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  Laboratori Analitici  
Spettrometria di Massa a Ioni Secondari (SIMS) - Microsonda ionica
Secondary Ion Mass Spectrometry (SIMS) - Ion microprobe
  Laboratori Analitici  
Laboratorio di Spettrometria di Massa a Ioni Secondari (SIMS) - Microsonda ionica
Secondary Ion Mass Spectrometry (SIMS) - Ion microprobe Laboratory
  Un nuovo articolo: Ultr...  
L'importanza di questi risultati, ottenuti mediante profili SIMS del rapporto di ioni 7Li/30Si in cristalli di plagioclasio provenienti da prodotti della sequenza parossistica del Mt. Etna (periodo 2011-2013), si basa sull'applicazione di metodi, recentemente utilizzati esclusivamente per vulcani a sistema-chiuso che producono eruzioni violente, a sistemi a condotto aperto caratterizzati da periodi di attività eruttiva generalmente tranquilla, a volte interrotti da un repentino risveglio ed eruzioni particolarmente energetiche.
The importance of these results, obtained by SIMS profiles of the 7Li/30Si ion ratio in plagioclase crystals from products of the paroxysmal sequence of Mt. Etna (period 2011–2013), relies on the application of methods, recently used exclusively for closed system volcanoes producing violent eruptions, to open-conduit systems characterized by generally quiet eruptive periods of activity, sometimes interrupted by sudden re-awakening and the production of anomalously energetic eruptions.
  Laboratori TIMS  
Nella tecnica TIMS, l'elemento da analizzare deve essere separato dalla matrice, tipicamente in un laboratorio con camere bianche, caricato su un filamento sottile di Re o Ta e quindi ionizzato in una sorgente ultra sottovuoto per effetto Joule.
In the TIMS technique, the element to be analyzed needs to be separated from the matrix, usually in a clean room laboratory, then loaded on a very thin Re or Ta ribbon and ionized in a ultra vacuum source by Joule’s effect. Produced ions, moved and focused by electromagnetic fields, enter into a magnetic separator, where they are differentially bent according to their mass/charge ratios. Then, the ion beams are collected and analyzed into one or more detectors.
  Bilaterale Italia-Taiwan  
I traccianti geochimici (ioni, molecole o isotopi non interessati da reazioni chimiche secondarie una volta che entrano in un sistema geologico come un serbatoio geotermico e i geoindicatori (ioni, molecole o isotopi) partecipano a reazioni chimiche secondarie in condizioni chimico-fisiche controllate sono dei parametri utili che possono essere applicati con successo ad acque termali e gas liberi durante l'esplorazione geotermica per stimare:
Geochemical tracers, i.e. ions, molecules or isotopes not affected by secondary chemical reactions once entering a geological system such a geothermal reservoir, and geoindicators, i.e. ions, molecules or isotopes expected to participate at secondary chemical reactions at controlled physical-chemical conditions, are useful parameters, which can successfully be applied to thermal water and gas discharges during geothermal exploration for estimating i) the geochemical features of geothermal reservoirs and ii) their equilibrium temperature and redox conditions. The main aim of the present proposal is that to depict a geological-geochemical conceptual model in the Ilan area (northern-eastern Taiwan), where this approach has not been applied, although geophysical studies and preliminary geochemical data have indicated this area as a potentially favorable site for geothermal exploitation. The previously described concepts will be applied to two Italian hydrothermal systems: a) the active volcanic system of Vulcano (characterized by relatively high temperature fumarolic discharges) and b) the extinct volcanic complex of Vicano-Cimini since previous investigations have suggested this area is a not exploited geothermal field.
  Bilaterale Italia-Taiwan  
I traccianti geochimici (ioni, molecole o isotopi non interessati da reazioni chimiche secondarie una volta che entrano in un sistema geologico come un serbatoio geotermico e i geoindicatori (ioni, molecole o isotopi) partecipano a reazioni chimiche secondarie in condizioni chimico-fisiche controllate sono dei parametri utili che possono essere applicati con successo ad acque termali e gas liberi durante l'esplorazione geotermica per stimare:
Geochemical tracers, i.e. ions, molecules or isotopes not affected by secondary chemical reactions once entering a geological system such a geothermal reservoir, and geoindicators, i.e. ions, molecules or isotopes expected to participate at secondary chemical reactions at controlled physical-chemical conditions, are useful parameters, which can successfully be applied to thermal water and gas discharges during geothermal exploration for estimating i) the geochemical features of geothermal reservoirs and ii) their equilibrium temperature and redox conditions. The main aim of the present proposal is that to depict a geological-geochemical conceptual model in the Ilan area (northern-eastern Taiwan), where this approach has not been applied, although geophysical studies and preliminary geochemical data have indicated this area as a potentially favorable site for geothermal exploitation. The previously described concepts will be applied to two Italian hydrothermal systems: a) the active volcanic system of Vulcano (characterized by relatively high temperature fumarolic discharges) and b) the extinct volcanic complex of Vicano-Cimini since previous investigations have suggested this area is a not exploited geothermal field.