fatigue delamination experiments on gfrp and cfrp specimens under single and mixed fracture modes

Abstract This paper deals with the experimental analysis of the delamination phenomena in composite materials under different loading conditions. Quasi-static and fatigue tests are performed on specimens made of glass-fibre (GFRP) and carbon-fibre (CFRP) reinforced plastic. In particular, experiments have been carried out under single fracture modes I and II (using standard DCB and ENF test configurations) and mixed modes I+II (using the MMB test configuration) with several mode mixtures. Results obtained for the two materials have been compared paying attention on the relationship between the parameters that describe the fatigue behaviour and the mode mixture acting during the crack propagation

A data sequence aquired at Mt. Etna during the 2002 - 2003 eruption highlights the potential of continuous gravity observations as a tool to monitor and study active volcanoes

A 2.5-month long gravity sequence, encompassing the starting period of the 2002–2003 Etna eruption and coming from a summit station only 1 km away from the new fractures, is presented and discussed. The sequence comprises some hours-long anomalies that have a great chance to reflect mass redistributions linked to the ensuing activity. In particular, the start of the eruptive activity on the northeastern flank was marked by a gravity decrease as strong as about 400 Gal, which reverted soon afterwards. This strong decrease/increase anomaly is interpreted as the opening, by tectonic forces, of a fracture system along the Northeastern Rift of Mt. Etna, followed by an intrusion of magma from the central conduit to the new fractures. They were used by the intruding magma as a path to the eruptive vents at lower elevations. Afterwards, on three occasions, in November and December 2002, 6–12 h-lasting gravity decreases, with amplitude ranging between 10 and 30 Gal, were observed simultaneously with increases in the amplitude of the volcanic tremor from four seismic stations. A correlation analysis, between the gravity signal and the overall spectral amplitude of each tremor sequence is performed over the 7 November–9 December period. A marked anti-correlation is found over each contemporaneous gravity decrease/tremor increase, while, over the rest of the investigated period, the correlation is negligible. Accordingly, a joint source is inferred to have acted during the occurrence of the three common anomalies. On the grounds of some volcanological observations spanning the period covered by our analysis, we propose the temporary accumulation of a gas cloud at some level within the plumbing system of the volcano to have acted as a joint source. The present work is a further evidence of the potential of continuous gravity observations as a tool to monitor and study active volcanoes and encourages their employment in spite of the difficulty of running spring gravimeters in a continuous fashion under the adverse conditions normally encountered on the summit zone of an active volcano

Localizzazione probabilistica 3D (NonLinLoc) applicata all’area calabro-peloritana

Sono presentati e discussi i risultati preliminari relativi ad una ri-localizzazione probabilistica non-lineare 3D dei terremoti dell’area compresa tra il Tirreno meridionale e l’Arco Calabro-Peloritano (Italia meridionale). Scopo del lavoro è dimostrare che l’applicazione di un’approccio probabilistico non-lineare nella localizzazione dei terremoti può fornire dei risultati più accurati ai fini della sorveglianza, ovviando al problema degli outlier, rispetto alle tecniche di localizzazione lineari (e.g. Hypoellipse), che minimizzano simultaneamente tutti i residui tra fasi osservate e calcolate. Il programma utilizzato è NonLinLoc [Lomax, et al., 2000; Lomax, et al., 2001; Lomax, 2005; http://www.alomax.net/nlloc; NonLinLoc di seguito] il quale permette di effettuare un’efficiente ricerca globale dello spazio dei parametri ipocentrali (coordinate spaziali e tempo origine) ottenendo una stima della funzione densità di probabilità (pdf, probability density function) a posteriori. La pdf fornisce una descrizione completa della localizzazione e delle sue incertezze; il campionamento dello spazio dei parametri ipocentrali è stato fatto mediante la tecnica Oct-tree nella regione compresa tra 37.75 e 39.40 N in latitudine e tra 14.80 e 16.80 E in longitudine, e utilizzando tutti gli eventi con profondità H ≤30 km. La struttura dell’Oct-tree è stata imposta in 100,000 celle ed un insieme di queste celle viene poi salvata in modo da poter rappresentare graficamente la pdf mediante nubi di punti a diversa densità. Il dataset utilizzato per le nostre analisi è composto da 1,304 terremoti, di 1.0<M<4.3, registrati nel periodo compreso tra il 1994 e il 2006; il modello di velocità 3D adottato è stato ottenuto da Barberi et al., 2008 [poster presentato a questo convegno] invertendo lo stesso dataset, mediante l’utilizzo del software TomoDD. I risultati ottenuti sono stati confrontati sia con le localizzazioni 1D (Hypoellipse) che con quelle 3D. Si evidenzia una maggiore clusterizzazione degli eventi e, soprattutto, un evidente miglioramento della qualità delle localizzazioni utilizzando il modello di velocità crostale 3D. Per cui riteniamo che, l’applicazione del metodo probabilistico associato ad un buon modello di velocità 3D, può essere utilizzato ai fini di sorveglianza

Comparative performance of precommercial cellulases hydrolyzing pretreated corn stover

<p>Abstract</p> <p>Background</p> <p>Cellulases and related hydrolytic enzymes represent a key cost factor for biochemical conversion of cellulosic biomass feedstocks to sugars for biofuels and chemicals production. The US Department of Energy (DOE) is cost sharing projects to decrease the cost of enzymes for biomass saccharification. The performance of benchmark cellulase preparations produced by Danisco, DSM, Novozymes and Verenium to convert pretreated corn stover (PCS) cellulose to glucose was evaluated under common experimental conditions and is reported here in a non-attributed manner.</p> <p>Results</p> <p>Two hydrolysis modes were examined, enzymatic hydrolysis (EH) of PCS whole slurry or washed PCS solids at pH 5 and 50°C, and simultaneous saccharification and fermentation (SSF) of washed PCS solids at pH 5 and 38°C. Enzymes were dosed on a total protein mass basis, with protein quantified using both the bicinchoninic acid (BCA) assay and the Bradford assay. Substantial differences were observed in absolute cellulose to glucose conversion performance levels under the conditions tested. Higher cellulose conversion yields were obtained using washed solids compared to whole slurry, and estimated enzyme protein dosages required to achieve a particular cellulose conversion to glucose yield were extremely dependent on the protein assay used. All four enzyme systems achieved glucose yields of 90% of theoretical or higher in SSF mode. Glucose yields were reduced in EH mode, with all enzymes achieving glucose yields of at least 85% of theoretical on washed PCS solids and 75% in PCS whole slurry. One of the enzyme systems ('enzyme B') exhibited the best overall performance. However in attaining high conversion yields at lower total enzyme protein loadings, the relative and rank ordered performance of the enzyme systems varied significantly depending upon which hydrolysis mode and protein assay were used as the basis for comparison.</p> <p>Conclusions</p> <p>This study provides extensive information about the performance of four precommercial cellulase preparations. Though test conditions were not necessarily optimal for some of the enzymes, all were able to effectively saccharify PCS cellulose. Large differences in the estimated enzyme dosage requirements depending on the assay used to measure protein concentration highlight the need for better consensus methods to quantify enzyme protein.</p

The MEV project: design and testing of a new high-resolution telescope for Muography of Etna Volcano

The MEV project aims at developing a muon telescope expressly designed for the muography of Etna Volcano. In particular, one of the active craters in the summit area of the volcano would be a suitable target for this experiment. A muon tracking telescope with high imaging resolution was built and tested during 2017. The telescope is a tracker based on extruded scintillating bars with WLS fibres and featuring an innovative read-out architecture. It is composed of three XY planes with a sensitive area of \SI{1}{m^2}; the angular resolution does not exceeds \SI{0.4}{\milli\steradian} and the total angular aperture is about $\pm$\SI{45}{\degree}. A special effort concerned the design of mechanics and electronics in order to meet the requirements of a detector capable to work in a hostile environment such as the top of a tall volcano, at a far distance from any facility. The test phase started in January 2017 and ended successfully at the end of July 2017. An extinct volcanic crater (the Monti Rossi, in the village of Nicolosi, about 15km from Catania) is the target of the measurement. The detector acquired data for about 120 days and the preliminary results are reported in this work

Localizzazione probabilistica 3D (NonLinLoc) applicata all’area calabro-peloritana

Sono presentati e discussi i risultati preliminari relativi ad una ri-localizzazione probabilistica non-lineare 3D dei terremoti dell’area compresa tra il Tirreno meridionale e l’Arco Calabro-Peloritano (Italia meridionale). Scopo del lavoro è dimostrare che l’applicazione di un’approccio probabilistico non-lineare nella localizzazione dei terremoti può fornire dei risultati più accurati ai fini della sorveglianza, ovviando al problema degli outlier, rispetto alle tecniche di localizzazione lineari (e.g. Hypoellipse), che minimizzano simultaneamente tutti i residui tra fasi osservate e calcolate. Il programma utilizzato è NonLinLoc [Lomax, et al., 2000; Lomax, et al., 2001; Lomax, 2005; http://www.alomax.net/nlloc; NonLinLoc di seguito] il quale permette di effettuare un’efficiente ricerca globale dello spazio dei parametri ipocentrali (coordinate spaziali e tempo origine) ottenendo una stima della funzione densità di probabilità (pdf, probability density function) a posteriori. La pdf fornisce una descrizione completa della localizzazione e delle sue incertezze; il campionamento dello spazio dei parametri ipocentrali è stato fatto mediante la tecnica Oct-tree nella regione compresa tra 37.75 e 39.40 N in latitudine e tra 14.80 e 16.80 E in longitudine, e utilizzando tutti gli eventi con profondità H ≤30 km. La struttura dell’Oct-tree è stata imposta in 100,000 celle ed un insieme di queste celle viene poi salvata in modo da poter rappresentare graficamente la pdf mediante nubi di punti a diversa densità. Il dataset utilizzato per le nostre analisi è composto da 1,304 terremoti, di 1.0<M<4.3, registrati nel periodo compreso tra il 1994 e il 2006; il modello di velocità 3D adottato è stato ottenuto da Barberi et al., 2008 [poster presentato a questo convegno] invertendo lo stesso dataset, mediante l’utilizzo del software TomoDD. I risultati ottenuti sono stati confrontati sia con le localizzazioni 1D (Hypoellipse) che con quelle 3D. Si evidenzia una maggiore clusterizzazione degli eventi e, soprattutto, un evidente miglioramento della qualità delle localizzazioni utilizzando il modello di velocità crostale 3D. Per cui riteniamo che, l’applicazione del metodo probabilistico associato ad un buon modello di velocità 3D, può essere utilizzato ai fini di sorveglianza

Advances in the study of geophysical signals from Mt. Etna volcano.

Long-period seismic signals, including LP events and tremor, observed on many volcanoes worldwide, may play a crucial role in the forecasting of volcanic eruptions as these signals are direct indicators of sub-surface magma dynamics. Their location is widely agreed to be useful for mapping the extension and geometry of the plumbing system and also for quantifying pressure transients caused by resonance or movement of fluids along the conduits. At Mt. Etna detailed investigations on these signals started systematically only after the installation of a broad-band seismic network (since 2003). Thereafter, we present the main results recently obtained on this volcano by analysing tremor, LP and VLP events during two eruptive episodes in the second half of 2007. We also discuss results of cross analysis performed between tremor and gravity sequences acquired simultaneously at Mt. Etna during the 2002-03 eruption and during the December 2005-January 2006 period of quiescence. We detected common anomalies which are indicative of a quasi-closed system, becoming progressively enriched in volatiles. These studies, carried out in the framework of the VOLUME Project, provide new insight into the shallow plumbing system of Etna and grant valuable tools for volcanic hazard forecasting and risk mitigation

Volume Flow Rate Estimation for Small Explosions at Mt. Etna, Italy, From Acoustic Waveform Inversion

Rapid assessment of the volume and the rate at which gas and pyroclasts are injected into the atmosphere during volcanic explosions is key to effective eruption hazard mitigation. Here, we use data from a dense infrasound network deployed in 2017 on Mt. Etna, Italy, to estimate eruptive volume flow rates (VFRs) during small gas-and-ash explosions.We use a finite-difference time-domain approximation to compute the acoustic Green's functions and perform a full waveform inversion for a multipole source, combining monopole and horizontal dipole terms. The inversion produces realistic estimates of VFR, on the order of 4 × 104 m3/s and well-defined patterns of source directivity. This is the first application of acoustic waveform inversion at Mt. Etna. Our results demonstrate that acoustic waveform inversion is a mature and robust tool for assessment of source parameters and holds potential as a tool to provide rapid estimates of VFR in near real time.This study was supported by NERC Grant NE/P00105X/1 and by European Unions Horizon 2020 Research and Innovation Programme Under the Marie Sklodowska-Curie Grant Agreement 798480

Messina 1908-2008: understanding crust dynamics and subduction in Southern Italy

To mark the centennial anniversary of the 1908 earthquake that shook Messina, Italy, the Istituto Nazionale di Geofisica e Vulcanologia (INGV) has begun the "Messina 1908- 2008" research project. The aim is to clarify the extension deformation processes that occur in the Messina Strait and to understand relationships between subduction and crustal deformation there by merging existing data and studies, and by collecting new and more detailed seismological, geodetic, historical, and satellite observations. More than 20 permanent seismic stations and about 15 temporary stations are located in the study region. A dense permanent geodetic network also operates in the region, several campaign surveys are newly available, and new geodetic campaign measurements were performed in March 2008. In addition, during July 2008, five ocean bottom seismometers (OBS) were deployed to better monitor the area largely covered by the sea. Records of historical earthquakes that struck the Strait of Messina will be analyzed, and synthetic aperture radar images will help define surface deformation of the region. The Messina 1908-2008 project's assemblage of a database and integration of innovative technologies could transform our understanding of the crust and mantle structure of the active tectonics and seismic hazards of the Strait of Messina

The Relationship between Gait Velocity and Walking Pattern in Hemiplegic Patients

Abstract: Background Gait speed represents a functional predictor and an impairment severity index in stroke survivors; gait analysis parameters are descriptors of walking strategies used to compensate for the muscle impairment such as vaulting, circumduction and hip hiking. The aim of this study was to assess if there is a relationship between the gait compensatory strategy and gait speed of progression. Methods A sample of 30 patients with post-stroke hemiparesis was assessed for gait compensatory patterns through gait analysis and videorecording. BMI, pain-VAS, Barthel Index, Nottingham Extended ADL Scale, Motricity Index, lower limb muscles strength and aROMs were also included in the assessment. Results In 19 patients it was possible to identify one or more compensatory strategies; in 11 patients no specific gait pattern was found. The vaulting and hip hiking combined gait strategy had an effect on gait speed. Gait speed was directly related to Barthel Index, Nottingham Extended ADL Scale, Motricity Index of the paretic side and in particular with quadriceps and iliopsoas strength and hip extension aROM. Gender, age and paretic side did not influence gait speed. Conclusion Compensatory gait strategies influence gait speed but studies with larger sample size are needed to better highlight their impact