Validation of the land water storage from gravity recovery and climate experiment (GRACE) with gauge data in the amazon basin

The Amazon basin is a region of constant scientific interest due to its environmental importance and its biodiversity and climate on a global scale. The seasonal variations in water volume are one of the examples of topics studied nowadays. In general, the variations in river levels depend primarily on the climate and physics characteristics of the corresponding basins. The main factor which influences the water level in the Amazon Basin is the intensive rainfall over this region as a consequence of the humidity of the tropical climate. Unfortunately, the Amazon basin is an area with lack of water level information due to difficulties in access for local operations. The purpose of this study is to compare and evaluate the Equivalent Water Height (Ewh) from GRACE (Gravity Recovery And Climate Experiment) mission, to study the connection between water loading and vertical variations of the crust due to the hydrologic. In order to achieve this goal, the Ewh is compared with in-situ information from limnimeter. For the analysis it was computed the correlation coefficients, phase and amplitude of GRACE Ewh solutions and in-situ data, as well as the timing of periods of drought in different parts of the basin. The results indicated that vertical variations of the lithosphere due to water mass loading could reach 7 to 5 cm per year, in the sedimentary and flooded areas of the region, where water level variations can reach 10 to 8 m.

Ricostruzione degli sforzi in elementi finiti di piastra

Nell’ambito dell’analisi computazionale delle strutture il metodo degli elementi finiti è probabilmente uno dei metodi numerici più efficaci ed impiegati. La semplicità dell’idea di base del metodo e la relativa facilità con cui può essere implementato in codici di calcolo hanno reso possibile l’applicazione di questa tecnica computazionale in diversi settori, non solo dell’ingegneria strutturale, ma in generale della matematica applicata. Ma, nonostante il livello raggiunto dalle tecnologie ad elementi finiti sia già abbastanza elevato, per alcune applicazioni tipiche dell’ingegneria strutturale (problemi bidimensionali, analisi di lastre inflesse) le prestazioni fornite dagli elementi usualmente utilizzati, ovvero gli elementi di tipo compatibile, sono in effetti poco soddisfacenti. Vengono in aiuto perciò gli elementi finiti basati su formulazioni miste che da un lato presentano una più complessa formulazione, ma dall’altro consentono di prevenire alcuni problemi ricorrenti quali per esempio il fenomeno dello shear locking. Indipendentemente dai tipi di elementi finiti utilizzati, le quantità di interesse nell’ambito dell’ingegneria non sono gli spostamenti ma gli sforzi o più in generale le quantità derivate dagli spostamenti. Mentre i primi sono molto accurati, i secondi risultano discontinui e di qualità scadente. A valle di un calcolo FEM, negli ultimi anni, hanno preso piede procedure di post-processing in grado, partendo dalla soluzione agli elementi finiti, di ricostruire lo sforzo all’interno di patch di elementi rendendo quest’ultimo più accurato. Tali procedure prendono il nome di Procedure di Ricostruzione (Recovery Based Approaches). Le procedure di ricostruzione qui utilizzate risultano essere la REP (Recovery by Equilibrium in Patches) e la RCP (Recovery by Compatibility in Patches). L’obbiettivo che ci si prefigge in questo lavoro è quello di applicare le procedure di ricostruzione ad un esempio di piastra, discretizzato con vari tipi di elementi finiti, mettendone in luce i vantaggi in termini di migliore accurattezza e di maggiore convergenza.

A new insight in stress recovery tecniques and hessian reconstruction methods

Stress recovery techniques have been an active research topic in the last few years since, in 1987, Zienkiewicz and Zhu proposed a procedure called Superconvergent Patch Recovery (SPR). This procedure is a last-squares fit of stresses at super-convergent points over patches of elements and it leads to enhanced stress fields that can be used for evaluating finite element discretization errors. In subsequent years, numerous improved forms of this procedure have been proposed attempting to add equilibrium constraints to improve its performances. Later, another superconvergent technique, called Recovery by Equilibrium in Patches (REP), has been proposed. In this case the idea is to impose equilibrium in a weak form over patches and solve the resultant equations by a last-square scheme. In recent years another procedure, based on minimization of complementary energy, called Recovery by Compatibility in Patches (RCP) has been proposed in. This procedure, in many ways, can be seen as the dual form of REP as it substantially imposes compatibility in a weak form among a set of self-equilibrated stress fields. In this thesis a new insight in RCP is presented and the procedure is improved aiming at obtaining convergent second order derivatives of the stress resultants. In order to achieve this result, two different strategies and their combination have been tested. The first one is to consider larger patches in the spirit of what proposed in [4] and the second one is to perform a second recovery on the recovered stresses. Some numerical tests in plane stress conditions are presented, showing the effectiveness of these procedures. Afterwards, a new recovery technique called Last Square Displacements (LSD) is introduced. This new procedure is based on last square interpolation of nodal displacements resulting from the finite element solution. In fact, it has been observed that the major part of the error affecting stress resultants is introduced when shape functions are derived in order to obtain strains components from displacements. This procedure shows to be ultraconvergent and is extremely cost effective, as it needs in input only nodal displacements directly coming from finite element solution, avoiding any other post-processing in order to obtain stress resultants using the traditional method. Numerical tests in plane stress conditions are than presented showing that the procedure is ultraconvergent and leads to convergent first and second order derivatives of stress resultants. In the end, transverse stress profiles reconstruction using First-order Shear Deformation Theory for laminated plates and three dimensional equilibrium equations is presented. It can be seen that accuracy of this reconstruction depends on accuracy of first and second derivatives of stress resultants, which is not guaranteed by most of available low order plate finite elements. RCP and LSD procedures are than used to compute convergent first and second order derivatives of stress resultants ensuring convergence of reconstructed transverse shear and normal stress profiles respectively. Numerical tests are presented and discussed showing the effectiveness of both procedures.

Progettazione e implementazione di una rete di sensori mobili Arduino per scenari di Disaster Recovery

Sommario Il progetto descritto in questo documento consiste nella realizzazione di una prima applicazione pratica di uno specifico studio di ricerca rivolto al ripristino di reti wireless in scenari post-calamità naturali. In principio è stata descritta un’ampia analisi delle problematiche di rete che si vengono a creare in seguito ad eventi catastrofici. Successivamente, analizzando le varie tecniche e tecnologie oggetto di studio di diversi gruppi di ricerca, si è scelto di collaborare con il progetto STEM-Mesh, essendo ancora in fase sperimentale, il quale affronta il problema di ristabilire la connettività di rete in questi particolari scenari, attraverso l’utilizzo di tecnologie Cognitive Radio (CR), mobilità controllata e principi di reti auto-organizzanti. Di questo primo approccio pratico sono state poi descritte le fasi di progettazione, implementazione e testing. Nella fase di progettazione sono state studiate le componenti hardware e software che rispettassero il più possibile i requisiti e le caratteristiche dei dispositivi “staminali” STEM-Node cuore del progetto STEM-Mesh, ovvero dei dispositivi wireless altamente auto-riconfiguranti ed auto-organizzanti che possono diventare dispositivi sostituivi ai nodi compromessi in una rete, riconfigurandosi appunto in base alle funzionalità interrotte. Nella fase di implementazione si è passati alla stesura del codice, in Python e Wiring, abilitante il dispositivo STEM-Node. Infine nella fase di testing si è verificato che i risultati fossero quelli desiderati e che il sistema realizzato funzionasse come previsto.

Static analysis of functionally graded cylindrical and conical shells or panels using the generalized unconstrained third order theory coupled with the stress recovery

A 2D Unconstrained Third Order Shear Deformation Theory (UTSDT) is presented for the evaluation of tangential and normal stresses in moderately thick functionally graded conical and cylindrical shells subjected to mechanical loadings. Several types of graded materials are investigated. The functionally graded material consists of ceramic and metallic constituents. A four parameter power law function is used. The UTSDT allows the presence of a finite transverse shear stress at the top and bottom surfaces of the graded shell. In addition, the initial curvature effect included in the formulation leads to the generalization of the present theory (GUTSDT). The Generalized Differential Quadrature (GDQ) method is used to discretize the derivatives in the governing equations, the external boundary conditions and the compatibility conditions. Transverse and normal stresses are also calculated by integrating the three dimensional equations of equilibrium in the thickness direction. In this way, the six components of the stress tensor at a point of the conical or cylindrical shell or panel can be given. The initial curvature effect and the role of the power law functions are shown for a wide range of functionally conical and cylindrical shells under various loading and boundary conditions. Finally, numerical examples of the available literature are worked out.

Travi in parete sottile con deformabilità a taglio e distorsione di sezione: formulazione teorica, modellazione numerica e applicazioni

Il presente lavoro di tesi ha riguardato una riformulazione teorica, una modellazione numerica e una serie di applicazioni della Generalized Beam Theory per lo studio dei profili in parete sottile con particolare riguardo ai profili in acciaio formati a freddo. In particolare, in questo lavoro è proposta una riscrittura della cinematica GBT che introduce in una forma originale la deformabilità a taglio della sezione. Tale formulazione consente di conservare il formato della GBT classica e introducendo uno spostamento di warping variabile lungo lo spessore della generica parete della sezione trasversale, garantisce perfetta coerenza tra la componente flessionale e tagliante della trave. E' mostrato, come tale riscrittura consente in maniera agevole di ricondursi alle teorie classiche di trave, anche deformabili a taglio. Inoltre, in tale contesto, è stata messa a punto una procedura di ricostruzione dello sforzo tridimensionale in grado ricostruire la parte reattiva delle componenti di tensioni dovuta al vincolamento interno proprio di un modello a cinematica ridotta. Sulla base di tali strumenti, è stato quindi proposto un approccio progettuale dedicato ai profili in classe 4, definito ESA (Embedded Stability Analysis), in grado di svolgere le verifiche coerentemente con quanto prescritto dalle normative vigenti. Viene infine presentata una procedura numerica per la progettazione di sistemi di copertura formati a freddo. Tale procedura permette di effettuare in pochi semplici passi il progetto dell'arcareccio e dei dettagli costruttivi relativi alla copertura.

Consequences of DNA damage for gene transcription : direct effects of modified nucleobases and the role of base excision repair = Folgen von DNA-Schäden für die Gentranskription

The presence of damaged nucleobases in DNA can negatively influence transcription of genes. One of the mechanisms by which DNA damage interferes with reading of genetic information is a direct blockage of the elongating RNA polymerase complexes – an effect well described for bulky adducts induced by several chemical substances and UV-irradiation. However, other mechanisms must exist as well because many of the endogenously occurring non-bulky DNA base modifications have transcription-inhibitory properties in cells, whilstrnnot constituting a roadblock for RNA polymerases under cell free conditions. The inhibition of transcription by non-blocking DNA damage was investigated in this work by employing the reporter gene-based assays. Comparison between various types of DNA damage (UV-induced pyrimidine photoproducts, oxidative purine modifications induced by photosensitisation, defined synthetic modified bases such as 8-oxoguanine and uracil, and sequence-specific single-strand breaks) showed that distinct mechanisms of inhibition of transcription can be engaged, and that DNA repair can influence transcription of the affectedrngenes in several different ways.rnQuantitative expression analyses of reporter genes damaged either by the exposure of cells to UV or delivered into cells by transient transfection supported the earlier evidence that transcription arrest at the damage sites is the major mechanism for the inhibition of transcription by this kind of DNA lesions and that recovery of transcription requires a functional nucleotide excision repair gene Csb (ERCC6) in mouse cells. In contrast, oxidisedrnpurines generated by photosensitisation do not cause transcriptional blockage by a direct mechanism, but rather lead to transcriptional repression of the damaged gene which is associated with altered histone acetylation in the promoter region. The whole chain of events leading to transcriptional silencing in response to DNA damage remains to be uncovered. Yet, the data presented here identify repair-induced single-strand breaks – which arise from excision of damaged bases by the DNA repair glycosylases or endonucleases – as arnputative initiatory factor in this process. Such an indirect mechanism was supported by requirement of the 8-oxoguanine DNA glycosylase (OGG1) for the inhibition of transcription by synthetic 8-oxodG incorporated into a reporter gene and by the delays observed for the inhibition of transcription caused by structurally unrelated base modifications (8-oxoguanine and uracil). It is thereby hypothesized that excision of the modified bases could be a generalrnmechanism for inhibition of transcription by DNA damage which is processed by the base excision repair (BER) pathway. Further gene expression analyses of plasmids containing single-strand breaks or abasic sites in the transcribed sequences revealed strong transcription inhibitory potentials of these lesions, in agreement with the presumption that BER intermediates are largely responsible for the observed effects. Experiments with synthetic base modifications positioned within the defined DNA sequences showed thatrninhibition of transcription did not require the localisation of the lesion in the transcribed DNA strand; therefore the damage sensing mechanism has to be different from the direct encounters of transcribing RNA polymerase complexes with DNA damage.rnAltogether, this work provides new evidence that processing of various DNA basernmodifications by BER can perturb transcription of damaged genes by triggering a gene silencing mechanism. As gene expression can be influenced even by a single DNA damage event, this mechanism could have relevance for the endogenous DNA damage induced in cells under normal physiological conditions, with a possible link to gene silencing in general.

Roasting and Leaching Bulk Copper-Zinc Sulfide Concentrates with the Subsequent Recovery of the Metals by Electrolysis

The aim of this research was to investigate the possibilities of roasting and leaching a bulk copper-zinc sulfide concentrate, and the subsequent separation of the metals from the leach solution by electro­lytic deposition.

Bending Shear: The Rate-Controlling Mechanism for Calving Ice Walls

Bending shear was observed to produce nearly vertical shear bands in a calving ice wall standing on dry land on Deception Island (Iat. 63.0 oS., long. 60.6 W.), and slabs calved straight downward when shear rupture occurred along these shear bands (Hughes, 1989). A formula for the calving rate was developed from the Deception Island data, and we have attempted to justify generalizing this formula to include ice walls standing along beaches or in water. These are environments in which a wave-washed groove develops along the base of the ice wall or along a water line above the base. The rate of wave erosion provides an alternative mechanism for controlling the calving rate in these environments. We have determined that the rate at which bending creep produces nearly vertical shear bands, along which shear r upture occurs, controls the calving rate in all environments. Shear rupture occurs at a calving shear stress of about I bar. Our results justify using the calving formula to compute the calving rate of ice walls in computer models of ice-sheet dynamics. This is especially important in simulating retreat of Northern Hemisphere ice sheets during the last deglaciation, when marine and lacustrine environments were common along retreating ice margins. These margins would have been ice walls standing along beaches or in water, because floating ice shelves are not expected in the ablation zone of retreating ice sheets.

Anelastic strain recovery and elastic properties of ODP Leg 123 oceanic basalt samples

A knowledge of rock stress is fundamental for improving our understanding of oceanic crustal mechanisms and lithospheric dynamic processes. However, direct measurements of stress in the deep oceans, and in particular stress magnitudes, have proved to be technically difficult. Anelastic strain recovery measurements were conducted on 15 basalt core samples from Sites 765 and 766 during Leg 123. Three sets of experiments were performed: anelastic strain recovery monitoring, dynamic elastic property measurements, and thermal azimuthal anisotropy observations. In addition, a range of other tests and observations were recorded to characterize each of the samples. One common feature of the experimental results and observations is that apparently no consistent orientation trend exists, either between the different measurements on each core sample or between the same sets of measurements on the various core samples. However, some evidence of correspondence between velocity anisotropy and anelastic strain recovery exists, but this is not consistent for all the core samples investigated. Thermal azimuthal anisotropy observations, although showing no conclusive correlations with the other results, were of significant interest in that they clearly exhibited anisotropic behavior. The apparent reproducibility of this behavior may point toward the possibility of rocks that retain a "memory" of their stress history, which could be exploited to derive stress orientations from archived core. Anelastic strain recovery is a relatively new technique. Because use of the method has extended to a wider range of rock types, the literature has begun to include examples of rocks that contracted with time. Strong circumstantial evidence exists to suggest that core-sample contractions result from the slow diffusion of pore fluids from a preexisting microcrack structure that permits the rock to deflate at a greater rate than the expansion caused by anelastic strain recovery. Both expansions and contractions of the Leg 123 cores were observed. The basalt cores have clearly been intersected by an abundance of preexisting fractures, some of which pass right through the samples, but many are intercepted or terminate within the rock matrix. Thus, the behavior of the core samples will be influenced not only by the properties of the rock matrix between the fractures, but also by how these macro- and micro-scale fractures mutually interact. The strain-recovery curves recorded during Leg 123 for each of the 15 basalt core samples may reflect the result of two competing time dependent processes: anelastic strain recovery and pore pressure recovery. Were these the only two processes to influence the gauge responses, then one might expect that given the additional information required, established theoretical models might be used to determine consistent stress orientations and reliable stress magnitudes. However, superimposed upon these competing processes is their respective interaction with the preexisting fractures that intersect each core. Evidence from our experiments and observations suggests that these fractures have a dominating influence on the characteristics of the recovery curves and that their effects are complex.

Compressional and shear wave velocities and elastic constants at DSDP Leg 59 Holes

Prior to the Deep Sea Drilling Project the composition of the oceanic crust could only be inferred from seismic-refraction and gravity data and the recovery of a wide variety of dredged rocks. Through the success of the Deep Sea Drilling Project, it is now clear that the top of oceanic Layer 2 usually consists of basalt. Several laboratory studies (e.g., Fox et al., 1972; Christensen and Shaw, 1970; Hyndman and Drury, 1976) have demonstrated that the seismic velocities of oceanic basalt are similar to velocities reported from refraction studies of Layer 2 and that the variability in Layer 2 velocities has many causes, the most important being fracturing and sea-floor alteration produced by the interaction of basalt and sea water (Christensen and Salisbury, 1973). To date, most reported measurements of velocities in oceanic basalts are from samples obtained from the main ocean basins. With the exception of an earlier study of velocities and related elastic properties of a suite of rocks from DSDP Sites 292, 293, 294, and 296 located in the Philippine Sea (Christensen et al., 1975; Fountain et al., 1975), elastic properties have not been determined for oceanic rocks from marginal basins. In this chapter compressional- and shear-wave velocities and elastic constants are reported at elevated confining pressures for basalt and volcanic breccias from Holes 447A, 448, and 448A.