TY - THES A1 - Kaiser, Michael T1 - Einfluss von Bewirtschaftungsmaßnahmen auf Menge und Zusammensetzung unterschiedlich stabiler Fraktionen der organischen Bodensubstanz N2 - Ziel dieser Arbeit ist es, ein sequentielles Extraktionsverfahren zur Erfassung unterschiedlich stabiler Anteile der orgnischen Bodensubstanz (OBS) zu entwickeln und zu klären, ob ein Zusammenhang zwischen Löslichkeit und Stabilität besteht. Darüber hinaus sollen der Einfluss von Bewirtschaftungsmaßnahmen auf Menge und Zusammensetzung dieser OBS-Anteile und Zusammenhänge zwischen Fourier Transform Infrarot (FT-IR)-Spektroskopiedaten und der Kationenaustauschkapazität (KAK) der OBS analysiert werden. Für die Untersuchungen wurden Böden der Langzeitfeldexperimente (LFE) in Halle, Bad Lauchstädt und Rotthalmünster beprobt. Zur Erfassung unterschiedlicher OBS-Fraktionen wurden im ersten Schritt die wasserlöslichen OBS-Anteile (OBS(W)-Fraktion) aus den Böden isoliert. Im zweiten Schritt wurden aus den Extraktionsrückständen der Wasserextraktion OBS-Anteile mit einer Natrium (Na)-Pyrophosphatlösung extrahiert (OBS(PY)-Fraktion). Die Stabilität der OBS-Fraktionen wurde anhand von δ13C-Bestimmungen und 14C-Messungen untersucht. Die Charakterisierung der Zusammensetzung der OBS-Fraktionen erfolgte mittels FT-IR Spektroskopie. Generell wird mit der OBS(PY)-Fraktion ein größerer Anteil am organischen Kohlenstoffgehalt der Böden erfasst als mit der OBS(W)-Fraktion. Die δ13C- und 14C-Daten zeigen, dass die OBS(W)-Fraktion höhere Anteile jungen organischen Materials als die OBS(PY)-Fraktion enthält. Das entwickelte sequentielle Extraktionsverfahren ist also prinzipiell geeignet unterschiedlich stabile OBS-Anteile anhand ihrer Löslichkeit zu isolieren. Mittels FT-IR spektroskopischer Untersuchungen wird festgestellt, dass Bewirtschaftungsmaßnahmen, wie die Düngung, sowie Standorteigenschaften die Zusammensetzung der OBS-Fraktionen beeinflussen. Für die OBS(PY)-Fraktion ist dies stärker ausgeprägt als für die OBS(W)-Fraktion. Die KAK der OBS(PY)-Fraktion aus den Böden der LFE in Halle und Bad Lauchstädt ist positiv mit der Absorptionsintensität der C=O-Bande in den FT-IR Spektren dieser OBS-Fraktion korreliert. N2 - The aim of this work is the development of a sequential extraction procedure for the isolation of different stable parts of soil organic matter (SOM) according to their solubility and to prove the relationship between solubility and stability. Additionally, the effects of management on amount and composition of different SOM fractions as well as relationships between data sets from Fourier Transform Infrared (FT-IR) spectroscopy and cation exchange capacitity (CEC) of SOM should be analysed. Soils from long term field experiments at Halle, Bad Lauchstädt and Rotthalmünster were sampled from the soil surface up to 30 cm depth. To obtain different SOM fractions water soluble SOM (SOM(W) fraction) were extracted at first before Na-pyrophosphat soluble SOM (SOM (PY) fraction) were isolated from the residue of water extraction. Stability of different SOM fractions were analyzed using 14C- and δ13C-measurements. Functional composition was studied with FT-IR spectroscopy. Generally, SOM(PY) represents a larger part of soil organic carbon (SOC) than SOM(W) in relation to the total SOC-content of the investigated soils. δ13C- and 14C-measurements show that SOM(W) contains more younger material than SOM(PY). The findings suggest that different stable SOM fractions can be obtained according to their solubility by the sequential extraction procedure. FTIR spectra show that SOM composition is influenced by management options like fertilization and field conditions. Such effects are more pronounced for SOM(PY) than for SOM(W). Furthermore data from FT-IR spectra and CEC measurements of SOMPY) show that the CEC is closely related to the C=O absorption intensities. T2 - Einfluss von Bewirtschaftungsmaßnahmen auf Menge und Zusammensetzung unterschiedlich stabiler Fraktionen der organischen Bodensubstanz KW - organische Bodensubstanz KW - unterschiedlich lösliche Fraktionen KW - Stabilität KW - FT-IR Spektroskopie KW - soil organic matter KW - different soluble fractions KW - stability KW - FT-IR spectroscopy Y1 - 2004 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-0001886 ER - TY - JOUR A1 - Lilie, Hauke A1 - Baer, Dorit A1 - Kettner, Karina A1 - Weininger, Ulrich A1 - Balbach, Jochen A1 - Naumann, Manfred A1 - Mueller, Eva-Christina A1 - Otto, Albrecht A1 - Gast, Klaus A1 - Golbik, Ralph A1 - Kriegel, Thomas T1 - Yeast hexokinase isoenzyme ScHxk2 stability of a two-domain protein with discontinuous domains JF - Protein engineering design & selection N2 - The hexokinase isoenzyme 2 of Saccharomyces cerevisiae (ScHxk2) represents an archetype of a two-domain protein with the active site located in a cleft between the two domains. Binding of the substrate glucose results in a rigid body movement of the two domains leading to a cleft closure of the active site. Both domains of this enzyme are composed of discontinuous peptide sequences. This structural feature is reflected in the stability and folding of the ScHxk2 protein. Structural transitions induced by urea treatment resulted in the population of a thermodynamically stable folding intermediate, which, however, does not correspond to a molecule with one domain folded and the other unfolded. As demonstrated by different spectroscopic techniques, both domains are structurally affected by the partial denaturation. The intermediate possesses only 40% of the native secondary structural content and a substantial increase in the Stokes radius as judged by circular dichroism and dynamic light scattering analyses. One-dimensional H-1 NMR data prove that all tryptophan residues are in a non-native environment in the intermediate, indicating substantial changes in the tertiary structure. Still, the intermediate possesses quite a high stability for a transition intermediate of about Delta G = -22 kJ mol(-1). KW - dynamic light scattering KW - NMR KW - ScHxk2 KW - stability KW - transition intermediate Y1 - 2011 U6 - https://doi.org/10.1093/protein/gzq098 SN - 1741-0126 VL - 24 IS - 1-2 SP - 79 EP - 87 PB - Oxford Univ. Press CY - Oxford ER - TY - THES A1 - Robinson, Alexander T1 - Modeling the Greenland Ice Sheet response to climate change in the past and future T1 - Modellierung der Reaktion des Grönländischen Inlandeises auf den vergangenen und zukünftigen Klimawandel N2 - The Greenland Ice Sheet (GIS) contains enough water volume to raise global sea level by over 7 meters. It is a relic of past glacial climates that could be strongly affected by a warming world. Several studies have been performed to investigate the sensitivity of the ice sheet to changes in climate, but large uncertainties in its long-term response still exist. In this thesis, a new approach has been developed and applied to modeling the GIS response to climate change. The advantages compared to previous approaches are (i) that it can be applied over a wide range of climatic scenarios (both in the deep past and the future), (ii) that it includes the relevant feedback processes between the climate and the ice sheet and (iii) that it is highly computationally efficient, allowing simulations over very long timescales. The new regional energy-moisture balance model (REMBO) has been developed to model the climate and surface mass balance over Greenland and it represents an improvement compared to conventional approaches in modeling present-day conditions. Furthermore, the evolution of the GIS has been simulated over the last glacial cycle using an ensemble of model versions. The model performance has been validated against field observations of the present-day climate and surface mass balance, as well as paleo information from ice cores. The GIS contribution to sea level rise during the last interglacial is estimated to be between 0.5-4.1 m, consistent with previous estimates. The ensemble of model versions has been constrained to those that are consistent with the data, and a range of valid parameter values has been defined, allowing quantification of the uncertainty and sensitivity of the modeling approach. Using the constrained model ensemble, the sensitivity of the GIS to long-term climate change was investigated. It was found that the GIS exhibits hysteresis behavior (i.e., it is multi-stable under certain conditions), and that a temperature threshold exists above which the ice sheet transitions to an essentially ice-free state. The threshold in the global temperature is estimated to be in the range of 1.3-2.3°C above preindustrial conditions, significantly lower than previously believed. The timescale of total melt scales non-linearly with the overshoot above the temperature threshold, such that a 2°C anomaly causes the ice sheet to melt in ca. 50,000 years, but an anomaly of 6°C will melt the ice sheet in less than 4,000 years. The meltback of the ice sheet was found to become irreversible after a fraction of the ice sheet is already lost – but this level of irreversibility also depends on the temperature anomaly. N2 - Das grönländische Inlandeis (GIS) besteht aus einem Wasservolumen das ausreicht, um den globalen Meeresspiegel um 7 Meter ansteigen zu lassen. Es ist ein Relikt der vergangenen Eiszeit, das in einer zunehmend wärmer werdenden Welt stark in Mitleidenschaft gezogen werden könnte. In der vorliegenden Dissertation ist ein neues Verfahren zur Modellierung des Antwortverhaltens des Inlandeises auf Klimaänderungen entwickelt und angewendet worden. Die Vorteile des neuen Verfahrens im Vergleich zu den bisherigen Verfahren sind, (i) dass es über einen groen Bereich von Klimaszenarien (sowohl für die ferne Vergangenheit als auch für die Zukunft) anwendbar ist, (ii) dass es die wesentlichen Rückkopplungsprozesse zwischen Klima und Inlandeis enthält und (iii) dass es wegen seiner guten Rechenzeiteffizienz Simulationen über sehr lange Zeitskalen erlaubt. Das neue Modell (REMBO) ist für die Modellierung des Klimas und der Massenbilanz an der grönländischen Oberfläche entwickelt worden und stellt ein verbessertes Verfahren im Vergleich zu den bisherigen dar. Die Entwicklung von GIS über den letzten glazialen Zyklus ist mittels eines Ensembles von verschiedenen Modellversionen simuliert worden. Anschließend ist die Tauglichkeit der Modellversionen durch Vergleich mit Beobachtungsdaten des gegenwärtigen Klimas und der Oberflächenmassenbilanz, sowie mit paleoklimatischen Rekonstruktionen von Eisbohrkernen verifiziert worden. Der Anteil von GIS am Meeresspiegelanstieg während des letzten Interglazials ist im Bereich von 0.5 bis 4.1 m berechnet worden, was konsistent mit bisherigen Schätzungen ist. Von den Ensemblesimulationen sind diejenigen ausgewählt worden, deren Ergebnisse gut mit den Daten übereinstimmen. Durch die Auswahl von geeigneten Modellversionen sind gleichzeitig die Unsicherheiten der Parameterwerte begrenzt worden, so dass sich nun mit dem neuen Verfahren die Sensitivität von GIS auf Klimaänderungen bestimmen lässt. Mit den ausgewählten Modellversionen ist die Sensitivität von GIS auf langfristige Klimaänderungen untersucht worden. Es zeigt sich, dass das GIS ein Hystereseverhalten besitzt (d.h., eine Multistabilität für gewisse Klimazustände) und dass ein Temperaturschwellwert existiert. Bei Überschreiten des Schwellwertes bleibt das GIS nicht erhalten und wird langsam eisfrei werden. Der Temperaturschwellwert der globalen Mitteltemperatur relativ zur vorindustriellen Mitteltemperatur ist im Bereich 1.3-2.3°C ermittelt worden und liegt damit deutlich niedriger als bisher angenommen. Die Zeitdauer bis zum völligen Abschmelzen zeigt ein nichtlineares Verhalten hinsichtlich einer Erwärmung über den ermittelten Schwellwert. Eine Erwärmung von 2°C relativ zur vorindustriellen Zeit führt zu einem Abschmelzen nach 50.000 Jahren, aber eine Erwärmung um 6°C lässt das Inlandeis bereits nach 4.000 Jahren abschmelzen. Ein weiteres Ergebnis ist, dass der Abschmelzvorgang irreversibel werden kann, nachdem ein gewisser Anteil des Inlandeises abgeschmolzen ist – jedoch ist die Irreversibilität eines Abschmelzvorganges auch von der Temperaturanomalie abhängig. KW - Grönland KW - Inlandeis KW - Klimawandel KW - Stabilität KW - Hysterese KW - Greenland KW - ice sheet KW - climate change KW - stability KW - hysteresis Y1 - 2011 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-50430 ER - TY - JOUR A1 - Venail, Patrick A1 - Gross, Kevin A1 - Oakley, Todd H. A1 - Narwani, Anita A1 - Allan, Eric A1 - Flombaum, Pedro A1 - Isbell, Forest A1 - Joshi, Jasmin Radha A1 - Reich, Peter B. A1 - Tilman, David A1 - van Ruijven, Jasper A1 - Cardinale, Bradley J. T1 - Species richness, but not phylogenetic diversity, influences community biomass production and temporal stability in a re-examination of 16 grassland biodiversity studies JF - Functional ecology : an official journal of the British Ecological Society N2 - Hundreds of experiments have now manipulated species richness (SR) of various groups of organisms and examined how this aspect of biological diversity influences ecosystem functioning. Ecologists have recently expanded this field to look at whether phylogenetic diversity (PD) among species, often quantified as the sum of branch lengths on a molecular phylogeny leading to all species in a community, also predicts ecological function. Some have hypothesized that phylogenetic divergence should be a superior predictor of ecological function than SR because evolutionary relatedness represents the degree of ecological and functional differentiation among species. But studies to date have provided mixed support for this hypothesis. Here, we reanalyse data from 16 experiments that have manipulated plant SR in grassland ecosystems and examined the impact on above-ground biomass production over multiple time points. Using a new molecular phylogeny of the plant species used in these experiments, we quantified how the PD of plants impacts average community biomass production as well as the stability of community biomass production through time. Using four complementary analyses, we show that, after statistically controlling for variation in SR, PD (the sum of branches in a molecular phylogenetic tree connecting all species in a community) is neither related to mean community biomass nor to the temporal stability of biomass. These results run counter to past claims. However, after controlling for SR, PD was positively related to variation in community biomass over time due to an increase in the variances of individual species, but this relationship was not strong enough to influence community stability. In contrast to the non-significant relationships between PD, biomass and stability, our analyses show that SR per se tends to increase the mean biomass production of plant communities, after controlling for PD. The relationship between SR and temporal variation in community biomass was either positive, non-significant or negative depending on which analysis was used. However, the increases in community biomass with SR, independently of PD, always led to increased stability. These results suggest that PD is no better as a predictor of ecosystem functioning than SR.Synthesis. Our study on grasslands offers a cautionary tale when trying to relate PD to ecosystem functioning suggesting that there may be ecologically important trait and functional variation among species that is not explained by phylogenetic relatedness. Our results fail to support the hypothesis that the conservation of evolutionarily distinct species would be more effective than the conservation of SR as a way to maintain productive and stable communities under changing environmental conditions. KW - biodiversity KW - community biomass KW - data synthesis KW - ecosystem functioning KW - grasslands KW - phylogenetic diversity KW - relatedness KW - stability Y1 - 2015 U6 - https://doi.org/10.1111/1365-2435.12432 SN - 0269-8463 SN - 1365-2435 VL - 29 IS - 5 SP - 615 EP - 626 PB - Wiley-Blackwell CY - Hoboken ER - TY - GEN A1 - Feldmann, Johannes A1 - Levermann, Anders T1 - Interaction of marine ice-sheet instabilities in two drainage basins BT - simple scaling of geometry and transition time T2 - Postprints der Universität Potsdam : Mathematisch-Naturwissenschaftliche Universität N2 - The initiation of a marine ice-sheet instability (MISI) is generally discussed from the ocean side of the ice sheet. It has been shown that the reduction in ice-shelf buttressing and softening of the coastal ice can destabilize a marine ice sheet if the bedrock is sloping upward towards the ocean. Using a conceptional flow-line geometry, we investigate the possibility of whether a MISI can be triggered from the direction of the ice divide as opposed to coastal forcing and explore the interaction between connected basins. We find that the initiation of a MISI in one basin can induce a destabilization in the other. The underlying mechanism of basin interaction is based on dynamic thinning and a consecutive motion of the ice divide which induces a thinning in the adjacent basin and a successive initiation of the instability. Our simplified and symmetric topographic setup allows scaling both the geometry and the transition time between both instabilities. We find that the ice profile follows a universal shape that is scaled with the horizontal extent of the ice sheet and that the same exponent of 1/2 applies for the scaling relation between central surface elevation and horizontal extent as in the pure shallow ice approximation (Vialov profile). Altering the central bed elevation, we find that the extent of grounding-line retreat in one basin determines the degree of interaction with the other. Different scenarios of basin interaction are discussed based on our modeling results as well as on a conceptual flux-balance analysis. We conclude that for the three-dimensional case, the possibility of drainage basin interaction on timescales on the order of 1 kyr or larger cannot be excluded and hence needs further investigation. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 511 KW - Pine Island Glacier KW - model PISM-PIK KW - West Antarctica KW - grounding-line KW - Thwaites Glacier KW - divide position KW - part 1 KW - stability KW - shelf KW - accumulation Y1 - 2019 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-408903 SN - 1866-8372 IS - 511 ER - TY - JOUR A1 - Cappel, Ute B. A1 - Svanstrom, Sebastian A1 - Lanzilotto, Valeria A1 - Johansson, Fredrik O. L. A1 - Aitola, Kerttu A1 - Philippe, Bertrand A1 - Giangrisostomi, Erika A1 - Ovsyannikov, Ruslan A1 - Leitner, Torsten A1 - Föhlisch, Alexander A1 - Svensson, Svante A1 - Martensson, Nils A1 - Boschloo, Gerrit A1 - Lindblad, Andreas A1 - Rensmo, Hakan T1 - Partially Reversible Photoinduced Chemical Changes in a Mixed-Ion Perovskite Material for Solar Cells JF - ACS applied materials & interfaces N2 - Metal halide perovskites have emerged as materials of high interest for solar energy-to-electricity conversion, and in particular, the use of mixed-ion structures has led to high power conversion efficiencies and improved stability. For this reason, it is important to develop means to obtain atomic level understanding of the photoinduced behavior of these materials including processes such as photoinduced phase separation and ion migration. In this paper, we implement a new methodology combining visible laser illumination of a mixed-ion perovskite ((FAP-bI(3))(0.85)(MAPbBr(3))(0.15)) with the element specificity and chemical sensitivity of core-level photoelectron spectroscopy. By carrying out measurements at a synchrotron beamline optimized for low X-ray fluxes, we are able to avoid sample changes due to X-ray illumination and are therefore able to monitor what sample changes are induced by visible illumination only. We find that laser illumination causes partially reversible chemistry in the surface region, including enrichment of bromide at the surface, which could be related to a phase separation into bromide- and iodide-rich phases. We also observe a partially reversible formation of metallic lead in the perovskite structure. These processes occur on the time scale of minutes during illumination. The presented methodology has a large potential for understanding light-induced chemistry in photoactive materials and could specifically be extended to systematically study the impact of morphology and composition on the photostability of metal halide perovskites. KW - photoelectron spectroscopy KW - laser illumination KW - lead halide perovskite KW - ion migration KW - phase separation KW - stability Y1 - 2017 U6 - https://doi.org/10.1021/acsami.7b10643 SN - 1944-8244 VL - 9 SP - 34970 EP - 34978 PB - American Chemical Society CY - Washington ER - TY - JOUR A1 - de Wiljes, Jana A1 - Reich, Sebastian A1 - Stannat, Wilhelm T1 - Long-Time stability and accuracy of the ensemble Kalman-Bucy Filter for fully observed processes and small measurement noise JF - SIAM Journal on Applied Dynamical Systems N2 - The ensemble Kalman filter has become a popular data assimilation technique in the geosciences. However, little is known theoretically about its long term stability and accuracy. In this paper, we investigate the behavior of an ensemble Kalman-Bucy filter applied to continuous-time filtering problems. We derive mean field limiting equations as the ensemble size goes to infinity as well as uniform-in-time accuracy and stability results for finite ensemble sizes. The later results require that the process is fully observed and that the measurement noise is small. We also demonstrate that our ensemble Kalman-Bucy filter is consistent with the classic Kalman-Bucy filter for linear systems and Gaussian processes. We finally verify our theoretical findings for the Lorenz-63 system. KW - data assimilation KW - Kalman Bucy filter KW - ensemble Kalman filter KW - stability KW - accuracy KW - asymptotic behavior Y1 - 2018 U6 - https://doi.org/10.1137/17M1119056 SN - 1536-0040 VL - 17 IS - 2 SP - 1152 EP - 1181 PB - Society for Industrial and Applied Mathematics CY - Philadelphia ER - TY - JOUR A1 - Rentzsch, Katrin A1 - Schröder-Abe, Michela T1 - Stability and change in domain-specific Self-esteem and global self-esteem JF - European journal of personality N2 - A notable uptick of interest in the stability of self-esteem has been observed over the past few years. Most researchers, however, have focused on unidimensional rather than multidimensional conceptualizations of self-esteem. The paucity of empirical research is surprising given conflicting theoretical perspectives on the stability of self-esteem. The goal of the present study was to thoroughly disentangle different conceptualizations of self-esteem and test opposing classical theories on (i) the stability and (ii) the direction of mutual influence of these different forms of self-esteem. We analysed two-year longitudinal data from participants (N=644 at T1, N=241 at T2) with an average age of 47.0years (SD=12.4). Analyses using a latent variable approach revealed that the domains of self-esteem were relatively stable in terms of rank order and mean levels. In fact, the size of the stability coefficients was comparable to that of other trait measures that have been reported in the literature and paralleled the stability observed for global self-esteem. Results did not provide support for either top-down or bottom-up effects between domain-specific and global self-esteem. These findings have important theoretical and practical implications regarding the stability and development of self-esteem in adulthood and advance the understanding of self-esteem in personality theory. (c) 2018 European Association of Personality Psychology KW - self-esteem KW - stability KW - multidimensional KW - domain specific KW - adulthood Y1 - 2018 U6 - https://doi.org/10.1002/per.2167 SN - 0890-2070 SN - 1099-0984 VL - 32 IS - 4 SP - 353 EP - 370 PB - Wiley CY - Hoboken ER - TY - GEN A1 - Raatz, Michael A1 - van Velzen, Ellen A1 - Gaedke, Ursula T1 - Co‐adaptation impacts the robustness of predator–prey dynamics against perturbations T2 - Postprints der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe N2 - Global change threatens the maintenance of ecosystem functions that are shaped by the persistence and dynamics of populations. It has been shown that the persistence of species increases if they possess larger trait adaptability. Here, we investigate whether trait adaptability also affects the robustness of population dynamics of interacting species and thereby shapes the reliability of ecosystem functions that are driven by these dynamics. We model co‐adaptation in a predator–prey system as changes to predator offense and prey defense due to evolution or phenotypic plasticity. We investigate how trait adaptation affects the robustness of population dynamics against press perturbations to environmental parameters and against pulse perturbations targeting species abundances and their trait values. Robustness of population dynamics is characterized by resilience, elasticity, and resistance. In addition to employing established measures for resilience and elasticity against pulse perturbations (extinction probability and return time), we propose the warping distance as a new measure for resistance against press perturbations, which compares the shapes and amplitudes of pre‐ and post‐perturbation population dynamics. As expected, we find that the robustness of population dynamics depends on the speed of adaptation, but in nontrivial ways. Elasticity increases with speed of adaptation as the system returns more rapidly to the pre‐perturbation state. Resilience, in turn, is enhanced by intermediate speeds of adaptation, as here trait adaptation dampens biomass oscillations. The resistance of population dynamics strongly depends on the target of the press perturbation, preventing a simple relationship with the adaptation speed. In general, we find that low robustness often coincides with high amplitudes of population dynamics. Hence, amplitudes may indicate the robustness against perturbations also in other natural systems with similar dynamics. Our findings show that besides counteracting extinctions, trait adaptation indeed strongly affects the robustness of population dynamics against press and pulse perturbations. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 809 KW - disturbance KW - evolutionary rescue KW - population dynamics KW - stability KW - trait adaptation Y1 - 2020 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-442489 SN - 1866-8372 IS - 809 ER - TY - GEN A1 - Schönemann, Eric A1 - Laschewsky, André A1 - Rosenhahn, Axel T1 - Exploring the long-term hydrolytic behavior of zwitterionic polymethacrylates and polymethacrylamides T2 - Postprints der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe N2 - The hydrolytic stability of polymers to be used for coatings in aqueous environments, for example, to confer anti-fouling properties, is crucial. However, long-term exposure studies on such polymers are virtually missing. In this context, we synthesized a set of nine polymers that are typically used for low-fouling coatings, comprising the well-established poly(oligoethylene glycol methylether methacrylate), poly(3-(N-2-methacryloylethyl-N,N-dimethyl) ammoniopropanesulfonate) (“sulfobetaine methacrylate”), and poly(3-(N-3-methacryamidopropyl-N,N-dimethyl)ammoniopropanesulfonate) (“sulfobetaine methacrylamide”) as well as a series of hitherto rarely studied polysulfabetaines, which had been suggested to be particularly hydrolysis-stable. Hydrolysis resistance upon extended storage in aqueous solution is followed by ¹H NMR at ambient temperature in various pH regimes. Whereas the monomers suffered slow (in PBS) to very fast hydrolysis (in 1 M NaOH), the polymers, including the polymethacrylates, proved to be highly stable. No degradation of the carboxyl ester or amide was observed after one year in PBS, 1 M HCl, or in sodium carbonate buffer of pH 10. This demonstrates their basic suitability for anti-fouling applications. Poly(sulfobetaine methacrylamide) proved even to be stable for one year in 1 M NaOH without any signs of degradation. The stability is ascribed to a steric shielding effect. The hemisulfate group in the polysulfabetaines, however, was found to be partially labile. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 1091 KW - polyzwitterions KW - stability KW - polymer degradation KW - hydrolysis KW - polysulfobetaine KW - polysulfabetaine KW - anti-fouling materials Y1 - 2021 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-473052 SN - 1866-8372 IS - 1091 ER -