Engineering Complex Computational Ecosystems

Self-organising pervasive ecosystems of devices are set to become a major vehicle for delivering infrastructure and end-user services. The inherent complexity of such systems poses new challenges to those who want to dominate it by applying the principles of engineering. The recent growth in number and distribution of devices with decent computational and communicational abilities, that suddenly accelerated with the massive diffusion of smartphones and tablets, is delivering a world with a much higher density of devices in space. Also, communication technologies seem to be focussing on short-range device-to-device (P2P) interactions, with technologies such as Bluetooth and Near-Field Communication gaining greater adoption. Locality and situatedness become key to providing the best possible experience to users, and the classic model of a centralised, enormously powerful server gathering and processing data becomes less and less efficient with device density. Accomplishing complex global tasks without a centralised controller responsible of aggregating data, however, is a challenging task. In particular, there is a local-to-global issue that makes the application of engineering principles challenging at least: designing device-local programs that, through interaction, guarantee a certain global service level. In this thesis, we first analyse the state of the art in coordination systems, then motivate the work by describing the main issues of pre-existing tools and practices and identifying the improvements that would benefit the design of such complex software ecosystems. The contribution can be divided in three main branches. First, we introduce a novel simulation toolchain for pervasive ecosystems, designed for allowing good expressiveness still retaining high performance. Second, we leverage existing coordination models and patterns in order to create new spatial structures. Third, we introduce a novel language, based on the existing ``Field Calculus'' and integrated with the aforementioned toolchain, designed to be usable for practical aggregate programming.

Nahfeld-induzierte Elektronenemissions-Mikrospektroskopie an stark gekoppelten Plasmonen und metallischen Mikrostrukturen

Plasmonen stellen elektromagnetische Moden in metallischen Strukturen dar, in denen die quasifreien Elektronen im Metall kollektiv oszillieren. Während des letzten Jahrzehnts erfuhr das Gebiet der Plasmonik eine rasante Entwicklung, basierend auf zunehmenden Fortschritten der Nanostrukturierungsmethoden und spektroskopischen Untersuchungsmethoden, die zu der Möglichkeit von systematischen Einzelobjektuntersuchungen wohldefinierter Nanostrukturen führte. Die Anregung von Plasmonen resultiert neben einer radiativen Verstärkung der optischen Streuintensität im Fernfeld in einer nicht-radiativen Überhöhung der Feldstärke in unmittelbarer Umgebung der metallischen Struktur (Nahfeld), die durch die kohärente Ladungsansammlung an der metallischen Oberfläche hervorgerufen wird. Das optische Nahfeld stellt folglich eine bedeutende Größe für das fundamentale Verständnis der Wirkung und Wechselwirkung von Plasmonen sowie für die Optimierung plasmonbasierter Applikationen dar. Die große Herausforderung liegt in der Kompliziertheit des experimentellen Zugangs zum Nahfeld, der die Entwicklung eines grundlegenden Verständisses des Nahfeldes verhinderte.rnIm Rahmen dieser Arbeit wurde Photoemissionselektronenmikroskopie (PEEM) bzw. -mikrospektroskopie genutzt, um ortsaufgelöst die Eigenschaften nahfeld-induzierter Elektronenemission zu bestimmen. Die elektrodynamischen Eigenschaften der untersuchten Systeme wurden zudem mit numerischen, auf der Finiten Integrationsmethode basierenden Berechnungen bestimmt und mit den experimentellen Resultaten verglichen.rnAg-Scheiben mit einem Durchmesser von 1µm und einer Höhe von 50nm wurden mit fs-Laserstrahlung der Wellenlänge 400nm unter verschiedenen Polarisationszuständen angeregt. Die laterale Verteilung der infolge eines 2PPE-Prozesses emittierten Elektronen wurde mit dem PEEM aufgenommen. Aus dem Vergleich mit den numerischen Berechnungen lässt sich folgern, dass sich das Nahfeld an unterschiedlichen Stellen der metallischen Struktur verschiedenartig ausbildet. Insbesondere wird am Rand der Scheibe bei s-polarisierter Anregung (verschwindende Vertikalkomponente des elektrischen Felds) ein Nahfeld mit endlicher z-Komponente induziert, während im Zentrum der Scheibe das Nahfeld stets proportional zum einfallenden elektrischen Feld ist.rnWeiterhin wurde erstmalig das Nahfeld optisch angeregter, stark gekoppelter Plasmonen spektral (750-850nm) untersucht und für identische Nanoobjekte mit den entsprechenden Fernfeldspektren verglichen. Dies erfolgte durch Messung der spektralen Streucharakteristik der Einzelobjekte mit einem Dunkelfeldkonfokalmikroskop. Als Modellsystem stark gekoppelter Plasmonen dienten Au Nanopartikel in sub-Nanometerabstand zu einem Au Film (nanoparticle on plane, NPOP). Mit Hilfe dieser Kombination aus komplementären Untersuchungsmethoden konnte erstmalig die spektrale Trennung von radiativen und nicht-radiativen Moden stark gekoppelter Plasmonen nachgewiesen werden. Dies ist insbesondere für Anwendungen von großer Relevanz, da reine Nahfeldmoden durch den unterdrückten radiativen Zerfall eine große Lebensdauer besitzen, so dass deren Verstärkungswirkung besonders lange nutzbar ist. Ursachen für die Unterschiede im spektralen Verhalten von Fern- und Nahfeld konnten durch numerische Berechnungen identifiziert werden. Sie zeigten, dass das Nahfeld nicht-spärischer NPOPs durch die komplexe Oszillationsbewegung der Elektronen innerhalb des Spaltes zwischen Partikel und Film stark ortsabhängig ist. Zudem reagiert das Nahfeld stark gekoppelter Plasmonen deutlich empfindlicher auf strukturelle Störstellen des Resonators als die Fernfeld-Response. Ferner wurde der Elektronenemissionsmechanismus als optischer Feldemissionsprozess identifiziert. Um den Vorgang beschreiben zu können, wurde die Fowler-Nordheim Theorie der statischen Feldemission für den Fall harmonisch oszillierender Felder modifiziert.

Applicazioni Android basate su tecnologia NFC: rassegna e sperimentazione in contesti di controllo degli accessi

Il documento illustra le funzionalita' della tecnologia NFC, descrive in maniera dettagliata le API pubblicate da Google per lavorare con NFC su Android, e mostra un caso di studio nel contesto di controllo degli accessi..

Progettazione e sviluppo di un sistema software di pagamenti basato su nfc - applicazione utente

L’obiettivo di questa tesi è quello di descrivere la progettazione e lo sviluppo di un’applicazione per la gestione di un sistema che permetta agli utenti di effettuare operazioni di pagamento, ricarica, check-in e altre funzionalità. Tutte queste operazioni saranno implementate tramite l’utilizzo della tecnologia NFC (Near Field Communication). Il sistema prevede un'applicazione "cassa" per le transazioni e un'applicazione "utente" per permettere al cliente di visualizzare i dati relativi al proprio conto. In questa tesi sarà analizzata l'applicazione "utente".

Progettazione e sviluppo di un sistema software di pagamenti basato su NFC - applicazione esercente

La tesi in questione ha l'obiettivo di descrivere la progettazione e lo sviluppo di un’applicazione per la gestione di un sistema che permetta agli utenti di effettuare vari tipi di operazioni, tra i quali pagamento, ricarica, check-in e altre funzionalità. Tutte queste operazioni saranno implementate tramite l’utilizzo della tecnologia NFC (Near Field Communication). Il sistema prevede un'applicazione "cassa" per gestire le varie transazioni e un'applicazione "utente" per permettere ai clienti di visualizzare i dati relativi al proprio conto. Dopo una breve introduzione nella quale verrà descritto il sistema nel suo complesso, la presente tesi si occuperà di analizzare nel dettaglio lo sviluppo dell'applicazione "cassa".

Optical properties of a nanomatch-like plasmonic structure

The optical properties of a match-like plasmonic nanostructure are numerically investigated using full-wave finite-difference time-domain analysis in conjunction with dispersive material models. This work is mainly motivated by the developed technique enabling reproducible fabrication of nanomatch structures as well as the growing applications that utilize the localized field enhancement in plasmonic nanostructures. Our research revealed that due to the pronounced field enhancement and larger resonance tunabilities, some nanomatch topologies show potentials for various applications in the field of, e.g., sensing as well as a novel scheme for highly reproducible tips in scanning near field optical microscopy, among others. Despite the additional degrees of freedom that are offered by the composite nature of the proposed nanomatch topology, the paper also reflects on a fundamental complication intrinsic to the material interfaces especially in the nanoscale: stoichiometric mixing. We conclude that the specificity in material modeling will become a significant issue in future research on functionalized composite nanostructures.

Laser Thomson scattering measurements of electron temperature and density in a Hall-effect plasma

Hall-effect thrusters (HETs) are compact electric propulsion devices with high specific impulse used for a variety of space propulsion applications. HET technology is well developed but the electron properties in the discharge are not completely understood, mainly due to the difficulty involved in performing accurate measurements in the discharge. Measurements of electron temperature and density have been performed using electrostatic probes, but presence of the probes can significantly disrupt thruster operation, and thus alter the electron temperature and density. While fast-probe studies have expanded understanding of HET discharges, a non-invasive method of measuring the electron temperature and density in the plasma is highly desirable. An alternative to electrostatic probes is a non-perturbing laser diagnostic technique that measures Thomson scattering from the plasma. Thomson scattering is the process by which photons are elastically scattered from the free electrons in a plasma. Since the electrons have thermal energy their motion causes a Doppler shift in the scattered photons that is proportional to their velocity. Like electrostatic probes, laser Thomson scattering (LTS) can be used to determine the temperature and density of free electrons in the plasma. Since Thomson scattering measures the electron velocity distribution function directly no assumptions of the plasma conditions are required, allowing accurate measurements in anisotropic and non-Maxwellian plasmas. LTS requires a complicated measurement apparatus, but has the potential to provide accurate, non-perturbing measurements of electron temperature and density in HET discharges. In order to assess the feasibility of LTS diagnostics on HETs non-invasive measurements of electron temperature and density in the near-field plume of a Hall thruster were performed using a custom built laser Thomson scattering diagnostic. Laser measurements were processed using a maximum likelihood estimation method and results were compared to conventional electrostatic double probe measurements performed at the same thruster conditions. Electron temperature was found to range from approximately 1 – 40 eV and density ranged from approximately 1.0 x 1017 m-3 to 1.3 x 1018 m-3 over discharge voltages from 250 to 450 V and mass flow rates of 40 to 80 SCCM using xenon propellant.

Antenna Simulations and Measurements of Focal Plane Array Facet Reflectors

We present a conceptual prototype model of a focal plane array unit for the STEAMR instrument, highlighting the challenges presented by the required high relative beam proximity of the instrument and focus on how edge-diffraction effects contribute to the array's performance. The analysis was carried out as a comparative process using both PO & PTD and MoM techniques. We first highlight general differences between these computational techniques, with the discussion focusing on diffractive edge effects for near-field imaging reflectors with high truncation. We then present the results of in-depth modeling analyses of the STEAMR focal plane array followed by near-field antenna measurements of a breadboard model of the array. The results of these near-field measurements agree well with both simulation techniques although MoM shows slightly higher complex beam coupling to the measurements than PO & PTD.

Coherent control of terahertz meta-materials

We present coherent control of a THz meta-material. Specifically, we show in detail the time and frequency dependent response of a single and a double split ring resonator upon excitation with a shaped THz field. Through far- and near-field measurements, we confirm the coherence transfer from the tailored THz field to the system and back to the radiated field and we demonstrate selective excitation of a designated system resonance with a suitably shaped THz pulse.

Geochemistry and age determination of sediments from teh Rainbow hydrothermal plume

A geochemical investigation has been conducted of a suite of four sediment cores collected from directly beneath the hydrothermal plume at distances of 2 to 25 km from the Rainbow hydrothermal field. As well as a large biogenic component (>80% CaCO3) these sediments record clear enrichments of the elements Fe, Cu, Mn, V, P, and As from hydrothermal plume fallout but only minor detrital background material. Systematic variations in the abundances of "hydrothermal" elements are observed at increasing distance from the vent site, consistent with chemical evolution of the dispersing plume. Further, pronounced Ni and Cr enrichments at specific levels within each of the two cores collected from closest to the vent site are indicative of discrete episodes of additional input of ultrabasic material at these two near-field locations. Radiocarbon dating reveals mean Holocene accumulation rates for all four cores of 2.7 to 3.7 cm.kyr?1, with surface mixed layers 7 to 10+ cm thick, from which a history of deposition from the Rainbow hydrothermal plume can be deduced. Deposition from the plume supplies elements to the underlying sediments that are either directly hydrothermally sourced (e.g., Fe, Mn, Cu) or scavenged from seawater via the hydrothermal plume (e.g., V, P, As). Holocene fluxes into to the cores' surface mixed layers are presented which, typically, are an order of magnitude greater than "background" authigenic fluxes from the open North Atlantic. One core, collected closest to the vent site, indicates that both the concentration and flux of hydrothermally derived material increased significantly at some point between 8 and 12 14C kyr ago; the preferred explanation is that this variation reflects the initiation/intensification of hydrothermal venting at the Rainbow hydrothermal field at this time - perhaps linked to some specific tectonic event in this fault-controlled hydrothermal setting.

Neodymium isotopes from fossil fish teeth and detrital sediment, and oxygen isotopes from benthic forams from ODP Hole 119-738 B

Ephemeral polar glaciations during the middle-to-late Eocene (48-34 Ma) have been proposed based on far-field ice volume proxy records and near-field glacigenic sediments, although the scale, timing, and duration of these events are poorly constrained. Here we confirm the existence of a transient cool event within a new high-resolution benthic foraminiferal d18O record at Ocean Drilling Program (ODP) Site 738 (Kerguelen Plateau; Southern Ocean). This event, named the Priabonian oxygen isotope maximum (PrOM) Event, lasted ~140 kyr and is tentatively placed within magnetochron C17n.1n (~37.3 Ma) based on the correlation to ODP Site 689 (Maud Rise, Southern Ocean). A contemporaneous change in the provenance of sediments delivered to the Kerguelen Plateau occurs at the study site, determined from the <63 µm fraction of decarbonated and reductively leached sediment samples. Changes in the mixture of bottom waters, based on fossil fish tooth epsilon-Nd, were less pronounced and slower relative to the benthic d18O and terrigenous epsilon-Nd changes. Terrigenous sediment epsilon-Nd values rapidly shifted to less radiogenic signatures at the onset of the PrOM Event, indicating an abrupt change in provenance favoring ancient sources such as the Paleoproterozoic East Antarctic craton. Bottom water epsilon-Nd reached a minimum value during the PrOM Event, although the shift begins much earlier than the terrigenous epsilon-Nd excursion. The origin of the abrupt change in terrigenous sediment provenance is compatible with a change in Antarctic terrigenous sediment flux and/or source as opposed to a reorganization of ocean currents. A change in terrigenous flux and/or source of Antarctic sediments during the oxygen isotope maximum suggests a combination of cooling and ice growth in East Antarctica during the early late Eocene.

Physical properties, velocity and attenuation characteristics, and mineralogy of gabbros from ODP Hole 176-735B

Laboratory compressional wave (Vp) and shear wave (Vs) velocities were measured as a function of confining pressure for the gabbros from Hole 735B and compared to results from Leg 118. The upper 500 m of the hole has a Vp mean value of 6895 m/s measured at 200 MPa, and at 500 meters below seafloor (mbsf), Vp measurements show a mean value of 7036 m/s. Vs mean values in the same intervals are 3840 m/s and 3857 m/s, respectively. The mean Vp and Vs values obtained from log data in the upper 600 m are 6520 and 3518 m/s, respectively. These results show a general increase in velocity with depth and the velocity gradients estimate an upper mantle depth of 3.32 km. This value agrees with previous work based on dredged samples and inversion of rare element concentrations in basalts dredged from the conjugate site to the north of the Atlantis Bank. Laboratory measurements show Vp anisotropy ranging between 0.4% and 8.8%, with the majority of the samples having values less than 3.8%. Measurements of velocity anisotropy seem to be associated with zones of high crystal-plastic deformation with predominant preferred mineral orientations of plagioclase, amphiboles, and pyroxenes. These findings are consistent with results on gabbros from the Hess Deep area and suggest that plastic deformation may play an important role in the seismic properties of the lower oceanic crust. In contrast to ophiolite studies, many of the olivine gabbros show a small degree of anisotropy. Log derived Vs anisotropy shows an average of 5.8% for the upper 600 m of Hole 735B and tends to decrease with depth where the overburden pressure and the age of the crustal section suggests closure of cracks and infilling of fractures by alteration minerals. Overall the results indicate that the average shear wave splitting in Hole 735B might be influenced by preferred structural orientations and the average value of shear wave splitting may not be a maximum because structural dips are <90°. The maximum fast-wave orientation values could be influenced by structural features striking slightly oblique to this orientation or by near-field stress concentrations. However, flexural wave dispersion analyses have not been performed to confirm this hypothesis or to indicate to what extent the near-field stresses may be influencing shear wave propagation. Acoustic impedance contrasts calculated from laboratory and logging data were used to generate synthetic seismograms that aid in the interpretation of reflection profiles. Several prominent reflections produced by these calculations suggest that Fe-Ti oxides and shear zones may contribute to the reflective nature of the lower oceanic crust. Laboratory velocity attenuation (Q) measurements from below 500 m have a mean value of 35.1, which is consistent with previous vertical seismic profile (VSP) and laboratory measurements on the upper 500 m.