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Quasifree one-proton knockout reactions have been employed in inverse kinematics for a systematic study of the structure of stable and exotic oxygen isotopes at the R3B/LAND setup with incident beam energies in the range of 300–450 MeV/u. The oxygen isotopic chain offers a large variation of separation energies that allows for a quantitative understanding of single-particle strength with changing isospin asymmetry. Quasifree knockout reactions provide a complementary approach to intermediate-energy one-nucleon removal reactions. Inclusive cross sections for quasifree knockout reactions of the type AO(p,2p)A−1N have been determined and compared to calculations based on the eikonal reaction theory. The reduction factors for the single-particle strength with respect to the independent-particle model were obtained and compared to state-of-the-art ab initio predictions. The results do not show any significant dependence on proton-neutron asymmetry.
The radiative electron capture (REC) into the K shell of bare Xe ions colliding with a hydrogen gas target has been investigated. In this study, the degree of linear polarization of the K-REC radiation was measured and compared with rigorous relativistic calculations as well as with the previous results recorded for U92+. Owing to the improved detector technology, a significant gain in precision of the present polarization measurement is achieved compared to the previously published results. The obtained data confirms that for medium-Z ions such as Xe, the REC process is a source of highly polarized x rays which can easily be tuned with respect to the degree of linear polarization and the photon energy. We argue, in particular, that for relatively low energies the photons emitted under large angles are almost fully linear polarized.
The proton-removal mechanism of the 12CB reaction induced on a carbon target via elementary nucleon-nucleon scattering is investigated in exclusive triple-coincidence measurements. The observed two-nucleon angular correlations are found to be consistent with quasi-free scattering of a projectile-like proton off a target-like nucleon. Exclusive cross sections for one-step pp and pn interactions are determined as [formula] and [formula], respectively. The extracted quasi-free component amounts up to 58(4)% of the total proton-removal cross section. The results are compared to total proton-removal cross sections obtained from the experiment and eikonal reaction theory.
Until quite recently, stem cell technology mainly focused on pure populations of embryonic stem cells (ES) derived from the inner cell mass of the blastocyst and induced pluripotent stem cells (iPS). Using organoids, a newly established culture technique, it is now possible to culture also organ and patient-specific adult stem (AS) and induced pluripotent stem (IPS) cells in vitro. Furthermore, it has been shown that adult stem cells, grown as organoids, are genetically stable, proliferate and maintain their multi-potency (often a bi-potency) for months. This is possible by providing conditions that recapitulate the stem cell niche of the corresponding organ. Particularly, defined growth factors and a physiological scaffold, which is provided by an extracellular matrix (ECM). Because of increasing research activities, organoids became influential in the recent years. Wide-ranging interest also led to a clearer definition: organoids must contain multiple organ-specific cell types, must be able to recapitulate some organ specific functions, and the cells must be spatially organized in a way similar to the organ they are derived from. The excitement about organoids is based on their high potential as a model to understand wound healing, cellular behaviour and differentiation processes in organogenesis. Furthermore, high potential in the drug development and in personalized stem cell therapeutic approaches has been shown. Specifically, for personalized stem cell therapy, one potential application is for chronic autoimmune diseases such as Diabetes type 1 (T1D). T1D is characterized by the immune-mediated destruction of ß-cells in the Pancreas that leads to absolute insulin deficiency. In T1D the first-line therapeutic approach is exogenous insulin replacement therapy, which always implicates the risk of high fluctuations in blood-sugar levels and therefore the risk of hypoglycaemia. Another therapeutic approach is the xenotransplantation of islets from human donors. A successful islet transplantation allows patients a years-long insulin independence. However, the therapeutic value of islet transplantation is highly limited by the availability of organ donors and by the need for chronic administration of immune suppressive medication. The use of pancreas organoids offers a promising alternative as a personalized cell therapeutic approach to treat T1D without the hypoglycaemia risks of the established therapies. In 2013 Meritxell Huch and colleagues established for the first-time organoids from the exocrine, ductal part of the pancreas. These pancreas organoids are characterized by a monolayered, spherical cell epithelium which comprises a liquid filled lumen. In addition, they showed that after transplantation of these cells into immunodeficient mice, they differentiate into ß-cells and cure T1D. However, basic knowledge of the culture growth behaviour is still lacking: to date, no growth parameters are defined and reliable and robust investigation approaches are still missing. Furthermore, basic knowledge about the organoid development and biochemical/biophysical mechanisms that generate the phenotypic structure are not identified. For a clinical approach these parameters are fundamental and therefore must be defined pre-clinically.
The aim of this study is the preclinical characterization of the hPOs...
Four new species of the braconid wasp genus Hecabolus Curtis, 1834 (Doryctinae Foerster, 1863) are described for the Neotropical region in south and southwestern Brazil: H. acutus sp. nov., H. chrisaxeli sp. nov., H. gavinbroadi sp. nov., and H. transversalis sp. nov. We also report the morphological variation of females and males of H. mexicanus Zaldívar-Riverón & Belokobylskij, 2009, originally described based on a single female, and provide its first precise geographical distribution records. An updated key to the 13 described species of Hecabolus is provided.
Anisotropic collective flow of protons resulting from non-central heavy ion collisions is a unique hadronic observable providing information about the early stage of the nuclear collision. The analysis of collective flow in the energy regime between 1-2 AGeV enables the study of the phase diagram of hadronic matter at a high baryochemical potential µb, as well as the analysis of the equation of state at densities up to the threefold of the ground state density ρ0.
The algorithms of the standard event plane method and the scalar product method are used to analyse directed and elliptic flow of protons in a centrality range of 0-40 % most central events.
Prior to the analysis of experimental data, the respective influence of the reconstruction procedure on the algorithms is examined using Monte Carlo simulations based on the Ultra relativistic Quantum Molecular Dynamics (UrQMD) model.
Subsequently, experimental data measured in April 2012 with the High Acceptance DiElectron Spectrometer (HADES) is analysed using both methods. About 7.3 · 109 Au+Au events at a kinetic beam energy of 1.23 AGeV, equivalent to a centre of mass energy of √sNN = 2.42 GeV were recorded. A multi-differential analysis is feasible as the HADES detector provides a good transverse momentum and rapidity coverage.
Both algorithms result in identical values for directed and elliptic flow across all centrality classes within the observable phase space of protons. The calculated integrated value of v2 at mid rapidity is in good agreement with world data.
In April and May 2012 data on Au+Au collisions at beam energies of Ekin = 1.23A GeV were collected with the High Acceptance Di-Electron Spectrometer (HADES) at the GSI Helmholtzzentrum für Schwerionenforschung facility in Darmstadt, Germany. In this thesis, the production of deuterons in this collision system is investigated.
A total number of 2.1 × 109 Au+Au events is selected, containing the most central 0-40% of events. After particle identification, based on a mass determination via time-of-flight and momentum and on a measurement of the energy loss, the transverse mass spectra of the deuteron candidates are extracted for various rapidities and subsequently corrected for acceptance and efficiency.
The inverse slope parameter of a Boltzmann fit applied to the transverse mass spectra at midrapidity, which is referred to as the effective temperature, is extracted. For a static thermal source, this parameter corresponds to the kinetic freeze-out temperature Tkin and is therefore expected to be smaller or equal to the chemical freeze-out temperature Tchem. The extracted effective temperature of Tef f = (190 ± 10) MeV however exceeds the chemical freeze-out temperature that was obtained by a statistical model fit to different particle yields. The effective temperatures of various particle species, obtained in previous analyses, suggest a systematic rise with increasing particle mass, which is confirmed by the deuteron results.
An explanation can be the influence of a collective expansion with a radial expansion velocity βr. By fitting a Siemens-Rasmussen function to the transverse mass spectra, the global temperature of T = (100 ± 8) MeV and radial expansion velocity βr = 0.37 ± 0.01 are obtained. This temperature is still very high and only takes into account the production of deuteron nuclei.
The simultaneous fit of a blast-wave function to the transverse mass spectra of deuterons and other particles, as obtained by previous analyses, considers a velocity profile for the radial expansion velocity and takes into account the production of various particle species. The resulting global temperature Tkin = (68 ± 1) MeV and average transverse expansion velocity hβri = 0.341 ± 0.003 are within the expected range for the collision energy.
The Siemens-Rasmussen fits are also used to extrapolate the transverse mass spectra into unmeasured regions, to integrate them and obtain a rapidity-dependent count rate. This count rate exhibits a thermal shape for central events and shows increasing spectator contributions for more peripheral events.
The invariant yield spectra of the deuterons are compared to those of protons, as obtained by a previous analysis, in the context of a nucleon coalescence model. The hereby extracted nucleon coalescence factor B2 = (4.6 ± 0.1) × 10−3 agrees with the expected result for the beam energy that was studied.
Carbon is an element that controls planetary habitability, and is fundamental for life on Earth. Its behaviour has important consequences for the global climate system, the origin and evolution of life on Earth. While the biosphere and atmosphere’s carbon cycle only accounts for less than 1% of the global carbon budget, hidden reservoirs of deep carbon in the Earth’s interior comprise the predominant storage of carbon on the planet. At the Earth’s surface, 60-70 % of carbon is hosted by carbonate minerals, which are then transported to the Earth’s interior, mainly in the form of sediments, by subduction of the oceanic lithosphere. Subducting plates are subjected to decarbonation, dehydration, and melting with CO2 release via supra-subduction volcanism. Nevertheless, part of the subducted carbonates’ may survive and be further transported to the deep mantle. Direct evidence of the existence of carbonates in the Earth’s interior, possibly reaching down to the lower mantle, comes from the finding of syngenetic inclusions of carbonates in diamonds and mantle xenoliths. The presence of carbonates in the deep Earth has a critical effect on the physical properties of the mantle. Melting and chemical speciation of the mantle are strongly affected by the form of C and carbonate stability. Therefore, the study of the stability and physical properties of carbonates at high pressures and temperatures is fundamental, because understanding the processes involved in the deep carbon cycle helps to improve our picture of the whole mantle.
The systematic characterization of the elastic properties of carbonates as a function of their structure and chemical composition is of great importance because it may allow to identify their presence and distribution by seismology. Inverting seismic observations to successfully constrain the chemical composition and mineralogy of the Earth’s interior requires knowledge of the physical properties of all possible Earth’s materials at pressures and temperatures applicable to the Earth’s interior. Up to now, a multitude of studies has focused on the construction of phase diagrams and structural transitions by means of X-ray diffraction and vibrational spectroscopy experiments.
Few studies are available on the complete elastic tensor of carbonates, however most of the datasets are not accompanied by an accurate characterization of the samples, which are often solid solutions and the exact chemical composition, density or the details about the experimental methods used are not presented. The aim of this thesis is to study the effect of chemical composition on the elastic properties of carbonates, providing a reliable dataset on the elasticity of the main carbonates. In particular, the elastic properties of crystalline aragonite, CaCO3, and Fe-dolomite, (Ca, Mg, Fe)(CO3)2, with different compositions were studied by Brillouin spectroscopy at ambient conditions. Brillouin spectroscopy was also used to investigate the elastic behaviour of amorphous calcium carbonate samples with different water contents (up to 18 wt%) at high pressures, up to 20 GPa.
Furthermore, the importance of cationic substitution on the structure and high pressure behaviour of carbonates was investigated by studying a synthetic CaCO3-SrCO3 solid solution at ambient conditions and at high pressures, up to 10 GPa, by single crystal X-ray diffraction. Finally, the study of the effect of composition on the elastic properties of families of isostructural solids was also extended to a different class of materials, the metal guanidinium formates. The elasticity of a family of perovskite metal organic frameworks, metal guanidinium formates C(NH2)3MII(HCOO)3, with MII =Mn, Zn, Cu, Co, Cd and Ca was investigated by combining Brillouin spectroscopy, resonant ultrasound spectroscopy, density functional theory and thermal diffuse scattering analysis.
Das Projekt anan ist ein Werkzeug zur Fehlersuche in verteilten Hochleistungsrechnern. Die Neuheit des Beitrags besteht darin, dass die bekannten Methoden, die bereits erfolgreich zum Debuggen von Soft- und Hardware eingesetzt werden, auf Hochleistungs-Rechnen übertragen worden sind. Im Rahmen der vorliegenden Arbeit wurde ein Werkzeug namens anan implementiert, das bei der Fehlersuche hilft. Außerdem kann es als dynamischeres Monitoring eingesetzt werden. Beide Einsatzzwecke sind
getestet worden.
Das Werkzeug besteht aus zwei Teilen:
1. aus einem Teil namens anan, der interaktiv vom Nutzer bedient wird
2. und aus einem Teil namens anand, der automatisiert die verlangten Messwerte erhebt und nötigenfalls Befehle ausführt.
Der Teil anan führt Sensoren aus — kleine mustergesteuerte Algorithmen —, deren Ergebnisse per anan zusammengeführt werden. In erster Näherung lässt anan sich als Monitoring beschreiben, welches (1) schnell umkonfiguriert werden (2) komplexere Werte messen kann, die über Korrelationen einfacher Zeitreihen hinausgehen.
The European Community has set a milestone in the European water policy in 2000: all water directives and policies were united into one comprehensive document – the European Water Framework Directive (EU WFD). The EU WFD requires the monitoring of 45 priority substances, primarily in the water phase, which is not related to a substantial amount of chemicals available on the market worldwide (about 50,000). About 60% of these are human and environmentally toxic. Hence, the currently monitored 45 priority substances are not even close to being sufficient to provide a comprehensive picture of the actual chemical pollution in the aquatic environment.
Furthermore, the EU WFD in its original shape paid less attention to sediments as an important source and sink for chemical contamination. Under stable hydrological conditions, polluted old sediments are covered by less polluted younger sediments preventing erosion of deeper sediment layers and, therefore, the release of particle-bound contaminants. However, urbanization, deforestation, flooding, dredging, riverbed renaturation, and stormwater overflow basin releases can lead to an unpredictable release of particle-bound pollutants. Therefore, in 2008, sediments were added to the EU WFD as a monitoring matrix for substances that tend to accumulate there. As a result, after 18 years of the EU WFD, less than half of all European waterbodies reached a good ecological (40%) and chemical (38%) status.
One of the primary pollution sources in aquatic ecosystems are wastewater treatment plants (WWTPs). Advanced wastewater treatment by ozonation is promising to remove most micropollutants. However, the knowledge about the possible improvement of the receiving waterbody is rare. The latter aspects were the main reasons for the start of the DemO3AC project in 2014. The study area was located in the federal state of North Rhine-Westphalia (Germany). The study area included the Wurm River and its tributary, the Haarbach River. Both waterbodies act as receiving waterbodies for WWTPs. One of them is the Aachen-Soers WWTP (receiving waterbody: Wurm River), upgraded by full stream ozonation as an advanced effluent treatment. Therefore, the extensive investigation program within the DemO3AC project included an investigation of the ecological and chemical status of both receiving waterbodies and the investigation of a possible improvement of the Wurm River after implementing advanced effluent treatment.
The current study was a part of the DemO3AC project and covered the sediment toxicity and a possible impact of the ozonation on aquatic organisms in the receiving waterbody. Time-resolved sampling campaigns allowed investigations under different hydrological conditions, mainly determined by the weather. The first sampling campaign took place in June 2017 during a prolonged dry period with low water flow in the receiving waterbodies. The second sampling campaign was performed exactly one year later (June 2018) after a long rainy period and corresponding high-water levels. Full-stream ozonation at the Aachen-Soers WWTP had been in operation for half a year. Furthermore, a wide range of organic micropollutants was investigated in the effluent of the studied WWTPs to assess a possible hazard emerging from contaminants released into the receiving waterbody.
The study design was developed based on the holistic approach to assessing the ecotoxicological pollution of surface waterbodies. It included the detection of chemical compounds combined with effect-based methods to identify possible drivers of toxicity. The sediment's ecotoxicological assessment included studies on endocrine-disrupting activity, genotoxic and embryotoxic potentials. These endpoints were evaluated using in vitro and in vivo bioassays. In addition, sediments’ chemical profiling was performed using modern analytical chemistry techniques.
The genotoxic potential was investigated using the Ames fluctuation assay with Salmonella typhimurium bacterial strains TA98, TA100, YG1041, and YG1042, sensitive to different classes of compounds, and the Micronucleus assay as a eukaryotic assay with mammalian cells. A unique feature of the present study was the implementation of non-standard Salmonella typhimurium bacterial strains YG1041 and YG1042 in the Ames fluctuation assay. Moreover, a comprehensive genotoxicity ranking of chemical compounds identified in sediments was used and combined with statistical analysis to identify the drivers of genotoxicity. The results of this study were published in Shuliakevich et al. (2022a) (see also Annex 1), describing the mutagenic potential of all sampling sites, which was primarily driven by polycyclic aromatic hydrocarbons, nitroarenes, aromatic amines, and polycyclic heteroarenes. In addition, the rainwater overflow basin was identified as a significant source for particle-bound pollutants from untreated wastewater, suggesting its role as a possible source of genotoxic potential. The present study showed high sensitivity and applicability of non-standard Salmonella typhimurium bacterial strains YG1041 and YG1042 in the Ames fluctuation assay to assess the different classes of mutagenic compounds. A combination of effect-based methods and a chemical analysis was shown as a suitable tool for a genotoxic assessment of freshwater sediments.
The sediments' endocrine-disruptive activity was investigated using the cell-based reporter gene CALUX® assay. A simultaneous launch of the full-scale effluent ozonation at the Aachen-Soers WWTP was used for investigation of the entrance of the ozonated effluent into the Wurm River and the endocrine-disrupting activity in the water phase. A particular focus of the present study was the unique investigation of PAHs as possible drivers of the endocrine-disrupting activity in sediments of the Wurm River. The results of this study were laid down in the publication by Shuliakevich et al. (2022b) (see also Annex 2), describing variations in endocrine-disrupting activity in the Wurm River under different weather conditions. Briefly, under stable hydrological conditions in June 2017, the estrogenic and the antiandrogenic activities in sediments of the Wurm River were within the range of 0.03-0.1 ng E2 equivalents (eq.)/g dry weight sediment equivalents (dw SEQ) and 3.0-13.9 µg Flu eq./g dw SEQ, respectively. After extensive rain events in June 2018, the sediments' estrogenic and antiandrogenic activities were detected within the range of 0.06-0.2 ng E2 eq./g dw SEQ and 1.7-39.2 µg Flu eq./g de SEQ, respectively. Increased endocrine-disruptive activity (up to 0.2 ng E2 eq./g dw SEQ in ERα- and 39.2 µg Flu eq./g dw SEQ in anti-AR-CALUX® assays) in sediments downstream of the rainwater overflow basin suggested it as a possible source of pollution. A unique result of the second study was finding a positive correlation between measured particle-bound antiandrogenic activity and detected polyaromatic hydrocarbons (PAHs) ...