UMTS rapid response real-time seismic networks: implementation and strategies at INGV

The benefits of portable real-time seismic networks are several and well known. During the management of a temporary experiment from the real-time data it is possible to detect and fix rapidly problems with power supply, time synchronization, disk failures and, most important, seismic signal quality degradation due to unexpected noise sources or sensor alignment/tampering. This usually minimizes field maintenance trips and maximizes both the quantity and the quality of the acquired data. When the area of the temporary experiment is not well monitored by the local permanent network, the real-time data from the temporary experiment can be fed to the permanent network monitoring system improving greatly both the real-time hypocentral locations and the final revised bulletin. All these benefits apply also in case of seismic crises when rapid deployment stations can significantly contribute to the aftershock analysis. Nowadays data transmission using meshed radio networks or satellite systems is not a big technological problem for a permanent seismic network where each site is optimized for the device power consumption and is usually installed by properly specialized technicians that can configure transmission devices and align antennas. This is not usually practical for temporary networks and especially for rapid response networks where the installation time is the main concern. These difficulties are substantially lowered using the now widespread UMTS technology for data transmission. A small (but sometimes power hungry) properly configured device with an omnidirectional antenna must be added to the station assembly. All setups are usually configured before deployment and this allows for an easy installation also by untrained personnel. We describe here the implementation of a UMTS based portable seismic network for both temporary experiments and rapid response applications developed at INGV. The first field experimentation of this approach dates back to the 2009 L’Aquila aftershock sequence and since then it has been customized and refined to overcome most reliability and security issues using an industry standard VPN architecture that allows to avoid UMTS provider firewall problems and does not expose to the Internet the usually weak and attack prone data acquisition ports. With this approach all the devices are protected inside a local network and the only exposed port is the VPN server one. This solution improves both the security and the bandwidth available to data transmission. While most of the experimentation has been carried out using the RefTek units of the INGV Mobile Network this solution applies equally well to most seismic data loggers available on the market. Overall the UMTS data transmission has been used in most temporary seismic experiments and in all seismic emergencies happened in Italy since 2010 and has proved to be a very cost effective approach with real-time data acquisition rates usually greater than 97% and all the benefits that result from the fast integration of the temporary data in the National Network monitoring system and in the EIDA data bank

UMTS rapid response real-time seismic networks: implementation and strategies at INGV

<abstract> <p>Universal Mobile Telecommunications System (UMTS) and its evolutions are nowadays the most affordable and widespread data communication infrastructure available almost world wide. Moreover the always growing cellular phone market is pushing the development of new devices with higher performances and lower power consumption. All these characteristics make UMTS really useful for the implementation of an â easy to deployâ temporary real-time seismic station. Despite these remarkable features, there are many drawbacks that must be properly taken in account to effectively transmit the seismic data: Internet security, signal and service availability, power consumption. <list list-type="bullet"><list-item> <p>Internet security: exposing seismological data services and seismic stations to the Internet is dangerous, attack prone and can lead to downtimes in the services, so we setup a dedicated Virtual Private Network (VPN) service to protect all the connected devices.</p></list-item><list-item> <p>Signal and service availability: while for temporary experiment a carefull planning and an accurate site selection can minimize the problem, this is not always the case with rapid response networks. Moreover, as with any other leased line, the availability of the UMTS service during a seismic crisis is basically unpredictable. Nowadays in Italy during a major national emergency a Committee of the Italian Civil Defense ensures unified management and coordination of emergency activities. Inside it the telecom companies are committed to give support to the crisis management improving the standards in their communication networks.</p></list-item><list-item> <p>Power consumption: it is at least of the order of that of the seismic station and, being related to data flow and signal quality is largely unpredictable. While the most secure option consists in adding a second independent solar power supply to the seismic station, this is not always a very convenient solution since it doubles the cost and doubles the equipment on site. We found that an acceptable trade-off is to add an inexpensive Low Voltage Disconnect (LVD) circuit to the UMTS router power supply that switches off the data transmission when the power is low. This greatly reduces the probability of data loss but lowers the real-time data availabilty. This approach guarantees on the average a satisfactory data acquistion rate, only in very few cases and when the real-time data is extremely important for a particular site we needed to double the power supply on the site.</p></list-item></list></p> <p>Overall the UMTS data transmission has been used in most temporary seismic experiments and in all seismic emergencies happened in Italy since 2010 and has proved to be a very cost effective approach with real-time data acquisition rates usually greater than 97â ¯% and all the benefits that result from the fast integration of the temporary data in the National Network monitoring system and in the EIDA data bank.</p> </abstract

UMTS rapid response real-time seismic networks: implementation and strategies at INGV

The benefits of portable real-time seismic networks are several and well known. During the management of a temporary experiment from the realtime data it is possible to detect and fix rapidly problems with power supply, time synchronization, disk failures and, most important, seismic signal quality degradation due to unexpected noise sources or sensor alignment/tampering. This usually minimizes field maintenance trips and maximizes both the quantity and the quality of the acquired data. When the area of the temporary experiment is not well monitored by the local permanent network, the real-time data from the temporary experiment can be fed to the permanent network monitoring system improving greatly both the real-time hypocentral locations and the final revised bulletin. All these benefits apply also in case of seismic crises when rapid deployment stations can significantly contribute to the aftershock analysis. Nowadays data transmission using meshed radio networks or satellite systems is not a big technological problem for a permanent seismic network where each site is optimized for the device power consumption and is usually installed by properly specialized technicians that can configure transmission devices and align antennas. This is not usually practical for temporary networks and especially for rapid response networks where the installation time is the main concern. These difficulties are substantially lowered using the now widespread UMTS technology for data transmission. A small (but sometimes power hungry) properly configured device with an omnidirectional antenna must be added to the station assembly. All setups are usually configured before deployment and this allows for an easy installation also by untrained personnel

Polarised kink waves in magnetic elements: evidence for chromospheric helical waves

In recent years, new high spatial resolution observations of the Sun's atmosphere have revealed the presence of a plethora of small-scale magnetic elements down to the resolution limit of the current cohort of solar telescopes (~100–120 km on the solar photosphere). These small magnetic field concentrations, due to the granular buffeting, can support and guide several magnetohydrodynamic wave modes that would eventually contribute to the energy budget of the upper layers of the atmosphere. In this work, exploiting the high spatial and temporal resolution chromospheric data acquired with the Swedish 1 m Solar Telescope, and applying the empirical mode decomposition technique to the tracking of the solar magnetic features, we analyze the perturbations of the horizontal velocity vector of a set of chromospheric magnetic elements. We find observational evidence that suggests a phase relation between the two components of the velocity vector itself, resulting in its helical motion

Experimental evaluation of the thermal polarization in direct contact membrane distillation using electrospun nanofiber membranes doped with molecular probes

Membrane distillation (MD) has recently gained considerable attention as a valid process for the production of fresh-water due to its ability to exploit low grade waste heat for operation and to ensure a nearly feed concentration-independent production of high-purity distillate. Limitations have been related to polarization phenomena negatively affecting the thermal efficiency of the process and, as a consequence, its productivity. Several theoretical models have been developed to predict the impact of the operating conditions of the process on the thermal polarization, but there is a lack of experimental validation. In this study, electrospun nanofiber membranes (ENMs) made of Poly(vinylidene fluoride) (PVDF) and doped with (1, 10-phenanthroline) ruthenium (II) Ru(phen) 3 were tested at different operating conditions (i.e., temperature and velocity of the feed) in direct contact membrane distillation (DCMD). The temperature sensitive luminophore, Ru(phen) 3 , allowed the on-line and non-invasive mapping of the temperature at the membrane surface during the process and the experimental evaluation of the effect of the temperature and velocity of the feed on the thermal polarization

Emergenza sismica nel Frusinate (Ottobre 2009 – Gennaio 2010): l’intervento della Rete Sismica Mobile stand-alone e l’analisi dati

Tra il 30 settembre ed il 22 ottobre del 2009 una piccola area della provincia di Frosinone, presso la località di Campoli Appennino, non lontana dalla città di Sora e dal confine con l’Abruzzo, è stata interessata da uno sciame sismico la cui fase più intensa è stata raggiunta nella notte tra il 7 e l’8 di ottobre con due scosse di magnitudo locale (ML) 3.6 e 3.4. Nei primi 23 giorni della sequenza (30 settembre – 22 ottobre) sono state registrate ben 1075 scosse, tutte con magnitudo non superiore a 3.6. In precedenza, nei mesi di maggio e giugno del 2009, si era attivata una piccola area posta ad una quindicina di chilometri a NW di Campoli Appennino, esattamente nella zona montuosa che separa la Val Roveto dalla Vallelonga in territorio abruzzese. Questo piccolo sciame è stato caratterizzato da 64 eventi con ML non superiore a 2.7. Diverse sono state le ragioni che hanno indotto il team scientifico alla guida della Rete Sismica Mobile della sede di Roma [Re.Mo., Moretti et al., 2010a] a disporre nei primi giorni del mese di ottobre un intervento di emergenza nell’area che include i comuni di Sora, Atina, San Donato in Val Comino e Pescasseroli tra le provincie di Frosinone e de L’Aquila: 1) la relativa vicinanza delle due zone epicentrali sopra descritte alla regione dell’Aquilano colpita solo pochi mesi prima dal forte evento sismico del 6 aprile 2009 (ML 5.8, MW 6.31) [Chiarabba et al., 2009; Margheriti et al., 2010], 2) l’emotività della popolazione originatasi a seguito del forte trauma vissuto e 3) non ultimo la psicosi collettiva notevolmente alimentata dai media locali e nazionali. In tutto, sono state installate 4 stazioni sismiche temporanee ad integrazione delle permanenti già presenti in area epicentrale al fine di migliorarne il monitoraggio. In questo lavoro viene presentato l’intervento della Re.Mo. riportando le motivazioni che lo hanno guidato e la tempistica delle operazioni svolte. Inoltre, verrà fornita una breve descrizione delle caratteristiche geologico-strutturali e sismotettoniche dell’area e saranno mostrate alcune analisi eseguite sui dati acquisiti in campagna

MESENCHIMAL STEM CELLS IN INFLAMMATORY BOWEL DISEASES: CLINICAL EVIDENCES AND POTENTIAL INSIGHTS FOR THE CLINICIANS

Mesenchimal stem cells (MSCs) have been used experimentally and clinically in the treatment of a wide variety of pathologies MSCs can be safely transplanted in autologous and allogenic ways as they are non-immunogenic, and consequently represent a therapeutic option for refractory connective tissue diseases, fibrosing diseases like scleroderma and fistulizing colitis like in Crohn's disease (CD). The immunomodulatory properties of MSCs have already shown promise when used as therapy for otherwise medically refractory CD. Accumulating evidence suggests that the properties may also be exploited of several other conditions. The currently available experimental and clinical data indicate that, similar to previously obtained data in the setting of HSCT, MSC treatment for IBD is feasible and safe. aim of this review is to analyze the pathophysiological insights for the use of MSCs in inflammatory bowel diseases, and to summarize the clinical evidences about the efficacy and safety of stem cell therapy in such disorders

Organoids of Human Endometrium: A Powerful In Vitro Model for the Endometrium-Embryo Cross-Talk at the Implantation Site

Embryo implantation has been defined as the "black box" of human reproduction. Most of the knowledge on mechanisms underlining this process derives from animal models, but they cannot always be translated to humans. Therefore, the development of an in vitro/ex vivo model recapitulating as closely and precisely as possible the fundamental functional features of the human endometrial tissue is very much desirable. Here, we have validated endometrial organoids as a suitable 3D-model to studying epithelial endometrial interface for embryo implantation. Transmission and scanning electron microscopy analyses showed that organoids preserve the glandular organization and cell ultrastructural characteristics. They also retain the responsiveness to hormonal treatment specific to the corresponding phase of the menstrual cycle, mimicking the in vivo glandular-like aspect and functions. Noteworthy, organoids mirroring the early secretive phase show the development of pinopodes, large cytoplasmic apical protrusions of the epithelial cells, traditionally considered as reliable key features of the implantation window. Moreover, organoids express glycodelin A (GdA), a cycle-dependent marker of the endometrial receptivity, with its quantitative and qualitative features accounting well for the profile detected in the endometrium in vivo. Accordingly, organoids deriving from the eutopic endometrium of women with endometriosis show a GdA glycosylation pattern significantly different from healthy organoids, confirming our prior data on endometrial tissues. The present results strongly support the idea that organoids may closely recapitulate the molecular and functional characteristics of their cells/tissue of origin

La Rete Sismica Mobile del Centro Nazionale Terremoti

Il monitoraggio sismico e vulcanico del territorio nazionale rappresenta uno dei principali compiti istituzionali dell’Istituto Nazionale di Geofisica e Vulcanologia (INGV). L’INGV svolge tale importante funzione attraverso la gestione e la manutenzione di reti sismiche di diversa tipologia e a differente scala che consentono di monitorare il territorio nazionale in tempo reale. Tre sale di sorveglianza, una sismica presso la sede centrale di Roma e due vulcaniche presso la Sezione di Catania e l’Osservatorio Vesuviano di Napoli, con personale qualificato in turno H24, consentono di elaborare e comunicare tempestivamente al Dipartimento della Protezione Civile Nazionale (DPC) e alle sue strutture regionali eventuali stati di allarme e il livello dell’emergenza. Il Centro Nazionale Terremoti (CNT) è la sezione dell’INGV preposta al monitoraggio sismico del territorio italiano ed interviene in questo importante servizio attraverso la gestione e la manutenzione della Rete Sismica Nazionale (RSN) in collaborazione con le altre sedi dell’INGV dislocate sul territorio e con gli uffici tecnici locali. Competenza del CNT è anche la rete sismica euro-mediterranea (MedNet): una rete di stazioni sismiche a larga banda dislocate nei Paesi che circondano il Mediterraneo in condivisione con molti istituti geofisici. Negli ultimi anni tali reti sono cresciute sia come numero di stazioni che come tecnologia, consentendo di controllare in maniera estesa lo spettro di frequenze emesse dalla sorgente sismica e la ciclicità delle strutture sismogenetiche. In alcune aree del territorio nazionale l’alta densità di tali reti sismiche rende possibile una soglia di detezione degli eventi molto bassa e localizzazioni di elevata precisione che permettono di associare la micro-sismicità alle strutture sismo-genetiche. Tuttavia questo non è tecnicamente ed economicamente possibile in maniera omogenea su tutto il territorio nazionale. Per tale motivo si fa spesso ricorso all’uso di reti temporanee in esperimenti mirati allo studio di aree a peculiare rischio sismico e vulcanico o, in caso di forti terremoti, per aumentare la densità della rete già presente e migliorare il monitoraggio in real-time in modo tale da analizzare con maggior dettaglio l’evoluzione della sequenza. Unità specializzate nella gestione di reti sismologiche temporanee sono presenti in diverse sedi dell’INGV. Esse lavorano in completa autonomia sul territorio di competenza ma sono in grado di realizzare un buon livello di sinergia là dove esperimenti ed emergenze sismiche richiedano una stretta collaborazione. La struttura più grande, sia come numero di strumenti a disposizione (più di 200 tra digitalizzatori e sensori) che come personale impegnato, è la Rete Sismica Mobile (RSM) del CNT che è organizzata in modo da rendere possibile l’impiego della strumentazione in più esperimenti mantenendo una quota di strumenti riservata per gli interventi di emergenza. In questo rapporto tecnico presentiamo la struttura organizzativa ed operativa della RSM del CNT, la strumentazione in uso presso di essa e le diverse configurazioni possibili per le stazioni sismometriche temporanee con l’obiettivo di fornire un manuale d’uso ai ricercatori, tecnologi e tecnici che si interfacciano con la RSM, sia durante l’attività scientifica ordinaria (esperimenti di sismica passiva e attiva) che straordinaria (emergenze sismiche)