. The X-ray powder diffraction profiles are reported for each of the three phases. This revised version was published online in August 2006 with corrections to the Cover Date.     

Thermal decomposition of synthetic hydrotalcites reevesite and pyroaurite

A combination of high resolution thermogravimetric analysis coupled to a gas evolution mass spectrometer has been used to study the thermal decomposition of synthetic hydrotalcites reevesite (Ni₆Fe₂(CO₃)(OH)₁₆·4H₂O) and pyroaurite (Mg₆Fe₂(SO₄,CO₃)(OH)₁₆·4H₂O) and the cationic mixtures of the two minerals. XRD patterns show the hydrotalcites are layered structures with interspacing distances of around 8.0. Å. A linear relationship is observed for the d(001) spacing as Ni is replaced by Mg in the progression from reevesite to pyroaurite. The significance of this result means the interlayer spacing in these hydrotalcites is cation dependent. High resolution thermal analysis shows the decomposition takes place in 3 steps. A mechanism for the thermal decomposition is proposed based upon the loss of water, hydroxyl units, oxygen and carbon dioxide.     

Synthesis and Thermal Behavior of the Hydrogen Praseodymium Diphosphate (HPrP2O7·3H2O)

The preparation of a new acid lanthanide diphosphate is reported. The acid praseodymium diphosphate, obtained as a trihydrate salt, is investigated by chemical analysis, X-ray powder diffraction and IR spectroscopy. The study of the thermal behavior of HPrP₂O₇·3H₂O shows that its dehydration begins at 367 K. A scheme of its decomposition is proposed.This revised version was published online in November 2005 with corrections to the Cover Date.     

Thermal decomposition of humboldtine: A high resolution thermogravimetric and hot stage Raman spectroscopic study

Evidence for the existence of primitive life forms such as lichens and fungi can be based upon the formation of oxalates. These oxalates form as a film like deposit on rocks and other host matrices. Humboldtine as the natural iron(II) oxalate mineral is a classic example. Thermogravimetry coupled to evolved gas mass spectrometry shows dehydration takes place in two steps at 130 and 141°C. Loss of the oxalate as carbon dioxide occurs at 312 and 332°C. Dehydration is readily followed by Raman microscopy in combination with a thermal stage and is observed by the loss of intensity of the OH stretching vibration at 3318 cm^-1. The application of infrared emission spectroscopy supports the results of the TG-MS. Three Raman bands are observed at 1470, 1465 and 1432 cm^-1 attributed the CO symmetric stretching mode. The observation of the three bands supports the concept of multiple iron(II) oxalate phases. The significance of this work rests with the ability of Raman spectroscopy to identify iron(II) oxalate which often occurs as a film on a host rock.This revised version was published online in November 2005 with corrections to the Cover Date.     

Thermal decomposition of polycrystalline [Ni(NH3)6](NO3)2

The thermal decompositions of polycrystalline samples of [Ni(NH₃)₆](NO₃)₂ were studied by thermogravimetric analysis with simultaneous gaseous products of the decomposition identified by a quadruple mass spectrometer. Two measurements were made for samples placed in alumina crucibles, heated from 303 K up to 773 K in the flow (80 cm³ min^?1) of Ar 6.0 and He 5.0, at a constant heating rate of 10 K min^?1. Thermal decomposition process undergoes two main stages. First, the deamination of [Ni(NH₃)₆](NO₃)₂ to [Ni(NH₃)₂](NO₃)₂ occurs in four steps, and 4NH₃ molecules per formula unit are liberated. Then, decomposition of survivor [Ni(NH₃)₂](NO₃)₂ undergoes directly to the final decomposition products: NiO_1+x, N₂, O₂, nitrogen oxides and H₂O, without the formation of a stable Ni(NO₃)₂, because of the autocatalytic effect of the formed NiO_1+x. Obtained results were compared both with those published by us earlier, by Farhadi and Roostaei-Zaniyani later and also with the results published by Rejitha et al. quite recently. In contradiction to these last ones, in the first and second cases agreement between the results was obtained.     

Thermal decomposition of [Co(NH3)6]Cl3

The thermal decomposition reactions of [Co(NH₃)₆]Cl₃ were determined in dynamic argon and air atmospheres. The investigations were carried out with simultaneous TG-DTG-DTA measurements under non-isothermal conditions, thermogravimetry under quasi-isothermal conditions, reflectance spectroscopy, absorption spectroscopy, X-ray diffraction and chemical analysis. The data show that the thermal decomposition of [Co(NH₃)₆]Cl₃ occurs in three and four stages in argon and air atmospheres, respectively. The determined sequences are in agreement with that proposed by Simons and Wendlandt [2, 5].The changes in the morphology of the studied complex crystalline powder in the course of thermal decomposition in air were followed by scanning electron microscopy.

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Zusammenfassung In bewegter Argon- und Luftatmosphäre wurden die Zersetzungsreaktionen für [Co(NH₃)₆]Cl₃ bestimmt. Zu den Untersuchungen wurden folgende Methoden zu Hilfe gezogen: simultane TG-DTG-DTA-Messungen unter nichtisothermen Bedingungen, Thermogravimetrie unter quasi-isothermen Bedingungen, Remissionsspektroskopie, Absorptionsspektroskopie, Röntgendiffraktion und chemische Analyse. Die Ergebnisse zeigen, daß sich [Co(NH₃)₆]Cl₃ in Argon in drei und in Luft in vier Schritten thermisch zersetzt. Die festgestellten Sequenzen stehen in Übereinstimmung mit den von Simon und Wendlandt [2, 5] vorgeschlagenen. Veränderungen in der Morphologie des untersuchten Komplexkristallpulvers wurden über die thermische Zersetzung in Luft mittels Scanning-Elektronen-Mikroskopie beobachtet.

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[Co(NH₃)₆]Cl₃. , , - , , , . , , , , , , .

     

Thermal decomposition of (NH4)2MoS4 and (NH4)2WS4heat of formation of (NH4)2MoS4

The reactions (NH₄)₂MeS₄ = 2 NH₃ + H₂S + MeS₃ (Me = Mo, W) were investigated by measuring the decomposition vapour pressures. Thermochemical data were obtained from these measurements: ΔH = 52 kcal/mole and ΔS = 105 cal/deg.mole for the decomposition of the tetrathiomolybdate. Similarly, ΔH = 69 kcal/mole and ΔS = 106 cal/deg.mole were obtained for the decomposition of the tetrathiotungstate. The normal heat of formation of (NH₄)₂MoS₄ was found to be ΔH = ?140 kcal/mole. The kinetics of thermal decomposition of the above reactions were also measured.     

Interpretation der Schwingungsspektren von (CH3)2SO2, (CH3)2SO(NH) und (CH3)2S(NH)2 unter Verwendung eines Kopplungsstufenverfahrens

Normal Coordinate Analysis of (CH₃)₂SO₂, (CH₃)₂SO(NH), and (CH₃)₂S(NH)₂ using the Method of Stepwise Coupling The qualitative assignment of the vibrational spectra of (CH₃)₂SO₂ ( 1 ), (CH₃)₂SO(NH) ( 2 a ), and (CH₃)₂S(NH)₂ ( 3 a ) and of the C and N deuterated derivatives of 2 a and 3 a is used in a normal coordinate analysis by the method of stepwise coupling. The force constants and the energy distributions are calculated in symmetry coordinates using a generalized valence force field.     

(NH4)6Nd(NO3)9, ein ammoniumreiches ternäres Lanthanidnitrat mit einsamen Nitrationen: (NH4)6[Nd(NO3)6](NO3)3

(NH₄)₆Nd(NO₃)₉, A Ternary Ammonium-Rich Lanthanide Nitrate with Lonesome Nitrate Ions: (NH₄)₆[Nd(NO₃)₆](NO₃)₃ . Single crystals of the ternary ammonium neodymium nitrate (NH₄)₆Nd(NO₃)₉ are obtained from a solution of Nd₂O₃ in a melt of NH₄NO₃. In the crystal structure (monoclinic, C 2/c, Z = 4, a = 1 775.1(4), b = 912.7(3), c = 2 072.3(5) pm; β = 125.56(1)°; R = 0.059, R_w = 0.036) the Nd³⁺ ion is surrounded by six bidentate nitrate ligands so that anionic units [Nd(NO₃)₆]^3? are formed. The units are isolated, but they are incorporated in layers parallel to (010). The structure is held together by a network of hydrogen bonds, built up by NH₄⁺ and NO₃^? ions lying between the layers. Due to the structure, the compound may be described as a double salt like (NH₄)₃[Nd(NO₃)₆] · 3 NH₄NO₃ or, better, as (NH₄)₆[Nd(NO₃)₆](NO₃)₃.     

Thermal behaviour of [CoCO3(NH3)4]2SO4 · 3H2O

The thermal behaviour of [CoCO₃(NH₃)₄]₂SO₄ · 3H₂O was studied using X-ray diffraction diagrams, DTA, TG and heating at constant temperatures for different periods of time. The X-ray study was made in order to characterize with the powder diagrams the phases obtained and to follow the reactions of the complex when heated in air up to 800. A parallel infrared spectral study was also made. The results obtained by the various experimental methods were compared with the theoretical weight losses.

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Zusammenfassung Das thermische Verhalten von [CoCO₃(NH₃)₄]₂SO₄ · 3H₂O wurde durch Röntgendiffraktion, DTA, TG und Erhitzen auf gleiche Temperatur in verschiedenen Zeiten, untersucht. Die röntgenographische Prüfung diente zum Kennzeichnen der erhaltenen Phasen durch Pulverdiagramme und zur Verfolgung der in Luft bis 800 im Komplex verlaufenden Reaktionen. Es wurde parallel auch eine Prüfung durch infrarote Spektroskopie unternommen. Die auf verschiedene Weise erhaltenen Ergebnisse wurden miteinander in Einklang gebracht.

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Résumé On a étudié le comportement thermique de [CoCO₃(NH₃)₄]₂SO₄ · 3H₂O par diffraction de rayons X, ATD et ATG avec maintien en thermostat. L'étude par rayons X a été menée dans le but de caractériser les phases obtenues par leur diagramme de poudre et de suivre les réactions données par le complexe chauffé dans l'air jusqu'à 800. En raison de l'impossibilité de suivre l'évolution thermique par rayons X, une étude parallèle a été effectuée par spectrographie infrarouge. On a essayé de rapprocher les résultats obtenus à l'aide de ces différentes méthodes.

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[CoCo₃(NH₃)₄]₂SO₄·3H₂O , , , . 800. . , , , .

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This work has been carried out, in part, through the Ayuda para el Fomento de la Investigación en la Universidad.