New data on the Pleistocene of Trani (Adriatic Coast, Southern Italy)

Along the Apulian Adriatic coast, in a cliff south of Trani, a succession of three units (superimposed on one another) of marine and/or paralic environments has been recognised. The lowest unit I is characterised by calcareous/siliciclastic sands (css), micritic limestones (ml), stromatolitic and characean boundstones (scb), characean calcarenites (cc). The sedimentary environment merges from shallow marine, with low energy and temporary episodes of subaerial exposure, to lagoonal with a few exchanges with the sea. The lagoonal stromatolites (scb subunit) grew during a long period of relative stability of a high sea level in tropical climate. The unit I is truncated at the top by an erosion surface on which the unit II overlies; this consists of a basal pebble lag (bpl), silicicla - stic sands (ss), calcareous sands (cs), characean boundstones (cb), brown paleosol (bp). The sedimentary environment varies from beach to lagoon with salinity variations. Although there are indications of seismic events within the subunits cs, unit II deposition took place in a context of relative stability. The unit II is referable to a sea level highstand. Unit III, trangressive on the preceding, consists of white calcareous sands (wcs), calcareous sands and calcarenites (csc), phytoclastic calcirudite and phytohermal travertine (pcpt), mixed deposits (csl, m, k, c), sands (s) and red/brown paleosols (rbp). The sedimentation of this unit was affected by synsedimentary tectonic, attested by seismites found at several heights. Also the unit III is referable to a sea level highstand. The scientific literature has so far generally attributed to the Tyrrhenian (auct.) the deposits of Trani cliff. As part of this work some datings were performed on 10 samples, using the amino acid racemization method (AAR) applied to ostracod carapaces. Four of these samples have been rejected because they have shown in laboratory recent contamination. The numerical ages indicate that the deposits of the Trani cliff are older than MIS 5. The upper part of the unit I has been dated to 355±85 ka BP, thus allowing to assign the lowest stromatolitic subunit (scb) at the MIS 11 peak and the top of the unit I at the MIS 11-MIS 10 interval. The base of the unit II has been dated to 333±118 ka BP, thus attributing the erosion surface that bounds the units I and II to the MIS 10 lowstand and the lower part of the unit II to MIS 9.3. The upper part of the unit II has been dated to 234±35 ka BP, while three other numerical ages come from unit III: 303±35, 267±51, 247±61 ka BP. At present, the numerical ages cannot distinguish the sedimentation ages of units II and III, which are both related to the MIS 9.3- MIS 7.1 time range. However, the position of the units, superimposed one another, and their respective age, allows us to recognise a subsidence phase between MIS 11 and MIS 7, followed by an uplift phase between the MIS 7 and the present day, which led the deposits in their current position. This tectonic pattern is not in full agreement with what is described in the literature for the Apulian foreland.

Nonlinear models for lateral dynamics of railway vehicles on bridges subject to wind action

The study of lateral dynamics of running trains on bridges is of importance mainly for the safety of the traffic, and may be relevant for laterally compliant bridges. These studies require threedimensional coupled vehicle-bridge models, wheree consideration of wheel to rail contact is a key aspect. Furthermore, an adequate evaluation of safety of rail traffic requires nonlinear models. A nonlinear coupled model is proposed here for vehicle-structure vertical and lateral dynamics. Vehicles are considered as fully three-dimensional multibody systems including gyroscopic terms and large rotation effects. The bridge structure is modeled by means of finite elements which may be of beam, shell or continuum type and may include geometric or material nonlinearities. The track geometry includes distributed track alignment irregularities. Both subsystems (bridge and vehicles) are described with coordinates in absolute reference frames, as opposed to alternative approaches which describe the multibody system with coordinates relative to the base bridge motion. The wheelrail contact employed is a semi-Hertzian model based on realistic wheel-rail profiles. It allows a detailed geometrical description of the contact patch under each wheel including multiple-point contact, flange contact and uplift. Normal and tangential stresses in each contact are integrated at each time-step to obtain the resultant contact forces. The models have been implemented within an existing finite element analysis software with multibody capabilities, Abaqus (Simulia Ltd., 2010). Further details of the model are presented in Antolín et al. (2012). Representative applications are presented for railway vehicles under lateral wind action on laterally compliant viaducts, showing the relevance of the nonlinear wheel-rail contact model as well as the interaction between bridge and vehicle.

Estudio dinámico de cimentaciones en obras portuarias

Los diques de abrigo verticales son estructuras monolíticas que sirven para reflejar el oleaje creando, de este modo, una zona abrigada en el lado tierra. Son estructuras de contención de gravedad, es decir, su peso es el elemento resistente fundamental. Las solicitaciones sobre estas estructuras son de tipo dinámico (oleaje) y consisten, fundamentalmente, en un empuje frontal y una subpresión en la base que varían en el tiempo. Habitualmente, las acciones sobre los diques de abrigo se establecen mediante fórmulas empíricas, que se describen en la presente tesis si bien, para obras de especial importancia, suelen medirse en modelos reducidos de laboratorio. Cuando el cimiento en que han de apoyarse estas estructuras no presenta una resistencia al corte suficiente, el apoyo se realiza en banquetas que redistribuyen la carga y que están formadas por materiales granulares. En la práctica habitual para conocer la estabilidad de estas estructuras frente a un temporal, tras establecer las acciones de cálculo (empuje frontal y subpresión) se efectúa un cálculo pseudoestático en el que se consideran condiciones drenadas o no drenadas del cimiento en función de su permeabilidad. Se conoce que en los suelos saturados, bajo cargas cíclicas, tiende a producirse una elevación de las presiones intersticiales y una reducción de tensiones efectivas así como una degradación del módulo de deformación tangencial en función del número de ciclos de carga, pudiéndose producir el fenómeno conocido como licuefacción (arenas) o movilidad cíclica (suelos más finos). El objeto de la tesis es explorar la posibilidad, con la tecnología actual, de analizar la estabilidad de los diques de abrigo verticales en cuyo cimiento existen suelos blandos, proponiendo un procedimiento para evaluar la estabilidad dinámica en este tipo de obras. Para ello se han revisado los procedimientos actualmente utilizados para definir las acciones de cálculo, los principales modelos de comportamiento dinámicos de suelos saturados disponibles y los procedimientos de cálculo. Una vez investigado el estado del arte sobre este tema, se propone un procedimiento de cálculo en el que, utilizando el programa comercial FLAC, se establecen las acciones cíclicas sobre un dique de abrigo vertical tipo con distintas condiciones de apoyo, aplicando, para el cimiento, un modelo de comportamiento tipo hiperbólico con generación de presiones intersticiales cuyos parámetros pueden obtenerse de ensayos de campo y laboratorio. Por último, una vez descrito el procedimiento, se aplica a un caso real en el que se produjo un fallo en la cimentación que desembocó en el hundimiento de parte de un dique vertical situado en el puerto de Barcelona, presentándose los resultados obtenidos del análisis efectuado y comparándolos con los obtenidos utilizando los métodos de cálculo habituales. Vertical breakwaters are monolithic structures built to reflect sea waves, thereby providing a sheltered area on the land side. They are gravity retaining structures, that is, their own weight is their basic resisting mechanism. Loads acting on these structures are dynamic (waves) and consist essentially in a frontal thrust and an uplift pressure on the base, which both vary over time. Usually, actions in breakwater design are established by empirical formulas, which are described in this thesis. For works of particular importance, such forces are measured in small-scale laboratory tests. When there are no soils with enough shear strength under the planned vertical breakwaters, they usually rest on granular berms which redistribute the load. Nowadays, after establishing the acting forces on the breakwater (front push and uplift pressure), a pseudostatic calculation (with drained or undrained conditions depending on the foundation permeability) is normally done to analyze the stability of these structures against storm waves. It is known that pore pressures tend to rise in saturated soils under cyclic loading and, consequently, there is a reduction of effective stress. A degradation of the shear modulus also occurs depending on the number of load cycles. All of these effects can bring about the phenomenon known as liquefaction in sands or cyclic mobility in fine-grained soils. The aim of the thesis is to explore the possibility that current technology provides to analyze the stability of vertical breakwaters founded on soft soils, and to suggest a method to evaluate the dynamic stability in this type of works. To this end, a review has been made of procedures currently used to define the actions in calculations, the main models of dynamic behaviour of saturated soils available and of calculation procedures. Once the state of the art on this subject has been reviewed, a method of calculation is proposed that uses the commercial program FLAC and is applied to a typical vertical breakwater on a range of different foundation conditions. For the foundation soil, a hyperbolic constitutive model with pore pressure generation has been employed, whose parameters can be obtained from field and laboratory tests. Finally, the described procedure is applied to an actual case where a foundation failure occurred that led to the sinking of several caissons in a vertical breakwater located in the port of Barcelona. The results obtained with the proposed method are compared with those obtained using conventional methods.

Estudio y diseño de un régimen fiscal que optimice la inversión en exploración y producción de hidrocarburos

Los regímenes fiscales que se aplican a los contratos de exploración y desarrollo de petróleo y gas, entre los propietarios del recurso natural (generalmente el país soberano representado por su gobierno) y las compañías operadoras internacionales (COI) que aportan capital, experiencia y tecnología, no han sabido responder a la reciente escalada de los precios del crudo y han dado lugar a que los países productores no estén recibiendo la parte de renta correspondiente al incremento de precios. Esto ha provocado una ola de renegociaciones llegándose incluso a la imposición unilateral de nuevos términos por parte de algunos gobiernos entre los que destacan el caso de Venezuela y Argentina, por ser los más radicales. El objetivo del presente trabajo es el estudio y diseño de un régimen fiscal que, en las actuales condiciones del mercado, consiga que los gobiernos optimicen sus ingresos incentivando la inversión. Para ello se simulan los efectos de siete tipos diferentes de fiscalidades aplicadas a dos yacimientos de características muy distintas y se valoran los resultados. El modelo utilizado para la simulación es el modelo de escenarios, ampliamente utilizado tanto por la comunidad académica como por la industria para comparar el comportamiento de diferentes regímenes fiscales. Para decidir cuál de las fiscalidades estudiadas es la mejor se emplea un método optimización multicriterio. Los criterios que se han aplicado para valorar los resultados recogen la opinión de expertos de la industria sobre qué factores se consideran deseables en un contrato a la hora invertir. El resultado permite delinear las características de un marco fiscal ideal del tipo acuerdo de producción compartida, sin royalties, con un límite alto de recuperación de crudo coste que permita recobrar todos los costes operativos y una parte de los de capital en cualquier escenario de precios, un reparto de los beneficios en función de un indicador de rentabilidad como es la TIR, con un mecanismo de recuperación de costes adicional (uplift) que incentive la inversión y con disposiciones que premien la exploración y más la de alto riesgo como la amortización acelerada de los gastos de capital o una ampliación de la cláusula de ringfence. Un contrato con estas características permitirá al gobierno optimizar los ingresos obtenidos de sus reservas de petróleo y gas maximizando la producción al atraer inversión para la exploración y mejorar la recuperación alargando la vida del yacimiento. Además al reducir el riesgo percibido por el inversor que recupera sus costes, menor será la rentabilidad exigida al capital invertido y por tanto mayor la parte de esos ingresos que irá a parar al gobierno del país productor. ABSTRACT Fiscal systems used in petroleum arrangements between the owners of the resource (usually a sovereign country represented by its government) and the international operating company (IOC) that provides capital, knowhow and technology, have failed to allocate profits from the recent escalation of oil prices and have resulted in producing countries not receiving the right share of that increase. This has caused a wave of renegotiations and even in some cases, like Venezuela and Argentina, government unilaterally imposed new terms. This paper aims to outline desirable features of a petroleum fiscal system, under current market conditions, for governments to maximize their revenues while encouraging investment. Firstly the impact of seven different types of fiscal regimes is studied with a simulation for two separate oil fields using the scenario approach. The scenario approach has been frequently employed by academic and business researchers to compare the performance of diverse fiscal regimes. In order to decide which of the fiscal regimes’ performance is best we used a multi-objective optimization decision making approach to assess the results. The criteria applied gather the preferences of a panel of industry experts about the desirable features of a contract when making investment decisions. The results show the characteristics of an ideal fiscal framework that closely resembles a production sharing contract, with no royalty payment and a high cost recovery limit that allows the IOC to recover all operating expenses and a share of its capital costs under any price scenario, a profit oil sharing mechanism based on a profitability indicator such as the ROR, with an uplift that allows to recover an additional percentage of capital costs and provisions that promote exploration investment, specially high-risk exploration, such as accelerated depreciation for capital costs and a wide definition of the ringfence clause. A contract with these features will allow governments to optimize overall revenues from its petroleum resources maximizing production by promoting investment on exploration and extending oil fields life. Also by reducing the investor’s perception of risk it will reduce the minimum return to capital required by the IOC and therefore it will increase the government share of those revenues.