TY - JOUR A1 - Sandev, Trifce A1 - Domazetoski, Viktor A1 - Kocarev, Ljupco A1 - Metzler, Ralf A1 - Chechkin, Aleksei T1 - Heterogeneous diffusion with stochastic resetting JF - Journal of physics : A, Mathematical and theoretical N2 - We study a heterogeneous diffusion process (HDP) with position-dependent diffusion coefficient and Poissonian stochastic resetting. We find exact results for the mean squared displacement and the probability density function. The nonequilibrium steady state reached in the long time limit is studied. We also analyse the transition to the non-equilibrium steady state by finding the large deviation function. We found that similarly to the case of the normal diffusion process where the diffusion length grows like t (1/2) while the length scale xi(t) of the inner core region of the nonequilibrium steady state grows linearly with time t, in the HDP with diffusion length increasing like t ( p/2) the length scale xi(t) grows like t ( p ). The obtained results are verified by numerical solutions of the corresponding Langevin equation. KW - heterogeneous diffusion KW - Fokker-Planck equation KW - Langevin equation KW - stochastic resetting KW - nonequilibrium stationary state KW - large deviation function Y1 - 2022 U6 - https://doi.org/10.1088/1751-8121/ac491c SN - 1751-8113 SN - 1751-8121 VL - 55 IS - 7 PB - IOP Publ. Ltd. CY - Bristol ER - TY - JOUR A1 - Sarabadani, Jalal A1 - Metzler, Ralf A1 - Ala-Nissila, Tapio T1 - Driven polymer translocation into a channel: Isoflux tension propagation theory and Langevin dynamics simulations JF - Physical Review Research N2 - Isoflux tension propagation (IFTP) theory and Langevin dynamics (LD) simulations are employed to study the dynamics of channel-driven polymer translocation in which a polymer translocates into a narrow channel and the monomers in the channel experience a driving force fc. In the high driving force limit, regardless of the channel width, IFTP theory predicts τ ∝ f βc for the translocation time, where β = −1 is the force scaling exponent. Moreover, LD data show that for a very narrow channel fitting only a single file of monomers, the entropic force due to the subchain inside the channel does not play a significant role in the translocation dynamics and the force exponent β = −1 regardless of the force magnitude. As the channel width increases the number of possible spatial configurations of the subchain inside the channel becomes significant and the resulting entropic force causes the force exponent to drop below unity. Y1 - 2022 U6 - https://doi.org/10.1103/PhysRevResearch.4.033003 SN - 2643-1564 VL - 4 SP - 033003-1 EP - 033003-14 PB - American Physical Society CY - College Park, Maryland, USA ET - 3 ER - TY - GEN A1 - Sarabadani, Jalal A1 - Metzler, Ralf A1 - Ala-Nissila, Tapio T1 - Driven polymer translocation into a channel: Isoflux tension propagation theory and Langevin dynamics simulations T2 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe N2 - Isoflux tension propagation (IFTP) theory and Langevin dynamics (LD) simulations are employed to study the dynamics of channel-driven polymer translocation in which a polymer translocates into a narrow channel and the monomers in the channel experience a driving force fc. In the high driving force limit, regardless of the channel width, IFTP theory predicts τ ∝ f βc for the translocation time, where β = −1 is the force scaling exponent. Moreover, LD data show that for a very narrow channel fitting only a single file of monomers, the entropic force due to the subchain inside the channel does not play a significant role in the translocation dynamics and the force exponent β = −1 regardless of the force magnitude. As the channel width increases the number of possible spatial configurations of the subchain inside the channel becomes significant and the resulting entropic force causes the force exponent to drop below unity. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 1292 Y1 - 2023 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-574387 SN - 1866-8372 IS - 1292 SP - 033003-1 EP - 033003-14 ER - TY - JOUR A1 - Schaerer, Daniel A1 - Izotov, Yuri I. A1 - Worseck, Gábor A1 - Berg, Danielle A1 - Chisholm, John A1 - Jaskot, Anne A1 - Nakajima, Kimihiko A1 - Ravindranath, Swara A1 - Thuan, Trinh X. A1 - Verhamme, Anne T1 - Strong Lyman continuum emitting galaxies show intense C IV λ 1550 emission JF - Astronomy and astrophysics N2 - Using the Space Telescope Imaging Spectrograph, we have obtained ultraviolet spectra from similar to 1200 to 2000 angstrom of known Lyman continuum (LyC) emitting galaxies at low redshift (z similar to 0.3-0.4) with varying absolute LyC escape fractions ( f(esc) similar to 0.01-0.72). Our observations include in particular the galaxy J1243+4646, which has the highest known LyC escape fraction at low redshift. While all galaxies are known Lyman alpha emitters, we consistently detect an inventory of additional emission lines, including C IV lambda 1550, He II lambda 1640, O III] lambda 1666, and C III] lambda 1909, whose origin is presumably essentially nebular. C IV lambda 1550 emission is detected above 4 sigma in six out of eight galaxies, with equivalent widths of EW(C IV) = 12-15 angstrom for two galaxies, which exceeds the previously reported maximum emission in low-z star-forming galaxies. We detect C IV lambda 1550 emission in all LyC emitters with escape fractions f(esc) > 0.1 and find a tentative increase in the flux ratio C IV lambda 1550 /C III] lambda 1909 with f(esc). Based on the data, we propose a new criterion to select and classify strong leakers (galaxies with f(esc) > 0.1): C IV lambda 1550 /C III] lambda 1909 greater than or similar to 0.75. Finally, we also find He II lambda 1640 emission in all the strong leakers with equivalent widths from 3 to 8 angstrom rest frame. These are among the highest values observed in star-forming galaxies and are primarily due to a high rate of ionizing photon production. The nebular He II lambda 1640 emission of the strong LyC emitters does not require harder ionizing spectra at >54 eV compared to those of typical star-forming galaxies at similarly low metallicity. KW - galaxies: starburst KW - galaxies: high-redshift KW - dark ages, reionization KW - first stars KW - ultraviolet: galaxies Y1 - 2022 U6 - https://doi.org/10.1051/0004-6361/202243149 SN - 0004-6361 SN - 1432-0746 VL - 658 PB - EDP Sciences CY - Les Ulis ER - TY - JOUR A1 - Schaffenroth, Veronika A1 - Pelisoli, Ingrid A1 - Barlow, Brad N. A1 - Geier, Stephan A1 - Kupfer, Thomas T1 - Hot subdwarfs in close binaries observed from space I. BT - orbital, atmospheric, and absolute parameters and the nature of their companions JF - Astronomy and astrophysics : an international weekly journal N2 - Context: About a third of the hot subdwarfs of spectral type B (sdBs), which are mostly core-helium-burning objects on the extreme horizontal branch, are found in close binaries with cool, low-mass stellar, substellar, or white dwarf companions. They can show light variations due to di fferent phenomena. Aims: Many hot subdwarfs now have space-based light curves with a high signal-to-noise ratio available. We used light curves from the Transiting Exoplanet Survey Satellite and the K2 space mission to look for more sdB binaries. Their light curves can be used to study the hot subdwarf primaries and their companions, and obtained orbital, atmospheric, and absolute parameters for those systems, when combined with other analysis methods. Methods: By classifying the light variations and combining these with the fit of the spectral energy distribution, the distance derived by the parallaxes obtained by Gaia, and the atmospheric parameters, mainly from the literature, we could derive the nature of the primaries and secondaries in 122 (75%) of the known sdB binaries and 82 newly found reflection e ffect systems. We derived absolute masses, radii, and luminosities for a total of 39 hot subdwarfs with cool, low-mass companions, as well 29 known and newly found sdBs with white dwarf companions. Results: The mass distribution of hot subdwarfs with cool, low-mass stellar and substellar companions, di ffers from those with white dwarf companions, implying they come from di fferent populations. By comparing the period and minimum companion mass distributions, we find that the reflection e ffect systems all have M dwarf or brown dwarf companions, and that there seem to be several di fferent populations of hot subdwarfs with white dwarf binaries - one with white dwarf minimum masses around 0.4 M-circle dot, one with longer periods and minimum companion masses up to 0.6 M-circle dot, and at the shortest period, another with white dwarf minimum masses around 0.8 M-circle dot. We also derive the first orbital period distribution for hot subdwarfs with cool, low-mass stellar or substellar systems selected from light variations instead of radial velocity variations. It shows a narrower period distribution, from 1.5 h to 35 h, compared to the distribution of hot subdwarfs with white dwarfs, which ranges from 1 h to 30 days. These period distributions can be used to constrain the previous common-envelope phase. KW - binaries: close KW - subdwarfs KW - white dwarfs KW - stars: late-type KW - stars: KW - horizontal-branch KW - stars: fundamental parameters Y1 - 2022 U6 - https://doi.org/10.1051/0004-6361/202244214 SN - 0004-6361 SN - 1432-0746 VL - 666 PB - EDP Sciences CY - Les Ulis ER - TY - THES A1 - Schemenz, Victoria T1 - Correlations between osteocyte lacuno-canalicular network and material characteristics in bone adaptation and regeneration T1 - Korrelationen zwischen dem lakuno-kanalikulären Netzwerk der Osteozyten und Materialeigenschaften bei der Knochenanpassung und -regeneration N2 - The complex hierarchical structure of bone undergoes a lifelong remodeling process, where it adapts to mechanical needs. Hereby, bone resorption by osteoclasts and bone formation by osteoblasts have to be balanced to sustain a healthy and stable organ. Osteocytes orchestrate this interplay by sensing mechanical strains and translating them into biochemical signals. The osteocytes are located in lacunae and are connected to one another and other bone cells via cell processes through small channels, the canaliculi. Lacunae and canaliculi form a network (LCN) of extracellular spaces that is able to transport ions and enables cell-to-cell communication. Osteocytes might also contribute to mineral homeostasis by direct interactions with the surrounding matrix. If the LCN is acting as a transport system, this should be reflected in the mineralization pattern. The central hypothesis of this thesis is that osteocytes are actively changing their material environment. Characterization methods of material science are used to achieve the aim of detecting traces of this interaction between osteocytes and the extracellular matrix. First, healthy murine bones were characterized. The properties analyzed were then compared with three murine model systems: 1) a loading model, where a bone of the mouse was loaded during its life time; 2) a healing model, where a bone of the mouse was cut to induce a healing response; and 3) a disease model, where the Fbn1 gene is dysfunctional causing defects in the formation of the extracellular tissue. The measurement strategy included routines that make it possible to analyze the organization of the LCN and the material components (i.e., the organic collagen matrix and the mineral particles) in the same bone volumes and compare the spatial distribution of different data sets. The three-dimensional network architecture of the LCN is visualized by confocal laser scanning microscopy (CLSM) after rhodamine staining and is then subsequently quantified. The calcium content is determined via quantitative backscattered electron imaging (qBEI), while small- and wide-angle X-ray scattering (SAXS and WAXS) are employed to determine the thickness and length of local mineral particles. First, tibiae cortices of healthy mice were characterized to investigate how changes in LCN architecture can be attributed to interactions of osteocytes with the surrounding bone matrix. The tibial mid-shaft cross-sections showed two main regions, consisting of a band with unordered LCN surrounded by a region with ordered LCN. The unordered region is a remnant of early bone formation and exhibited short and thin mineral particles. The surrounding, more aligned bone showed ordered and dense LCN as well as thicker and longer mineral particles. The calcium content was unchanged between the two regions. In the mouse loading model, the left tibia underwent two weeks of mechanical stimulation, which results in increased bone formation and decreased resorption in skeletally mature mice. Here the specific research question addressed was how do bone material characteristics change at (re)modeling sites? The new bone formed in response to mechanical stimulation showed similar properties in terms of the mineral particles, like the ordered calcium region but lower calcium content compared to the right, non-loaded control bone of the same mice. There was a clear, recognizable border between mature and newly formed bone. Nevertheless, some canaliculi went through this border connecting the LCN of mature and newly formed bone. Additionally, the question should be answered whether the LCN topology and the bone matrix material properties adapt to loading. Although, mechanically stimulated bones did not show differences in calcium content compared to controls, different correlations were found between the local LCN density and the local Ca content depending on whether the bone was loaded or not. These results suggest that the LCN may serve as a mineral reservoir. For the healing model, the femurs of mice underwent an osteotomy, stabilized with an external fixator and were allowed to heal for 21 days. Thus, the spatial variations in the LCN topology with mineral properties within different tissue types and their interfaces, namely calcified cartilage, bony callus and cortex, could be simultaneously visualized and compared in this model. All tissue types showed structural differences across multiple length scales. Calcium content increased and became more homogeneous from calcified cartilage to bony callus to lamellar cortical bone. The degree of LCN organization increased as well, while the lacunae became smaller, as did the lacunar density between these different tissue types that make up the callus. In the calcified cartilage, the mineral particles were short and thin. The newly formed callus exhibited thicker mineral particles, which still had a low degree of orientation. While most of the callus had a woven-like structure, it also served as a scaffold for more lamellar tissue at the edges. The lamelar bone callus showed thinner mineral particles, but a higher degree of alignment in both, mineral particles and the LCN. The cortex showed the highest values for mineral length, thickness and degree of orientation. At the same time, the lacunae number density was 34% lower and the lacunar volume 40% smaller compared to bony callus. The transition zone between cortical and callus regions showed a continuous convergence of bone mineral properties and lacunae shape. Although only a few canaliculi connected callus and the cortical region, this indicates that communication between osteocytes of both tissues should be possible. The presented correlations between LCN architecture and mineral properties across tissue types may suggest that osteocytes have an active role in mineralization processes of healing. A mouse model for the disease marfan syndrome, which includes a genetic defect in the fibrillin-1 gene, was investigated. In humans, Marfan syndrome is characterized by a range of clinical symptoms such as long bone overgrowth, loose joints, reduced bone mineral density, compromised bone microarchitecture, and increased fracture rates. Thus, fibrillin-1 seems to play a role in the skeletal homeostasis. Therefore, the present work studied how marfan syndrome alters LCN architecture and the surrounding bone matrix. The mice with marfan syndrome showed longer tibiae than their healthy littermates from an age of seven weeks onwards. In contrast, the cortical development appeared retarded, which was observed across all measured characteristics, i. e. lower endocortical bone formation, looser and less organized lacuno-canalicular network, less collagen orientation, thinner and shorter mineral particles. In each of the three model systems, this study found that changes in the LCN architecture spatially correlated with bone matrix material parameters. While not knowing the exact mechanism, these results provide indications that osteocytes can actively manipulate a mineral reservoir located around the canaliculi to make a quickly accessible contribution to mineral homeostasis. However, this interaction is most likely not one-sided, but could be understood as an interplay between osteocytes and extra-cellular matrix, since the bone matrix contains biochemical signaling molecules (e.g. non-collagenous proteins) that can change osteocyte behavior. Bone (re)modeling can therefore not only be understood as a method for removing defects or adapting to external mechanical stimuli, but also for increasing the efficiency of possible osteocyte-mineral interactions during bone homeostasis. With these findings, it seems reasonable to consider osteocytes as a target for drug development related to bone diseases that cause changes in bone composition and mechanical properties. It will most likely require the combined effort of materials scientists, cell biologists, and molecular biologists to gain a deeper understanding of how bone cells respond to their material environment. N2 - Knochen haben eine komplexe hierarchische Struktur, die einen lebenslangen Umbauprozess durchläuft, bei dem der Knochen sich seinen mechanischen Anforderungen anpasst. Um ein gesundes und stabiles Organ zu erhalten müssen Knochenresorption (durch Osteoklasten) und Knochenbildung (durch Osteoblasten) ausgewogen sein. Osteozyten lenken dieses Wechselspiel, indem sie mechanische Belastungen wahrnehmen und sie in biochemische Signale übersetzen. Die Osteozyten sitzen in Lakunen und sind durch Kanälchen untereinander und mit anderen Knochenzellen über ein Netzwerk (LCN) verbunden, das in der Lage ist, Ionen zu transportieren und eine Kommunikation von Zelle zu Zelle zu ermöglichen. Außerdem vermutet man, dass Osteozyten auch durch direkte Wechselwirkungen mit der umgebenden Matrix zur Mineralhomöostase beitragen könnten. Im Mittelpunkt dieser Arbeit steht die Frage, ob Osteozyten ihre materielle Umgebung aktiv verändern können. Um Spuren dieser Wechselwirkung zwischen Osteozyten und der extrazellulären Matrix nachzuweisen, werden materialwissenschaftliche Charakterisierungsmethoden eingesetzt. Zunächst wurden gesunde Mäuseknochen charakterisiert. Die erworbenen Ergebnisse wurden dann mit drei murinen Modellsystemen verglichen: 1) einem Belastungsmodell; 2) ein Heilungsmodell und 3) ein Krankheitsmodell, bei dem das Fbn1-Gen dysfunktional ist und Defekte in der Bildung des extrazellulären Gewebes verursacht werden. Die Messstrategie umfasste Routinen, die es ermöglichen, die Organisation des LCN und der Materialkomponenten (d.h. die organische Kollagenmatrix und die mineralischen Partikel) in denselben Knochenvolumina zu analysieren und die räumliche Verteilung der verschiedenen Datensätze zu vergleichen. Die dreidimensionale Netzwerkarchitektur des LCN wird durch konfokale Laser-Scanning-Mikroskopie nach Rhodamin-Färbung gemessen und anschließend quantifiziert. Der Kalziumgehalt wird mittels quantitativer Rückstreuelektronenbildgebung bestimmt, während Klein- und Weitwinkel-Röntgenstreuung verwendet werden, um die Dicke und Länge der Mineralpartikel zu bestimmen. Zunächst wurden Querschnitte der Unterschenkel von gesunden Mäusen charakterisiert, um zu untersuchen, ob Veränderungen in der LCN-Architektur auf Wechselwirkungen von Osteozyten mit der umgebenden Knochenmatrix zurückgeführt werden können. Die Kortizes zeigten zwei Hauptregionen, ein Band mit ungeordneter LCN-Architektur, umgeben von einer Region mit geordneter LCN. Die ungeordnete Region ist ein Überbleibsel der frühen Knochenbildung und wies kurze und dünne Mineralpartikel auf. Der umgebende, stärker ausgerichtete Knochen zeigte ein geordnetes und dichtes LCN, sowie dickere und längere Mineralpartikel. Der Kalziumgehalt blieb bei beiden Regionen unverändert. Im Mausbelastungsmodell wurde das linke Schienbein zwei Wochen lang mechanisch stimuliert, was zu einer erhöhten Knochenbildung führt. Hier sollte die Forschungsfrage beantwortet werden, wie sich Knochenmaterialeigenschaften an (Re-)Modellierungsstellen aufgrund von Belastung ändern. Der, als Reaktion auf die mechanische Stimulation, gebildete neue Knochen zeigte ähnliche Eigenschaften in Bezug auf die Mineralpartikel, wie die geordnete Kortexregion. Es gab eine klar erkennbare Grenze zwischen reifem und neu gebildetem Knochen. Trotzdem gingen einige Kanälchen durch diese Grenze, die die LCN aus reifem und neu gebildetem Knochen verband. Für das Heilungsmodell wurden die Oberschenkel von Mäusen einer Osteotomie unterzogen (einer Operation, bei der durch einen Schnitt in der Diaphyse ein Bruch erzeugt wird). Danach konnte die Fraktur 21 Tage heilen. Dadurch konnten in diesem Modell gleichzeitig verkalkter Knorpel, knöcherner Kallus und Kortex untersucht werden. Dafür wurde die räumliche Verteilung der LCN-Topologie sowie die Mineraleigenschaften der verschiedenen Gewebetypen und ihrer Grenzflächen visualisiert und verglichen. Alle Gewebetypen zeigten strukturelle Unterschiede über mehrere Längenskalen hinweg. Der Kalziumgehalt nahm von kalzifiziertem Knorpel zu knöchernem Kallus zu lamellarem kortikalem Knochen zu und wurde homogener. Der Grad der LCN-Organisation nahm ebenfalls zu, während die Lakunen vom Kallus zum Kortexgewebe kleiner wurden, ebenso wie die Lakunendichte. Im verkalkten Knorpel waren die Mineralpartikel kurz und dünn. Der größte Teil des Kallus wies eine Geflechtsknochenstruktur auf und diente als Gerüst für lamellares Gewebe, das dünnere Mineralpartikel, aber einen höheren Grad an Ausrichtung sowohl in den Mineralpartikeln als auch im LCN aufwies. Der Kortex zeigte die höchsten Werte für Minerallänge, Dicke und Orientierungsgrad. Obwohl nur wenige Kanälchen den Kallus und kortikale Regionen verbinden, weist dies darauf hin, dass eine Kommunikation zwischen Osteozyten beider Gewebe möglich sein sollte. Es wurde auch ein Mausmodell für das Marfan-Syndrom untersucht, das einen Gendefekt im Fibrillin-1-Gen beinhaltet. Beim Menschen ist das Marfan-Syndrom durch eine Reihe klinischer Symptome gekennzeichnet, wie z. B. übermäßiges Wachstum der Gliedmaßen, überstreckbare Gelenke, verringerte Knochenmineraldichte, beeinträchtigte Knochenmikroarchitektur und erhöhte Frakturraten. Somit scheint Fibrillin-1 eine Rolle in der Skeletthomöostase zu spielen. Deswegen untersuchte die vorliegende Arbeit, ob und wie das Marfan-Syndrom die LCN-Architektur und die umgebende Knochenmatrix verändert. Die Mäuse mit Marfan-Syndrom zeigten bereits ab einem Alter von sieben Wochen längere Schienbeine als ihre gesunden Wurfgeschwister. Im Gegensatz dazu erschien die kortikale Entwicklung verzögert, was über alle gemessenen Merkmale hinweg beobachtet wurde, d.h. niedrigere endokortikale Knochenbildung, lockereres und weniger organisiertes LCN, geringerer Grad an Kollagenorientierung sowie ein Trend zu dünneren und kürzeren Mineralpartikel. In jedem der drei Modellsysteme fand diese Studie, dass Änderungen in der LCN-Architektur räumlich mit Parametern des Knochenmatrixmaterials korrelierten. Obwohl der genaue Mechanismus nicht bekannt ist, liefern diese Ergebnisse Hinweise darauf, dass Osteozyten ein Mineralreservoir aktiv manipulieren können. Dieses Reservoir befindet sich um die Kanälchen herum und dieser Prozess würde es ermöglichen, einen schnell zugänglichen Beitrag zur Mineralhomöostase zu leisten. Diese Interaktion ist jedoch höchstwahrscheinlich nicht einseitig, sondern könnte als Wechselspiel zwischen Osteozyten und extrazellulärer Matrix verstanden werden, da die Knochenmatrix biochemische Signalmoleküle enthält, die das Verhalten von Osteozyten verändern können. Knochen(re)modellierung kann daher nicht nur als Methode zur Defektbeseitigung oder Anpassung an äußere mechanische Reize verstanden werden, sondern auch zur Effizienzsteigerung möglicher Osteozyten-Mineral-Interaktionen während der Knochenhomöostase. Angesichts dieser Ergebnisse erscheint es sinnvoll, Osteozyten als Ziel für die Arzneimittelentwicklung im Zusammenhang mit Knochenerkrankungen in Betracht zu ziehen, die Veränderungen der Knochenzusammensetzung und deren mechanischen Eigenschaften verursachen. KW - bone KW - lacunae KW - mineralization KW - SAXS KW - lacuno-canalicular network KW - µCT KW - CLSM KW - konfokales Laser-Scanning-Mikroskop KW - Kleinwinkelröntgenstreuung KW - Knochen KW - Lakunen KW - lakuno-kanaliculäres Netzwerk KW - Mineralisierung KW - µCT Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-559593 ER - TY - THES A1 - Schlemm, Tanja T1 - The marine ice cliff instability of the Antarctic ice sheet T1 - Die marine Eisklippeninstabilität des antarktischen Eisschildes BT - a theory of mélange-buttressed cliff calving and its application in the Parallel Ice Sheet Model BT - eine Theorie des Mélange-gebremsten Klippenkalbens und ihre Anwendung im Parallel Ice Sheet Model N2 - The Antarctic ice sheet is the largest freshwater reservoir worldwide. If it were to melt completely, global sea levels would rise by about 58 m. Calculation of projections of the Antarctic contribution to sea level rise under global warming conditions is an ongoing effort which yields large ranges in predictions. Among the reasons for this are uncertainties related to the physics of ice sheet modeling. These uncertainties include two processes that could lead to runaway ice retreat: the Marine Ice Sheet Instability (MISI), which causes rapid grounding line retreat on retrograde bedrock, and the Marine Ice Cliff Instability (MICI), in which tall ice cliffs become unstable and calve off, exposing even taller ice cliffs. In my thesis, I investigated both marine instabilities (MISI and MICI) using the Parallel Ice Sheet Model (PISM), with a focus on MICI. N2 - Der antarktische Eisschild ist das größte Süßwasserreservoir der Welt. Würde er vollständig schmelzen, würde der globale Meeresspiegel um etwa 58 m ansteigen. Die Ermittlung von Prognosen über den Beitrag der Antarktis zum Anstieg des Meeresspiegels infolge der globalen Erwärmung ist ein fortlaufender Prozess, der große Unterschiede in den Vorhersagen zur Folge hat. Einer der Gründe dafür sind Ungewissheiten im Zusammenhang mit der Physik der Eisschildmodellierung. Zu diesen Unsicherheiten gehören zwei Prozesse, die zu einem unkontrollierten Eisrückzug führen könnten: die Marine Ice Sheet Instability (MISI), die zu einem schnellen Rückzug der Grundlinie auf rückläufigem Grundgestein führt, und die Marine Ice Cliff Instability (MICI), bei der hohe Eisklippen instabil werden und abkalben, wodurch noch höhere Eisklippen freigelegt werden. In meiner Dissertation untersuchte ich beide marinen Instabilitäten (MISI und MICI) mit Hilfe des Parallel Ice Sheet Model (PISM), wobei der Schwerpunkt auf MICI lag. KW - Antarctica KW - ice sheet modelling KW - iceberg calving KW - Antarktis KW - Eisschildmodellierung KW - Eisbergkalbung Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-586333 ER - TY - JOUR A1 - Schlemm, Tanja A1 - Feldmann, Johannes A1 - Winkelmann, Ricarda A1 - Levermann, Anders T1 - Stabilizing effect of melange buttressing on the marine ice-cliff instability of the West Antarctic Ice Sheet JF - The Cryosphere : TC ; an interactive open access journal of the European Geosciences Union N2 - Owing to global warming and particularly high regional ocean warming, both Thwaites and Pine Island Glaciers in the Amundsen region of the Antarctic Ice Sheet could lose their buttressing ice shelves over time. We analyse the possible consequences using the parallel ice sheet model (PISM), applying a simple cliff-calving parameterization and an ice melange-buttressing model. We find that the instantaneous loss of ice-shelf buttressing, due to enforced ice-shelf melting, initiates grounding-line retreat and triggers marine ice sheet instability (MISI). As a consequence, the grounding line progresses into the interior of the West Antarctic Ice Sheet and leads to a sea level contribution of 0.6 m within 100 a. By subjecting the exposed ice cliffs to cliff calving using our simplified parameterization, we also analyse marine ice cliff instability (MICI). In our simulations it can double or even triple the sea level contribution depending on the only loosely constrained parameter that determines the maximum cliff-calving rate. The speed of MICI depends on this upper bound of the calving rate, which is given by the ice melange buttressing the glacier. However, stabilization of MICI may occur for geometric reasons. Because the embayment geometry changes as MICI advances into the interior of the ice sheet, the upper bound on calving rates is reduced and the progress of MICI is slowed down. Although we cannot claim that our simulations bear relevant quantitative estimates of the effect of ice-melange buttressing on MICI, the mechanism has the potential to stop the instability. Further research is needed to evaluate its role for the past and future evolution of the Antarctic Ice Sheet. Y1 - 2022 U6 - https://doi.org/10.5194/tc-16-1979-2022 SN - 1994-0416 SN - 1994-0424 VL - 16 IS - 5 SP - 1979 EP - 1996 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Schmidt, Thomas A1 - Cioni, Maria-Rosa L. A1 - Niederhofer, Florian A1 - Bekki, Kenji A1 - Bell, Cameron P. M. A1 - de Grijs, Richard A1 - El Youssoufi, Dalal A1 - Ivanov, Valentin D. A1 - Oliveira, Joana M. A1 - Ripepi, Vincenzo A1 - van Loon, Jacco Th. T1 - The VMC survey: XLV. Proper motion of the outer LMC and the impact of the SMC JF - Astronomy and astrophysics N2 - Context. The Large Magellanic Cloud (LMC) is the most luminous satellite galaxy of the Milky Way and, owing to its companion, the Small Magellanic Cloud (SMC), represents an excellent laboratory to study the interaction of dwarf galaxies. Aims. The aim of this study is to investigate the kinematics of the outer regions of the LMC by using stellar proper motions to understand the impact of interactions, for example with the SMC about 250 Myr ago. Methods. We calculate proper motions using multi-epoch K s -band images from the VISTA survey of the Magellanic Cloud system (VMC). Observations span a time baseline of 2-5 yr. We combine the VMC data with data from the Gaia Early Data Release 3 and introduce a new method to distinguish between Magellanic and Milky Way stars based on a machine learning algorithm. This new technique enables a larger and cleaner sample selection of fainter sources as it reaches below the red clump of the LMC. Results. We investigate the impact of the SMC on the rotational field of the LMC and find hints of stripped SMC debris. The southeastern region of the LMC shows a slow rotational speed compared to the overall rotation. N-body simulations suggest that this could be caused by a fraction of stripped SMC stars located in that particular region that move opposite to the expected rotation. KW - Galaxy: kinematics and dynamics KW - Magellanic Clouds KW - galaxies: KW - interactions KW - proper motions KW - surveys Y1 - 2022 U6 - https://doi.org/10.1051/0004-6361/202142148 SN - 0004-6361 SN - 1432-0746 VL - 663 PB - EDP Sciences CY - Les Ulis ER - TY - JOUR A1 - Schröder, Jakob A1 - Evans, Alexander A1 - Polatidis, Efthymios A1 - Mohr, Gunther A1 - Serrano-Munoz, Itziar A1 - Bruno, Giovanni A1 - Čapek, Jan T1 - Understanding the impact of texture on the micromechanical anisotropy of laser powder bed fused Inconel 718 JF - Journal of materials science N2 - The manufacturability of metallic alloys using laser-based additive manufacturing methods such as laser powder bed fusion has substantially improved within the last decade. However, local melting and solidification cause hierarchically structured and crystallographically textured microstructures possessing large residual stress. Such microstructures are not only the origin of mechanical anisotropy but also pose metrological challenges for the diffraction-based residual stress determination. Here we demonstrate the influence of the build orientation and the texture on the microstructure and consequently the mechanical anisotropy of as-built Inconel 718. For this purpose, we manufactured specimens with [001]/[011]-, [001]- and [011]/[11 (1) over bar]-type textures along their loading direction. In addition to changes in the Young's moduli, the differences in the crystallographic textures result in variations of the yield and ultimate tensile strengths. With this in mind, we studied the anisotropy on the micromechanical scale by subjecting the specimens to tensile loads along the different texture directions during in situ neutron diffraction experiments. In this context, the response of multiple lattice planes up to a tensile strain of 10% displayed differences in the load partitioning and the residual strain accumulation for the specimen with [011]/[(1) over bar 11]-type texture. However, the relative behavior of the specimens possessing an [001] /[011]- and [001]-type texture remained qualitatively similar. The consequences on the metrology of residual stress determination methods are discussed. Y1 - 2022 U6 - https://doi.org/10.1007/s10853-022-07499-9 SN - 0022-2461 SN - 1573-4803 VL - 57 IS - 31 SP - 15036 EP - 15058 PB - Springer CY - New York ER -