06 Fakultät Luft- und Raumfahrttechnik und Geodäsie
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Item Open Access Towards improved targetless registration and deformation analysis of TLS point clouds using patch-based segmentation(2023) Yang, Yihui; Schwieger, Volker (Prof. Dr.-Ing. habil. Dr. h.c.)The geometric changes in the real world can be captured by measuring and comparing the 3D coordinates of object surfaces. Traditional point-wise measurements with low spatial resolution may fail to detect inhomogeneous, anisotropic and unexpected deformations, and thus cannot reveal complex deformation processes. 3D point clouds generated from laser scanning or photogrammetric techniques have opened up opportunities for an area-wise acquisition of spatial information. In particular, terrestrial laser scanning (TLS) exhibits rapid development and wide application in areal geodetic monitoring owing to the high resolution and high quality of acquired point cloud data. However, several issues in the process chain of TLS-based deformation monitoring are still not solved satisfactorily. This thesis mainly focuses on the targetless registration and deformation analysis of TLS point clouds, aiming to develop novel data-driven methods to tackle the current challenges. For most deformation processes of natural scenes, in some local areas no shape deformations occur (i.e., these areas are rigid), and even the deformation directions show a certain level of consistency when these areas are small enough. Further point cloud processing, like stability and deformation analyses, could benefit from the assumptions of local rigidity and consistency of deformed point clouds. In this thesis, thereby, three typical types of locally rigid patches - small planar patches, geometric primitives, and quasi-rigid areas - can be generated from 3D point clouds by specific segmentation techniques. These patches, on the one hand, can preserve the boundaries between rigid and non-rigid areas and thus enable spatial separation with respect to surface stability. On the other hand, local geometric information and empirical stochastic models could be readily determined by the points in each patch. Based on these segmented rigid patches, targetless registration and deformation analysis of deformed TLS point clouds can be improved regarding accuracy and spatial resolution. Specifically, small planar patches like supervoxels are utilized to distinguish the stable and unstable areas in an iterative registration process, thus ensuring only relatively stable points are involved in estimating transformation parameters. The experimental results show that the proposed targetless registration method has significantly improved the registration accuracy. These small planar patches are also exploited to develop a novel variant of the multiscale model-to-model cloud comparison (M3C2) algorithm, which constructs prisms extending from planar patches instead of the cylinders in standard M3C2. This new method separates actual surface variations and measurement uncertainties, thus yielding lower-uncertainty and higher-resolution deformations. A coarse-to-fine segmentation framework is used to extract multiple geometric primitives from point clouds, and rigorous parameter estimations are performed individually to derive high-precision parametric deformations. Besides, a generalized local registration-based pipeline is proposed to derive dense displacement vectors based on segmented quasi-rigid areas that are corresponded by areal geometric feature descriptors. All proposed methods are successfully verified and evaluated by simulated and/or real point cloud data. The choice of proposed deformation analysis methods for specific scenarios or applications is also provided in this thesis.Item Open Access Ein Beitrag zur Stützung eines Software GNSS Empfängers mit MEMS-Inertialsensoren(2016) Gäb, Michael; Kleusberg, Alfred (Prof. Dr.-Ing.)Die genaue Bestimmung von Position und Geschwindigkeit mit einem globalen Navigationssatellitensystem (engl. Global Navigation Satellite System) (GNSS) in Echtzeit bildet eine essentielle Grundlage für viele Anwendungen in der Navigation. Bei mobilen Navigationsanwendungen finden häufig GNSS-Messungen unter ungünstigen Beobachtungsbedingungen statt, so dass Fehler in den Ergebnissen auftreten können. In diesem Fall ist der GNSS-Empfänger in Bewegung, so dass die Empfangsumgebung sich ständig ändert. So können Objekte, wie z.B. Gebäude, Bäume, Tunnel usw. zu Reflektionen, Dämpfung bzw. Abschattung der GNSS-Signale führen. Eine hohe zusätzliche Dynamik bzgl. der beobachteten Dopplerfrequenzverschiebung erfährt das empfangene GNSS-Signal durch die Bewegung des GNSS-Empfängers. Das beeinflusst die Signalnachführung (Tracking) und verursacht Fehler bei der Positions- und Geschwindigkeitsbestimmung oder eine Bestimmung ist sogar unmöglich. Eine Verbesserung der Positions- und Geschwindigkeitsbestimmung wird durch die gleichzeitige Messung mit einem GNSS-Empfänger und einem inertialen Navigationssystem (engl. Inertial Navigation System) (INS) ermöglicht. Kostengünstige INS beinhalten heute Mikro-Elektro-Mechanische Systeme (engl. Micro Electro Mechanical Systems) (MEMS), die als MEMS-Inertialsensoren bezeichnet werden. Die gemeinsame Nutzung der Messdaten von GNSS und INS wird als GNSS/INS-Integration bezeichnet. Diese Arbeit befasst sich mit der Tiefen GNSS/INS-Integration, so dass mit der Information eines INSs in die Tracking Loop des GNSS-Empfängers eingegriffen wird, um Verbesserungen beim Tracking des Signals und der daraus bestimmten GNSS-Beobachtungen zu erzielen. Dieser Eingriff wird auch als Stützung (engl. aiding) bezeichnet. Die Stützung erfolgt über die Regelgrößen (Dopplerfrequenz und Codephase) in der Tracking Loop für den jeweiligen Kanal des GNSS-Empfängers. Dazu werden die Regelgrößen zunächst prädiziert, bevor diese beim Tracking des empfangenen GNSS-Signals berücksichtigt werden können. Für die Prädiktion müssen die Position und Geschwindigkeit des Satelliten und des Empfängers vorliegen. Außerdem müssen die Uhrenfehlerrate des Satelliten und des Empfängers bekannt sein. Aus diesen Größen kann die Dopplerfrequenz und daraus die Rate der Codephase berechnet werden. Die zeitliche Integration der Codephasenrate ergibt die aktuelle Codephase. Aus den Ephemeriden des GNSS-Satelliten kann die Position, die Geschwindigkeit und die Uhrenfehlerrate für einen zeitnahen beliebigen Zeitpunkt berechnet werden. Die Uhrenfehlerrate des Empfängers wird hierbei mittels einer Extrapolation vorausbestimmt. Mit den MEMS-Inertialsensoren kann die Position und Geschwindigkeit des Empfängers fortgeführt werden. Diese Fortführung erfolgt über eine Lose GNSS/INS-Integration mittels einer Strapdown-Rechnung und einem Kalman-Filter für 15 Fehlerzustände. Als Stützwerte für den Kalman-Filter dienen hier die Position und Geschwindigkeit des SGEs. Die Stützung sollte bei einem Signalabriss oder für die Stabilisierung des Trackings eingeschaltet werden. Die Stützungsmethode wird mit einem Software GNSS-Empfänger (SGE) und einer Inertiale Messeinheit (engl. inertial measurement unit) (IMU) aus MEMS-Inertialsensoren (MEMS-IMU) in der Landfahrzeugnavigation getestet und analysiert. Der SGE ist für die Signale des globalen Positionierungssystem (engl. Global Positioning System) (GPS) mit dem C/A-Code auf der L1-Frequenz entwickelt und bestimmt die Position und Geschwindigkeit mit einer Messrate von 1 kHz. Die MEMS-IMU beeinhaltet 6 Freiheitsgrade mit jeweils einem 3-achsigen MEMS-Beschleunigungs- und MEMSDrehratensensor. Die Messrate des MEMS-Beschleunigungssensors beträgt 1 kHz und die Messrate des MEMS-Drehratensensors beträgt 800 Hz. Mit diesem Messsystem ist es möglich, die Prädiktion der Regelgrößen für jede Millisekunde durchzuführen, so dass diese bei jedem Tracking-Durchlauf mit dem C/A-Code vorliegen. Aufgrund der hohen Messraten können nur wenige Minuten Messdaten erfasst werden und die Auswertung erfolgt in der Nachbearbeitung (engl. post-processing). Die Stützungsmethode wird durch Fahrten mit einem Messfahrzeug getestet. Dazu werden Messfahrten mit verschiedenen Fahrmanöver ausgeführt, um im empfangenen GPS-Signal unterschiedliche Raten in der Dopplerfrequenz zu erzeugen. Eine Fahrt unter Bäumen ermöglicht den Einfluss des zeitlichen Verlaufs im Signal-Rauschverhältnis (engl. signal-to-noise ratio) (S/N) des empfangenen GPS-Signals auf die Stützungsmethode zu untersuchen. Bei dieser Messfahrt treten auch immer wieder kurzzeitige Signalabrisse auf. Die in der vorliegenden Arbeit dokumentierten Messfahrten und Ergebnisse zeigen, dass die Stützung für einen SGE erfolgreich in der Landfahrzeugnavigation durchgeführt werden kann. Die prädizierten Regelgrößen werden für die verschiedenen Messfahrten zuverlässig berechnet und das Tracking kann damit stabilisiert und sogar bei einem Signalabriss vorgesteuert werden. Außerdem können Ausreißer direkt in den Beobachtungen minimiert werden, so dass Verbesserungen in der Positions- und Geschwindigkeitsbestimmung des SGEs erzielt werden können.Item Open Access Lebensdauerabschätzung von metallischen Strukturen mittels der Diskrete-Elemente-Methode im gekoppelten thermo-mechanischen Feld(2012) Hahn, Manfred; Kröplin, Bernd (Prof. Dr.-Ing. habil.)Aufgrund der hohen Streubreite der physikalischen Eigenschaften von metallischen Werkstoffen kann man deren Verhalten nicht zuverlässig voraussagen. Dies stellt insbesondere bei der Lebensdauervorhersage von industriell gefertigten Konstruktionen ein Problem dar. Der atomare Aufbau eines metallischen Werkstoffs besteht in der Regel aus einem Hauptelement und einem oder mehreren Nebenkomponenten was dazu führt, dass beim Erstarren einer Metallschmelze auf der Atomskala die Anreihung der Atome nicht strukturiert erfolgt, sondern mit zufällig verteilten Fehlern. Betrachtet man den Werkstoff auf einer göberen Skala so fällt auf, dass metallische Schmelzen an vielen Stellen zu erstarren beginnen und dass die Erstarrungskeime und die Grenzen der Erstarrungsfronten stochastisch verteilt sind. Die metallischen Werkstoffe sind also bei genauerer Betrachtung kein Kontinuum sondern ein Diskontinuum in dem die physikalischen Eigenschaften global betrachtet zu den in den Laborexperimenten beobachteten Werten verschmieren. Ziel der vorliegenden Arbeit ist es, den Werkstoff als ein Diskontinuum darzustellen, um die stochastisch verteilten physikalischen Eigenschaften auf einer kleinen Skala zu erfassen. Im Weiteren sollen auf einer größeren Skala die physikalischen Eigenschaften zu den global beobachteten Werten verschmieren. Dabei soll die in dieser Arbeit vorgestellte numerische Methode der diskreten Elemente im mechanischen Feld ausgebaut und im Folgenden auf andere physikalische Felder übertragen werden. In metallischen Werkstoffen gehen bei zyklischen Belastungen im Inneren des Werkstoffs mikroplastische Verformungen vonstatten, welche mit zunehmender Zyklenzahl den Werkstoff an diskreten Stellen mit Mikroschäden sättigen. Dabei schreitet die diskrete Sättigung solange voran, bis der diskrete Ort übersättigt bzw.~geschwächt ist und im Folgenden versagt. Die mikroplastischen Verformungen sind, wie auch die anderen physikalischen Parameter, mit einer statistischen Größe behaftet. Die diskrete Akkumulation der statistisch verteilten mikroplastischen Schädigung soll in das numerische Modell der Diskreten-Elemente-Methode (DEM) mit aufgenommen werden, so dass sich auf numerischem Weg Lebensdauersimulationen durchführen lassen. Ein wesentlicher Teil dieser Arbeit beschäftigt sich mit den mathematischen Beweisen für die Gültigkeit der DEM als numerische Methode, sowohl für das mechanische als auch für das thermische Feld. Die Beweisführung erfolgt über eine vergleichende Betrachtung mit der Finite-Volumen-Methode (FVM), der Finite-Differenzen-Methode (FDM) und der Finite-Elemente-Methode (FEM). Dabei wird aus der FVM die Idee übernommen, dass physikalische Flüsse übertragen werden. Im Weiteren ergibt die Assemblierung von sechs Stäben, welche die physikalische Feldgröße übertragen, zusammen mit dem lokalen physikalischen Gleichgewicht den Finite-Differenzen-Stern der FDM. Zuletzt wird das globale Gleichgewicht mittels der FEM gewonnen. Im Nachlauf der Finite-Elemente-Rechnung lassen sich die Flussgrößen zurückbestimmen. In dieser Arbeit wird gezeigt, wie die Kopplung des mechanischen und thermischen Feldes mittels der DEM vorgenommen werden kann. Dazu wird ausgeführt, wie die beiden Felder zusammen wirken und wie stark deren Kopplung ist. Abschließend wird eine Lebensdauersimulation an einer thermo-mechanisch belasteten virtuellen Probe vorgeführt. Das Ergebnis dieser Arbeit zeigt, dass die DEM eine Methode ist, um partielle Differentialgleichungen zu lösen, sowohl für Einzelfelder, als auch für gekoppelte Felder. Außerdem kann der Werkstoff durch die Methode als ein Diskontinuum betrachtet werden, so dass sich Lebensdauersimulationen mittels eines erweiterten Werkstoffmodells vornehmen lassen.Item Open Access "A la recherche du temps perdu" : on geological condensation, with examples from the Jurassic Subbetic Plateau in Southeastern Spain(1993) Fels, Alexander; Seyfried, HartmutEine kondensierte Ablagerung ist eine marine Rückstandsbildung, die sich autochthon und kontinuierlich über einen längeren Zeitraum hinweg gebildet hat. Kondensation kann synsedimentar durch Abschirmung, Ablenkung oder Abtragung von Schlamm erfolgen; diagenetisch läuft Kondensation vor allem über Bioerosion auf Hartboden in Verbindung mit unterschiedlich tiefgreifender Erosion ab. Im Jura des subbetischen Plateaus (früher "externes Subbetikum") wird das Umkippen in eine Kondensations-Situation durch tektonische Bewegungen gesteuert, indem benachbarte Plattformen den Export von Schlamm selbssteuernd regulieren. Das subbetische Plateau durchlief vier Phasen stark reduzierter Sedimentation: Carixien - Unter-Domerien(Kondensatlonsepisode 1), Obertoarcien - Unter-Bajocien (Kondensationsepisode 2), Unterbathonien - Unter-Oxfordien (Kondensationsepisode 3) und unterstes Kimmeridgien (Kondensationsepisode 4). Hartboden, die sich während dieser Episoden bildeten, sind meistens von Goethitkrusten und Goethitonkoiden bedeckt. Die meisten Goethitkrusten bestehen entweder aus sehr dünnen (20 - 50 p.) Laminae mit krümeligem und pseudofilamentösem Gefüge, die für einen mikrobiellen Ursprung der Krusten sprechen, oder sie bestehen aus strukturlosem, "sterilen" Goethiterz. Aus einer Abschätzung der Wachstumsraten folgern wir, daß der überwiegende Teil der Zeit, die in solchen Krusten versteckt ist, entweder im nur wenige Milimeter dicken Goethiterz dokumentlert ist oder in Hartböden bzw. Erosionsflächen gelöscht wurde. Kondensierte Abfolgen zelgen meistens eine hierarchische Gliederung in Sequenzen, die vom Meter- bis zum Millimeterbereich reichen und nahezu stets denselben Aufbau haben: sie beginnen mit reduzierter Sedimentation, auf die ein Omissionsstadium folgt und schließen melstens mlt Goethitkrusten ab. Unter den vielen Faktoren, die für eine solche Abfolge verantwortlich sein konnen, kristallisiert sich als kleinster gemeinsamer Nenner ein (nicht eindeutig kalibrierbares) eustatisches Signal heraus. Wir betrachten deshalb kondensierte Sequenzen, die Goethitkrusten enthalten, als pelagische Parasequenzen.Item Open Access Thermodynamic analysis and numerical modeling of supercritical injection(2015) Banuti, Daniel; Weigand, Bernhard (Prof. Dr.-Ing. habil.)Although liquid propellant rocket engines are operational and have been studied for decades, cryogenic injection at supercritical pressures is still considered essentially not understood. This thesis intends to approach this problem in three steps: by developing a numerical model for real gas thermodynamics, by extending the present thermodynamic view of supercritical injection, and finally by applying these methods to the analysis of injection. A new numerical real gas thermodynamics model is developed as an extension of the DLR TAU code. Its main differences to state-of-the-art methods are the use of a precomputed library for fluid properties and an innovative multi-fluid-mixing approach. This results in a number of advantages: There is effectively no runtime penalty of using a real gas model compared to perfect gas formulations, even for high fidelity equations of state (EOS) with associated high computational cost. A dedicated EOS may be used for each species. The model covers all fluid states of the real gas component, including liquid, gaseous, and supercritical states, as well as liquid-vapor mixtures. Numerical behavior is not affected by local fluid properties, such as diverging heat capacities at the critical point. The new method implicitly contains a vaporization and condensation model. In this thesis, oxygen is modeled using a modified Benedict-Webb-Rubin equation of state, all other involved species are treated as perfect gases. A quantitative analysis of the supercritical pseudo-boiling phenomenon is given. The transition between supercritical liquid-like and gas-like states resembles subcritical vaporization and is thus called pseudo-boiling in the literature. In this work it is shown that pseudo-boiling differs from its subcritical counterpart in that heating occurs simultaneously to overcoming molecular attraction. In this process, the dividing line between liquid-like and gas-like, the so called Widom line, is crossed. This demarcation is characterized by the set of states with maximum specific heat capacity. An equation is introduced for this line which is more accurate than previous equations. By analyzing the Clausius-Clapeyron equation towards the critical limit, an expression is derived for its sole parameter. A new nondimensional parameter evaluates the ratio of overcoming molecular attraction to heating: It diverges towards the critical point but shows a significant pseudo-boiling effect for up to reduced pressures of 2.5 for various fluids. It appears reasonable to interpret the Widom-line, which divides liquid-like from gas-like supercritical states, as a definition of the boundary of a dense supercritical fluid. This may be used to uniquely determine the radius of a droplet or the dense core length of a jet. Then, a quantitative thermodynamic analysis is possible. Furthermore, as the pseudo-boiling process may occur during moderate heat addition, this allows for a previously undescribed thermal jet disintegration mechanism which may take place within the injector. This thermal jet break-up hypothesis is then applied to an analysis of Mayer’s and Branam’s nitrogen injection experiments. Instead of the constant density cores as predicted by theory, the majority of their cases show an immediate drop in density upon entering the chamber. Here, three different axial density modes are identified. The analysis showed that heat transfer did in fact take place in the injector. The two cases exhibiting a dense core are the cases which require the largest amount of power to reach the pseudo-boiling temperature. After this promising application of pseudo-boiling analysis, thermal break-up is tested numerically. By accounting for heat transfer inside the injector, a non dense-core injection can indeed be simulated for the first time with CFD. Finally, the CFD model is applied to the A60 Mascotte test case, a reactive GH2/LOX single injector operating at supercritical pressure. The results are compared with experimental and other researcher’s numerical data. The flame shape lies well within the margins of other CFD results. Maximum OH* concentration is found in the shear layer close to the oxygen core and not in the shoulder, in agreement with experimental data. The axial temperature distribution is matched very well, particularly concerning position and value of the maximum temperature.Item Open Access Volcanic evolution of Southern Tenerife (Canary Islands) during the Pleistocene and Holocene(2009) Kröchert, Jörg; Buchner, Elmar (PD Dr.)The Canary Islands are a group of volcanic ocean islands in the Central Atlantic near the continental margin of northwest Africa. Tenerife, with a volcanic history of more than 12 Ma of subaerial eruptions, is the largest island of the Canaries and is situated in the centre of the Archipelago. The Quaternary Bandas del Sur Formation in the South of Tenerife comprises a complex sequence of pyroclastic rocks and lavas and is part of the southern rift zone. In contrast to the northwest and northeast rift zones on Tenerife, the southern rift zone comprises a number of characteristics with respect to the morphological features, eruption cyclicity, and the geochemistry of the volcanic deposits. Various flank eruptions of the Las Cañadas volcano associated with basaltic lavas and the formation of cinder cones within the Bandas del Sur are important volcanic units for understanding the explosive volcanic cycles during the Pleistocene on Tenerife. Paleomagnetic studies, geochemical analysis of major and trace elements, and two radioisotopic dating (K-Ar) have been carried out on prominent cinder cones, to determine their stratigraphic position. By combining the results with previous K-Ar data in the Literature, the cones and lavas can be subdivided into three stratigraphic units. Cinder cones that belong to the first unit show reverse magnetization and Y/Nb ratios between 0.37-0.41; cinder cones of the second unit show normal magnetization and Y/Nb ratios of <0.35. The third unit comprises cinder cones with normal magnetization and Y/Nb ratios of about 0.47. The first two units were constructed between ~0.948-0.779 Ma and 0.323-0.300 Ma. These units define volcanic cycles that culminated in violent Plinian eruptions. The third and youngest unit possibly marks the beginning of a further volcanic cycle that started ~0.095 Ma ago. In order to reconstruct the uplift history of Tenerife, numerous uplifted fossil beaches and tuff cones were investigated. In the North and Northeast of Tenerife, the positions of fossil beaches indicate stable conditions since 130 ka. The uplift rates in southern Tenerife (within the Bandas del Sur) amount to a minimum of 15 m since 778 ka at Montaña Pelada and to a maximum of up to 45 m since 10 ka in the area of El Médano, suggesting an asymmetrical uplift of the island complex. The uplift in the South could be caused by seismic activity or mass loss due to flank collapse events. However, uplift due to ascending magma is more plausible. The fossil beach deposits of the El Médano area exhibit tubular-shaped concretions and concretionary dykes. These sediment structures have been interpreted as the result of a) the interaction between hot ignimbrites that overflowed wet beaches, b) fast accumulation of beach sands on hot and degassing ignimbrites, c) paleoliquefaction caused by an earthquake (seismites). Based on the interpretation as seismites, an intense paleoearthquake was proposed to be responsible for the generation of the paleoliquefaction structures. However, the sedimentary structures in question show the general criteria diagnostic for rhizocretions and root tubules with respect to their orientation, size, branching system, and style of cementation. Faults of a well-defined strike direction that precisely coincides with the southern rift fault system occur in the El Médano site. This fault system was generated contemporaneously with a chain of cinder cones ~948 ka ago. Open fractures in ignimbrites (~668 ka) and the fossil beach deposits (~10 ka) of the El Médano area suggest that the rift-associated fault system has been seismically active in the aftermath and probably is still active. A further fault system striking perpendicular to the rift-associated faults probably originates from a Holocene paleoearthquake of moderate intensity. Earthquake-induced ground effects in the fossil beach deposits of the study area are consistent with seismically induced ground effects of several recent and well-documented earthquakes and gravitational sliding triggered by an intense earthquake in Nicoya/Costa Rica in 1990. Both, the rift-associated and the earthquake-induced fault system, initially produced open cracks in the fossil beach deposits that were occupied by plants and subsequently stabilized by cementation. These results accentuate that the densely settled southern part of Tenerife is latently endangered by volcanic and seismic activity, though, currently, there are no indications of increasing volcanic activity in this region. Uplift due to recent magma loading is not observable and the intensity of a paleoearthquake in the El Médano area was probably considerably lower than mentioned in the literature.Item Open Access Experimental investigation of low-frequency sound and infrasound induced by onshore wind turbines(2024) Blumendeller, Esther; Cheng, Po Wen (Prof. Dr.)Climate change has a global impact and is increasingly affecting our environment. This is driving the continuous expansion of renewable energies, with wind energy playing a major role. As wind energy becomes more widespread, an increasing number of people will live near wind turbines in complex terrain. In such scenarios, wind turbines are often positioned at elevated locations, while residents live in valleys. In complex terrain, such as a steep escarpment, local turbulence, wind speed, and direction are strongly influenced by topography, contributing to the complexity of sound propagation or impacts the background noise situation in valleys, for example, due to shielding effects. The operation of wind turbines is associated with both visual and sound-related impact, with sound being generated at various frequencies. There is a growing interest in low-frequency sound and infrasound, characterized by long wavelengths that propagate over considerable distances without significant attenuation. This is in contrast to higher-frequency sound, and might increase the impact of wind turbine sound at residential areas located several hundred meters or a few kilometers away from the wind farm. In the context of complex terrain, this work investigates wind turbines in complex terrain as sources of low-frequency sound and infrasound. The investigations on characterization of sound generation and propagation are based on measurements in the vicinity of two wind farms. Measurements were conducted within four measurement campaigns at two wind farms located close to an escarpment at the Swabian Alb in Southern Germany over a period of about nine month. Acoustic data was obtained in the proximity of the wind turbines and at residential buildings in 1–1.7km distance to the wind farms in municipalities located within a valley. Besides acoustic measurements including the infrasonic frequency range, a comprehensive data set with ground motion data, wind turbine operating data, meteorological data and data from a noise reporting app supports the investigation. Two aspects require analysis: Firstly, the aspect of generation and propagation of wind turbine low-frequency sound and infrasound in complex terrain, and secondly, the relation with annoyance. Results show that sounds within the infrasonic range assigned to the blade passage at the tower are transmitted through the air over distances of 1 km. Low-frequency sounds were found to be amplitude-modulated and were investigated as amplitude modulation. Infrasound and amplitude modulation occurrences were more likely during morning, evening and night hours and during atmospheric conditions with positive lapse rate, vertical wind shear and low turbulence intensity. The occurrence of both infrasound and amplitude modulation was typically observed during rated rotational speed but below-rated power. To allow predictions, a standard prediction method was extended to include the lowfrequency sound and infrasound range and adapted to the measurement data in order to apply it to complex terrain. The sound level difference of the measured data aligns well with the predictions within the frequency range of 8 Hz and 250 Hz. Investigations regarding outdoor-to-indoor sound reductions showed influences from structural resonances and room modes, which depend on the characteristics of the building and the specific room under investigation. Combining acoustic measurements with annoyance reports showed that rated wind turbine operation appears to be a contributing factor in annoyance ratings obtained through a noise reporting app, ranging from “somewhat” to “very” levels. Furthermore, the analysis indicates that varying levels of annoyance at a distance of 1km from the wind farm, both outside and inside buildings, do not correspond to significant differences in the averaged and A-weighted sound pressure levels. Overall, this work contributes to a better understanding of the low-frequency sound and infrasound generated from wind turbines and provides insight into the sound characteristics of measured wind turbine sound at residential locations in complex terrains.Item Open Access Comparison of feedforward and model predictive control of wind turbines using LIDAR(2012) Schlipf, David; Pao, Lucy Y.; Cheng, Po WenLIDAR systems are able to provide preview information of wind disturbances at various distances in front of wind turbines. This technology paves the way for new control concepts such as feedforward control and model predictive control. This paper compares a nonlinear model predictive controller and a feedforward controller to a baseline controller. Realistic wind "measurements" are obtained using a detailed simulation of a LIDAR system. A full lifetime comparison shows the advantages of using the wind predictions to reduce wind turbine fatigue loads on the tower and blades as well as to limit the blade pitch rates. The results illustrate that the feedforward controller can be combined with a tower feedback controller to yield similar load reductions as the model predictive controller.Item Open Access Application-specific UML profiles for multidisciplinary product data integration(2011) Reichwein, Axel; Rudolph, Stephan (Priv.Doz. Dr.-Ing.)This thesis examines the suitability of the UnifiedModeling Language (UML) to establish a central product model for multidisciplinary product data integration. Computer-aided product design involves the use of specialized discipline-specific software applications in order to model and simulate various product aspects. Dependencies between models are thereby frequent as the same product information often appears redundantly in various engineering models. In addition, dependencies exist due to relationships between distinct features of various models. As a result, model modifications frequently require the update of dependent models. Data consistency between models is achieved automatically through model-to-model data exchange software. The use of a central product model enables to reduce the required number of data exchange connections. Central product models store product information which is spread across several models and achieve data consistency through data exchange connections between themselves and specific models as in a hub-and-spoke network. Central product models are especially useful for automatic data consistency in design scenarios which include a high number of inter-model dependencies and model modifications. The integration of geometry and therefrom derived models such as structural analysis or computational fluid dynamics models has already been successfully addressed in numerous central product models. However, the multidisciplinary integration of more diverse models, such as geometric, software, controller and multibody system models, currently presents a challenge. Although several central product models have been developed for multidisciplinary design, none has yet gained, in contrast to geometry-focused central product models, wide acceptance nor reached the status of an international standard. The unmanageable high number of diverse discipline- and application-specific modeling concepts hinders the development of a standardized holistic central product representation. This thesis investigates the possibility of establishing an interdisciplinary central product model based on the common modular structure of models from various disciplines. Most models which are edited with current state-of-the-art software applications are composed of modular components in order to support the exchange and reuse of model information. Models from different disciplines therefore share common modeling concepts for the specification of modular model components. However, there is yet no overarching modeling standard to describe the common characteristics of modular model components from various disciplines. Object-oriented modeling concepts currently mainly describe software modules called objects. Object-oriented modeling concepts are generic and can be used to represent modular components in general. The Unified Modeling Language (UML) has been since its emergence in 1997 the de facto standard for object-oriented modeling. This thesis examines the use of the object-oriented modeling concepts of the UML to uniformly describe widely used application-specific geometric, dynamic and multibody system models in a central product model. Application-specific model information was represented in UML through generic UML modeling concepts in combination with lightweight UML extensions in the form of stereotypes. UML profiles regrouped stereotypes which corresponded to a specific modeling application. The automatic translation of UML model information into the specific models and vice versa was implemented in order to test and validate the application-specific UML profiles. The UML-based central product model was used in several test cases to automatically generate consistent models for the simulation and evaluation of various product configurations. The test cases included models for the simulation of slider-crank mechanisms, the evaluation of cabin pressure control systems, the design of conveyor system configurations, the evaluation of satellite configurations and the generation of customized aircraft geometry. The workflows within the test cases included the automatic creation and modification of UML models as well as the invocation of data exchange connections. The workflows were described in executable UML activity diagrams or Java programs. The thesis demonstrates that the UML can be used beyond conventional software modeling to establish a central holistic product representation. The modeling concepts of geometric, dynamic and multibody system models were translated mostly according to one-to-one mappings into corresponding UML modeling concepts with their respective stereotype. As a result, the specific model information is easily recognizable in the UML-based central product model. Furthermore, the use of a UML-based central product model is facilitated for the many modelers who are already familiar with the widespread and standardized UML modeling language.Item Open Access A MATLAB toolbox for the Scintrex CG-5 gravimeter at GIS(2017) Gu, SiyunThis thesis is about a MATLAB toolbox for the Scintrex CG-5 gravimeter. The aim of this toolbox is to offer a basic data process for gravity measurement, which is compatible for most applications in geodesy. In particular, the toolbox covers: 1. data selection, 2. adjustment, 3. gravity gradient computation, 4. gravity visualization, 5. calibration factor estimation. A graphical user interface enables users without deeper programming knowledge to operate this toolbox and obtain the results like adjusted values or figures.