463 search hits
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Biogeochemical Consequences of Hydrologic Conditions in a Tropical Montane Rain Forest in Ecuador
(2004)
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Rainer Goller
- Tropical montane forests regulate the hydrological cycles of high-elevation areas being an important service for the local population. The objectives of my work were (1) to determine the major hydrological flow paths, (2) to quantify concentrations of dissolved organic C and organic and inorganic forms of N, P, and S, and (3) to identify the major controls of the dissolved C, N, P, and S dynamics in a tropical montane forest in south Ecuador. Three 8-13 ha large microcatchments (MCs) under montane forest at an altitude of 1900-2200 m above sea level were selected. Scientific equipment was installed on five transects, about 20 m long with an altitude range of 10 m. Three unforested sites near the microcatchments were used for rainfall gauging. Within the three monitored years between May 1999 and April 2002, on average 2448 mm of precipitation fell on the study area. The delta 18O of rainfall shows large variations (-12.6 to +2.1 per mil) related to different air-masses. The delta 18O values of throughfall and lateral flow are similar to those in rainfall. Variations in delta 18O values of the soil solution and the stream water are smaller (-9.1 to -3.0 and -5.8 to -8.7 per mil) than those of rainfall, throughfall, and lateral flow. The delta 18O values in stream water increased immediately after an intense rainstorm event to isotope values similar to those of rainfall and lateral flow. This indicated that during elevated rainfall the water flows rapidly in the organic layers to the stream channel paralleling the surface. During this time the water content of the organic layer was higher than of the upper mineral soil. Results from an isotope two-component hydrograph separation for the three microcatchments showed that new rain water ('event water') contributed 44-81 % to the total stormflow runoff during one selected peak discharge. The canopy was a small and the organic layer the major source of DON, DOP, and DOS, which were almost completely retained in the mineral soil. The organically bound forms contributed, on average in all solutions, 54 %, 78 %, and 59 % to the total concentrations of N, P, and S, respectively. The contribution of organically bound forms to total nutrient concentrations was element-specific and differed among the ecosystem fluxes. The portions of DON (23-81 %) were similar and those of DOP (5-100 %) highly variable in all solutions. There were high DOS portions in the aboveground fluxes (51-100 %) and lower portions in the mineral soil (8-47 %). The pH was positively correlated with the DOC and organic N, P, and S concentrations at the scale of pedons. Increasing DOC concentrations in stream water following rainstorms indicated that rainstorms were an important control of the dissolved organic matter dynamics on a regional scale. During the passage of the water through the forest, dissolved inorganic N (DIN) and DIP concentrations increased between the canopy and the mineral soil and strongly decreased in the mineral soil. In contrast, DIS concentrations were highest in the mineral soil and stream water. Thus, the organic layer was the major source for DIN, the canopy for DIP and the mineral soil for DIS. The mineral soil was a sink for DIN and particularly for DIP. Soil drying and rewetting promoted the release of inorganic N. High discharge levels following heavy rainstorm events were associated with pulses of NO3-N and partly also NH4-N concentrations in stream water. Nitrate-N concentrations in the stream water were positively related to runoff conditions. The DIP and DIS concentrations in throughfall and stemflow were negatively correlated to the respective water fluxes, whereas DIS concentrations in the mineral soil solutions of both studied soil depths were positively related to the rainfall volume. DIN and DIP concentrations and fluxes tended to be positively related to the pH of the organic layer. My results demonstrate that nutrient dynamics were mainly controlled by hydrological conditions in the studied steep forested catchments. Furthermore, small ecosystem inputs and outputs indicated tight cycles of dissolved N, P and S in the study forest, except for DIS.
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Biogeochemical Investigations in Old Growth and Disturbed Forest Sites at Mount Kilimanjaro
(2004)
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Marion Schrumpf
- Areas covered by mountain rainforests in East Africa have important functions as catchment areas for the streams in the savannah. Still, little is known about the biogeochemical processes in these often threatened ecosystems. The current study aims to present basic information on soils and different parameters of the water and nutrient cycle in intact as well as disturbed tropical mountain rainforest sites at Mt. Kilimanjaro in order to assess the long term effects of forest dissection on biogeochemical parameters. For this purpose, the chemical and physical soil properties, soil water tension, rainfall, throughfall, litter percolate and soil solution were determined on twelve study sites in mature forest, secondary forest and elder clearings between 2100 and 2300 m a.s.l. on the southwestern slopes of the mountain. The soil water tension was monitored from May 2000 to August 2002. The simultaneously collected water samples were combined to form fortnight samples and subsequently analysed for their content of K, Mg, Ca, Na, NO3-N, NH4-N, TOC, TON, TOS and TOP. The soils, which comprised of several buried horizons, were Andisols with high C and N stocks, some hydromorphic properties and comparatively low pH values. The latter led to very small ECEC values and low base saturation. Consequently, the retention of cationic nutrients in the soil was considered to be poor. Rainfall amounts were slightly less at the higher sampling sites where the mature forest was located and differed between the study years (2600 mm and 2480 mm at 2100 m, 2210 mm and 1960 mm at 2250 m). Rainfall interception was close to zero in the clearings, but reached up to 30% of incident rainfall in both studied forest types. The analyses of the soil water tension revealed the driest conditions to be under secondary forests. The reason for this was probably a combination of the topographic position of the secondary forest sites and the forest fragmentation. Since the secondary forest sites and the clearings had higher sand contents, the water holding capacity of these sites was lower than in the mature forest. With the exception of NO3-N in the forests, all nutrients in rainfall were increased upon passage through the forest canopy, but nutrient fluxes in rainfall as well as throughfall were still low compared to other mountain rainforests, especially for Mg, Ca and K. Considering the lower biomass of the clearings compared to the forest, the amount of nutrients leached from the vegetation of the clearings was relatively high. Since NO3-N was not assimilated by the vegetation of the clearings, NO3-N throughfall fluxes were higher in the clearings as were the K fluxes, which was probably attributable to different leaf properties of the vegetation at the different sites. In the mature forest, the highest concentrations of nutrients were found in the litter percolate, followed by a pronounced decline in the soil solution. This was especially the case for K. NO3-N was an exception since it exhibited the highest concentrations only in the topsoil solution. Nutrient concentrations in litter percolate and the topsoil solution were usually higher in the clearings than in both forest types. This probably resulted in higher belowground nutrient fluxes since greater water amounts reached the ground surface in the clearings. The high belowground nutrient concentrations were likely the result of the higher mineralisation rates in the clearings induced by higher temperatures and the greater nutrient contents of the litter. With increasing soil depths, nutrient concentrations in seepage water below the clearings declined so that the differences among sites were not significant at deeper soil layers. The contribution of organically bound nutrients to the total concentrations of respective nutrients was highest in throughfall water and lowest in the soil solution, in which OM concentrations were overall lower than in other mountain forests. This was most likely attributable to the adsorption of organically bound nutrients to the mineral phase of the Andisols studied. Again, the highest concentrations in seepage water were measured in the clearings. The results show that mature forests at Mt. Kilimanjaro exhibit a more closed nutrient cycle, especially for basic cations, while the nutrient cycle in the clearings is more open. This probably reflects the different nutrient usage and conservation strategies of the pioneer and the late successional vegetation. Therefore, the forest disturbance on Mt. Kilimanjaro leads to long term changes in biogeochemical cycles. The opening of the forest at lower elevations, which resulted in the formation of large clearings with impeded regeneration and highly fragmented secondary forest patches, led to a higher spatial and seasonal variability of soil moisture and nutrient contents in seepage water. The large scale effects of these forest conversions on water yields and nutrient outputs need to be tested in the future.
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Supercurrents in Restricted Geometries and Driven by Time-Dependent Electric Fields
(2004)
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Martin Endres
- NS Contact We studied the linear response of a normal metal superconducting metal contact to a small electric field. In a preparatory section the order-parameter profile and the density of states were calculated in equilibrium. We showed that the density of states in the normal metal is unaltered if the impurity self-energies are not taken into account while the coherence in the superconductor is always affected by the presence of the normal metal. Self-consistent calculations result in an impurity-induced proximity effect in the normal metal. This proximity effect causes a spatially constant gap in the density of states of the normal metal if the normal metal is sandwiched between two superconductors. The dynamics of the NS contact is strongly dominated by the conservation law for charge and local charge neutrality which together fully determine the current in one-dimensional systems. For answering the question how this constant current is established in the non-homogeneous NS contact, the quasiclassical equations were solved including the self-consistencies for the order parameter, the impurity self-energies, and the electrochemical potential. The latter was used to deduce an internal electric field as response to the external perturbation. The internal field is of same order as the perturbation and is caused by charges which are either bound to the interface or spread over several coherence lengths. The surface charges are not due to the step in the order parameter at the interface but solely to abrupt changes of the impurity scattering. The order parameter itself can only produce continuous charge densities. The charges are indirectly calculated using Maxwell's equations. They are of higher order in the expansion parameters of Fermi-liquid theory and are hence beyond this theory. Nevertheless, their effect has to be considered to be consistent in leading order. Weak links in He3 We investigated several methods of calculating the current-phase relation of weak links in He3. In the limit of small holes the hole itself and the current through it does not affect the order parameter in the superfluid and the current can hence be calculated using the pinhole model. This leads to a periodic current-phase relation. It was shown that the pair-breaking effect of the separating wall has no significant influence on the functional dependence of the current on the phase difference. The wall mainly reduces the amplitude of the current. For orifices with radii comparable with the coherence length, self-consistent order-parameter fields were calculated. The two fixed phases of the pinhole model are then replaced by a field which allows the phase to wind up continuously. This not only breaks the periodicity, but also leads to multivalued current-phase relations. Over a wide range the current through the orifice is linear in the phase difference between the reservoirs. Although this is expected in the hydrodynamic limit, the hydrodynamic equations are not applicable as they always fail at the edges of the circular apertures. However, calculating the current quasiclassically with the phase determined via the Laplace equation gives a fairly good approximation to the fully self-consistent solution. This approximation becomes weak for larger phase differences when pair-breaking due to the current itself has to be taken into account. Remarkably, the maximal current through the aperture is sandwiched between the pinhole current and the depairing current for a homogeneous superfluid which differ only by a factor of about two at low temperature in spite of the drastic difference of the models. A quasiclassical free-energy functional was introduced and it was stressed that this choice is not unique and that a whole zoo of different functionals exists. The functional was used to investigate the change in free energy due to the wall, the orifice, and the phase difference.
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Dynamics of vortices in the two-dimensional anisotropic Heisenberg model with magnetic fields.
(2003)
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Juan Pablo Zagorodny
- The subject of this work is the dynamics of a vortex in a classical 2-dimensional spin system with anisotropic exchange interaction under the combined action of magnetic fields and damping. Static as well as dynamic magnetic fields were employed (as dynamical field we used a homogeneous field which is rotating in the XY-plane). The most important goal of this work was to demonstrate that there is a coupling between the inner and translational freedom degrees of the vortex, coupling which is responsible for at least 2 phenomena that we study in detail in this Thesis: 1. the switching or flipping of the vortex polarization (for negative field frequency), and 2. the formation of stable orbits of the vortex center around the center of the system driven by the rotating field (for positive frequency). It was known to us that the polarization can change abruptly its sign under the action of a field rotating in the XY-plane, for p omega < 0 and appropriate field amplitudes. In the Chapter 4 we have investigated the possible underlying mechanisms for this phenomenon. Our main results can be summarized as follows: a) The flipping times do not depend essentially on the size of the system, provided that the lattice is large enough (radius L >~ 36 lattice constants). In other words, the switching of the vortex polarization is not much affected by the presence of boundaries. b) In our numerical simulations we observed a clear correlation between the core magnetization dynamics (the oscillations of the core spins in the out-of-plane direction) and the velocity of the vortex center in the plane of the lattice. c) A diagram of flipping events as a function of the field parameters, from extensive numerical simulations with an OP vortex in a rotating magnetic field, was presented. We found out that in the (omega, h) parameters space there is no well-defined curve which separates the regime where the flips do not occur from the regime where they do. We found intervals ("windows'') of intermittent flip and non-flip events. d) The switching of the vortex polarization can be achieved also by applying a static magnetic field with both in-plane (IP) and out-of-plane (OP) components. The IP component of the field sets the vortex into translational movement in the XY-plane, while the OP component breaks the vertical symmetry favoring one of the two possible orientations. e) The switching dynamics may be described in terms of a core model which takes into account a coupling between the vortex polarization dynamics and the motion of the vortex center. We showed that a reduced core model, which is valid near the threshold of the IP-OP vortex instability (lambda ~ lambda c), can be mapped to a generalized Thiele equation with an inertial term. f) It is plausible that the phenomenon of switching we described will not be essentially affected by the inclusion of a dipole-dipole interaction. The experimental works on nanodisks mentioned in the Introduction of this Thesis reported the observation of vortices in either of two polarization states, and the switching between them was forced by means of static fields perpendicular to the plane of the disks. Rotating magnetic fields might be used as well static fields with both IP and OP components to make this switching more favorable. In the Chapter 5 we turned to the study of the movement of the vortex in the XY plane, in the presence of the IP rotating field. Attention was directed to the existence of stable orbits, where the vortex stays inside the system in a stationary movement, forming circular limit cycles. We discussed then the failure of the conventional Thiele approach to describe this phenomenon, and this motivated us to formulate an extended collective coordinate Theory, which leads to a qualitative agreement with the results of the simulations. A diagram of the different types of trajectories, as a function of the field parameters, showed the presence of non-monotonous effects and "windows'', like in the case of the switching diagram. We are led to conclude that for some regions of the field parameters space, the system exhibits chaos -which is typical for many-body systems-, though no particular tool of the chaos theory was used to study our discrete and collective coordinate models, from this viewpoint. Our theoretical work qualitatively suggests that it would be interesting to apply in the experiments weak rotating fields like those used here, to control both the mean position of a vortex in larger magnetic dots (where the vortex center could show dynamics) and at the same time the sign of the out-of-plane core magnetization. Future directions of this work may include the use of inhomogeneous fields, particularly with a gaussian localization in a small region of the lattice or "spot'', as a model of the field of a laser beam.
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Coordinated Tree Responses to Drought -Vulnerability and Sustainable Production: Hypotheses on Arid Ecosystem Adjustments to Limitations in Water Resources
(2004)
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Dennis Otieno
- Field and controlled greenhouse experiments were carried out to investigate tree responses to declining soil water content. Field experiments were conducted on naturally growing trees of Acacia tortilis and A. xanthophloea in the savanna region of Kenya and Quercus suber in the Mediterranean region of Portugal. The selected field sites were regions that experience regular drought periods during the year. Greenhouse experiments constituted two watering regimes. Seedlings of A. tortilis and A. xanthophloea grown from seeds initially obtained from the Kenya field site were raised and arranged on a greenhouse bench into two groups per species. The first set of plants were watered every other day (controls) while the second set were watered every seven days (water stress treatments). Field measurements included weather parameters, soil and plant water status, growth, sap flux density, leaf transpiration and stomatal conductance, tissue water relations and isotope labeling. Similar measurements were conducted on plants growing in the greenhouse. Also examined in the greenhouse were root biomass, root structure as well as whole plant biomass accumulation. A second set of experiments was carried out in the greenhouse by subjecting plants initially stressed and non-stressed to severe water stress by withholding water until plants were wilted overnight. The wilted plants were then re-watered regularly and their recovery after stress alleviation was monitored. Declining soil water content significantly affected plant water status in all the trees studied. Lowest psi pd recorded during the study period occurred in the month of June and were –2.0 and –1.1 MPa for A. xanthophloea and A. tortilis respectively. The same species subjected to repeated water stress in the greenhouse attained mean minimum psi pd of –2.4 and –1.2 MPa for A. xanthophloea and A. tortilis respectively at the end of the drying cycle. Mean minimum psi pd recorded for Q. suber during summer was –1.8 MPa and occurred in September. There were however, significant differences among trees. Decline in psi associated with increasing soil drought led to decline in leaf initiation and leaf expansion and both processes ceased at higher water stress levels. For the Acacia species, even leaf shedding occurred at higher stress levels. There was also a decline in stomatal conductance (gs) during water stress, leading to decrease in transpiration rates (E). Maximum stomatal conductance of 340 mmol m-2 s-1 were observed during rainy seasons for the Acacia trees while mean maximum values of 300 mmol m-2 s-1 were recorded for Q. suber when soil moisture conditions were favorable. Stomatal conductance declined by 31%, 67% and 67% in A. tortilis and A. xanthophloea in the savanna and Q. suber in the Mediterranean regions respectively. Daily tree water use (Qtree) as well as leaf transpiration reflected changes in psi and gs. Root to leaf hydraulic conductance equally declined with increasing soil drought. Q. suber trees adjusted osmotically by a magnitude of 0.7 MPa, while bulk modulus of elasticity (epsilon) increased by a magnitude of 17 MPa. Osmotic adjustment of 0.48 MPa was observed in greenhouse plants of A. tortilis while epsilon declined by a magnitude of 7 MPa in A. xanthophloea. A. tortilis plants in the greenhouse showed increased absolute root growth, root depth and root:shoot (r:s) ratio. The dimorphic rooting pattern in Q. suber resulted into hydraulic lift and this could as well occur in A. tortilis because of similarity in their rooting patterns. Most plant responses were reactionary and were aimed at enhancing soil water uptake and reducing transpiration water loss when soil water content was declining. Similar responses were observed for both greenhouse and naturally growing field plants of the same species. Decline in leaf initiation and leaf expansion as well as leaf senescence reduced tree crown size hence potential tree transpiration. This however, had negative impact on plant productivity. Increased root growth as well as osmotic adjustment increased tree water uptake from the soil. The balance between root water uptake and leaf transpiration through growth and stomatal regulation was aimed at protecting xylem integrity. The overall results showed that soil characteristics, root activities and root distribution patterns are the main factors determining tree functioning and productivity in drylands, while the coordinated interaction between the aboveground shoot and belowground root activities ensures survival during drought. Maintained production and survival will ensure distribution and success in the arid environments. Repeated water stress imparted water stress resistance qualities on seedlings enabling them to survive longer during severe stress. The study emphasizes the role of soil resource base as well as species interactions in the functioning and balance of dryland ecosystems.
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Biogeochemistry of Organotin and Organolead compounds in a Forested Catchment in NE-Bavaria, Germany
(2004)
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Jen-How Huang
- Organotin-compunds (OTC) and Trimethyllead (TML) have a higher toxicity than their corresponding inorganic forms and may affect the functioning of ecosystems. Little is known about their behaviour and fate in the terrestrial environment. The goal of this thesis was to investigate the biogeochemistry of OTC (methyltin, butyltin and octyltin compounds) and TML in a forested catchment, especially their input and output budget. The occurrence of OTC, TML, Sntotal and Pbtotal in the atmosphere, soils, precipitation, and runoff in a forested ecosystem in NE-Bavaria, Germany were investigatedand the inputs and outputs in the solute phase determined. In addition, their ad-desorption and transformation (degradation) in forest soils was studied using batch experiments and long term incubations, respectively. OTC and TML concentrations in the gas phase during April to June 2003 was on average 110 pg Sn m–3 and 0,34 pg Sn m–3. Tri-, di-substituted and octyl species were the dominant OTC in the gas phase. In aerosols, only butyltin compounds, dimethyltin and monomethyltin (<500 pg Sn m–3) were found and mono-substituted OTC predominated. For OTC, the washout factors were in the order: mono- >= di- > tri-substituted OTC, and the gas / particle partition coefficients were mono- >> di- >> tri-substituted OTC. Aerosol particles serve as a sink for OTC in the atmosphere, especially for monomethyltin and monobutyltin. From August 2001 to August 2002, the concentrations of tin and lead compounds in precipitation were in the order: fog > throughfall > bulk precipitation. Average concentrations of OTCtotal ranged from 57 ng Sn l–1 in fog to 5.8 ng Sn l–1 in bulk precipitation. The concentrations of Sntotal were between 490 ng Sn l–1 in fog and 140 ng Sn l–1 in bulk precipitation, on average. Average concentrations of TML were 1 ng Pb l–1 in fog and 0.1 ng Pb l–1 in bulk precipitation and 9.6 and 0.76 micro-g Pb l–1 in case of Pbtotal. The annual total deposition from the atmosphere, estimated as throughfall + litterfall fluxes, amounted to 3.7 mg Pb ha-1 yr-1 for TML and 52 g Pb ha-1 yr-1 for Pbtotal. The contribution of litterfall was 1.5% and 32%, respectively. The annual total deposition of OTCtotal was 172 mg Sn ha–1 yr–1, with 26% represented by litterfall. The total deposition of Sntotal was 4.9 g Sn ha–1 yr–1, of which 4.1% was litterfall. The annual flux with runoff from the catchment was 0.5 mg Pb ha-1 yr-1 for TML and 2.8 g Pb ha-1 yr-1 for Pbtotal. The annual runoff of OTCtotal and Sntotal amounted to 25 mg Sn ha–1 yr–1 and 2.4 g Sn ha–1 yr–1, respectively. The mass balance showed high retention of tin and lead compounds in the catchment. The total soil storage of OTCtotal and Sntotal in the catchment were 6.7 g Sn ha–1 and 1.9 kg Sn ha–1. Total soil storage in the catchment was 11.6 mg Pb ha-1 for TML and 222 kg Pb ha-1 for Pbtotal. The dominance of mono-substituted compounds in precipitation is well reflected in the concentrations and storages of OTC in both upland and wetland soils. More than 90% of the soil storage of TML was found in the wetland soils of the catchment representing only 30 % of the area. Most Pbtotal (>90%) was found in the upland soils. In upland soils, TML was only detectable in the forest floor. OTC degraded slowly in soils with half-lives (t½) estimated from 0.5 to 15 years. The degradation rates in soils were generally in the order mono- >= di- > tri-substituted OTC. Decomposition rates of OTC in the forest floor were higher than in wetland and mineral soils. TML degraded rapidly in the forest floor (Oa) with a t½ of 0.09 years. The degradation of TML in Fen (t½ = 1.2 years) and in the mineral soil (Bw-C, t½ = 1.7 years) was much slower. Emission of tetramethyltin and tetramethyllead from wetland soils was not observed, suggesting little Sn and Pb methylation in the wetland soils. The adsorption and desorption isotherms for all species and soils were linear over the concentration range of 10–100 ng Sn, Pb ml–1. The strength of OTC adsorption correlated well with the carbon content and cation exchange capacity of the soil and was in the order mono- > di- > tri-substituted OTC and butyltin > methyltin compounds. The adsorption and desorption showed a pronounced hysteresis. The ratio of total soil storages in the catchment to the present annual input was 3.6 years for TML, reflecting the rapid degradation of TML in forest soils. The ratios of OTC soil storages to their present annual deposition ranged from 4.3 to 400 years. These high ratios reflect probably the high stability, low mobility of OTC in soils and the variation of the annual total deposition.
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Nanostructure formation in thin polymer films
(2004)
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Nicolaus Rehse
- In the first part of this thesis an improved process is presented to prepare laterally structured substrates via hierarchical self organization. A miscut silicon surface annealed at 1400 K under ultra high vacuum conditions is used. The resulting facets are stable against oxidation and form a topographic pattern which can be further modified to a chemical pattern via evaporation of gold on every other facet. By controlling the time of annealing, we create structures with a reproducible mean width ranging from 40 to 400 nm. Despite the rather complex ultra high vacuum treatment and an additional evaporation step, we are able to produce substrates in a relatively short time (36 h). These substrates show a nanometer sized structure over an area of 0.5 cm². The automation of the cleaning process and a controlled heating during the annealing increases the yield of high-quality, stepped substrates. These structures allowed us to study the behavior of ultra-thin polystyrene films on topographically structured substrates. The film thickness of some nanometers is comparable to the radius of gyration of the polymers. The substrate corrugation causes a regular variation of the film thickness. We start with a homogeneous film, which is annealed above the glass transition temperature. During annealing the films are stable or form long polymer nanochannels, which lie in the grooves of the substrate structure. The balance of the radius of gyration and the film thickness controls the stability of the polymer film, while the corrugation only triggers the dewetting. The same behavior is found for films on flat substrates. Here small contaminations nucleate the formation of holes. Evaporation of gold stripes and their modification with self assembled monolayers leads to chemical patterned substrates. This expands the possibilities to manipulate the substrate wettability on the nanometer scale. The second part of the thesis describes the formation of ordered structures in block copolymer films. ABC triblock copolymers show a large variety of morphologies in thin films. We have shown that surface reconstructions play an important role in the structure formation process of these structures. In very thin films, where the film thickness is smaller than the long period of the polymer's micro domains, confinement effects overlap with the surface effects. The component with the lowest surface energy is accumulated at the free surface. It needs a subtle balance between the different surface energies (external fields) and the interaction of the three polymer blocks (internal fields) to create a surface reconstruction. This was shown by variation of the chemistry of the end block and by changing the sequence of blocks in the experiment. To analyze the surface reconstruction we used selective staining along with scanning electron microscopy, selective etching in oxygen plasma in combination with scanning probe microscopy, as well as quantitative TappingMode atomic force microscopy. Surface reconstructions of block copolymers show remarkable similarities with reconstructions of single crystal surfaces. In both cases the driving force for a rearrangement is the decrease in surface free energy of the ideal surface. A second analogy between the lamella forming SBM triblock copolymer and Si(100) is the fact that two non-equivalent layers of matter aligned parallel to the free surface lead to two different terminations at the surface. This shows that the phenomenon of surface reconstructions is not limited to classic crystals. The results of this thesis give new insights in the behavior of polymers at surfaces and in thin films. This gives the opportunity to create or manipulate nanometer sized structures accurately via self assembly, external stimuli, or a combination of both.
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Keteneylidenetriphenylphosphorane as a 'C2O building block' in the synthesis of highly functionalised tetramic and tetronic acids
(2004)
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Claire Melanophy
- Naturally occurring 4-hydroxy-pyrrol-2(5H)-ones and 4-hydroxy-furan-2(5H)-ones are known to possess a wide range of biological activities such as anti-viral and tumour inhibition. For this reason, the synthesis of a number of these compounds was attempted, namely Tenuazonic Acid, Reutericyclin and Carlosic acid. A general synthesis of 4-hydroxy-pyrrol-2-ones was established by reaction of a phosphorus ylide (Ph3PCCO) with a variety of amino esters. A number of derivatives were prepared with varying substituents at the 3- and 5-positions of the nitrogen heterocycle. A general method for the preparation of highly functionalised furan-2-ones from simple alpha-hydroxy esters was also developed. Progress has been made in the synthesis of N-substituted pyrrol-2-ones where simple amide esters were reacted with a phosphorus ylide (Ph3PCCO) in the construction of highly functionalised nitrogen heterocycles. A new acylation procedure was developed in order to selectively introduce an acetyl residue to pyrrolidine-2-ones and furan-2-ones. A phosphorus ylide (Ph3PCCO) and its solid supported variant were used as acylating agents under relatively mild, basic conditions. Complex heterocycles were prepared using the Diels-Alder methodology and from reaction of Ph3PCCO with relatively simple molecules.
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Equilibrium and Dynamic Phase Behavior in Thin Films of Cylinder-Forming Block Copolymers
(2004)
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Armin Knoll
- The equilibrium and dynamic phase behavior in thin films of cylinder-forming block copolymers has been studied. The results range from an extension of an advanced strong segregation theory to the treatment of cylindrical microdomains in a thin film, over the detailed analysis of the phase behavior and the microdomain dimensions of a cylinder forming model system, to the first in-situ measurements of phase transitions and microdomain dynamics in a thin block copolymer film. The first result concerns the characterization of thin films of the model system, a polystyrene-b-polybutadiene-b-polystyrene (SBS) triblock copolymer, by tapping mode scanning force microscopy (TM-SFM). We present a procedure to establish reliably with TM-SFM the true surface topography of a soft polymeric sample. The measurement of an array of amplitude phase distance (APD) curves enables us to distinguish quantitatively between the ¡°real¡± surface topography and lateral differences in tip indentation. We find that conventional TM-SFM height images are not necessarily reflecting the surface topography of the sample. In the case of SBS we find that the surface is flat and that conventional TM-SFM height images only reflect lateral differences of tip indention. A theoretical treatment of the phase behavior in thin films of cylinder forming block copolymers within an advanced strong segregation theory (SST) framework of Olmsted and Milner is developed. Although the theory is strictly valid only for highly stretched chains and does not account for minority domain structures other than cylinders, the predicted results are in good agreement to the experimental results in this thesis. The microdomain structures under consideration are in plane oriented cylinders terminating with either the matrix component CP or a half cylinder CH at the surface and cylinders oriented perpendicular to the film CS. The thin film phase behavior of concentrated solutions of SBS in chloroform is studied experimentally. The stable phases are mapped as a function of film thickness and polymer concentration phi. The variation of phi can be interpreted as a variation of the molecular interactions between the two polymer components and between the components and the boundary surfaces. The preferential attraction of the majority component to the surface, the surface field, causes the cylinders to align parallel to the plane of the film, whenever the thickness fits an integer multiple of cylinder layers. At intermediate thickness the cylinders align perpendicular to the film plane. At higher polymer concentration, i.e., at stronger surface fields, a perforated lamella (PL) of polystyrene forms. The surface field needed for PL formation increases with increasing film thickness. A wetting layer exists underneath all films, which either consists of pinned molecules or of a half lamella. Furthermore the principal microdomain spacings of the thin film microdomain structure are investigated in detail and compared to the SST results. A new image analysis algorithm provides the recognition and the localization of the different structures in the SFM phase contrast images. The microdomain spacings are discussed as a function of various parameters like the film thickness, the polymer concentration and the local curvature of the structure. An examination of the dependence of the spacing in the C¨U structure from the local curvature of the cylinders yields an effect of second order, which can be explained in terms of density conservation of the polymer blocks. The spacing of the CP structure also depends on the local thickness of the thin film. The CP phase is stable in a certain thickness range close to its preferred thickness. Within this range it has to adapt the cylinder "height" to be commensurable with the film thickness. Minimization of the interface between the blocks leads to a smaller or larger lateral cylinder spacing if the cylinder has to stretch or shrink its dimension perpendicular to the plane of the film, respectively. Finally the first in-situ observation of phase transitions in thin block copolymer films is presented. During annealing with a controlled atmosphere of chloroform vapor the film develops islands and holes. The development of the microdomain structure and its spacial fluctuations are captured. The rather high polymer concentration in the thin film results in a time scale of the fluctuations in the order of seconds to minutes. The decreasing film thickness inside of the holes triggers phase transitions from CS to CP to PL according to the phase diagram of the system.
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The complex foraging strategy of the specialised gallfly Urophora cardui (Diptera: Tephritidae) for host plants (Cirsium arvense, Asteraceae)
(2004)
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Wiltrud Daniels
- Nearly all herbivorous insects in terrestrial ecosystems depend on plants for their survival and reproduction. They dominate terrestrial ecosystems due to species and individual abundance. Interactions between these two groups are thus of a high significance for the analysis and the understanding of complex interactions in terrestrial ecosystems. Foraging for host plants by herbivorous insects is of a central importance. In the present thesis the foraging strategy of the specialised gall fly Urophora cardui on the creeping thistle, Cirsium arvense, was investigated as an example for the foraging of a specialised herbivorous insect. Males and females of U. cardui use the larval host plant as rendezvous place. The males establish territories on the plant, which they defend against conspecifics. The females lay eggs into axillary buds in order to initiate gall development. Male and female body size, measured as weight at eclosure or capsule width, was not correlated with male respectively female longevity. Males lived shorter than females. Capsule width of males and females was not significantly different, while weight at eclosure and fresh weight at death was. Females weighed more, which may be due to their higher need of energy during adult life. Both sexes lost body weight during life. All behaviours, which are performed by males and females on the host plant were defined, recorded and analysed. Females spent most of the time on resting, probing axillary buds, running on the plant and grooming. Males spent most of the time on copulation and patrolling their territory. The behaviour of both sexes was highly variable between individuals. Concerning the movement pattern on an already chosen host plant, females concentrate on the upper parts of the host plant. They were mainly occupied with extensive probing of various axillary buds, which occurred in a suitable developmental stage at the top of the plant. In contrast males patrolled the whole plant, although only the upper leaves became marked. If they encountered another male threatening and fighting were inevitable. Fights lasted several hours interrupted by threatening periods. Mating of males and females usually followed oviposition. Neither females nor males accepted modified host plants or models of thistles. Their behaviour on modified thistles was reduced mainly to running around the plant and grooming. These results indicate a rigid host plant template using the input of several senses, the flies always recognise models and modified plants as a non-host plant. Both sexes were able to discriminate host plants and non-host plants from a distance of 0.8-2m. The time male and female flies needed until they selected one of the host plants in a particular host plant stand depended on the number of non-host plants, host plants and the number of suitable hosts. The decision-time became shorter, if there were not too many suitable host plants. This may be due to decreasing sampling time of the host plants present. U. cardui females did not prefer plants of a certain height. In contrast the branching level, which indicates the number of axillary buds, and the number of flower buds played a significant role during foraging for host plants. Plants with an intermediate branching level were preferred, while those with many flower buds were avoided. Males of U. cardui were able to select their territorial plant on olfactory cues or on visual cues likewise. In contrast, emales were not able to recognise their host plant on olfactorial cues alone. But, if male-marked and unmarked host plants were available they significantly preferred the marked thistles. The differentiation between marked and unmarked C. arvense was made according to olfactorial cues, since plants did not differ in their height, nor in their branching level, nor in the number of flower buds. Thus, female selection of larval host plants depended on male choice for territories. This result is remarkable, especially in evolutionary terms, since males select the larval host for the offspring of their predecessor. Interestingly males preferred plants marked by conspecifics also. On the tip of the females’ ovipositor there is a receptor field with several morphological different receptor types. Mainly they seem to have mechanoreceptive as well as chemosensory functions. These receptors enable the females to measure and analyse the inner structure of the plant tissue at the axillary bud. The width of the apical meristem of the axillary buds was proven to influence female choice of the oviposition site. Axillary buds with an apical meristem-diameter above 0.62mm had a higher probability to became chosen by the U. cardui females. The clutch size was adjusted to the diameter of the apical meristem, indicating, that females were able to estimate the quality of the respective axillary bud influencing larval performance. These results were summarized in a model of the foraging strategy of U. cardui.
