GaMnAs: Position of Mn-d levels and majority spin band gap predicted from GGA-1/2 calculations

Among all magnetic semiconductors, GaMnAs seems to be the most important one. In this work, we present accurate first-principles calculations of GaMnAs within the GGA-1/2 approach: We concentrate our efforts in obtaining the position of the peak of Mn-d levels in the valence band and also the majority spin band gap. For the position of the Mn-d peak, we find a value of 3.3 eV below the Fermi level, in good agreement with the most recent experimental results of 3.5 and 3.7 eV. An analytical expression that fits the calculated E-g(x) for majority spin is derived in order to provide ready access to the band gap for the composition range from 0 to 0.25. We found a value of 3.9 eV for the gap bowing parameter. The results agree well with the most recent experimental data. (C) 2012 American Institute of Physics. [http://dx.doi.org/10.1063/1.4718602]

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

(Table 1) Contents of tungsten and other metals in Fe-Mn nodules from the Pacific Ocean

Tungsten contents in iron-manganese nodules and crusts from different parts of the World Ocean, as well as its relationships with a number of chemical elements are under consideration. A trend to correlation of tungsten with Fe, Ti, W, Pb, and Co is noticed. Comparison of tungsten contents in the nodules and host sediments indicates its low geochemical mobility.

Geochemistry of Fe-Mn crusts in sediments of the Central Indian Ridge

Layered Fe-Mn crusts from the off-axis region of the first segment of the Central Indian Ridge north of the Rodrigues Triple Junction were studied geochemically and mineralogically. Vernadite (delta-MnO2) is the main mineral oxide phase. 230Thxs and Co concentrations suggest high growth rates of up to 29 mm/Myr and a maximum age of the basal crust layer of 1 Ma. Whereas most of the major and minor elements show concentrations which are typical of hydrogenetic formation, Co, Pb, Ni and Ti concentrations are strikingly lower. Concentrations and distribution of the strictly trivalent rare-earths and yttrium (REY) are typical of hydrogenetic ferromanganese oxide precipitates, but in marked contrast, the crusts are characterized by negative CeSN (shale normalized) anomalies and (Ce/Pr)SN ratios less than unity. Profiles through the crusts reveal only minor variations of the REY distribution and (Ce/Pr)SN ratios range from 0.45 to 0.68 (compared to ratios of up to 2 for typical hydrogenetic crusts from the Central Indian Basin). The apparent bulk partition coefficients between the crusts and seawater suggest that for the strictly trivalent REY the adsorption-desorption equilibrium has been reached. Positive Ce anomalies in the partition coefficient patterns reveal preferential uptake of Ce, but to a lesser extent than in normal hydrogenetic crusts. A new parameter (excess Ce, Cexs) to quantify the degree of decoupling of Ce from REY(III) is established on the basis of partition coefficients. Cexs/Cebulk ratios suggest that the CIR crusts formed by precipitation of Fe-Mn oxides from a hydrothermal plume and that in hydrothermal plumes and normal seawater the enrichment of Ce results from the same oxidative sorption process. The growth rates, calculated with 230Thxs data as well as with the Co formula, are inversely related to Cexs.

Geochemical analyses of chert nodules and beds from deep-sea sediments (Table 1)

Concentrations of Fe, Mg, Ca, Sr, Mn, Zn, and other heavy metals were analyzed by atomic absorption spectrometry in 27 chert samples from the Pacific deep sea, 17 chert samples from land, and 4 associated sediments from the Pacific Ocean. Among the elements, Fe and Mg concentrations are highly correlatable as are the relationships between Ca and Sr, or between Ca and CO2. The correlation between Fe and Mg is particularly high for Pacific deep-sea flints and cherts, and for cherts of deep-sea origin from outcrops on land. Enrichments in heavy metals were recognized in some deep-sea cherts; volcanogenic cherts are enriched in Fe, a chert nodule containing basaltic fragments is enriched in Zn and Cr, and biogenically enclosed carbonates in flint nodules are enriched in Mn. The correlation of Fe and Mg and their constant ratio [Mg(%)/Fe(%)] of around 0.33 might be characteristic features in the pelagic clays contained in deep-sea flints and cherts, and the concentrations of heavy metals in them would be controlled by the concentrations of Fe-Mg correlated clays. Although the mineralogical nature of the Fe-Mg clay in deep-sea cherts was not clarified by dissolution experiments on opaline minerals in chert, the high concentrations of Fe-montmorillonite and fine-grained olivine or other ferromagnesian silicate minerals in the clay may result in the high correlations between Fe and Mg.

Geochemical provenance analysis of fine-grained sediment of sediment core AND1-1

Bulk chemical fine-grained sediment compositions from southern Victoria Land glacimarine sediments provide significant constraints on the reconstruction of sediment provenance models in the McMurdo Sound during Late Cenozoic time. High-resolution (~ 1 ka) geochemical data were obtained with a non-destructive AVAATECH XRF Core Scanner (XRF-CS) on the 1285 m long ANDRILL McMurdo Ice Shelf Project (MIS) sediment core AND-1B. This data set is complemented by high-precision chemical analyses (XRF and ICP-OES) on discrete samples. Statistical analyses reveal three geochemical facies which are interpreted to represent the following sources for the sediments recovered in the AND-1B core: 1) local McMurdo Volcanic Group (MVG) rocks, 2) Transantarctic Mountain rocks west of Ross Island (W TAM), and 3) Transantarctic Mountain rocks from more southerly areas (S TAM). Data indicate in combination with other sediment facies analyses (McKay et al., 2009, doi:10.1130/B26540.1) and provenance scenarios (Talarico and Sandroni, 2009, doi:10.1016/j.gloplacha.2009.04.007) that diamictites at the drill site are largely dominated by local sources (MVG) and are interpreted to indicate cold polar conditions with dry-based ice. MVG is interpreted to indicate cold polar condition with dry-based ice. A mixture of MVG and W TAM is interpreted to represent polar conditions and the S TAM facies is interpreted to represent open-marine conditions. Down-core variations in geochemical facies in the AND-1B core are interpreted to represent five major paleoclimate phases over the past 14 Ma. Cold polar conditions with major MVG influence occur below 1045 mbsf and above 120 mbsf. A section of warmer climate conditions with extensive peaks of S TAM influence characterizes the rest of the core, which is interrupted by a section from 525 to 855 mbsf of alternating influences of MVG and W TAM.

(Table 1) Platinoids in Fe-Mn crusts and nodules from the Pacific Ocean

Platinoid element contents were determined in 16 samples of Fe-Mn crusts and nodules collected during dredging deep-sea mound slopes of the Pacific Ocean from the equator to 27°N. The method of neutron activation analysis with pre-concentration of the platinoids was used for these determinations. There is no relationship between platinoid contents in deep-sea (>3000 m) Fe-Mn nodules with depth of sampling, as well as with age of nodule layers. It is concludet that ultramafic rocks are the primary source of platinoids in Fe-Mn nodules.