@phdthesis{Spooner2021,
  author    = {Spooner, Cameron},
  title     = {How does lithospheric configuration relate to deformation in the Alpine region?},
  doi       = {10.25932/publishup-51644},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-516442},
  school      = {Universit{\"a}t Potsdam},
  pages     = {xiv, 138},
  year      = {2021},
  abstract  = {Forming as a result of the collision between the Adriatic and European plates, the Alpine orogen exhibits significant lithospheric heterogeneity due to the long history of interplay between these plates, other continental and oceanic blocks in the region, and inherited features from preceeding orogenies. This implies that the thermal and rheological configuration of the lithosphere also varies significantly throughout the region. Lithology and temperature/pressure conditions exert a first order control on rock strength, principally via thermally activated creep deformation and on the distribution at depth of the brittle-ductile transition zone, which can be regarded as the lower bound to the seismogenic zone. Therefore, they influence the spatial distribution of seismicity within a lithospheric plate. In light of this, accurately constrained geophysical models of the heterogeneous Alpine lithospheric configuration, are crucial in describing regional deformation patterns. However, despite the amount of research focussing on the area, different hypotheses still exist regarding the present-day lithospheric state and how it might relate to the present-day seismicity distribution. This dissertaion seeks to constrain the Alpine lithospheric configuration through a fully 3D integrated modelling workflow, that utilises multiple geophysical techniques and integrates from all available data sources. The aim is therefore to shed light on how lithospheric heterogeneity may play a role in influencing the heterogeneous patterns of seismicity distribution observed within the region. This was accomplished through the generation of: (i) 3D seismically constrained, structural and density models of the lithosphere, that were adjusted to match the observed gravity field; (ii) 3D models of the lithospheric steady state thermal field, that were adjusted to match observed wellbore temperatures; and (iii) 3D rheological models of long term lithospheric strength, with the results of each step used as input for the following steps. Results indicate that the highest strength within the crust (~ 1 GPa) and upper mantle (> 2 GPa), are shown to occur at temperatures characteristic for specific phase transitions (more felsic crust: 200 - 400 °C; more mafic crust and upper lithospheric mantle: ~600 °C) with almost all seismicity occurring in these regions. However, inherited lithospheric heterogeneity was found to significantly influence this, with seismicity in the thinner and more mafic Adriatic crust (~22.5 km, 2800 kg m-3, 1.30E-06 W m-3) occuring to higher temperatures (~600 °C) than in the thicker and more felsic European crust (~27.5 km, 2750 kg m-3, 1.3-2.6E-06 W m-3, ~450 °C). Correlation between seismicity in the orogen forelands and lithospheric strength, also show different trends, reflecting their different tectonic settings. As such, events in the plate boundary setting of the southern foreland correlate with the integrated lithospheric strength, occurring mainly in the weaker lithosphere surrounding the strong Adriatic indenter. Events in the intraplate setting of the northern foreland, instead correlate with crustal strength, mainly occurring in the weaker and warmer crust beneath the Upper Rhine Graben. Therefore, not only do the findings presented in this work represent a state of the art understanding of the lithospheric configuration beneath the Alps and their forelands, but also a significant improvement on the features known to significantly influence the occurrence of seismicity within the region. This highlights the importance of considering lithospheric state in regards to explaining observed patterns of deformation.},
  language  = {en}
}
@phdthesis{Ibarra2021,
  author    = {Ibarra, Federico},
  title     = {The thermal and rheological state of the Central Andes and its relationship to active deformation processes},
  doi       = {10.25932/publishup-50622},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-506226},
  school      = {Universit{\"a}t Potsdam},
  pages     = {xvi, 149},
  year      = {2021},
  abstract  = {The Central Andes region in South America is characterized by a complex and heterogeneous deformation system. Recorded seismic activity and mapped neotectonic structures indicate that most of the intraplate deformation is located along the margins of the orogen, in the transitions to the foreland and the forearc. Furthermore, the actively deforming provinces of the foreland exhibit distinct deformation styles that vary along strike, as well as characteristic distributions of seismicity with depth. The style of deformation transitions from thin-skinned in the north to thick-skinned in the south, and the thickness of the seismogenic layer increases to the south. Based on geological/geophysical observations and numerical modelling, the most commonly invoked causes for the observed heterogeneity are the variations in sediment thickness and composition, the presence of inherited structures, and changes in the dip of the subducting Nazca plate. However, there are still no comprehensive investigations on the relationship between the lithospheric composition of the Central Andes, its rheological state and the observed deformation processes. The central aim of this dissertation is therefore to explore the link between the nature of the lithosphere in the region and the location of active deformation. The study of the lithospheric composition by means of independent-data integration establishes a strong base to assess the thermal and rheological state of the Central Andes and its adjacent lowlands, which alternatively provide new foundations to understand the complex deformation of the region. In this line, the general workflow of the dissertation consists in the construction of a 3D data-derived and gravity-constrained density model of the Central Andean lithosphere, followed by the simulation of the steady-state conductive thermal field and the calculation of strength distribution. Additionally, the dynamic response of the orogen-foreland system to intraplate compression is evaluated by means of 3D geodynamic modelling. The results of the modelling approach suggest that the inherited heterogeneous composition of the lithosphere controls the present-day thermal and rheological state of the Central Andes, which in turn influence the location and depth of active deformation processes. Most of the seismic activity and neo--tectonic structures are spatially correlated to regions of modelled high strength gradients, in the transition from the felsic, hot and weak orogenic lithosphere to the more mafic, cooler and stronger lithosphere beneath the forearc and the foreland. Moreover, the results of the dynamic simulation show a strong localization of deviatoric strain rate second invariants in the same region suggesting that shortening is accommodated at the transition zones between weak and strong domains. The vertical distribution of seismic activity appears to be influenced by the rheological state of the lithosphere as well. The depth at which the frequency distribution of hypocenters starts to decrease in the different morphotectonic units correlates with the position of the modelled brittle-ductile transitions; accordingly, a fraction of the seismic activity is located within the ductile part of the crust. An exhaustive analysis shows that practically all the seismicity in the region is restricted above the 600°C isotherm, in coincidence with the upper temperature limit for brittle behavior of olivine. Therefore, the occurrence of earthquakes below the modelled brittle-ductile could be explained by the presence of strong residual mafic rocks from past tectonic events. Another potential cause of deep earthquakes is the existence of inherited shear zones in which brittle behavior is favored through a decrease in the friction coefficient. This hypothesis is particularly suitable for the broken foreland provinces of the Santa Barbara System and the Pampean Ranges, where geological studies indicate successive reactivation of structures through time. Particularly in the Santa Barbara System, the results indicate that both mafic rocks and a reduction in friction are required to account for the observed deep seismic events.},
  language  = {en}
}
@phdthesis{Tunn2020,
  author    = {Tunn, Isabell},
  title     = {From single molecules to bulk materials: tuning the viscoelastic properties of coiled coil cross-linked hydrogels},
  doi       = {10.25932/publishup-47595},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-475955},
  school      = {Universit{\"a}t Potsdam},
  pages     = {XVI, 140},
  year      = {2020},
  abstract  = {The development of bioinspired self-assembling materials, such as hydrogels, with promising applications in cell culture, tissue engineering and drug delivery is a current focus in material science. Biogenic or bioinspired proteins and peptides are frequently used as versatile building blocks for extracellular matrix (ECM) mimicking hydrogels. However, precisely controlling and reversibly tuning the properties of these building blocks and the resulting hydrogels remains challenging. Precise control over the viscoelastic properties and self-healing abilities of hydrogels are key factors for developing intelligent materials to investigate cell matrix interactions. Thus, there is a need to develop building blocks that are self-healing, tunable and self-reporting. This thesis aims at the development of α-helical peptide building blocks, called coiled coils (CCs), which integrate these desired properties. Self-healing is a direct result of the fast self-assembly of these building blocks when used as material cross-links. Tunability is realized by means of reversible histidine (His)-metal coordination bonds. Lastly, implementing a fluorescent readout, which indicates the CC assembly state, self-reporting hydrogels are obtained. Coiled coils are abundant protein folding motifs in Nature, which often have mechanical function, such as in myosin or fibrin. Coiled coils are superhelices made up of two or more α-helices wound around each other. The assembly of CCs is based on their repetitive sequence of seven amino acids, so-called heptads (abcdefg). Hydrophobic amino acids in the a and d position of each heptad form the core of the CC, while charged amino acids in the e and g position form ionic interactions. The solvent-exposed positions b, c and f are excellent targets for modifications since they are more variable. His-metal coordination bonds are strong, yet reversible interactions formed between the amino acid histidine and transition metal ions (e.g. Ni2+, Cu2+ or Zn2+). His-metal coordination bonds essentially contribute to the mechanical stability of various high-performance proteinaceous materials, such as spider fangs, Nereis worm jaws and mussel byssal threads. Therefore, I bioengineered reversible His-metal coordination sites into a well-characterized heterodimeric CC that served as tunable material cross-link. Specifically, I took two distinct approaches facilitating either intramolecular (Chapter 4.2) and/or intermolecular (Chapter 4.3) His-metal coordination. Previous research suggested that force-induced CC unfolding in shear geometry starts from the points of force application. In order to tune the stability of a heterodimeric CC in shear geometry, I inserted His in the b and f position at the termini of force application (Chapter 4.2). The spacing of His is such that intra-CC His-metal coordination bonds can form to bridge one helical turn within the same helix, but also inter-CC coordination bonds are not generally excluded. Starting with Ni2+ ions, Raman spectroscopy showed that the CC maintained its helical structure and the His residues were able to coordinate Ni2+. Circular dichroism (CD) spectroscopy revealed that the melting temperature of the CC increased by 4 °C in the presence of Ni2+. Using atomic force microscope (AFM)-based single molecule force spectroscopy, the energy landscape parameters of the CC were characterized in the absence and the presence of Ni2+. His-Ni2+ coordination increased the rupture force by ~10 pN, accompanied by a decrease of the dissociation rate constant. To test if this stabilizing effect can be transferred from the single molecule level to the bulk viscoelastic material properties, the CC building block was used as a non-covalent cross-link for star-shaped poly(ethylene glycol) (star-PEG) hydrogels. Shear rheology revealed a 3-fold higher relaxation time in His-Ni2+ coordinating hydrogels compared to the hydrogel without metal ions. This stabilizing effect was fully reversible when using an excess of the metal chelator ethylenediaminetetraacetate (EDTA). The hydrogel properties were further investigated using different metal ions, i.e. Cu2+, Co2+ and Zn2+. Overall, these results suggest that Ni2+, Cu2+ and Co2+ primarily form intra-CC coordination bonds while Zn2+ also participates in inter-CC coordination bonds. This may be a direct result of its different coordination geometry. Intermolecular His-metal coordination bonds in the terminal regions of the protein building blocks of mussel byssal threads are primarily formed by Zn2+ and were found to be intimately linked to higher-order assembly and self-healing of the thread. In the above example, the contribution of intra-CC and inter-CC His-Zn2+ cannot be disentangled. In Chapter 4.3, I redesigned the CC to prohibit the formation of intra-CC His-Zn2+ coordination bonds, focusing only on inter-CC interactions. Specifically, I inserted His in the solvent-exposed f positions of the CC to focus on the effect of metal-induced higher-order assembly of CC cross-links. Raman and CD spectroscopy revealed that this CC building block forms α-helical Zn2+ cross-linked aggregates. Using this CC as a cross-link for star-PEG hydrogels, I showed that the material properties can be switched from viscoelastic in the absence of Zn2+ to elastic-like in the presence of Zn2+. Moreover, the relaxation time of the hydrogel was tunable over three orders of magnitude when using different Zn2+:His ratios. This tunability is attributed to a progressive transformation of single CC cross-links into His-Zn2+ cross-linked aggregates, with inter-CC His-Zn2+ coordination bonds serving as an additional, cross-linking mode. Rheological characterization of the hydrogels with inter-CC His-Zn2+ coordination raised the question whether the His-Zn2+ coordination bonds between CCs or also the CCs themselves rupture when shear strain is applied. In general, the amount of CC cross-links initially formed in the hydrogel as well as the amount of CC cross-links breaking under force remains to be elucidated. In order to more deeply probe these questions and monitor the state of the CC cross-links when force is applied, a fluorescent reporter system based on F{\"o}rster resonance energy transfer (FRET) was introduced into the CC (Chapter 4.4). For this purpose, the donor-acceptor pair carboxyfluorescein and tetramethylrhodamine was used. The resulting self-reporting CC showed a FRET efficiency of 77 \% in solution. Using this fluorescently labeled CC as a self-reporting, reversible cross-link in an otherwise covalently cross-linked star-PEG hydrogel enabled the detection of the FRET efficiency change under compression force. This proof-of-principle result sets the stage for implementing the fluorescently labeled CCs as molecular force sensors in non-covalently cross-linked hydrogels. In summary, this thesis highlights that rationally designed CCs are excellent reversibly tunable, self-healing and self-reporting hydrogel cross-links with high application potential in bioengineering and biomedicine. For the first time, I demonstrated that His-metal coordination-based stabilization can be transferred from the single CC level to the bulk material with clear viscoelastic consequences. Insertion of His in specific sequence positions was used to implement a second non-covalent cross-linking mode via intermolecular His-metal coordination. This His-metal binding induced aggregation of the CCs enabled for reversibly tuning the hydrogel properties from viscoelastic to elastic-like. As a proof-of-principle to establish self-reporting CCs as material cross-links, I labeled a CC with a FRET pair. The fluorescently labelled CC acts as a molecular force sensor and first preliminary results suggest that the CC enables the detection of hydrogel cross-link failure under compression force. In the future, fluorescently labeled CC force sensors will likely not only be used as intelligent cross-links to study the failure of hydrogels but also to investigate cell-matrix interactions in 3D down to the single molecule level.},
  language  = {en}
}
@phdthesis{Meessen2019,
  author    = {Meeßen, Christian},
  title     = {The thermal and rheological state of the Northern Argentinian foreland basins},
  doi       = {10.25932/publishup-43994},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-439945},
  school      = {Universit{\"a}t Potsdam},
  pages     = {xviii, 151},
  year      = {2019},
  abstract  = {The foreland of the Andes in South America is characterised by distinct along strike changes in surface deformational styles. These styles are classified into two end-members, the thin-skinned and the thick-skinned style. The superficial expression of thin-skinned deformation is a succession of narrowly spaced hills and valleys, that form laterally continuous ranges on the foreland facing side of the orogen. Each of the hills is defined by a reverse fault that roots in a basal d{\´e}collement surface within the sedimentary cover, and acted as thrusting ramp to stack the sedimentary pile. Thick-skinned deformation is morphologically characterised by spatially disparate, basement-cored mountain ranges. These mountain ranges are uplifted along reactivated high-angle crustal-scale discontinuities, such as suture zones between different tectonic terranes. Amongst proposed causes for the observed variation are variations in the dip angle of the Nazca plate, variation in sediment thickness, lithospheric thickening, volcanism or compositional differences. The proposed mechanisms are predominantly based on geological observations or numerical thermomechanical modelling, but there has been no attempt to understand the mechanisms from a point of data-integrative 3D modelling. The aim of this dissertation is therefore to understand how lithospheric structure controls the deformational behaviour. The integration of independent data into a consistent model of the lithosphere allows to obtain additional evidence that helps to understand the causes for the different deformational styles. Northern Argentina encompasses the transition from the thin-skinned fold-and-thrust belt in Bolivia, to the thick-skinned Sierras Pampeanas province, which makes this area a well suited location for such a study. The general workflow followed in this study first involves data-constrained structural- and density-modelling in order to obtain a model of the study area. This model was then used to predict the steady-state thermal field, which was then used to assess the present-day rheological state in northern Argentina. The structural configuration of the lithosphere in northern Argentina was determined by means of data-integrative, 3D density modelling verified by Bouguer gravity. The model delineates the first-order density contrasts in the lithosphere in the uppermost 200 km, and discriminates bodies for the sediments, the crystalline crust, the lithospheric mantle and the subducting Nazca plate. To obtain the intra-crustal density structure, an automated inversion approach was developed and applied to a starting structural model that assumed a homogeneously dense crust. The resulting final structural model indicates that the crustal structure can be represented by an upper crust with a density of 2800 kg/m³, and a lower crust of 3100 kg/m³. The Transbrazilian Lineament, which separates the Pampia terrane from the R{\´i}o de la Plata craton, is expressed as a zone of low average crustal densities. In an excursion, we demonstrate in another study, that the gravity inversion method developed to obtain intra-crustal density structures, is also applicable to obtain density variations in the uppermost lithospheric mantle. Densities in such sub-crustal depths are difficult to constrain from seismic tomographic models due to smearing of crustal velocities. With the application to the uppermost lithospheric mantle in the north Atlantic, we demonstrate in Tan et al. (2018) that lateral density trends of at least 125\,km width are robustly recovered by the inversion method, thereby providing an important tool for the delineation of subcrustal density trends. Due to the genetic link between subduction, orogenesis and retroarc foreland basins the question rises whether the steady-state assumption is valid in such a dynamic setting. To answer this question, I analysed (i) the impact of subduction on the conductive thermal field of the overlying continental plate, (ii) the differences between the transient and steady-state thermal fields of a geodynamic coupled model. Both studies indicate that the assumption of a thermal steady-state is applicable in most parts of the study area. Within the orogenic wedge, where the assumption cannot be applied, I estimated the transient thermal field based on the results of the conducted analyses. Accordingly, the structural model that had been obtained in the first step, could be used to obtain a 3D conductive steady-state thermal field. The rheological assessment based on this thermal field indicates that the lithosphere of the thin-skinned Subandean ranges is characterised by a relatively strong crust and a weak mantle. Contrarily, the adjacent foreland basin consists of a fully coupled, very strong lithosphere. Thus, shortening in northern Argentina can only be accommodated within the weak lithosphere of the orogen and the Subandean ranges. The analysis suggests that the d{\´e}collements of the fold-and-thrust belt are the shallow continuation of shear zones that reside in the ductile sections of the orogenic crust. Furthermore, the localisation of the faults that provide strain transfer between the deeper ductile crust and the shallower d{\´e}collement is strongly influenced by crustal weak zones such as foliation. In contrast to the northern foreland, the lithosphere of the thick-skinned Sierras Pampeanas is fully coupled and characterised by a strong crust and mantle. The high overall strength prevents the generation of crustal-scale faults by tectonic stresses. Even inherited crustal-scale discontinuities, such as sutures, cannot sufficiently reduce the strength of the lithosphere in order to be reactivated. Therefore, magmatism that had been identified to be a precursor of basement uplift in the Sierras Pampeanas, is the key factor that leads to the broken foreland of this province. Due to thermal weakening, and potentially lubrication of the inherited discontinuities, the lithosphere is locally weakened such that tectonic stresses can uplift the basement blocks. This hypothesis explains both the spatially disparate character of the broken foreland, as well as the observed temporal delay between volcanism and basement block uplift. This dissertation provides for the first time a data-driven 3D model that is consistent with geophysical data and geological observations, and that is able to causally link the thermo-rheological structure of the lithosphere to the observed variation of surface deformation styles in the retroarc foreland of northern Argentina.},
  language  = {en}
}
@phdthesis{Kristen2011,
  author    = {Kristen, Juliane Ute},
  title     = {Amphiphilic BAB-triblock copolymers bearing fluorocarbon groups : synthesis and self-organization in aqueous media},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-61782},
  school      = {Universit{\"a}t Potsdam},
  year      = {2011},
  abstract  = {In this work new fluorinated and non-fluorinated mono- and bifunctional trithiocarbonates of the structure Z-C(=S)-S-R and Z-C(=S)-S-R-S-C(=S)-Z were synthesized for the use as chain transfer agents (CTAs) in the RAFT-process. All newly synthesized CTAs were tested for their efficiency to moderate the free radical polymerization process by polymerizing styrene (M3). Besides characterization of the homopolymers by GPC measurements, end- group analysis of the synthesized block copolymers via 1H-, 19F-NMR, and in some cases also UV-vis spectroscopy, were performed attaching suitable fluorinated moieties to the Z- and/or R-groups of the CTAs. Symmetric triblock copolymers of type BAB and non-symmetric fluorine end- capped polymers were accessible using the RAFT process in just two or one polymerization step. In particular, the RAFT-process enabled the controlled polymerization of hydrophilic monomers such as N-isopropylacrylamide (NIPAM) (M1) as well as N-acryloylpyrrolidine (NAP) (M2) for the A-blocks and of the hydrophobic monomers styrene (M3), 2-fluorostyrene (M4), 3-fluorostyrene (M5), 4-fluorostyrene (M6) and 2,3,4,5,6-pentafluorostyrene (M7) for the B-blocks. The properties of the BAB-triblock copolymers were investigated in dilute, concentrated and highly concentrated aqueous solutions using DLS, turbidimetry, 1H- and 19F-NMR, rheology, determination of the CMC, foam height- and surface tension measurements and microscopy. Furthermore, their ability to stabilize emulsions and microemulsions and the wetting behaviour of their aqueous solutions on different substrates was investigated. The behaviour of the fluorine end-functionalized polymers to form micelles was studied applying DLS measurements in diluted organic solution. All investigated BAB-triblock copolymers were able to form micelles and show surface activity at room temperature in dilute aqueous solution. The aqueous solutions displayed moderate foam formation. With different types and concentrations of oils, the formation of emulsions could be detected using a light microscope. A boosting effect in microemulsions could not be found adding BAB-triblock copolymers. At elevated polymer concentrations, the formation of hydrogels was proved applying rheology measurements.},
  language  = {en}
}
@phdthesis{Hoechner2010,
  author    = {H{\"o}chner, Andreas},
  title     = {GPS based analysis of earthquake induced phenomena at the Sunda Arc},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-53166},
  school      = {Universit{\"a}t Potsdam},
  year      = {2010},
  abstract  = {Indonesia is one of the countries most prone to natural hazards. Complex interaction of several tectonic plates with high relative velocities leads to approximately two earthquakes with magnitude Mw>7 every year, being more than 15\% of the events worldwide. Earthquakes with magnitude above 9 happen far more infrequently, but with catastrophic effects. The most severe consequences thereby arise from tsunamis triggered by these subduction-related earthquakes, as the Sumatra-Andaman event in 2004 showed. In order to enable efficient tsunami early warning, which includes the estimation of wave heights and arrival times, it is necessary to combine different types of real-time sensor data with numerical models of earthquake sources and tsunami propagation. This thesis was created as a result of the GITEWS project (German Indonesian Tsunami Early Warning System). It is based on five research papers and manuscripts. Main project-related task was the development of a database containing realistic earthquake scenarios for the Sunda Arc. This database provides initial conditions for tsunami propagation modeling used by the simulation system at the early warning center. An accurate discretization of the subduction geometry, consisting of 25x150 subfaults was constructed based on seismic data. Green's functions, representing the deformational response to unit dip- and strike slip at the subfaults, were computed using a layered half-space approach. Different scaling relations for earthquake dimensions and slip distribution were implemented. Another project-related task was the further development of the 'GPS-shield' concept. It consists of a constellation of near field GPS-receivers, which are shown to be very valuable for tsunami early warning. The major part of this thesis is related to the geophysical interpretation of GPS data. Coseismic surface displacements caused by the 2004 Sumatra earthquake are inverted for slip at the fault. The effect of different Earth layer models is tested, favoring continental structure. The possibility of splay faulting is considered and shown to be a secondary order effect in respect to tsunamigenity for this event. Tsunami models based on source inversions are compared to satellite radar altimetry observations. Postseismic GPS time series are used to test a wide parameter range of uni- and biviscous rheological models of the asthenosphere. Steady-state Maxwell rheology is shown to be incompatible with near-field GPS data, unless large afterslip, amounting to more than 10\% of the coseismic moment is assumed. In contrast, transient Burgers rheology is in agreement with data without the need for large aseismic afterslip. Comparison to postseismic geoid observation by the GRACE satellites reveals that even with afterslip, the model implementing Maxwell rheology results in amplitudes being too small, and thus supports a biviscous asthenosphere. A simple approach based on the assumption of quasi-static deformation propagation is introduced and proposed for inversion of coseismic near-field GPS time series. Application of this approach to observations from the 2004 Sumatra event fails to quantitatively reconstruct the rupture propagation, since a priori conditions are not fulfilled in this case. However, synthetic tests reveal the feasibility of such an approach for fast estimation of rupturing properties.},
  language  = {en}
}
@phdthesis{Drzikova2005,
  author    = {Drzikova, Barbora},
  title     = {Haferprodukte mit modifiziertem Gehalt an β-Glucanen und resistenter St{\"a}rke und ihre Effekte auf den Gastrointestinaltrakt unter In-vitro- und In-vivo-Bedingungen},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-5926},
  school      = {Universit{\"a}t Potsdam},
  year      = {2005},
  abstract  = {In einer Zeit, in der eine Zunahme von ern{\"a}hrungsbedingten Erkrankungen in steigendem Maße zu beobachten ist, wird dem Getreide als Grundlage der menschlichen Ern{\"a}hrung erh{\"o}hte Aufmerksamkeit gewidmet. Ein hoher Verzehr von Ballaststoffen ist ein wesentlicher Aspekt in der pr{\"a}ventiv-medizinischen Ern{\"a}hrung. Die von der Deutschen Gesellschaft f{\"u}r Ern{\"a}hrung vorgeschlagene t{\"a}gliche Ballaststoffzufuhr liegt bei 30 g. Die Aufnahme von Ballaststoffen ist jedoch in Deutschland deutlich unterhalb dieser empfohlenen Menge. Getreideprodukte, besonders vom Vollkorntyp, sind die wichtigste Quelle f{\"u}r Ballaststoffe. Deshalb sollten im Rahmen dieser Arbeit direkt verzehrsf{\"a}hige, Ballaststoff-angereicherte Haferprodukte (vorwiegend Extrudate) mit hohen Gehalten an b-Glucanen und resistenter St{\"a}rke hergestellt, analysiert und nachfolgend auf relevante ern{\"a}hrungsphysiologische Wirkungen gepr{\"u}ft werden. Als Basis f{\"u}r die Produkte wurden Hafermehl und Haferkleie eingesetzt. Der erste Teil der Arbeit besch{\"a}ftigte sich mit der Analyse der Haferprodukte. Diese wiesen eine hohe Wasserbindungskapazit{\"a}t auf. Bei den Untersuchungen am Tiermodell wurde gezeigt, dass im D{\"u}nndarm eine gr{\"o}ßere Menge an Wasser durch die Haferprodukte gebunden wurde, was zu einem h{\"o}heren Feuchtigkeitsanteil der gastrointestinalen Inhalte der Tiere f{\"u}hrte, die ballaststoffreiches Futter erhielten. Trotz der hydrothermischen Behandlung w{\"a}hrend der Extrusion wurden Produkte gewonnen, deren β-Glucane im hochmolekularen Zustand erhalten blieben und somit eine hohe Viskosit{\"a}t in w{\"a}ssrigen L{\"o}sungen beibehielten. In rheologischen Untersuchungen wurde best{\"a}tigt, dass die aus Haferprodukten isolierten β-Glucane ein pseudoplastisches Fließverhalten besitzen. Demgegen{\"u}ber f{\"u}hrte ein Autoklavieren der Produkte zu einer starken Depolymerisation der b-Glucane, was sich in einer {\"A}nderung der funktionellen Eigenschaften der b-Glucane widerspiegelte. Im Mittelpunkt der Untersuchungen standen ern{\"a}hrungsphysiologische In-vitro- und In-vivo-Experimente mit Extrudaten und Proben auf der Basis von Hafer, die einen erh{\"o}hten Anteil an Ballaststoffen, speziell an b-Glucan und an resistenter St{\"a}rke, besaßen und die direkt verzehrbar sind. Diese Haferprodukte zeigten eine Reihe von ern{\"a}hrungsphysiologisch vorteilhaften und protektiven Wirkungen in In-vitro-Experimenten. So traten sie mit Gallens{\"a}uren unter den Bedingungen des D{\"u}nndarms in Wechselwirkung und waren gut mit Faecesflora vom Menschen fermentierbar. Die In-vitro-Verdauung von Maisst{\"a}rke durch Pankreatin, wurde durch die ballaststoffreichen Haferprodukte partiell gehemmt. Dieser Befund l{\"a}sst eine Abschw{\"a}chung des postprandialen Glukoseanstieges erwarten. In einem sechsw{\"o}chigen F{\"u}tterungsversuch erhielten Ratten Di{\"a}ten, die zu 50 \% aus ballaststoffreichen Haferprodukten bestanden. Diese Haferprodukte bewirkten einen erh{\"o}hten Transport von Gallens{\"a}uren und neutralen Sterolen in den unteren Intestinaltrakt sowie deren verst{\"a}rkte Ausscheidung. Durch den Verzehr der ballaststoffreichen Haferprodukte kam es zu Ver{\"a}nderungen in der Mikroflora, wobei sich besonders die coliformen Keime verminderten und die Keimzahlen der Lactobacillen sowie die Bifidobakterien erh{\"o}hten. Die Fermentation der Ballaststoffe f{\"u}hrte zur erh{\"o}hten Bildung von kurzkettigen Fetts{\"a}uren einschließlich von Butyrat. Die Bildung der kurzkettigen Fetts{\"a}uren geht mit einer pH-Wert-Absenkung im Caecum und Colon einher, die wiederum f{\"u}r eine geringere Bildung von sekund{\"a}ren Gallens{\"a}uren verantwortlich ist. Die Ergebnisse des F{\"u}tterungsversuchs an Ratten wurden prinzipiell durch eine vierw{\"o}chige Pilotstudie am Menschen, in der Probanden t{\"a}glich 100 g Haferextrudat erhielten, best{\"a}tigt. Das Extrudat wurde von den Probanden gut akzeptiert. In der 4. Woche wurden eine geringe Abnahme der Cholesterolfraktionen im Serum, h{\"o}here Keimzahlen f{\"u}r Lactobacillen, Bifidobacterien und Bacteroides, geringere pH-Werte und Trockenmassegehalte in den Faeces, eine Zunahme der individuellen und Gesamt-SCFA sowie des Butyratanteils in den Faeces, eine erh{\"o}hte Ausscheidung an Steroiden, eine Zunahme der prim{\"a}ren Gallens{\"a}uren und eine Abnahme des prozentualen Anteils an sekund{\"a}ren Gallens{\"a}uren sowie der Cholesterol-Metaboliten gefunden. Diese Parameter gingen 2 Wochen nach Beendigung der Intervention mit dem Haferextrudat wieder in Richtung der Ausgangswerte (0. Woche) zur{\"u}ck. Die untersuchten Haferprodukte erwiesen sich als gut fermentierbare Substrate f{\"u}r die intestinale Mikroflora und k{\"o}nnen deshalb als ein Pr{\"a}biotikum mit Ballaststoffcharakter eingesch{\"a}tzt werden. Diese Produkte, die mit einem erh{\"o}hten Anteil an resistenter St{\"a}rke und wertvollen Haferballaststoffen hergestellt wurden, k{\"o}nnen dazu beitragen, die Ballaststoffl{\"u}cke in unserer Ern{\"a}hrung zu schließen und positive ern{\"a}hrungsphysiologische Effekte zu bewirken.},
  subject      = {Ballaststoffe},
  language  = {de}
}