5 resultados para low oxygen

em ArchiMeD - Elektronische Publikationen der Universität Mainz - Alemanha


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Due to its high Curie temperature of 420K and band structure calculations predicting 100% spin polarisation, Sr2FeMoO6 is a potential candidate for spintronic devices. However, the preparation of good quality thin films has proven to be a non-trivial task. Epitaxial Sr2FeMoO6 thin films were prepared by pulsed laser deposition on different substrates. Differing from previous reports a post-deposition annealing step at low oxygen partial pressure (10-5 mbar) was introduced and enabled the fabrication of reproducible, high quality samples. According to the structural properties of the substrates the crystal structure and morphology of the thin films are modified. The close interrelation between the structural, magnetic and electronic properties of Sr2FeMoO6 was studied. A detailed evaluation of the results allowed to extract valuable information on the microscopic nature of magnetism and charge transport. Smooth films with a mean roughness of about 2 nm have been achieved, which is a pre-requisite for a possible inclusion of this material in future devices. In order to establish device-oriented sub-micron patterning as a standard technique, electron beam lithography and focussed ion beam etching facilities have been put into operation. A detailed characterisation of these systems has been performed. To determine the technological prospects of new spintronics materials, the verification of a high spin polarisation is of vital interest. A popular technique for this task is point contact Andreev reflection (PCAR). Commonly, the charge transport in a transparent metal-superconductor contact of nanometer dimensions is attributed solely to coherent transport. If this condition is not fulfilled, inelastic processes in the constriction have to be considered. PCAR has been applied to Sr2FeMoO6 and the Heusler compound Co2Cr0.6Fe0.4Al. Systematic deviations between measured spectra and the standard models of PCAR have been observed. Therefore existing approaches have been generalised, in order to include the influence of heating. With the extended model the measured data was successfully reproduced but the analysis has revealed grave implications for the determination of spin polarisation, which was found to break down completely in certain cases.

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Dunite, wehrlite and websterite xenoliths occur amongst a large abundance of mantle xenoliths in kimberlites of the Kimberley cluster in South Africa. Up to know they have mostly been neglected. On the basis of texture, major and trace elements, oxygen isotopes as well as Re-Os isotope characteristics, they can be subdivided into two groups. A coarse-grained mantle peridotite group, comprising dunite, wehrlite and websterite xenoliths, that are similar to fertile peridotites and represent upper mantle assemblages that are differently influenced by mantle metasomatism. And a cumulate group, containing fine-grained Fe-rich dunite xenoliths that represent cumulates of flood basalt magmatism related to ~183 Ma Karoo and ~2.7 Ga Ventersdorp events in southern Africa. Dunite, wehrlite and websterite xenoliths have preserved a complex history of melt depletion and metasomatic re-enrichment events, which gives information about the different re-enrichment stages of the subcratonic lithospheric mantle and the spatial differences within the Kaapvaal craton upper mantle. Websterite xenoliths comprise orthopyroxene (40-85 Vol. %), clinopyroxene (5-42 Vol. %), garnet (4-10 Vol. %) and subordinately olivine, while dunite and wehrlite xenoliths contain predominantly olivine (65-100 Vol %) and subordinately orthopyroxene, clinopyroxene and garnet. High melt depletion and a dunitic to harzburgitic protolith composition are reflected by high forsterite (Fo90-92) and high olivine NiO contents (2800-5000 ppm) and high orthopyroxene Mg# (Mg/(Mg+Fe)) of 0.91-0.93. Re-depletion ages of predominantly 2.9 Ga reflect a minimum age of melt depletion. Melt depletion ceased in conjunction with collision of the Kimberley block with the Witwatersrand block ~2.9 Ga ago. Subduction related re-fertilisation of the previously depleted mantle xenoliths is documented by i) amoeboid textured orthopyroxene, clinopyroxene and garnet, which crystallized in schlieren along olivine grain boundaries, ii) high whole-rock SiO2, Al2O3, CaO, TiO2, FeO contents, iii) low oxygen isotope ratios in clinopyroxene and garnet of 4.8-5.4 ‰ and 4.7-5.3 ‰, respectively and iv) trace element compositions of wehrlitic clinopyroxene and garnet in equilibrium with high-pressure partial melts of eclogite. Trace element disequilibrium of orthopyroxene with clinopyroxene and garnet indicates a separate origin for orthopyroxene, on one side as primary mantle orthopyroxene in dunite and wehrlite xenoliths and on the other side as reaction product with Si-rich melts produced by partial melting of eclogite. This reaction triggered replacement of olivine by orthopyroxene in the surrounding mantle and produced the typical Si-rich composition of Kaapvaal mantle peridotites. Partial melting of eclogite at higher temperatures produced a second metasomatic melt with lower SiO2, but higher Al2O3, CaO, FeO, Ti, Zr, Hf and a low oxygen isotope ratio. This melt triggered clinopyroxene and locally garnet and rutile crystallization in percolation veins, replacing olivine and orthopyroxene in the Kaapvaal upper mantle. Additionally, websterite xenoliths have experienced late stage cryptic metasomatism by the host kimberlite melt, changing the trace element composition of clinopyroxene, orthopyroxene and garnet to different extent. Hence websterite and most fertile lherzolite xenoliths have experienced three metasomatic events: i) reaction with high-Si melt, ii) percolation of subduction related silica melt with lower SiO2 content and iii) cryptic metasomatism by kimberlite. In contrast, dunite and wehrlite xenoliths have only experienced the second metasomatic event. They represent mantle lithologies further away from metasomatising agents. The Fe-rich dunites comprise olivine neoblasts with subordinate olivine porphyroclasts and parallel-orientated needles of ilmenite, which may enclose spinel. The lower forsterite and NiO contents of olivine in Fe-rich dunites compared to mantle peridotite xenoliths (Fo87-89 vs. Fo93-95 and 1300-2800ppm vs. 2200-3900 ppm, respectively), rules out a restitic origin. Cr-rich spinels are remnants of the original cumulate mineralogy that survived a late stage metasomatic overprint related to the production of the host kimberlite, producing ilmenite and phlogopite in some samples. Olivine porphyroclasts and neoblasts have different trace element compositions, the latter having high Ti, V, Cr and Ni and low Zn, Zr and Nb contents, indicating contrasting origins for neoblasts and porphyroclasts. The dunites have high 187Os/188Os ratios (0.11-0.15) indicating young (Phanerozoic) model ages for most samples, whereas three samples show isotopic mixtures between Phanerozoic neoblasts and ancient porphyroclastic material. Most Fe-rich dunite xenoliths can be interpreted as cumulates of fractional crystallization of Karoo magmatism, whereas the porphyroclasts are interpreted to be remnants from the much earlier Archaean Ventersdorp magmatism.

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Hypoxie ist ein Zustand des Sauerstoffmangels, hervorgerufen durch fehlende Verfügbarkeit von Sauerstoff in der Umgebung eines Organismus oder durch pathologisch bedingte unzureichende Nutzbarkeit des Sauerstoffs von Geweben. Die Sensitivität gegenüber Hypoxie variiert enorm im Tierreich zwischen verschiedenen Phyla und Spezies. Die meisten Säugetiere sind nur unzureichend an niedrige Sauerstoffkonzentrationen angepasst, wohingegen einige unterirdisch lebende Säuger sehr resistent gegen Hypoxiestress sind. Um die molekulare Basis der Hypoxietoleranz zu bestimmen, wurden in der vorliegenden Arbeit Globine untersucht, die potenziell in der Lage sind, als respiratorische Proteine zur Hypoxietoleranz von Tieren beizutragen. Dazu wurde die Expression der Globine in der hypoxieresistenten, in Israel lebenden Blindmaus Spalax ehrenbergi mit der Genexpression in der hypoxiesensitiven Ratte (Rattus norvegicus) verglichen. In der vorliegenden Arbeit wurden die erst vor wenigen Jahren entdeckten Globine Neuroglobin und Cytoglobin untersucht, deren exakte physiologische Rolle noch unklar ist, und mit Daten des viel detaillierter untersuchten Myoglobins verglichen. Beim Vergleich der Expression von Cytoglobin und Neuroglobin in Spalax versus Ratte fällt auf, dass Neuroglobin und Cytoglobin bereits unter normoxischen Bedingungen auf mRNA- und Proteinebene in der Blindmaus um einen Faktor von mindesten 2 bis 3 verstärkt exprimiert werden. Bei Myoglobin (als dem Kontrollgen mit bekannter Funktion) konnte auf mRNA-Ebene eine noch weitaus stärkere Expression in Spalax vs. Ratte gefunden werden. Das übergreifende Phänomen der verstärkten Genexpression von Globinen in Spalax kann im Sinne einer Präadaptation an das unterirdische, häufig hypoxische Leben der Blindmaus interpretiert werden. Einen weiteren Hinweis auf eine besondere, spezialisierte Funktion von Neuroglobin in Spalax geben immunhistochemische Daten, die zeigen, dass Neuroglobin im Gehirn von Spalax im Gegensatz zur Ratte nicht nur in Neuronen, sondern auch in Gliazellen exprimiert wird. Dies impliziert Änderungen des oxidativen Stoffwechsels im Nervensystem der hypoxietoleranten Spezies. Die zellulären Expressionsmuster von Cytoglobin erscheinen hingegen in beiden Säugerspezies weitgehend identisch. Es wurde der Frage nachgegangen, ob und wie experimentell induzierte Hypoxie die Genexpression der Globine verändert. Dabei zeigten sich für Neuroglobin und Cytoglobin unterschiedliche Expressionsmuster. Neuroglobin wird unter diversen Sauerstoffmangelbedingungen sowohl in der Ratte als auch in Spalax auf mRNA- und Proteinebene herunterreguliert. Ein ähnliches Regulationsverhalten wurde auch für Myoglobin beobachtet. Die verminderte Expression von Neuroglobin (und evtl. auch Myoglobin) unter Hypoxie ist mit einer gezielten Verringerung der Sauerstoff-Speicherkapazität in Abwesenheit von O2 zu erklären. Ein weiterer denkbarer Grund könnte auch die allgemeine Tendenz sein, unter Hypoxie aus Energiespargründen den Metabolismus herunter zu regulieren. Cytoglobin, das bei normalen Sauerstoffbedingungen nur im Gehirn von Spalax (nicht jedoch in Herz und Leber) ebenfalls um Faktor 2 bis 3 stärker exprimiert wird als in der Ratte, ist mit einiger Sicherheit ebenfalls von adaptivem Nutzen für die Anpassung von Spalax an niedrige Sauerstoffbedingungen, wenngleich seine Funktion unklar bleibt. Unter Hypoxie wird die Cytoglobin-mRNA sowohl in Spalax als auch in der Ratte hochreguliert. Es konnte in der vorliegenden Arbeit dargelegt werden, dass die Expression von Cygb höchstwahrscheinlich durch den Transkriptionsfaktor Hif-1 gesteuert wird, der die molekulare Hypoxieantwort vieler Tierarten zentral steuert. In der vorliegenden Arbeit wurde ebenfalls die Expression von Ngb und Cygb im Gehirn des Hausschweins (Sus scrofa) untersucht. Diese Spezies diente in der Arbeit als weiterer hypoxiesensitiver Organismus sowie als biomedizinisch relevantes Modell für eine Operation an Säuglingen mit angeborenen Herzkrankheiten. Die Versuche haben gezeigt, dass die Gabe bestimmter Medikamente wie dem Immunsuppressivum FK506 zu einer erhöhten Ngb-Konzentration auf mRNA-Ebene führen kann, was potenziell im Zusammenhang mit beobachteten protektiven Effekten der Medikamentengabe während und nach der Herzoperation steht.

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Chondrocytes live isolated in the voluminous extracellular matrix of cartilage, which they secrete and is neither vascularized nor innervated. Nutrient and waste exchanges occur through diffusion leading to low oxygen tension around the cells. Consequently even normal cartilage under normal physiological conditions suffers from a poor reparative potential that predisposes to degenerative conditions, such as osteoarthritis of the joints, with significant clinical effects.rnOne of the key challenges in medicine is the structural and functional replacement of lost or damaged tissues. Current therapeutical approaches are to transplant cells, implant bioartificial tissues, and chemically induce regeneration at the site of the injury. None of them reproduces well the biological and biomechanical properties of hyaline cartilage.rnThis thesis investigates the re-differentiation of chondrocytes and the repair of cartilage mediated by signaling molecules, biomaterials, and factors provided in mixed cellular cultures (co-culture systems). As signaling molecules we have applied prostaglandin E2 (PGE2) and bone morphogenetic protein 1 (BMP-1) and we have transfected chondrocytes with BMP-1 expressing vectors. Our biomaterials have been hydrogels of type-I collagen and gelatin-based scaffolds designed to mimic the architecture and biochemistry of native cartilage and provide a suitable three-dimensional environment for the cells. We have brought chondrocytes to interact with osteosarcoma Cal 72 cells or with murine preosteoblastic KS483 cells, either in a cell-to-cell or in a paracrine manner.rnExogenous stimulation with PGE2 or BMP-1 did not improve the differentiation or the proliferation of human articular chondrocytes. BMP-1 induced chondrocytic de-differentiation in a dose-dependent manner. Prostaglandin stimulation from gelatin-based scaffolds (three-dimensional culture) showed a certain degree of chondrocyte re-differentiaton. Murine preosteoblastic KS483 cells had no beneficial effect on human articular chondrocytes jointly cultivated with them in hydrogels of type I collagen. Although the hydrogels provided the chondrocytes with a proper matrix in which the cells adopted their native morphology; additionally, the expression of chondrocytic proteoglycan increased in the co-cultures after two weeks. The co-culture of chondrocytes with osteoblast-like cells (in transwell systems) resulted in suppression of the regular de-differentiation program that passaged chondrocytes undergo when cultured in monolayers. Under these conditions, the extracellular matrix of the chondrocytes, rich in type-II collagen and aggrecan, was not transformed into the extracellular matrix characteristic of de-differentiated human articular chondrocytes, which is rich in type-I collagen and versican.rnThis thesis suggests novel strategies of tissue engineering for clinical attempts to improve cartilage repair. Since implants are prepared in vitro (ex-vivo) by expanding human articular chondrocytes (autologous or allogeneic), we conclude that it will be convenient to provide a proper three-dimensional support to the chondrocytes in culture, to supplement the culture medium with PGE2, and to stimulate chondrocytes with osteoblastic factors by cultivating them with osteoblasts.rn

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This thesis investigates phenomena of vortex dynamics in type II superconductors depending on the dimensionality of the flux-line system and the strength of the driving force. In the low dissipative regime of Bi_2Sr_2CaCu_2O_{8+delta} (BSCCO) the influence of oxygen stoichiometry on flux-line tension was examined. An entanglement crossover of the vortex system at low magnetic fields was identified and a comprehensive B-T phase diagram of solid and fluid phases derived.In YBa_2Cu_3O_7 (YBCO) extremely long (>100 mm) high-quality measurement bridges allowed to extend the electric-field window in transport measurements by up to three orders of magnitude. Complementing analyses of the data conclusively produced dynamic exponents of the glass transition z~9 considerably higher than theoretically predicted and previously reported. In high-dissipative measurements a voltage instability appearing in the current-voltage characteristics of type II superconductors was observed for the first time in BSCCO and shown to result from a Larkin-Ovchinnikov flux-flow vortex instability under the influence of quasi-particle heating. However, in an analogous investigation of YBCO the instability was found to appear only in the temperature and magnetic-field regime of the vortex-glass state. Rapid-pulse measurements fully confirmed this correlation of vortex glass and instability in YBCO and revealed a constant rise time (~µs).