M. Tech. Digital Technology. / This dissertation reports on an optical-based two-dimensional position sensor for use in Active Magnetic Bearings (AMB) to measure the position of the levitated rotor. The motivation for the deployment of optical technology is the well-known advantage of high precision contactless displacement measurement. The radial and axial edges of the rotor are illuminated by red and green laser beams respectively. The position of the rotor is determined from its image projected on a Charge Coupled Device (CCD) sensor. The measuring principle is demonstrated as a position sampler in the closed loop control of an active magnetic bearing model. The image representing the position is processed with a real-time algorithm on a Field Programmable Logic Gate Array. The principle of operation of a CCD as a position sensor is analysed in order to establish how the image captured by the CCD can be processed to determine the position of the rotor. A simple AMB is modelled in which the sensor acts as a feedback position device. The main objective of the model is to evaluate the accuracy of the system. The purpose of the overall sensing technique to be used is to achieve highly accurate and precise measurements with CCD-based optical metrology.

Although inductively coupled plasma mass spectrometry (ICP-MS) is generally considered a reliable analytical technique, increasing demands on its capabilities require continued research and improvements. ICP-MS is susceptible to both matrix effects and drift, leading to a decline in accuracy and precision. A number of techniques are routinely used to compensate for these issues. Internal standardization is one such solution that requires relatively simple sample preparation and yet offers the possibility of improving both accuracy and precision. In order to be effective, an optimal analyte/internal standard pair must be chosen. Traditionally, analyte/internal standard pairs are chosen based on similarities in mass and/or ionization potential. The present studies sought to develop a program that determined standards based on the minimization of analytical error. 102 masses were monitored over 27 perturbations, i.e., changes to sample matrix and operating parameters. The standard deviations of the analyte/internal standard ratios were then used as a measure of internal standard performance. A thorough statistical analysis was conducted to determine trends between a good analyte/internal standard pair and similarities in chemical property. Similarities in mass offered the strongest relationship to a good internal standard choice, although many exceptions existed. The program was then tested over time and multiple instrument optimizations as well as on a completely different ICP-MS instrument. Results of these tests suggest that the data originally collected for the prediction program is not instrument-specific and thus provided a broader base of useful applications. Due to its unmatched sensitivity and multielement capabilities, ICP-MS is frequently utilized for biological samples. A more recent application, however, seeks to use ICPMS for the purpose of determining specific associations between metals and proteins. Such speciation requires a high resolution and reproducible separation prior to ICPMS analysis. Gel electrophoresis offers good separation and is well matched with the scanning properties of laser ablation sample introduction. The present study utilized native gel electrophoresis coupled with a uniquely modified electroblot system to improve sensitivity and to elucidate additional information. Chemically modified quartz fiber filters were successfully used as the transfer membrane to improve protein and metal capture efficiency. / text

WINDMI is a low dimensional plasma physics-based model of the coupled magnetosphere-ionosphere system. The nonlinear system of ordinary differential equations describes the energy balance between the basic nightside components of the system using the solar wind driving voltage as input. Of the eight dynamical variables determined by the model, the region 1 field aligned current and ring current energy is compared to the westward auroral electrojet AL index and equatorial geomagnetic disturbance storm time Dst index. The WINDMI model is used to analyze the magnetosphere-ionosphere system during major geomagnetic storms and substorms which are community campaign events. Numerical experiments using the WINDMI model are also used to assess the question of how much interplanetary shock events contribute to the geoeffectiveness of solar wind drivers. For two major geomagnetic storm intervals, it is found that the magnetic field compressional jump is important to producing the changes in the AL index. Further, the WINDMI model is implemented to compute model AL and Dst predictions every ten minutes using real-time solar wind data from the ACE satellite as input. Real-Time WINDMI has been capturing substorm and storm activity, as characterized by the AL and Dst indices, reliably since February 2006 and is validated by comparison with ground-based measurements of the indices. Model results are compared for three different candidate input solar wind driving voltage formulas. Modeling of the Dst index is further developed to include the additional physical processes of tail current increases and sudden commencement. A new model, based on WINDMI, is developed using the dayside magnetopause and magnetosphere current systems to model the magnetopause boundary motion and the dayside region 1 field aligned current which is comparable to the auroral upper AU index. / text

Σε αυτήν την εργασία μελετήθηκε και σχεδιάστηκε ένας ψηφιακά ελεγχόμενος ταλαντωτής (DCO) με σκοπό GSM εφαρμογή. Οι συχνότητες λειτουργίας κυμαίνονται στο φάσμα 1.6GHz – 2GHz με βήμα 20kHz. Ο θόρυβος φάσης ποσοτικοποιείται στα -160dB/Hz σε 20 MHz απόκλιση. Ο έλεγχος του DCO γίνεται πλήρως ψηφιακά επιτρέποντας την υλοποίηση πλήρους ψηφιακού βρόχου κλειδώματος φάσης (ADPLL) και καθολικού system on chip design (SoC). Ο ταλαντωτής καταναλώνει 4,5 mWatt με 3,76 mA ρεύμα σε 1.2 V τροφοδοσία. / A Digitally Controlled Oscillator is studied and designed for GSM application. The operating frequencies are 1.6-2GHz with tuning range of 400MHz and finest step size 20 KHz. A fully digital control is achieved form where arises the opportunity for fabrication of an All-Digital Phase Locked Loop (ADPLL) and the whole system on chip (SoC). The proposed DCO core consumes 3.76mA from a 1.2V supply.

Τις τελευταίες δεκαετίες, οι διεργασίες πλάσματος με τάση διέγερσης ραδιοσυχνότητας χρησιμοποιούνται ολοένα και περισσότερο και απαντώνται σε διάφορες εφαρμογές όπως στην εναπόθεση υλικών, στην επεξεργασία επιφανειών κα. Αυτό έχει ως αποτέλεσμα οι εκκενώσεις αίγλης ραδιοσυχνότητας να προσελκύσουν έντονο επιστημονικό ενδιαφέρον. Μπορεί τα τελευταία χρόνια να έχει σημειωθεί σημαντική πρόοδος στον τομέα αυτό ωστόσο υπάρχει ακόμα και σήμερα ενδιαφέρον που αφορά το σχεδιασμό των συστημάτων αυτών καθώς και την ανάπτυξη μεθόδων που αφορούν την επαναληψιμότητα των διεργασιών καθώς και τον έλεγχο των ιδιοτήτων του πλάσματος. Ένας από αυτούς τους τομείς είναι ο ηλεκτρικός χαρακτηρισμός ηλεκτροδίων ραδιοσυχνότητας πηγών πλάσματος και η εύρεση της κατανεμημένης εμπέδησής τους και ακολούθως ο υπολογισμός της καταναλισκόμενης ισχύος σε εκκενώσεις αίγλης. Αυτές οι τεχνικές μπορούν να μας προσφέρουν σημαντικές πληροφορίες για τους μηχανισμούς και τα φαινόμενα που λαμβάνουν χώρα σε εκκενώσεις ραδιοσυχνότητας, οι οποίες αν στη συνεχεία αξιοποιηθούν να μας οδηγήσουν στον ακριβή προσδιορισμό και έλεγχο των συνθηκών. Στην εργασία αυτή αναλύονται μέθοδοι από τις οποίες προκύπτουν αποτελέσματα που αφορούν παραμέτρους του πλάσματος μέσω μετρήσεων τάσης, ρεύματος και διαφοράς φάσης σε κάποιο σημείο εξωτερικά του αντιδραστήρα. Παρουσιάζονται τα αποτελέσματα ηλεκτρικών μετρήσεων σε εκκενώσεις αργού που πραγματοποιήθηκαν σε μια χωρητικά συζευγμένη πηγή πλάσματος. Αρχικά παρουσιάζεται ο ηλεκτρικός χαρακτηρισμός της πηγής και αναλύονται τρεις μέθοδοι για τη μέτρηση και τον υπολογισμό της καταναλισκόμενης ισχύος της εκκένωσης. Στην πρώτη μέθοδο οι ηλεκτρικές μετρήσεις χρησιμοποιούνται για το προσδιορισμό ενός ισοδύναμου ηλεκτρικού κυκλώματος με κατανεμημένα στοιχεία (πυκνωτές, πηνία αντιστάσεις) το οποίο μπορεί να περιγράψει την εμπέδηση ανάμεσα στο σημείο μέτρησης εξωτερικά του αντιδραστήρα και την επιφάνεια του ηλεκτροδίου ραδιοσυχνότητας. Το ισοδύναμο αυτό κύκλωμα επιλύεται με βάση τους κανόνες του Kirchhoff και προκύπτουν οι τιμές της μιγαδικής τάσης και ρεύματος της εκκένωσης. Στη δεύτερη μέθοδο, η τάση καθώς και το ρεύμα της εκκένωσης υπολογίζονται μέσω ενός πίνακα ABCD, τα στοιχεία του οποίου έχουν υπολογιστεί από μετρήσεις σε ανοικτό και βραχυκυκλωμένο κύκλωμα. Η τρίτη μέθοδος, μοιάζει αρκετά με τη δεύτερη μόνο που έχει το πλεονέκτημα να είναι πιο απλή λόγω του ότι δεν απαιτεί τη μέτρηση της φάσης της εμπέδησης (της φάσης της τάσης σε σχέση με την τάση του ρεύματος). / Over the last decades, plasma processing has been widely used in various applications such as the deposition of thin films, surface modification, dry etching etc. As a result, radio-frequency discharges have attracted particular scientific interest. Despite the steps forward, there are still open issues especially concerning the design of plasma systems and the effective control of plasma parameters. A part of these issues is related to the electrical characterization of the stray impedance of the plasma electrode and the subsequent measurement and calculation of the real power consumption during the process. These techniques can lead to better understanding of the plasma processes and can also lead to more stable, reliable and almost ideal performing plasma systems. The aim of this study is to point out externally measured non-intrusive plasma parameters that could ease design, control and transferability of plasma conditions. In this work we demonstrate results of electrical characteristics of argon discharges carried out in a high vacuum capacitively coupled parallel plate reactor. Initially, the electrical characterization of the plasma reactor is presented and three methods for measuring and calculating the real power consumed in the discharge are analyzed.. At the first method, the electrical measurements are used to determine a simple equivalent circuit that can describe the parasitic impedances that interfere between the point of measurement and the RF electrode’s surface. The equivalent circuit model is then solved through Kirchhoff’s laws and values of the complex electrode’s voltage and current are obtained from the measured voltage and current at some point located outside the reactor. At the second method, the reactor is treated as a two-port network. The electrode’s voltage and current are calculated through the ABCD matrix of the reactor whose values a, b, c, d are extracted from open and short circuit measurements. The third method is a simplification of the second method as it does not require the phase of the impedance (the phase of the voltage relative to the current) for the calculations.

Da geologische Störungen können als Grundwasserleiter, -Barrieren oder als gemischte leitende /stauende Fluidsysteme wirken. Aufgrund dessen können Störungen maßgeblich den Grundwasserfluss im Untergrund beeinflussen, welcher deutliche Veränderungen des tiefen thermischen Feldes bewirken kann. Grundwasserdynamik und Temperaturveränderungen sind wiederum entscheidende Faktoren für die Exploration geothermischer Energie. Diese Studie untersuchte den Einfluss von Störungen auf das Fluidsystem und das thermische Feld im Untergrund. Sie erforschte die physikalischen Prozesse, welche das Fluidverhalten und die Temperaturverteilung in Störungen und in den umgebenden Gesteinen. Dazu wurden 3D Finite Elemente Simulationen des gekoppelten Fluid und Wärmetransports für synthetische sowie reale Modelszenarien auf unterschiedlichen Skalen durchgeführt. Um den Einfluss einer schräg einfallenden Störung systematisch durch die schrittweise Veränderung der hydraulischen Öffnungsweite und der Permeabilität, zu untersuchen, wurde ein klein-skaliges synthetisches Modell entwickelt. Ein inverser linearer Zusammenhang wurde festgestellt, welcher zeigt, dass sich die Fluidgeschwindigkeit in der Störung jeweils um ~1e-01 m/s verringert, wenn die Öffnungsweite der Störung um jeweils eine Magnitude vergrößert wird. Ein hoher Permeabilitätskontrast zwischen Störung und umgebender Matrix begünstigt die Fluidadvektion hin zur Störung und führt zu ausgeprägten Druck- und Temperaturveränderungen innerhalb und um die Störung herum. Bei geringem Permeabilitätskontrast zwischen Störung und umgebendem Gestein findet hingegen kein Fluidfluss in der Störung statt, wobei das hydrostatische Druck- sowie das Temperaturfeld unverändert bleiben. Auf Grundlage der synthetischen Modellierungsergebnisse wurde der Einfluss von Störungen auf einer größeren Skala anhand eines komplexeren (realen) geologischen Systems analysiert. Dabei handelt es sich um ein 3D Modell des Geothermiestandortes Groß Schönebeck, der ca. 40 km nördlich von Berlin liegt. Die Integration von einer permeablen und drei impermeablen Hauptstörungen, zeigte unterschiedlich starke Einflüsse auf Fluidzirkulation, Temperatur – und Druckfeld. Die modellierte konvektive Zirkulation in der permeablen Störung verändert das thermische Feld stark (bis zu 15 K). In den gering durchlässigen Störungen wird die Wärme ausschließlich durch Diffusion geleitet. Der konduktive Wärmetransport beeinflusst das thermische Feld nicht, bewirkt jedoch lokale Veränderungen des hydrostatischen Druckfeldes. Um den Einfluss großer Störungszonen mit kilometerweitem vertikalen Versatz auf das geothermische Feld der Beckenskala zu untersuchen, wurden gekoppelte Fluid- und Wärmetransportsimulationen für ein 3D Strukturmodell des Gebietes Brandenburg durchgeführt (Noack et al. 2010; 2013). Bezüglich der Störungspermeabilität wurden verschiedene geologische Szenarien modelliert, von denen zwei Endgliedermodelle ausgewertet wurden. Die Ergebnisse zeigten, dass die undurchlässigen Störungen den Fluidfluss nur lokal beeinflussen. Da sie als hydraulische Barrieren wirken, wird der Fluidfluss mir sehr geringen Geschwindigkeiten entlang der Störungen innerhalb eines Bereichs von ~ 1 km auf jeder Seite umgelenkt. Die modellierten lokalen Veränderungen des Grundwasserzirkulationssystems haben keinen beobachtbaren Effekt auf das Temperaturfeld. Hingegen erzeugen permeable Störungszonen eine ausgeprägte thermische Signatur innerhalb eines Einflussbereichs von ~ 2.4-8.8 km in -1000 m Tiefe und ~6-12 km in -3000 m Tiefe. Diese thermische Signatur, in der sich kältere und wärmere Temperaturbereiche abwechseln, wird durch auf- und abwärts gerichteten Fluidfluss innerhalb der Störung verursacht, der grundsätzlich durch existierende Gradienten in der hydraulischen Druckhöhe angetrieben wird. Alle Studien haben gezeigt, dass Störungen einen beachtlichen Einfluss auf den Fluid-, und Wärmefluss haben. Es stellte sich heraus, dass die Permeabilität in der Störung und in den umgebenden geologischen Schichten so wie der spezifische geologische Rahmen entscheidende Faktoren in der Ausbildung verschiedener Wärmetransportmechanismen sind, die sich in Störungen entwickeln können. Die von permeablen Störungen verursachten Temperaturveränderungen können lokal, jedoch groß sein, genauso wie die durch hydraulisch leitende und nichtleitende Störungen hervorgerufenen Veränderungen des Fluidystems. Letztlich haben die Simulationen für die unterschiedlich skalierten Modelle gezeigt, dass die Ergebnisse sich nicht aufeinander übertragen lassen und dass es notwendig ist, jeden geologischen Rahmen hinsichtlich Konfiguration und Größenskala gesondert zu betrachten. Abschließend hat diese Studie demonstriert, dass die Betrachtung von Störungen in 3D Finiten Elementen Modellen für die Simulation von gekoppeltem Fluid- und Wärmetransport auf unterschiedlichen Skalen möglich ist. Da diese Art von numerischen Simulationen sowohl die geologische Struktur des Untergrunds sowie die im Erdinnern ablaufenden physikalischen Prozesse integriert, können sie einen wertvollen Beitrag leisten, indem sie Feld- und Laborgestützte Untersuchungen vervollständigen. / Faults can act as conduits, barriers or mixed conduit/barrier systems to fluid flow. Therefore, faults may significantly influence fluid flow regimes operating in the subsurface, possibly resulting in distinct variations of the deep thermal field. Both, flow dynamics and temperature changes are in turn crucial factors that need to be taken into account for geothermal energy exploration. This study investigated the influence of faults on the subsurface fluid system and thermal field and explored the processes controlling fluid behavior and thermal distribution both within host rocks and faults. For this purpose, 3D finite element simulations of coupled fluid and heat transport have been carried out, both for synthetic and real-case model scenarios on different scales. A small-scale synthetic model was developed to systematically assess the impact of an inclined fault by changing gradually its hydraulic width and its permeability within the simulations. An observed linear inverse relationship revealed that changing the fault width by one order of magnitude results in a fluid velocity decrease (~1e-01 m/s) within the fault. A high permeability contrast between fault and matrix favors fluid advection into the fault and leads to pronounced pressure and temperature changes in and around the same domain. When the permeability contrast between fault domain and host rock is low, however, no fluid flow is observed in the fault, thus resulting in undisturbed hydrostatic pressure and temperature fields. On the basis of these synthetic fault modelling results, the influence of faults on a larger scale have been analyzed within a more complex (real-case) geological setting,- a 3D model of the geothermal site Groß Schönebeck / located ~40 km north of Berlin. The integration of one permeable and three impermeable major faults, resulted in distinct changes observed in the local fluid circulation, thermal and pressure field. Modelled convective circulation within the permeable fault decisively modifies the thermal field (up to 15 K). Within the low permeable faults, heat is transferred only by conduction, inducing no thermal imprint but local deviations of the hydrostatic pressure field. To investigate the impact of major fault zones on the basin-scale geothermal field, coupled fluid and heat transport simulations have been conducted for a 3D structural model for Brandenburg region (Noack et al. 2010; 2013). Different geological scenarios in terms of modelled fault permeability have been carried out of which two end member models are analyzed. The results showed that tight fault zones affect the flow field locally. Acting as hydraulic barriers, fluid flow is deviated with very low velocities along them within a range of ~ 1 km on either sides. The modelled local changes in the groundwater circulation system have no considerable effect on the temperature field. By contrast, permeable fault zones induce a pronounced signature on the thermal field extending over a distance of ~ 2.4-8.8 km at -1000 m depth and ~6-12 km at -3000 m depth. This thermal signature, characterized by alternating cooler and hotter temperature domains, is controlled by up- and downward directed flow within the fault domain, principally driven by existing hydraulic head gradients. All studies demonstrated that faults have a considerable impact on the fluid and heat flow. The permeability in faults and surrounding geological layers as well as the specific geological setting turned out to be crucial factors in controlling the different kinds of heat transfer mechanisms that may evolve in faults. Temperature variations caused by permeable faults may be local but significant as well as changes in fluid dynamics by both conduits and barriers. Thus, the results demonstrated the importance to consider faults in geothermal energy exploration. In the final analysis, the simulations for the small-, regional- and basin-scale models showed that the outcomes cannot be transferred by upscaling and that it is necessary to consider each geological setting separately with respect to its configuration and scale dimension. In summary, this study demonstrated that the consideration of faults in 3D finite element models for coupled fluid and heat transport simulations on different scales is feasible. As these type of numerical simulations integrate both, the structural setting of the subsurface and the physical processes controlling subsurface transport, the outcomes of this thesis may provide positive contributions in that they valuably complement field- and laboratory-based investigations.

Cerebral ischemia is the principal cause of morbidity and mortality worldwide. In addition to neuronal loss associated with hypoxic-ischemic damage, cerebral ischemia is characterized by a neuromicrovascular injury. Nitrative stress and lipid peroxidation increase in hypoxic-ischemic damages and play an essential role in neuromicrovascular injury leading to cerebral ischemia. We hypothesized that newly described lipid peroxidation products, termed trans-arachidonic acids (TAA), could be implicated in the pathogenesis of hypoxia-ischemia by affecting the cerebral vasomotricity and microvascular integrity. / The effects of TAA on neuromicrovascular tone were tested ex vivo by monitoring the changes in vascular diameter of rat cerebral pial microvessels. Four isomers of TAA, namely 5 E-AA, 8E-AA, IIE-AA and 14 E-AA induced an endothelium-dependent vasorelaxation. Possible mechanisms involved in TAA-induced vasorelaxation were thoroughly investigated. Collectively, data enclosed revealed that TAA induce cerebral vasorelaxation through the interactive activation of BKCa channels with heme oxygenase-2. This interaction leads to generation of carbon monoxide which in turn activates soluble guanylate cyclase and triggers vasorelaxation. / Chronic effects of TAA on microvascular integrity were examined by generating a unilateral hypoxic-ischemic (HI) model of cerebral ischemia on newborn rat pups. Our HI model showed microvascular degeneration as early as 24h post-HI, preceded by an increase in cerebral TAA levels. HI-induced microvascular lesions were dependent on nitric oxide synthase activation and ensued TAA formation. Although the molecular mechanisms leading to TAA-induced microvascular degeneration were, in part uncovered for the retina, the primary site of action of TAA remains unknown. We demonstrated that TAA binds and activates GPR40 receptor, a newly described free fatty acid receptor. Importantly, GPR40 receptor knock-out prevents TAA-induced reduction in cerebral microvascular density and limits HI-induced brain infarct.

Le facteur de l’ADP-ribosylation 6 (ARF6) et Rac1 sont des petites protéines liant le GTP qui régulent plusieurs voies de signalisation comprenant le trafic de vésicules, la modification des lipides membranaires et la réorganisation du cytosquelette d’actine. Cependant, les mécanismes moléculaires par lesquels ARF6 et Rac1 agissent de concert afin de contrôler ces différents processus cellulaires restent méconnus. Dans cette étude, nous montrons que, dans les cellules HEK293, ARF6 et Rac1 sont retrouvées en complexe suite à la stimulation du récepteur à l’angiotensine. Des expériences réalisées in vitro nous indiquent que ces deux GTPases interagissent ensemble directement, et que ARF6 s’associe préférentiellement avec la forme inactive de Rac1. L’inhibition de l’expression de ARF6 par interférence à l’ARN entraîne une activation marquée en cellule de Rac1 via le facteur PIX, indépendamment de la stimulation d’un récepteur, ce qui provoque la migration non contrôlée des cellules. Les arrestines, protéines de régulation de la désensibilisation des récepteurs couplés aux protéines G, servent de protéines d’échafaudage pour Rac1 et ARF6, en interagissant directement avec les GTPases et en augmentant leur association stimulée par l’angiotensine. De plus, les arrestines permettent l’activation, en s’en dissociant, de la MAP Kinase p38 qui régule l’activité de ARF6 et son interaction précoce avec les arrestines. Mis ensemble, ces résultats montrent que les arrestines contrôlent l’activité de ARF6, en influençant p38. ARF6 joue un rôle inhibiteur sur l’activation basale de Rac1 pour permettre ensuite son recrutement et son activation dépendante de l’angiotensine. Cette étude nous a permis de préciser le mode de régulation mis en jeu dans l’initiation de la migration cellulaire, suite à l’activation d’un récepteur couplé aux protéines G. Par le fait même, nous avons identifié certains des acteurs impliqués dans ce processus, offrant ainsi de nouvelles cibles pour le traitement des déséquilibres pathophysiologiques de la migration cellulaire. / The ADP-ribosylation factor 6 (ARF6) and Rac1 are small GTP-binding proteins that regulate several signaling events ranging from vesicle trafficking, to modification of membrane lipids and reorganization of the actin cytoskeleton. However, the molecular mechanisms by which ARF6 and Rac1 act in concert to control these different cellular processes remain unclear. Here, we show that in HEK 293 cells, ARF6 and Rac1 can be found in complex upon stimulation of the angiotensin receptor (ATR). In vitro experiments indicate that these two small G proteins can directly interact together, and that ARF6 preferentially interacts with the GDP-bound form of Rac1. Depletion of ARF6 by RNA interference leads to a marked PIX-dependent Rac1 activation in cells, independently of receptor stimulation, leading to uncontrolled cell migration. Arrestins, which are known for their role in G protein-coupled receptor desensitization, act as scaffold proteins toward Rac1 and ARF6, by directly interacting with the GTPases and by increasing their agonist-promoted association. Besides, arrestins allow p38 MAP Kinase activation, by releasing it, which regulates ARF6 activity and early association occurring between arrestins and ARF6. Taken together, this study shows that arrestins control ARF6 activity, by managing p38. ARF6 is an inhibitor of basal Rac1 activation to further allow the protein to be recruited and activated following angiotensin treatment. This study allowed us to precise how cell migration induction is regulated following G protein-coupled receptor activation. As a result, we identified some of the key players implicated in this process, providing new targets in the treatment of patho-physiological inbalance in cell migration.

Steel Catenary Riser (SCR) is a popular solution for a floating production facility in the deep and ultra-deep ocean. In the analysis of SCR, the behavioral characteristics are investigated to check the failure modes by assessing the magnitude and the frequency of the stress and strain which SCR goes through in time series. SCR is affected by the motions of connected floating production facility and exciting environmental loads. The driven force and motion of SCR has an interaction with seabed soil which represents the stiffness and friction force where SCR touches the seabed. Dynamic response of SCR is primarily caused by the coupled motion of floating structure. The displacement of floating structure is often large and fast enough to cause short cycles of negative and positive tension on SCR. The interaction between SCR and seabed is concentrated at the touchdown zone resulting into the compression and corresponding deformation of pipeline at the position. This paper presents models of floating production facilities and connected mooring lines and SCRs in 100-year hurricane environmental loads and seabed, focusing on the motional characteristics of SCR at the touchdown zone. In time series simulation, the model of SCR is first analyzed as a pipeline with indefinite elasticity so that the SCR does not fail even if the exciting loads exceed the property limit of SCR. Then the SCR design is manually checked using criteria for each failure mode to estimate the integrity.

The thesis describes development and application of coupled resonant coil sensors, which is of growing interest for remote monitoring applications. An interrogation technique, which improves the accuracy and interrogation range of coupled resonant coil sensors, is introduced. The method uses time-domain gating to produce measurements that are dominated by the response of the sensor coil and are immune to surrounding object interference. For application in structural health monitoring a low cost embeddable coupled coil sensor, which is able to monitor the corrosion potential of reinforcement steel is presented. Results of an accelerated corrosion test using the sensor indicate that corrosion potential can be monitored with a resolution less than 10 mV and a sensitivity of 0.76 kHz/mV. The last part describes a coupled-coil pH sensor based on pH electrode potential measurement. A linear response over a 4 to 10 pH dynamic range and 50 kHz/pH sensitivity are achieved with a 0.1 pH resolution and 30 s response time.