Synthesis, characterization and thermal study of solid mandelate of some bivalent transition metal ions in CO2 and N2 atmospheres

Solid state M-L, where M stands for bivalent transition metals (Mn(II), Fe(II), Co(II), Ni(II), Cu(II) and Zn(II)) and L is mandelate, were synthesized. Simultaneous thermogravimetry and differential scanning calorimetry, elemental analysis and complexometry were used to establish the stoichiometry and to study the thermal behaviour of these compounds in CO2 and N2 atmospheres. The results show that all the compounds were obtained in the anhydrous state and in agreement with the general formula ML2. The thermal decomposition of the compounds occurs in a single (Cu(II)), two (Ni(II)) three (Fe(II), Co(II)), four (Mn(II)) and five (Zn(II)) steps. The results also provided information concerning the ligand's denticity, thermal behaviour, final residues and identification of gaseous products evolved during the thermal decomposition of these compounds. © 2012 Akadémiai Kiadó, Budapest, Hungary.

Thermal behaviour of α-hydroxyisobutyric acid, sodium α-hydroxyisobutyrate and its compounds with some bivalent transition metal ions

Synthesis, characterization and thermal decomposition of bivalent transition metal α-hydroxyisobutyrates, M(C4H7O 3)2·nH2O (M = Mn(II), Fe(II), Co(II), Ni(II), Cu(II), Zn(II)), as well as the thermal behaviour of α-hydroxyisobutyric acid and its sodium salt were investigated employing simultaneous thermogravimetry and differential scanning calorimetry (TG-DSC), infrared spectroscopy (FTIR), TG-DSC coupled to FTIR, elemental analysis and complexometry. All the compounds were obtained as dihydrated, except the copper one which was obtained in the anhydrous state. The thermal decomposition of the anhydrous compounds occurs in a single or two steps and the final residue up to 235 C (Mn), 300 C (Fe), 305 C (Co), 490 C (Ni), 260 C (Cu) and 430 C (Zn) is Mn2O3, Fe2O3, Co3O 4, NiO, CuO and ZnO, respectively. The results also provided information concerning the ligand's denticity and identification of the gaseous products evolved during the thermal decomposition of these compounds. Copyright © 2013 Published by Elsevier B.V. All rights reserved.

Síntese, caracterização e estudo termoanalítico dos succinatos de alguns metais de transição bivalentes no estado sólido

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Síntese, caracterização e estudo termoanalítico dos mandelatos de alguns metais de transição bivalentes no estado sólido

Pós-graduação em Química - IQ

Sistemas de uso e manejo do solo: acúmulo de carbono e atributos físicos

Pós-graduação em Agronomia (Produção Vegetal) - FCAV

Determinação de metais em água produzida de petróleo

In order to enable the reuse of the large surplus volume of petroleum produced water for irrigation of crops inedible, the quality evaluation of this water is very important. This work aimed to evaluate the effectiveness of the diffusive gradient in thin films technique (DGT) for the determination of labile Cu (II), Mn (II) and Zn (II) in petroleum produced water destined to reuse in agriculture. Samples were collected at the exit of the wastewater treatment plant (WWTP) (after separation oil/water and flotation) of a Petrobrás onshore production region. Basically, the laboratory experiments with DGT devices involved the evaluation of the behavior of the main variables of the technique for determination of analytes in the samples (diffusion coefficients, immersion time, fractionation of organic and inorganic species, and performance of diffusion gels with different porosities, among others). Also, experiments were conducted based on the solid phase extraction (SPE) protocol with Chelex- 100 resin using previously established protocols to support the study. During the project the possibility of in situ immersions in water treatment plants was evaluated. The DGT technique presented satisfactory results for determination of Mn in produced water, and can be used for in situ determinations. However, the results obtained for Cu and Zn show the need of additional studies

Single-wall carbon nanotube interactions with copper-oxamato building block of molecule-based magnets probed by resonance Raman spectroscopy

The electronic interactions between the [Cu(opba)]2- anions (where opba is orthophenylenebis (oxamato)) and single-wall carbon nanotubes (SWCNTs) were investigated by resonance Raman spectroscopy. The opba can form molecular magnets, and the interactions of opba with SWCNTs can produce materials with very different magnetic/electronic properties. It is observed that the electronic interaction shows a dependence on the SWCNT diameter independent of whether they are metallic or semiconducting, although the interaction is stronger for metallic tubes. The interaction also is dependent on the amount of complex that is probably adsorbed on the carbon surface of the SWCNTs. Some charge transfer can be also occurring between the metallic complex and the SWCNTs. Copyright (c) 2012 John Wiley & Sons, Ltd.

Continuous-Flow Magnetic Separation with Permanent Magnets for Water Treatment

More efficient water treatment technologies would decrease the water bodies’ pollution and the actual intake of water resource. The aim of this thesis is an in-depth analysis of the magnetic separation of pollutants from water by means of a continuous-flow magnetic filter subjected to a field gradient produced by permanent magnets. This technique has the potential to improve times and efficiencies of both urban wastewater treatment plants and drinking water treatment plants. It might also substitute industrial wastewater treatments. This technique combines a physico-chemical phase of adsorption and a magnetic phase of filtration, having the potential to bond magnetite with any conventional adsorbent powder. The removal of both Magnetic Activated Carbons (MACs) and zeolite-magnetite mix with the addition of a coagulant was investigated. Adsorption tests of different pollutants (surfactants, endocrine disruptors, Fe(III), Mn(II), Ca(II)) on these adsorbents were also performed achieving good results. The numerical results concerning the adsorbent removals well reproduced the experimental ones obtained from two different experimental setups. In real situations the treatable flow rates are up to 90 m3/h (2000 m3/d).

Zweikernige 3d-Übergangsmetall-Komplexe mit Derivaten des para-Phenylendiamins als redoxaktive Brückenliganden

Die vorliegende Arbeit beschäftigt sich mit der Darstellung zweikerniger Koordinationsverbindungen, bei denen zweiwertige Ionen der 3d-Übergangsmetalle über einen bestimmten Liganden verbrückt sind. Dieser Brückenligand, das N,N,N‘,N‘-Tetrakis-(2-methylpyridyl)-benzol-1,4-diamin (TPBD), besteht aus einem p-Phenylendiamin-Gerüst, an dessen Stickstoffe je zwei Methylpyridin-Gruppen gebunden sind. In diesen zwei jeweils dreizähnigen Bindungstaschen wurden 3d-Übergangsmetallionen komplexiert, wobei deren Koordinationssphäre mit einem zweizähnigen capping-Liganden vom Typ des 1,10-Phenanthrolins und einem einzähnigen dritten Liganden abgesättigt wird. Die strukturellen, magnetischen und elektronischen Eigenschaften der so erhaltenen homometallischen Komplexe mit Mn(II), Fe(II), Co(II), Ni(II), Cu(II) und Zn(II) wurden untersucht. Dabei wurde besonderes Augenmerk auf die Veränderung dieser Eigenschaften bei dem Einsatz unterschiedlicher capping- und dritter Liganden gerichtet. Die schwach antiferromagnetische Wechselwirkung der metallzentrierten Spins über den Brückenliganden führt dabei stets zu einem diamagnetischen Grundzustand, was diese als mögliche Einzelmolekülmagnete ausschließt. Mit der Oxidierbarkeit des Liganden zu seiner radikalischen Spezies besteht die Möglichkeit, einen zusätzlichen Spin in dem System zu erzeugen, woraus ein Spingrundzustand von ungleich null resultiert. Es zeigte sich, dass die Lebensdauer der radikalischen Spezies eine starke Abhängigkeit sowohl von den eingesetzten Metallionen als auch den weiteren Liganden besitzt. Auch vier Derivate des ursprünglichen Brückenliganden konnten synthetisiert und deren Oxidierbarkeit zu den entsprechenden Radikalformen gezeigt werden. Neben der Darstellung homometallischer Komplexe gelang zudem die Synthese und Strukturaufklärung dreier heterometallischer zweikerniger Komplexe mit Mn(II), Co(II) und Ni(II) als Metallionen. Es konnte gezeigt werden, dass diese auch ohne die Oxidation des Brückenliganden bei schwacher antiferromagnetischer Wechselwirkung der Spins einen paramagnetischen Spingrundzustand besitzen.

Modellkomplexe zur Sauerstoffaktivierung auf Basis des 1,3,4-Thiadiazols

Das Ziel der vorliegenden Arbeit waren die Synthese und Untersuchung von Modellverbindungen zur Sauerstoffaktivierung auf der Basis neuer Ligandensysteme des 1,3,4-Thiadiazols unter Ausarbeitung einer Synthesestrategie zur Derivatisierung der heteroaromatischen 1,3,4-Thiadiazol-Liganden, deren Koordinationsverhalten in Abhängigkeit ihres 2,5-Substitutionsmusters untersucht wurde, sowie die fortführende Bearbeitung bereits bekannter Ligandensysteme zur Erzeugung von homo- und heterovalenten Übergangsmetallkomplexverbindungen.rnDie unter der Verwendung der modifizierten Liganden TPDE, H1TPDP und H1BPMP resultierenden dinuklearen Komplexverbindungen zeigen unterschiedlich starke antiferromagnetische Wechselwirkungen in Abhängigkeit der vorhandenen Brückenliganden. In der Verbindung [Fe6O2(OH)(L´)2(OOCMe3)9(OEt)2] trat eine Fragmentierung des Liganden H1TPDP auf. Das cisoide Ligandensubstitutionsmuster der entstandenen sechskernigen Verbindung ist verantwortlich für die interessanten magnetischen Eigenschaften des Komplexes. rnNeue Perspektiven zur Erzeugung von Modellverbindungen zur Sauerstoffaktivierung wurden mit dem Mono-Chelatliganden H1ETHP und den Bis-Chelatliganden HL2H, H2L2H und H2BATP aufgezeigt. Die Umsetzung von H1ETHP mit verschiedenen Übergangsmetallsalzen resultierte für die Metalle Cr(III), Fe(III), Co(III) und Ni(II) in mononuklearen Verbindungen des Typs [M(ETHP)2]X (X = ClO4, FeCl4, OMe, Cl, Br) sowie in zwei tetranuklearen Verbindungen mit Mn(II) und Cu(II). [Mn4(ETHP)6] besitzt ein propellerförmiges, planares [Mn4O6]2+-System mit einen Spingrundzustand von S = 5. In allen Verbindungen von H1ETHP konnte eine mono-κN-Koordination des 1,3,4-Thiadiazol-Rückgrates über eines seiner beiden endozyklischen Stickstoffdonoratome beobachtet werden. rnAus Umsetzungen der Bis-Chelatliganden wurden fast ausschließlich polynukleare Übergangsmetallkomplexe erhalten. Insbesondere der Ligand H2L2H zeigt eine ausgeprägte Tendenz zur Ausbildung trinuklearer, linearer Komplexe, welche auf Grund ihrer ungeraden Anzahl von Übergangsmetallionen einen Spingrundzustand S ≠ 0 aufweisen.rn Die mit dem Liganden HL2H erhaltenen Verbindungen unterstreichen die hohe Flexibilität dieser Systeme hinsichtlich der Erzeugung polynuklearer und heterovalenter Komplexverbindungen. So konnten in Abhängigkeit vom verwendeten Übergangsmetallsalz trinukleare, pentanukleare, aber auch hepta- und oktanukleare Verbindungen synthetisiert werden. Insbesondere die Komplexe des Mangans und des Cobalts zeigen ein heterovalentes [MnIIMnIII4]- bzw. [CoII2CoIII3]-Motiv, was sich in Spingrundzuständen von S ≠ 0 äußert. Der diamagnetische, achtkernige Fe8-Cluster besitzt eine pseudo C3-symmetrische Anordnung der Metall-Zentren, während für die heptanukleare Cu7-Kette durch ihre stark unterschiedlichen Kupfer-Koordinationsgeometrien interessante magnetische Austauschwechselwirkungen beobachtet werden konnten. Der dreikernige µ3-oxo-verbrückte Komplex des Liganden H2BATP zeigt als interessante strukturelle Eigenschaft ein ein µ3-Verbrückungsmuster des eingesetzten Sulfat-Anions. rnIn allen Komplexen der Bis-Chelatliganden HL2H, H2L2H und H2BATP konnte ein µ2-κN,κN-Koordiantionsmodus des 1,3,4-Thiadiazols und somit eine Abhängigkeit der Verbrückung vom Ligandensubstitutionsmuster beobachtet werden.rn

Crystalline, Mixed-Valence Manganese Analogue of Prussian Blue: Magnetic, Spectroscopic, X-ray and Neutron Diffraction Studies

The compound of stoichiometry Mn(II)3[Mn(III)(CN)6]2·zH2O (z = 12−16) (1) forms air-stable, transparent red crystals. Low-temperature single crystal optical spectroscopy and single crystal X-ray diffraction provide compelling evidence for N-bonded high-spin manganese(II), and C-bonded low-spin manganese(III) ions arranged in a disordered, face-centered cubic lattice analogous to that of Prussian Blue. X-ray and neutron diffraction show structured diffuse scattering indicative of partially correlated (rather than random) substitutions of [Mn(III)(CN)6] ions by (H2O)6 clusters. Magnetic susceptibility measurements and elastic neutron scattering experiments indicate a ferrimagnetic structure below the critical temperature Tc = 35.5 K.

Geochemistry on sediments in Lake Biwa

Thirty sediment cores (30-40 cm in length), 47 Ekman dredge sediments, and Mn concretions were collected from Lake Biwa. The concentrations of 36 elements in the samples were determined by instrumental neutron activation, X-ray fluorescence, atomic absorption, and colorimetric analyses. The elements determined included Mn, P, As, Sb, Fe, Ni, Co, Zn, Cu, Pb, Hg, Cr, Ti, Na, K, Rb, Cs, Mg, Ca, Sr, Ba, Sc, Hf, La, Ce, Sm, Eu, Yb, Lu, U, Th, Au, Ta, Nd, Br and N. Based on statistical considerations and calculation of the concentration factors of the elements, the features of the elemental distribution in Lake Biwa sediment were determined. The main results are summarized as follows : (1) Concentrations of Mn and As were very high in the uppermost oxidized layer of the offshore sediment and Mn concretions. This resulted from the dissolution-deposition cycles of these elements within the sedimentary column and the bottom water. The fixation of As at the sediment surface is mainly attributed to the adsorption of arsenate onto Mn (II) -rich hydrous Mn (IV) oxide. (2) There were high concentrations of Zn, Cu, Pb and Hg in the recent sediments. Although the source of these elements is attributed to human activities, the individual distributions of Zn and Cu in the sediment may result from the deposition of metal-rich planktonic debris and subsequent degradation of the debris. (3) The orders of increasing concentrations of alkali metals and lanthanides in the sediment from the central region compared with the nearshore pediment were identical to the orders of increasing atomic numbers from Na to Cs and from La to Lu, respectively.

Major and rare earth element composition of ODP Site 191-1179 sediments, northwest Pacific

Depth profiles of major element and rare earth element (REE) abundances in sediment samples (mainly siliceous ooze and clay) recovered from Holes 1179B and 1179C at Site 1179, Ocean Drilling Program Leg 191 (41.4°N, 159.6°E) were determined. The oxidation states of Mn and Ce were determined by X-ray absorption near-edge structure. Some geochemical indicators were tested, including the MnO/TiO2 ratios, a bivariate diagram of La/Ce vs. Al2O3/(Al2O3+Fe2O3), and other discrimination diagrams. The oxidation state of Mn is reduced Mn(II) in the depth profile below 0.60 meters below seafloor (mbsf), which is consistent with relatively low and high abundances of Mn in the sediments and pore waters, respectively. It is possible that the diagenetic effect on the oxidation state and abundance of Mn makes it difficult for the MnO/TiO2 ratio to reflect the depositional environment. The normalized ratio of La and Ce does not change very much with depth, suggesting that the diagenetic effect does not affect the REE signature in the sediments. On the diagram of La/Ce vs. Al2O3/(Al2O3+Fe2O3), the sediments studied here plot at the boundary of the pelagic and continental margin fields. This suggests that continental material has contributed to the sediment to some degree, even though Site 1179 is in a pelagic region of the northwestern Pacific Ocean, >1600 km from Japan.

Composition of rocks, minerals, water, and gases from uplift areas of the Central Atlantic

Original geological, geophysical, lithological, mineralogical data on uplifts of the Central Atlantic are given in the book based on materials of Cruise 1 of the R/V Akademik Nikolaj Strakhov. Geological and geophysical studies include description of the obtained material and analysis of structural and morphological elements of the ocean floor. Results of lithological, petrochemical and geochemical studies were extremely innovative and develop a conceptual model. The latter include studies of petrochemical evolution of tholeiitic alkaline plate volcanism, large-scale hydrothermal transformation of basement rocks - palygorskitization, phosphatization and ferromanganese mineralization. Showing imposition Superposition of hydrogenic alteration on hydrothermally altered rocks and its role in Cenozoic history of sedimentation is shown.

Coordinate regulation of Bacillus subtilis peroxide stress genes by hydrogen peroxide and metal ions.

The Bacillus subtilis mrgA gene encodes an abundant DNA-binding protein that protects cells against the lethal effects of H2O2. Transcription of mrgA is induced by H2O2 or by entry into stationary phase when manganese and iron levels are low. We have selected for strains derepressed for transcription of mrgA in the presence of Mn(II). The resulting cis-acting mutants define an operator site just upstream of the mrgA promoter. Similar sequences flank the promoters for the catalase gene, katA, and the heme biosynthesis operon, hemAXCDBL. Like mrgA, transcription of the katA and hem genes is repressed by Mn(II), which thereby potentiates the killing action of H2O2. We identified two classes of trans-acting mutants derepressed for mrgA transcription in the presence of Mn(II): some exhibit a coordinate derepression of MrgA, catalase, heme biosynthesis, and alkyl hydroperoxide reductase and are H2O2 resistant, while others have reduced catalase activity and are H2O2 sensitive. These data indicate that the peroxide stress response of B. subtilis is regulated by a repressor that senses both metal ion levels and H2O2.