Spectroscopic and Catalytic Characterization of a Functional (FeFeII)-Fe-III Biomimetic for the Active Site of Uteroferrin and Protein Cleavage

A mixed-valence complex, [Fe(III)Fe(II)L1(mu-OAc)(2)]BF4 center dot H2O, where the ligand H(2)L1 = 2-{[[3-[((bis-(pyridin-2-ylmethyl)amino)methyl)-2-hydroxy-5-methylbenzyl](pyridin-2-ylmethyl)amino]methyl]phenol}, has been studied with a range of techniques, and, where possible, its properties have been compared to those of the corresponding enzyme system purple acid phosphatase. The (FeFeII)-Fe-III and Fe-2(III) oxidized species were studied spectroelectrochemically. The temperature-dependent population of the S = 3/2 spin states of the heterovalent system, observed using magnetic circular dichroism, confirmed that the dinuclear center is weakly antiferromagnetically coupled (H = -2JS(1).S-2, where J = -5.6 cm(-1)) in a frozen solution. The ligand-to-metal charge-transfer transitions are correlated with density functional theory calculations. The (FeFeII)-Fe-III complex is electron paramagnetic resonance (EPR)-silent, except at very low temperatures (<2 K), because of the broadening caused by the exchange coupling and zero-field-splitting parameters being of comparable magnitude and rapid spin-lattice relaxation. However, a phosphate-bound Fe-2(III) complex showed an EPR spectrum due to population of the S-tot = 3 state (J= -3.5 cm(-1)). The phosphatase activity of the (FeFeII)-Fe-III complex in hydrolysis of bis(2,4-dinitrophenyl)phosphate (k(cat.) = 1.88 x 10(-3) s(-1); K-m = 4.63 x 10(-3) mol L-1) is similar to that of other bimetallic heterovalent complexes with the same ligand. Analysis of the kinetic data supports a mechanism where the initiating nucleophile in the phosphatase reaction is a hydroxide, terminally bound to Fe-III. It is interesting to note that aqueous solutions of [Fe(III)Fe(II)L1(mu-OAc)(2)](+) are also capable of protein cleavage, at mild temperature and pH conditions, thus further expanding the scope of this complex's catalytic promiscuity.

Molecular chemistry and the missing mass problem in planetary nebulae

Context. Detections of molecular lines, mainly from H-2 and CO, reveal molecular material in planetary nebulae. Observations of a variety of molecules suggest that the molecular composition in these objects differs from that found in interstellar clouds or in circumstellar envelopes. The success of the models, which are mostly devoted to explain molecular densities in specific planetary nebulae, is still partial however. Aims. The present study aims at identifying the influence of stellar and nebular properties on the molecular composition of planetary nebulae by means of chemical models. A comparison of theoretical results with those derived from the observations may provide clues to the conditions that favor the presence of a particular molecule. Methods. A self-consistent photoionization numerical code was adapted to simulate cold molecular regions beyond the ionized zone. The code was used to obtain a grid of models and the resulting column densities are compared with those inferred from observations. Results. Our models show that the inclusion of an incident flux of X-rays is required to explain the molecular composition derived for planetary nebulae. We also obtain a more accurate relation for the N(CO)/N(H-2) ratio in these objects. Molecular masses obtained by previous works in the literature were then recalculated, showing that these masses can be underestimated by up to three orders of magnitude. We conclude that the problem of the missing mass in planetary nebulae can be solved by a more accurate calculation of the molecular mass.

Electrochemically activated coordenative assembly of a triruthenium cluster metallopolymer

A general strategy for electrochemically induced assembly of coordination metallopolymers is demonstrated using the tritopic bridging [Ru-3(mu(3)-O)(CH3COO)(6)(pytpy)(3)](+) cluster complex, where pytpy is the 4'-(4-pyridyl)-2,2':6',2 ''-terpyridine ligand, and iron(III) ions. The concept of such an electrochemically induced coordinative assembly was proven exploring the large difference in the [Fe(pytpy)2 complex formation constants depending on the iron ion oxidation state. Much more stable bridging complexes are formed in the presence of Fe(II) in contrast to Fe(III) ions. The build-up of electrochemically active films on FTO electrodes was confirmed by the growth of the corresponding voltammetric peaks concomitantly with the rise of typical triruthenium cluster and [Fe(pytpy)(2)](2+) complex absorption bands. The metallopolymer was constituted by agglomerates of more or less fused tape like structures, exhibiting large voids and pinholes, as revealed by SEM and AFM images. The adhesion/deposition on FTO was improved by functionalizing the surface with TES-tpy and HOOC-tpy, which increased the surface coverage up to 80%, as estimated by impedance spectroscopy. (C) 2012 Elsevier Ltd. All rights reserved.

Air pollution and health: bridging the gap from sources to health outcomes: conference summary

Air Pollution and Health: Bridging the Gap from Sources to Health Outcomes, an international specialty conference sponsored by the American Association for Aerosol Research, was held to address key uncertainties in our understanding of adverse health effects related to air pollution and to integrate and disseminate results from recent scientific studies that cut across a range of air pollution-related disciplines. The Conference addressed the science of air pollution and health within a multipollutant framework (herein "multipollutant" refers to gases and particulate matter mass, components, and physical properties), focusing on five key science areas: sources, atmospheric sciences, exposure, dose, and health effects. Eight key policy-relevant science questions integrated across various parts of the five science areas and a ninth question regarding findings that provide policy-relevant insights served as the framework for the meeting. Results synthesized from this Conference provide new evidence, reaffirm past findings, and offer guidance for future research efforts that will continue to incrementally advance the science required for reducing uncertainties in linking sources, air pollutants, human exposure, and health effects. This paper summarizes the Conference findings organized around the science questions. A number of key points emerged from the Conference findings. First, there is a need for greater focus on multipollutant science and management approaches that include more direct studies of the mixture of pollutants from sources with an emphasis on health studies at ambient concentrations. Further, a number of research groups reaffirmed a need for better understanding of biological mechanisms and apparent associations of various health effects with components of particulate matter (PM), such as elemental carbon, certain organic species, ultrafine particles, and certain trace elements such as Ni, V, and Fe(II), as well as some gaseous pollutants. Although much debate continues in this area, generation of reactive oxygen species induced by these and other species present in air pollution and the resulting oxidative stress and inflammation were reiterated as key pathways leading to respiratory and cardiovascular outcomes. The Conference also underscored significant advances in understanding the susceptibility of populations, including the role of genetics and epigenetics and the influence of socioeconomic and other confounding factors and their synergistic interactions with air pollutants. Participants also pointed out that short-and long-term intervention episodes that reduce pollution from sources and improve air quality continue to indicate that when pollution decreases so do reported adverse health effects. In the limited number of cases where specific sources or PM2.5 species were included in investigations, specific species are often associated with the decrease in effects. Other recent advances for improved exposure estimates for epidemiological studies included using new technologies such as microsensors combined with cell phone and integrated into real-time communications, hybrid air quality modeling such as combined receptor-and emission-based models, and surface observations used with remote sensing such as satellite data.

Shear force and torsion in reinforced concrete beam elements: theoretical analysis based on Brazilian Standard Code ABNT NBR 6118:2007

Reinforced concrete beam elements are submitted to applicable loads along their life cycle that cause shear and torsion. These elements may be subject to only shear, pure torsion or both, torsion and shear combined. The Brazilian Standard Code ABNT NBR 6118:2007 [1] fixes conditions to calculate the transverse reinforcement area in beam reinforced concrete elements, using two design models, based on the strut and tie analogy model, first studied by Mörsch [2]. The strut angle θ (theta) can be considered constant and equal to 45º (Model I), or varying between 30º and 45º (Model II). In the case of transversal ties (stirrups), the variation of angle α (alpha) is between 45º and 90º. When the equilibrium torsion is required, a resistant model based on space truss with hollow section is considered. The space truss admits an inclination angle θ between 30º and 45º, in accordance with beam elements subjected to shear. This paper presents a theoretical study of models I and II for combined shear and torsion, in which ranges the geometry and intensity of action in reinforced concrete beams, aimed to verify the consumption of transverse reinforcement in accordance with the calculation model adopted As the strut angle on model II ranges from 30º to 45º, transverse reinforcement area (Asw) decreases, and total reinforcement area, which includes longitudinal torsion reinforcement (Asℓ), increases. It appears that, when considering model II with strut angle above 40º, under shear only, transverse reinforcement area increases 22% compared to values obtained using model I.

Molekularer Magnetismus und Multistabilitäten in sternförmigen cyanidgebrückten Eisen- und Übergangsmetall-Komplexverbindungen

In der hier vorliegenden Arbeit wurden neue eisenhaltige Spincrossover-Komplexerndargestellt und deren magnetische Eigenschaften untersucht. Ausgehend von früheren Ergebnissen wurden verschiedene Strategien zur Optimierung der Eisen-Spincrossover Verbindungen verfolgt. Wie schon früher dokumentiert finden sich bei Eisen-Übergangsmetall Komplexen eine Vielzahl von Spincrossover Phänomenen. Ebenso gut dokumentiert sind die Möglichen Änderungen des Spin Zustandes durch äußere Einflüsse wie Temperatur, Druck oder Licht. Darauf aufbauend wurden nunrnverschiedene Eisenkomplexe synthetisiert und auf das Spincrossover Phänomen hin untersucht. Dazu wurden zum Einen Fe(II) Komplexe vom Typ [FeL1(NCS)2] (L1 = pmea, pmap, tepa and tmpa) betrachtet und zum anderen Sternförmige Fe(III) Komplexe vom Typ [M{(CN-FeIIIL2}x]y+. (M=Fe(II), Co(III), Mo(IV), Ru(II)) undrndodecanukleare Komplexe vom Typ [(L2Fe(III)NC)5Fe(II)CNCo(III)(CNFe(III)L2)5]4+. L2= Bis(R2,3,4 -salicylidenaminoalkyl-R1-amin. Thermischen Spincrossover und LIESST zeigen [3,3/N-H/Sal-H/Fe/Co]; [3,3/N-H/Sal-H/Fe/Ru]; [3,3/N-H/sal-H/Fe/Mo]; [3,3/N-H/Sal-H/Fe/W]; FeII(pmea)(SCN)2; thermischen Spinübergang zeigt [2,3/N-H/Sal-H/Fe/Fe-Co]. Die Ethylen gebrückten Komplexe zeigen weniger guten oder gar keinen Schalteffekt im Gegensatz zum Propylen gebrückten Komplexe. Fe(II)(PMEA)(SCN)2 zeigt vollständigen thermischen Spinübergang von High Spin nach Low Spin ein LIESST und einen LiPTH Effekt.

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.

Elementspeziation von Neptunium im Ultraspurenbereich

In der vorliegenden Arbeit wurde der Nachweis des Isotops Np-237 mit Resonanzionisations-Massenspektrometrie (RIMS) entwickelt und optimiert. Bei RIMS werden Probenatome mehrstufig-resonant mit Laserstrahlung angeregt, ionisiert und anschließend massenspektrometrisch nachgewiesen. Die Bestimmung geeigneter Energiezustände für die Anregung und Ionisation von Np-237 erfolgte durch Resonanzionisationsspektroskopie (RIS), wobei über 300 bisher unbekannte Energieniveaus und autoionisierende Zustände von Np-237 identifiziert wurden. Mit in-source-RIMS wird für das Isotop eine Nachweisgrenze von 9E+5 Atome erreicht. rnrnDie Mobilität von Np in der Umwelt hängt stark von seiner Elementspeziation ab. Für Sicherheitsanalysen potentieller Endlagerstandorte werden daher Methoden benötigt, die Aussagen über die unter verschiedenen Bedingungen vorliegenden Neptuniumspezies ermöglichen. Hierzu wurde eine online-Kopplung aus Kapillarelektrophorese (CE) und ICP-MS (inductively coupled plasma mass spectrometry) genutzt, mit der die Np-Redoxspezies Np(IV) und Np(V) noch bei einer Konzentrationen von 1E-9 mol/L selektiv nachgewiesen werden können. Das Verfahren wurde eingesetzt, um die Wechselwirkung des Elements mit Opalinuston unter verschiedenen Bedingungen zu untersuchen. Dabei konnte gezeigt werden, dass bei Gegenwart von Fe(II) Np(V) zu Np(IV) reduziert wird und dieses am Tongestein sorbiert. Dies führt insgesamt zu einer deutlich erhöhten Sorption des Np am Ton.

Molecular genetic causes of columnar growth in apple (Malus x domestica)

The columnar growth habit of apple is interesting from an economic point of view as the pillar-like trees require little space and labor. Genetic engineering could be used to speed up breeding for columnar trees with high fruit quality and disease resistance. For this purpose, this study dealt with the molecular causes of this interesting phenotype. The original bud sport mutation that led to the columnar growth habit was found to be a novel nested insertion of a Gypsy-44 LTR retrotransposon on chromosome 10 at 18.79 Mb. This subsequently causes tissue-specific differential expression of nearby downstream genes, particularly of a gene encoding a 2OG-Fe(II) oxygenase of unknown function (dmr6-like) that is strongly upregulated in developing aerial tissues of columnar trees. The tissue-specificity of the differential expression suggests involvement of cis-regulatory regions and/or tissue-specific epigenetic markers whose influence on gene expression is altered due to the retrotransposon insertion. This eventually leads to changes in genes associated with stress and defense reactions, cell wall and cell membrane metabolism as well as phytohormone biosynthesis and signaling, which act together to cause the typical phenotype characteristics of columnar trees such as short internodes and the absence of long lateral branches. In future, transformation experiments introducing Gypsy-44 into non-columnar varieties or excising Gypsy-44 from columnar varieties would provide proof for our hypotheses. However, since site-specific transformation of a nested retrotransposon is a (too) ambitious objective, silencing of the Gypsy-44 transcripts or the nearby genes would also provide helpful clues.

Geochemical parameters of sediments and water of the Black Sea, data of Cruise 8 of R/V Vityaz-2

The book presents results of comprehensive geological investigations carried out during Cruise 8 of R/V "Vityaz-2" to the western part of the Black Sea in 1984. Systematic studies in the Black Sea during about hundred years have not weakened interest in the sea. Lithological and geochemical studies of sediments in estuarine areas of the Danube and the Kyzyl-Irmak rivers, as well as in adjacent parts of the deep sea and some other areas were the main aims of the cruise. Data on morphological structures of river fans, lithologic and chemical compositions of sediments in the fans and their areal distribution, forms of occurrence of chemical elements, role of organic matter and gases in sedimentation and diagenesis are given and discussed in the book.

Results of magnetic analysis

Microorganisms are a primary control on the redox-induced cycling of iron in the environment. Despite the ability of bacteria to grow using both Fe(II) and Fe(III) bound in solid-phase iron minerals, it is currently unknown if changing environmental conditions enable the sharing of electrons in mixed-valent iron oxides between bacteria with different metabolisms. We show through magnetic and spectroscopic measurements that the phototrophic Fe(II)-oxidizing bacterium Rhodopseudomonas palustris TIE-1 oxidizes magnetite (Fe3O4) nanoparticles using light energy. This process is reversible in co-cultures by the anaerobic Fe(III)-reducing bacterium Geobacter sulfurreducens. These results demonstrate that Fe ions bound in the highly crystalline mineral magnetite are bioavailable as electron sinks and electron sources under varying environmental conditions, effectively rendering a naturally occurring battery.

Rare earth and other element contents in surface layer bottom sediments and ferromanganese nodules along the Transatlantic profile

Behavior of rare earth elements (REE) and Th is studied along the Transatlantic transect at 22°N. It is shown that both REE and Th contents relative to Al (the most lithogenic element) increase toward the pelagic region. The increasing trend becomes more complicated due to variations in content of biogenic calcium carbonate that acts as a diluting component in sediments. REE composition varies symmetrically relative to the Mid-Atlantic Ridge (MAR) emphasizing weak hydrothermal influence on sediments of the ridge axis, although the well-known criteria for hydrothermal contribution, such as Al/(Al+Mn+Fe) and (Fe+Mn)/Ti, do not reach critical values. Variations in REE content and composition allowed to distinguish the following five sediment zones in the transect: (I) terrigenous sediments of the Nares abyssal plain; (II) pelagic sediments of the North American Basin; (III) carbonate ooze of the MAR axis; (IV) pelagic sediments of the Canary Basin; and (V) terrigenous clay and calcareous mud of the African continental slope and slope base. Ferromanganese nodules of the hydrogenous type with extremely high Ce (up to 1801 ppm) and Th (up to 138 ppm) contents occur in pelagic sediments. It is ascertained that P, REE, and Th contents depend on Fe content in Atlantic sediments. Therefore, one can suggest that only minor amount of phosphorus is bound with bone debris. Low concentration of bone debris phosphorus is a result of relatively high sedimentation rates in the Atlantic Ocean, as compared with those in pelagic regions of the Pacific Ocean.

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.

Geochemistry of Cretaceous sediments from Argo and Gascoyne Abyssal Plains

The accumulation of organic matter, ferrous and pyrite iron, and the ratios of organic carbon/total sulfur and organic carbon/total phosphorus in the Lower Cretaceous sediments from the Argo and Gascoyne abyssal plains have been used as indicators of both the source and reactivity of organic matter in the sediments and the depositional environment. Total sulfur, used as an indicator of pyrite sulfur, is more abundant in sediments from the Gascoyne Abyssal Plain than in those from the Argo Abyssal Plain. Sulfur positively correlates with TOC at both sites (although poorly at the Argo Abyssal Plain site, R = 0.48), with an extension of the line of best-fit through the origin, indicating that pyrite (TOC <2 wt%) is diagenetic and deposited from normal marine conditions. The average ratio of C/S for samples of TOC <2 wt% is 5.4 at Argo Abyssal Plain (compared to the modern normal marine value of 2.8) indicating deposition of organic matter probably of mixed terrestrial and oxidized marine sources that is unreactive to the sulfate-reducing bacteria. One sample from the Aptian sediments is rich in TOC (5.1 wt%) and has a C/S ratio of 0.5. The average C/S ratio in Gascoyne Abyssal Plain sediments is 0.8 (R = 0.97), which indicates the formation of abundant pyrite in addition to burial and preservation of relatively fresh organic matter that is reactive to the sulfate-reducing bacteria. Organic carbon to phosphorus ratios (C/P) in the sediments indicate preferential remobilization of organic carbon over phosphorus with increasing water depth. Estimates of the degree of pyritization (DOP) increase with increasing TOC at both sites, indicating iron is not limiting and pyrite is formed diagenetically. The one sample with a TOC content of 5.1 wt%, from the Argo Abyssal Plain near the Barremian-Aptian boundary, is composed mostly of framboidal pyrite, finely laminated and not bioturbated, and hence may have been deposited during a brief period of anoxia in the overlying waters.