46 results on '"Di Genova, D."'
Search Results
2. The effect of iron and alkali on the nanocrystal-free viscosity of volcanic melts: A combined Raman spectroscopy and DSC study
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Stabile, P., Sicola, S., Giuli, G., Paris, E., Carroll, M.R., Deubener, J., and Di Genova, D.
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- 2021
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3. A compositional tipping point governing the mobilization and eruption style of rhyolitic magma
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Di Genova, D., Kolzenburg, S., Wiesmaier, S., Dallanave, E., Neuville, D. R., Hess, K. U., and Dingwell, D. B.
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Observations ,Measurement ,Viscosity -- Observations -- Measurement ,Magma -- Observations ,Rhyolite -- Observations - Abstract
Author(s): D. Di Genova (corresponding author) [1, 2]; S. Kolzenburg [2]; S. Wiesmaier [2]; E. Dallanave [2]; D. R. Neuville [3]; K. U. Hess [2]; D. B. Dingwell [2] The [...]
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- 2017
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4. Heat capacity, configurational heat capacity and fragility of hydrous magmas
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Di Genova, D., Romano, C., Giordano, D., and Alletti, M.
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- 2014
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5. The effect of CO2 and H2O on Etna and Fondo Riccio (Phlegrean Fields) liquid viscosity, glass transition temperature and heat capacity
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Di Genova, D., Romano, C., Alletti, M., Misiti, V., and Scarlato, P.
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- 2014
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6. Crystallisation in basaltic magmas revealed via in situ 4D synchrotron X-ray microtomography
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Polacci, M., Arzilli, F., La Spina, G., Le Gall, N., Cai, B., Hartley, M. E., Di Genova, D., Vo, N. T., Nonni, S., Atwood, R. C., Llewellin, E. W., Lee, P. D., and Burton, M. R.
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- 2018
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7. Modeling Viscosity of Volcanic Melts With Artificial Neural Networks
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Langhammer, D., primary, Di Genova, D., additional, and Steinle‐Neumann, G., additional
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- 2022
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8. Heat capacity of hydrous trachybasalt from Mt Etna: comparison with CaAl2Si2O8 (An)–CaMgSi2O6 (Di) as basaltic proxy compositions
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Giordano, D., Nichols, A. R. L., Potuzak, M., Di Genova, D., Romano, C., and Russell, J. K.
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- 2015
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9. A calibrated database of Raman spectra for natural silicate glasses: implications for modelling melt physical properties
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Giordano D.[1, 2, 3, Gonzalez-Garcia D.[1], Russell J.K.[5], Raneri S.[6], Bersani D.[7], Fornasini L.[7], Di Genova D.[8], Ferrando S.[1], Kaliwoda M.[4, Lottici P.P.[7], Smit M.[5], and Dingwell D.B.[4]
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Materials science ,Analytical chemistry ,silicate-melts ,glasses ,symbols.namesake ,Viscosity ,Raman spectroscopy ,viscosity ,symbols ,General Materials Science ,Silicate glass ,Spectroscopy - Abstract
The physical properties of silicate melts are of critical importance for understanding magmatic and volcanic processes on Earth and other planets. Most physical properties of melts are, ultimately, a consequence of the structural organization of the melt. Robust and fully generalizable strategies for the prediction of properties of naturally occurring melts as functions of composition, temperature, and pressure remain a challenging goal. Given the structural origin of macroscopic properties, Raman spectroscopy of glasses, which provides information on melt and glass structure, may provide a useful technique to understanding and quantify variations in macroscopic melt properties. Here, with the aim of providing a generalizable model for predicting the viscosity of silicate melts, we present the results of a Raman spectroscopy campaign performed on 30 anhydrous multicomponent silicate glasses resulting from quenching of remelted and homogenized volcanic rocks and synthetic equivalents. The sample suite comprises one of the largest databases of multicomponent melts for which (a) chemical compositions and (b) physical properties (i.e., viscosity, fragility, heat capacity, and glass transition temperature) are known. Raman spectra have been collected using green light sources at wavelengths of 532 nm. Spectra were collected on the same sample suite in four independent laboratories involving instruments from different manufacturers and, thus, using different spectrometers, detectors, and analytical conditions. Our results are also compared and integrated with published data on some of the same samples derived from two others setups using green light sources with 514.5 and 532 nm wavelegths. For the same sample, the Raman spectra acquired using different setups show different intensities and intensity ratios. However, a strategy based on the ratio between the lowâEUR and highâEURwavenumber peaks (R) was developed to standardize the data to normalized Raman ratios (Rn) and thus to remove interlaboratory differences. Using these advances, we predict melt viscosity solely with the use of Raman spectral measurements of multicomponent silicate glasses, thus demonstrating the potential of the method in describing physical properties of silicate melts.
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- 2019
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10. Explosivity of basaltic lava fountains is controlled by magma rheology, ascent rate and outgassing
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La Spina, G., Arzilli, F., Llewellin, E.W., Burton, M.R., Clarke, A.B., de' Michieli Vitturi, M., Polacci, M., Hartley, M.E., Di Genova, D., and Mader, H.M.
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- 2021
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11. Modeling the Viscosity of Anhydrous and Hydrous Volcanic Melts
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Langhammer, D., primary, Di Genova, D., additional, and Steinle‐Neumann, G., additional
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- 2021
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12. The microanalysis of iron and sulphur oxidation states in silicate glass - Understanding the effects of beam damage
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Hughes, E C, primary, Buse, B, additional, Kearns, S L, additional, Brooker, R A, additional, Di Genova, D, additional, Kilgour, G, additional, Mader, H M, additional, and Blundy, J D, additional
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- 2020
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13. Quantifying Microstructural Evolution in Moving Magma
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Dobson, K.J., Allabar, A., Bretagne, E., Coumans, J., Cassidy, M., Cimarelli, C., Coats, R., Connolley, T., Courtois, L., Dingwell, D.B., Di Genova, D., Fernando, B., Fife, J.L., Fyfe, F., Gehne, S., Jones, T., Kendrick, J.E., Kinvig, H., Kolzenburg, S., Lavallée, Y., Liu, E., Llewellin, E.W., Madden-Nadeau, A., Madi, K., Marone, F., Morgan, C., Oppenheimer, J., Ploszajski, A., Reid, G., Schauroth, J., Schlepütz, C.M., Sellick, C., Vasseur, J., von Aulock, F.W., Wadsworth, F.B., Wiesmaier, S., Wanelik, K., Dobson, K.J., Allabar, A., Bretagne, E., Coumans, J., Cassidy, M., Cimarelli, C., Coats, R., Connolley, T., Courtois, L., Dingwell, D.B., Di Genova, D., Fernando, B., Fife, J.L., Fyfe, F., Gehne, S., Jones, T., Kendrick, J.E., Kinvig, H., Kolzenburg, S., Lavallée, Y., Liu, E., Llewellin, E.W., Madden-Nadeau, A., Madi, K., Marone, F., Morgan, C., Oppenheimer, J., Ploszajski, A., Reid, G., Schauroth, J., Schlepütz, C.M., Sellick, C., Vasseur, J., von Aulock, F.W., Wadsworth, F.B., Wiesmaier, S., and Wanelik, K.
- Abstract
Many of the grand challenges in volcanic and magmatic research are focused on understanding the dynamics of highly heterogeneous systems and the critical conditions that enable magmas to move or eruptions to initiate. From the formation and development of magma reservoirs, through propagation and arrest of magma, to the conditions in the conduit, gas escape, eruption dynamics, and beyond into the environmental impacts of that eruption, we are trying to define how processes occur, their rates and timings, and their causes and consequences. However, we are usually unable to observe the processes directly. Here we give a short synopsis of the new capabilities and highlight the potential insights that in situ observation can provide. We present the XRheo and Pele furnace experimental apparatus and analytical toolkit for the in situ X-ray tomography-based quantification of magmatic microstructural evolution during rheological testing. We present the first 3D data showing the evolving textural heterogeneity within a shearing magma, highlighting the dynamic changes to microstructure that occur from the initiation of shear, and the variability of the microstructural response to that shear as deformation progresses. The particular shear experiments highlighted here focus on the effect of shear on bubble coalescence with a view to shedding light on both magma transport and fragmentation processes. The XRheo system is intended to help us understand the microstructural controls on the complex and non-Newtonian evolution of magma rheology, and is therefore used to elucidate the many mobilization, transport, and eruption phenomena controlled by the rheological evolution of a multi-phase magmatic flows. The detailed, in situ characterization of sample textures presented here therefore represents the opening of a new field for the accurate parameterization of dynamic microstructural control on rheological behavior.
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- 2020
14. The effect of oxygen fugacity on the rheological evolution of crystallizing basaltic melts
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Kolzenburg, S., Di Genova, D., Giordano, D., Hess, K.U., and Dingwell, D.B.
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- 2018
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15. Magmatic sulfide immiscibility at an active magmatic-hydrothermal system: The case of La Fossa (Vulcano, Italy)
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Fulignati, P., primary, Gioncada, A., additional, Costa, S., additional, Di Genova, D., additional, Di Traglia, F., additional, and Pistolesi, M., additional
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- 2018
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16. Raman spectra of Martian glass analogues: a tool to approximate their chemical composition
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Di Genova, D., Kolzenburg, Stephan, V. o. n. a., A., C. h. e. v. r. e. l., M. O., Hess, K. U., N. e. u. v. i. l. l. e., D. R., Ertel I. n. g. r. i. s. c. h., W., R. o. m. a. n. o., C., and Dingwell, D. B.
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- 2016
17. EP-1374: Hypofractionated radiotherapy in nonmelanoma skin cancer ≥ 3 cm in elderly PTS
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Ferella, L., primary, Parente, S., additional, Gravina, G.L., additional, Bonfili, P., additional, Di Staso, M., additional, Franzese, P., additional, La Verghetta, M.E., additional, Cerasani, M., additional, Di Genova, D., additional, and Di Cesare, E., additional
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- 2017
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18. New insights on the rheological properties of a rocksalt
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Speranza, G., Vinciguerra, S., Di Genova, D., Romano, C., Vona, A., Mollo, Silvio, Iarocci, A., Speranza, G, Vinciguerra, S, Di Genova, D, Romano, Claudia, Vona, Alessandro, Mollo, S, and Iarocci, A.
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- 2013
19. Explosive mafic eruptions: the fall-out phase of the 'Pozzolane Nere Fm.' (Colli Albani Volcanic District, Rome)
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CAMPAGNOLA, SILVIA, VONA, ALESSANDRO, ROMANO, Claudia, GIORDANO, Guido, Di Genova D., Campagnola, Silvia, Romano, Claudia, Giordano, Guido, Vona, Alessandro, and Di Genova, D.
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- 2012
20. Spectra of volcanic rocks glasses as analogues of Mercury surface spectra
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Carli C, Capaccioni F, De Sanctis M, Filacchione G, Sgavetti M, Di Genova D, Visonà D, Ammannito E., VONA, ALESSANDRO, Carli, C, Capaccioni, F, De Sanctis, M, Filacchione, G, Sgavetti, M, Di Genova, D, Vona, Alessandro, Visonà, D, and Ammannito, E.
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- 2010
21. Rheological and Thermodynamic Properties of Volatile-bearing Magmas from Pantelleria, Etna and Phlegrean Fields Magmas
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Di Genova, D., Romano, C., Alletti, Marina, Behrens, H., Scaillet, Bruno, Paläontologisches Institut und Museum, Universität Zürich [Zürich] = University of Zurich (UZH), Institut des Sciences de la Terre d'Orléans (ISTO), and Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)
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Experimental volcanism ,[1011] GEOCHEMISTRY ,[SDE.MCG]Environmental Sciences/Global Changes ,[8445] VOLCANOLOGY ,[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology ,Geochemical modeling ,Thermodynamics ,Lava rheology and morphology ,[8429] VOLCANOLOGY ,[1009] GEOCHEMISTRY - Abstract
International audience; The rheological and thermodynamic properties of silicate melts control fluid-dynamics of transport, eruption style and rates of physico-chemical processes (degassing and crystallization) in natural magmas. In this study we investigated the effect of H2O and CO2 on the liquid viscosity and heat capacity on several multicomponent systems. Measurements were conducted on four series of melts, obtained by remelting and homogenization of natural pantelleritic (Khaggiar dome, Pantelleria), trachytic (Agnano Monte Spina eruption, Phlegrean Fields), latitic (Fondo Riccio eruption, Phlegrean Fields) and trachybasaltic (Etna 1992 eruption) magmas. CO2 or H2O synthesis experiments were conducted in piston cylinder apparatus. The volatile -bearing samples were measured with a differential scanning calorimeter (DSC) and a vertical dilatometer (micropenetration technique). Water and CO2 content were measured by Karl Fisher Titration and FTIR spectroscopy. Compositions were analyzed over a range of water contents up to 5.3 wt% and CO2 content up to 4000 ppm. Viscosity ranged from 108 to 1013 Pa s with decreasing temperature from 630 to 1100 K. Viscosity is strongly affected by H2O and CO2. The effect of CO2 on viscosity appears to be a function of speciation and chemical composition. The heat capacity of glasses and liquids and the glass transition interval were also investigated. Base chemical composition have a strong influences on Tg: high alkali contents can lower Tg of low NBO/T liquids. This behavior is demonstrated by Pantellerite samples. Glass transition temperatures are also strongly affected by H2O and CO2. The CO2 effect, such as water, is to decrease Tg and it appears to be a function of chemical composition. We present data for partial molar CpH2Omol and CpOH- and derive a simple expression to evaluate the relative contributions of different H-bearing species to the total heat capacity of hydrous melts. Experimental viscosity and calorimetric data were fitted according to the Adam and Gibbs theory in which configurational entropy (Sconf) is the main factor controlling the viscosity of melts. From calorimetric measurements, and assuming that the vibrational contribution to the liquid Cp remains constant above Tg, we determined the configurational contribution to Cpliq and thus calculated the variation of the Sconf as a function of T, H2O and CO2 content in the liquid state. Combining viscosity measurements with the configurational entropies for our liquids, we parameterized the variation of viscosity as a function of temperature and volatiles content within the framework of the Adam and Gibbs theory of structural relaxation.
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- 2011
22. A combined integrated multi-method approach for the assessment of the thermal maturity of sedimentary basins
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Di Paolo, L.., additional, Corrado, S.., additional, Romano, C.., additional, Aldega, L.., additional, Di Genova, D.., additional, and Grigo, D.., additional
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- 2014
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23. PO-0941: MEK/ERK inhibition radiosensitizes rhabdomyosarcoma cells by downregulating growth and DNA repair signals
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Marampon, F., primary, Gravina, G.L., additional, La Verghetta, M.E., additional, Cerasani, M., additional, Parente, S., additional, Mancini, M., additional, Di Genova, D., additional, Ferella, L., additional, Reale, M., additional, and Di Cesare, E., additional
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- 2014
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24. EP-1369: PDRNs intravesical instillations reduces symptoms of interstitial radiation-induced cystitis
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Bonfili, P., primary, Franzese, P., additional, Di Staso, M., additional, Ruggieri, V., additional, Di Genova, D., additional, Mancini, M., additional, Cerasani, M., additional, Reale, M., additional, Ferella, L., additional, and Di Cesare, E., additional
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- 2014
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25. EP-1377: Percutaneous radiofrequency ablation followed by radiotherapy in the management of painful bone metastases
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Di Staso, M., primary, Bonfili, P., additional, Franzese, P., additional, Gravina, G.L., additional, Ruggieri, V., additional, Marampon, F., additional, Mancini, M., additional, Di Genova, D., additional, Vittorini, F., additional, and Di Cesare, E., additional
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- 2014
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26. PO-0942: MEK/ERK-AURORA-B/DNA-PK Pathway activation regulates radioresistance of gynecological cancer cell lines
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Marampon, F., primary, La Verghetta, M.E., additional, Cerasani, M., additional, Gravina, G.L., additional, Parente, S., additional, Mancini, M., additional, Di Genova, D., additional, Ferella, L., additional, Reale, M., additional, and Di Cesare, E., additional
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- 2014
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27. The rheology of peralkaline rhyolites from Pantelleria Island
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Di Genova, D., primary, Romano, C., additional, Hess, K.-U., additional, Vona, A., additional, Poe, B.T., additional, Giordano, D., additional, Dingwell, D.B., additional, and Behrens, H., additional
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- 2013
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28. IBM System z10 Open Systems Adapter Ethernet data router
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Haynie, H. M., primary, Turner, J. M., additional, Hanscom, J. C., additional, Cadigan, M., additional, Hadzic, N., additional, Di Genova, D., additional, Aylward, J., additional, Salisbury, S. W., additional, Sciuto, P., additional, Needham, T. D., additional, Bubb, C. E., additional, and Tremaine, R. B., additional
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- 2009
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29. Determination of cooling rates of glasses over four orders of magnitude
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Alex Scarani, Alessandro Vona, Danilo Di Genova, Raschid Al-Mukadam, Claudia Romano, Joachim Deubener, Scarani, A., Vona, A., Di Genova, D., Al-Mukadam, R., Romano, C., and Deubener, J.
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Geophysics ,Parallel shift factor ,Differential scanning calorimetry ,Viscosity ,Geochemistry and Petrology ,Cooling rate ,Gla - Abstract
Volcanic materials can experience up to eleven orders of magnitude of cooling rate (qc) starting from 10–5 K s−1. The glassy component of volcanic material is routinely measured via differential scanning calorimeter (DSC) to obtain qc through the determination of the glass fictive temperature (Tf). Conventional DSC (C-DSC), which has been employed for decades, can only access a relatively small range of qc (from ~ 10–2 to ~ 1 K s−1). Therefore, extrapolations up to six orders of magnitude of C-DSC data are necessary to derive qc of glasses quenched both at extremely low and high qc. Here, we test the reliability of such extrapolations by combining C-DSC with the recently introduced flash calorimetry (F-DSC). F-DSC enables to extend the qc exploration up to 104 K s−1. We use three synthetic glasses as analogs of volcanic melts. We first apply a normalization procedure of heat flow data for both C-DSC and F-DSC to derive Tf as a function of experimental qc, following the “unified area-matching” approach. The obtained Tf–qc relationship shows that Arrhenius models, widely adopted in previous studies, are only valid for qc determination within the calibration range. In contrast, a non-Arrhenius model better captures qc values, especially when a significant extrapolation is required. We, therefore, present a practical “how-to” protocol for estimating qc using DSC.
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- 2022
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30. Modeling the Viscosity of Anhydrous and Hydrous Volcanic Melts
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Danilo Di Genova, D. Langhammer, Gerd Steinle-Neumann, Di Genova, D., 1 Bayerisches Geoinstitut Universität Bayreuth Bayreuth Germany, and Steinle‐Neumann, G.
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geography ,geography.geographical_feature_category ,Thermodynamics ,volcanoes ,magmas ,glasses ,crystal ,DSC ,Crystal ,Viscosity ,Geophysics ,Volcano ,Geochemistry and Petrology ,viscosity ,ddc:550.724 ,Anhydrous ,ddc:552.2 ,Geology - Abstract
The viscosity of volcanic melts is a dominant factor in controlling the fluid dynamics of magmas and thereby eruption style. It can vary by several orders of magnitude, depending on temperature, chemical composition, and water content. The experimentally accessible temperature range is restricted by melt crystallization and gas exsolution. Therefore, modeling viscosity as a function of temperature and water content is central to physical volcanology. We present a model that describes these dependencies by combining a physically motivated equation for temperature dependence of viscosity and a glass transition temperature (Tg) model for the effects of water. The equation uses the viscosity at infinite temperature η∞, Tg, and the steepness factor m as fitting parameters. We investigate the effect of leaving η∞ free as a parameter and fixing its value, by fitting anhydrous viscosity data of 45 volcanic melts using the temperature dependent model. Both approaches describe experimental data well. Using a constant η∞ therefore provides a viable route for extrapolating viscosity from data restricted to small temperature intervals. Our model describes hydrous data over a wide compositional range of terrestrial magmas (26 data sets) with comparable or better quality than literature fits. With η∞ constrained, we finally apply our model to viscosities derived by differential scanning calorimetry and find—by comparing to viscometry based data and models—that this approach can be used to reliably describe the dependence of viscosity on temperature and water content. This introduces important implications for modeling the effects of nanostructure formation on viscosity., Plain Language Summary: How violently a volcano erupts strongly depends on the viscosity of the ascending magma. Temperature and the amount of dissolved water in the magma significantly impact viscosity. Therefore, models that predict it as a function of these parameters are of great interest and can be calibrated by measured data. We find a model that performs comparably to or better than other published ones. One model parameter describes the viscosity at infinite temperature; we investigate whether this is a constant value for all melts, and find this to be a justifiable assumption that leads to accurate predictions. Finally, we explore the possibility of deriving viscosity via differential scanning calorimetry (DSC). This approach avoids or significantly reduces melt crystallization which is a possible consequence of using more common measurement methods. By combining the constant value for the infinite temperature viscosity with DSC‐derived data, our model can accurately predict viscosity at any relevant temperature., Key Points: We provide a temperature‐ and water‐dependent viscosity model for volcanic melts that performs better or comparable to literature models. Anhydrous data are fit to explore the constant infinite temperature viscosity. Polymerized melts skew results toward lower values. Differential scanning calorimetry data enable extrapolation of viscosity to any temperature using a constant value at infinite temperature., Deutsche Forschungsgemeinschaft (DFG) http://dx.doi.org/10.13039/501100001659
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- 2021
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31. The unexpected explosive sub-Plinian eruption of Calbuco volcano (22–23 April 2015; southern Chile): Triggering mechanism implications
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Margherita Polacci, Margaret E. Hartley, Jonathan Fellowes, Danilo Di Genova, Daniele Morgavi, Laura Spina, Maurizio Petrelli, Juan Díaz-Alvarado, Jorge E. Romero, Fabio Arzilli, Diego Perugini, Mike Burton, Giuseppe La Spina, Arzilli, F., Morgavi, D., Petrelli, M., Polacci, M., Burton, M., Di Genova, D., Spina, L., La Spina, G., Hartley, M. E., Romero, J. E., Fellowes, J., Diaz-Alvarado, J., and Perugini, D.
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geography ,Volcanic hazards ,geography.geographical_feature_category ,010504 meteorology & atmospheric sciences ,Explosive material ,Calbuco ,Crystallisation ,Internal trigger ,Sub-Plinian eruption ,Volcanic hazard ,Geochemistry ,Pyroclastic rock ,010502 geochemistry & geophysics ,01 natural sciences ,Intrusion ,Geophysics ,Volcano ,13. Climate action ,Geochemistry and Petrology ,Magma ,Geology ,0105 earth and related environmental sciences - Abstract
Plinian-type eruptions are extremely hazardous, producing pyroclastic fallout and flows extending many kilometres from the vent. The most commonly invoked eruption trigger for Plinian-type eruptions is the intrusion of fresh magma, generally associated with precursory ground deformation and seismicity days/weeks before eruption. Closed-system internal triggering has also been proposed, such as protracted crystallisation of magma, which can produce a build-up of exsolved volatiles and thus pressurise the system prior to eruption. On 22–23 April 2015 Calbuco volcano, Chile, produced a sub-Plinian eruption with 2O) and formed phenocrysts of titanomagnetite, orthopyroxene, clinopyroxene and plagioclase cores (An78–93). Gradual cooling of the magma chamber produced thermal gradients and magma convection, evidenced by plagioclase overgrowth rims (An58–77) and blocky microlites (25–250 μm). Our interpretation is that this continuing crystallisation induced second boiling and an over-pressurisation of the system, leading to the rapid onset of the 2015 eruption. Petrological and geochemical evidence therefore shows that a closed-system magma chamber can evolve into a highly explosive eruption with very little precursory warning, posing a challenge for current volcano monitoring paradigms. We propose that internal triggering should be carefully considered as a mechanism for unexpected sub-Plinian eruptions, prompting a potential revision of existing hazard management strategies.
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- 2019
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32. Mixed electrical conduction in a hydrous pantellerite glass
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Brent T. Poe, Claudia Romano, Danilo Di Genova, Piergiorgio Scarlato, Harald Behrens, Poe B., T, Romano, Claudia, Di Genova, D, Behrens, H, and Scarlato, P.
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Diffusion ,Inorganic chemistry ,silicate melt ,Geology ,Activation energy ,Conductivity ,Thermal conduction ,Polaron ,Geochemistry and Petrology ,Electrical resistivity and conductivity ,pantellerites ,Anhydrous ,Ionic conductivity ,electrival conductivity - Abstract
Electrical conductivity measurements were carried out on pantelleritic trachyte glasses containing up to 3.5 wt.% dissolved H 2 O. At temperatures below about 700 K, we find evidence for small polaron conduction due to the presence of both ferrous and ferric iron in the glass. At the higher temperatures of the investigation (up to 973 K), a marked change in the conductivity–temperature relation is observed, which suggests that an ionic conduction mechanism becomes the dominant means of charge transport. In the ionic conduction regime, conductivity increases with increasing H 2 O concentration. Activation energies are similar for both the anhydrous and hydrous glasses, indicating that the conductivity is controlled by sodium diffusion even for the highest H 2 O concentration examined. A slight variation in activation energy is observed depending on the H 2 O concentration, which is most likely associated with the depolymerising effect of dissolved water on the silicate network structure. At low temperatures, we find a dramatic effect of fO 2 on the conductivity that supports an electronic conduction mechanism based on small polaron hopping between Fe 3+ and Fe 2+ sites. This electronic pathway controls the overall electrical conductivity in these alkali-rich glasses at temperatures exceeding 500 °C if conditions remain anhydrous at an oxygen fugacity of 0.2 atm.
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- 2012
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33. Heat capacity of hydrous trachybasalt from Mt Etna: comparison with CaAl2Si2O8 (An)–CaMgSi2O6 (Di) as basaltic proxy compositions
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Claudia Romano, James K. Russell, Alexander R. L. Nichols, Danilo Di Genova, Marcel Potuzak, Daniele Giordano, Giordano, D, Nichols, A. R. L., Potuzak, M., Di Genova, D., Romano, Claudia, and Russell, J. K.
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Specific heat ,Chemistry ,Mineralogy ,Anorthite–diopside ,Hydrous silicate melt ,engineering.material ,Anorthite ,Etna trachybasalt ,Heat capacity ,Crystallography ,Differential scanning calorimetry ,Geophysics ,Polymerization ,Geochemistry and Petrology ,engineering ,Hydrous silicate melts ,Glass transition ,Natural bond orbital ,Trachybasalt - Abstract
The specific heat capacity (C p) of six variably hydrated (~3.5 wt% H2O) iron-bearing Etna trachybasaltic glasses and liquids has been measured using differential scanning calorimetry from room temperature across the glass transition region. These data are compared to heat capacity measurements on thirteen melt compositions in the iron-free anorthite (An)–diopside (Di) system over a similar range of H2O contents. These data extend considerably the published C p measurements for hydrous melts and glasses. The results for the Etna trachybasalts show nonlinear variations in, both, the heat capacity of the glass at the onset of the glass transition (i.e., C p g ) and the fully relaxed liquid (i.e., C p l ) with increasing H2O content. Similarly, the “configurational heat capacity” (i.e., C p c = C p l − C p g ) varies nonlinearly with H2O content. The An–Di hydrous compositions investigated show similar trends, with C p values varying as a function of melt composition and H2O content. The results show that values in hydrous C p g , C p l and C p c in the depolymerized glasses and liquids are substantially different from those observed for more polymerized hydrous albitic, leucogranitic, trachytic and phonolitic multicomponent compositions previously investigated. Polymerized melts have lower C p l and C p c and higher C p g with respect to more depolymerized compositions. The covariation between C p values and the degree of polymerization in glasses and melts is well described in terms of SMhydrous and NBO/T hydrous. Values of C p c increase sharply with increasing depolymerization up to SMhydrous ~ 30–35 mol% (NBO/T hydrous ~ 0.5) and then stabilize to an almost constant value. The partial molar heat capacity of H2O for both glasses ( $$ C_{{{\text{p}}\;{\text{H}}_{2} {\text{O}}}}^{\text{g}} $$ ) and liquids ( $$ C_{{{\text{p}}\;{\text{H}}_{2} {\text{O}}}}^{\text{l}} $$ ) appears to be independent of composition and, assuming ideal mixing, we obtain a value for $$ C_{{{\text{p}}\;{\text{H}}_{2} {\text{O}}}}^{\text{l}} $$ of 79 J mol−1 K−1. However, we note that a range of values for $$ C_{{{\text{p}}\;{\text{H}}_{2} {\text{O}}}}^{\text{l}} $$ (i.e., ~78–87 J mol−1 K−1) proposed by previous workers will reproduce the extended data to within experimental uncertainty. Our analysis suggests that more data are required in order to ascribe a compositional dependence (i.e., nonideal mixing) to $$ C_{{{\text{p}}\;{\text{H}}_{2} {\text{O}}}}^{\text{l}} $$ .
- Published
- 2015
34. The effect of CO2 and H2O on Etna and Fondo Riccio (Phlegrean Fields) liquid viscosity, glass transition temperature and heat capacity
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Danilo Di Genova, Claudia Romano, Valeria Misiti, Marina Alletti, Piergiorgio Scarlato, Dipartimento di Scienze [Roma], Università degli Studi Roma Tre, Department of Earth and Environmental Sciences [München], Ludwig-Maximilians-Universität München (LMU), Institut des Sciences de la Terre d'Orléans - UMR7327 (ISTO), Centre National de la Recherche Scientifique (CNRS)-Université d'Orléans (UO)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers en région Centre (OSUC), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Bureau de Recherches Géologiques et Minières (BRGM) (BRGM), Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Palermo, INGV-DPC V1 (2012-2013), DI GENOVA, D, Romano, Claudia, Alletti, M, Misiti, V, and Scarlato, P.
- Subjects
010504 meteorology & atmospheric sciences ,[SDE.MCG]Environmental Sciences/Global Changes ,Thermodynamics ,Calorimetry ,010502 geochemistry & geophysics ,01 natural sciences ,Heat capacity ,Viscosity ,Phlegrean Fields ,Differential scanning calorimetry ,Fragility ,Geochemistry and Petrology ,[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology ,glass transition ,Dissolution ,0105 earth and related environmental sciences ,Chemistry ,Geology ,volatiles ,Temperature dependence of liquid viscosity ,13. Climate action ,viscosity ,Etna ,CO2 ,Glass transition ,calorimetry - Abstract
International audience; Viscosity (η), glass transition (Tg) and heat capacity (Cp) of Etna trachybasalt and Fondo Riccio latite (Phlegrean Fields, Italy) were determined at low and high temperature for dry, hydrous and CO2 bearing samples. High temperature experiments have been performed in the range of 1499 to 1700 K by concentric cylinder measurements, while low temperature experiments were carried out in the interval between 633 and 1093 K using the micropenetration technique. Glass transition temperature, glassy and liquid heat capacities were investigated using differential scanning calorimetry (DSC) up to 955 K. The H2O content in the melts ranged from nominally dry to 6.32 wt%, while CO2 ranged from 229 to 1907 ppm. We combined low- and high-temperature viscosities and parameterized them by the use of a modified Vogel-Fulcher-Tamman equation, which accommodates the non-Arrhenian temperature dependence of melt viscosity. Experimental measurements show that melt viscosity decreases with increasing temperature, water and CO2 content. For latitic samples at 893 K, the introduction of CO2 (up to 732 ppm) decreases the liquid viscosity up to one order of magnitude with respect to the measured viscosity for H2O-bearing liquid. Moreover, the results of calorimetric measurements indicate that the glass transition temperature decreases with increasing volatiles content (H2O + CO2). The glass transition temperature decreases by about 25 K by adding up to 1907 ppm of CO2 in the trachybasaltic samples. No appreciable effect on glassy [Cpg (Tg)] and liquid (Cpliq) heat capacity was observed with the addition of water and CO2. Structural and volcanological implication (i.e. volatiles speciation and melt fragility) for water and CO2 dissolution in silicate melts are discussed in light of the presented results.
- Published
- 2014
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35. Unique formation of organic glass from a human brain in the Vesuvius eruption of 79 CE.
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Giordano G, Pensa A, Vona A, Di Genova D, Al-Mukadam R, Romano C, Deubener J, Frontoni A, and Petrone P
- Subjects
- Humans, Male, Vitrification, Brain physiology, Glass chemistry, Volcanic Eruptions
- Abstract
Glass forms when a liquid is fast cooled preventing crystallization, across a reversible process known as the glass transition. Organic tissues are commonly preserved as glass by processes of vitrification at very low temperatures, known as cryopreservation, and can return to their original soft state when heated back to ambient temperature. It would therefore be impossible to find organic glass embedded in volcanic deposits that have reached several hundred of Celsius degrees. Here we demonstrate that material with glassy appearance found within the skull of a seemingly male human body entombed within the hot pyroclastic flow deposits of the 79 CE Vesuvius eruption formed by a unique process of vitrification of his brain at very high temperature, and is the only such occurrence on Earth. Calorimetric analyses show that the temperature at which the brain transformed into glass was well above 510 °C, implying that the body was exposed to the passage and vanishing of a short-lived, dilute and much hotter pyroclastic flow, explaining its early fast heating and the following very fast cooling. The glass that formed as a result of such a unique process attained a perfect state of preservation of the brain and its microstructures., Competing Interests: Declarations. Competing interests: The authors declare no competing interests., (© 2025. The Author(s).)
- Published
- 2025
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36. Prevalence of Gastrointestinal Parasites in Small Ruminant Farms in Southern Spain.
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Rufino-Moya PJ, Zafra Leva R, Gonçalves Reis L, Acosta García I, Ruiz Di Genova D, Sánchez Gómez A, García García F, and Martínez-Moreno FJ
- Abstract
The primary population of small ruminants in Spain is concentrated in the southern region, a critical area for the country's livestock production. Indirect economic losses can occur when this livestock is affected by gastrointestinal parasites. This study aimed to determine the prevalence of these parasites in small ruminant herds (159 sheep and 39 goats) through coprological analyses and conducted a survey on farmers' management practices related to gastrointestinal parasite control. The survey results revealed some important aspects: monitoring through coprological analyses is not a common practice; veterinarians are not typically involved in deworming plans; anthelmintic treatment in adults is often applied twice a year in sheep and once a year in goats; and finally, drug rotation was higher in sheep farms. Coprological analyses showed Eimeria spp. as the most common parasitic infection, followed by Strongyles infection. Other parasites like Moniezia spp., Trichuris spp., and D. dendriticum were less important, although their prevalence was higher in sheep than goats. This constitutes the first report on the epidemiological status of gastrointestinal parasites in small ruminants in southern Spain. Based on the survey findings, the introduction of certain management measures on farms could potentially mitigate parasite infections.
- Published
- 2024
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37. Dendritic crystallization in hydrous basaltic magmas controls magma mobility within the Earth's crust.
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Arzilli F, Polacci M, La Spina G, Le Gall N, Llewellin EW, Brooker RA, Torres-Orozco R, Di Genova D, Neave DA, Hartley ME, Mader HM, Giordano D, Atwood R, Lee PD, Heidelbach F, and Burton MR
- Abstract
The majority of basaltic magmas stall in the Earth's crust as a result of the rheological evolution caused by crystallization during transport. However, the relationships between crystallinity, rheology and eruptibility remain uncertain because it is difficult to observe dynamic magma crystallization in real time. Here, we present in-situ 4D data for crystal growth kinetics and the textural evolution of pyroxene during crystallization of trachybasaltic magmas in high-temperature experiments under water-saturated conditions at crustal pressures. We observe dendritic growth of pyroxene on initially euhedral cores, and a surprisingly rapid increase in crystal fraction and aspect ratio at undercooling ≥30 °C. Rapid dendritic crystallization favours a rheological transition from Newtonian to non-Newtonian behaviour within minutes. We use a numerical model to quantify the impact of rapid dendritic crystallization on basaltic dike propagation, and demonstrate its dramatic effect on magma mobility and eruptibility. Our results provide insights into the processes that control whether intrusions lead to eruption or not., (© 2022. The Author(s).)
- Published
- 2022
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38. Development of a CAPS Marker and a LAMP Assay for Rapid Detection of Xylella fastidiosa Subsp. multiplex and Differentiation from X. fastidiosa Subsp. fastidiosa on Blueberry.
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Waliullah S, Di Genova D, Oliver JE, and Ali ME
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- DNA Primers genetics, Polymerase Chain Reaction methods, Blueberry Plants microbiology, Genetic Markers genetics, Molecular Diagnostic Techniques methods, Nucleic Acid Amplification Techniques methods, Plant Diseases microbiology, Xylella genetics
- Abstract
Bacterial leaf scorch (BLS), caused by Xylella fastidiosa ( Xf ), is a prevalent disease of blueberries in the southeastern United States. Initially, this disease was reported to be caused by X. fastidiosa subsp. multiplex ( Xfm ). However, a recent survey revealed the presence of another subspecies, X. fastidiosa subsp. fastidiosa ( Xff ), within naturally infected blueberry plantings in Georgia. Since knowledge regarding the origins of isolates causing Xf outbreaks can impact management recommendations, a routine method for identifying the pathogen at the subspecies level can be beneficial. Several detection strategies are available to identify Xf infection at the subspecies level. However, none of these have been developed for the routine and rapid differentiation of the blueberry-infecting Xf subspecies. Here, we developed two separate straightforward and rapid detection techniques, a cleaved amplified polymorphic sequence (CAPS) marker, and a loop-mediated isothermal amplification (LAMP) assay, targeting the RNA polymerase sigma-70 factor ( rpoD ) gene sequence of Xfm to discriminate between the two Xf subspecies infecting blueberry. With the CAPS marker, specific detection of Xfm isolates was possible from pure cultures, inoculated greenhouse-grown plant samples, and field infected blueberry samples by restriction digestion of the rpoD gene PCR product (amplified with primers RST31 and RST33) using the Bts I enzyme. The LAMP assay allowed for specific real-time amplification of a 204-bp portion of the Xfm rpoD gene from both pure bacterial cultures and infected plant material using the Genie
® III system, a result further affirmed by gel electrophoresis and SYBR™ Green I DNA staining for visual observation. These detection strategies have the potential to greatly aid existing diagnostic methods for determining the distribution and prevalence of these Xf subspecies causing bacterial leaf scorch (BLS) in blueberries in the southeastern United States.- Published
- 2022
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39. Using the Social Robot NAO for Emotional Support to Children at a Pediatric Emergency Department: Randomized Clinical Trial.
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Rossi S, Santini SJ, Di Genova D, Maggi G, Verrotti A, Farello G, Romualdi R, Alisi A, Tozzi AE, and Balsano C
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- Aminoacridines, Child, Emergency Service, Hospital, Female, Humans, Male, Parents, Social Interaction, Robotics
- Abstract
Background: Social robots (SRs) have been used for improving anxiety in children in stressful clinical situations, such as during painful procedures. However, no studies have yet been performed to assess their effect in children while waiting for emergency room consultations., Objective: This study aims to assess the impact of SRs on managing stress in children waiting for an emergency room procedure through the assessment of salivary cortisol levels., Methods: This was an open randomized clinical trial in children attending a pediatric emergency department. Children accessing the emergency room were randomized to 1 of 3 groups: (1) playing with a NAO SR, (2) playing with a study nurse, or (3) waiting with parents. The salivary cortisol levels of all children were measured through a swab. Salivary cortisol levels before and after the intervention were compared in the 3 groups. We calculated the effect size of our interventions through the Cohen d-based effect size correlation (r)., Results: A total of 109 children aged 3-10 years were enrolled in the study, and 94 (86.2%) had complete data for the analyses. Salivary cortisol levels significantly decreased more in the group exposed to robot interaction than in the other two groups (r=0.75). Cortisol levels decreased more in girls (r=0.92) than in boys (r=0.57)., Conclusions: SRs are efficacious in decreasing stress in children accessing the emergency room and may be considered a tool for improving emotional perceptions of children and their families in such a critical setting., Trial Registration: ClinicalTrials.gov NCT04627909; https://clinicaltrials.gov/ct2/show/study/NCT04627909., (©Silvia Rossi, Silvano Junior Santini, Daniela Di Genova, Gianpaolo Maggi, Alberto Verrotti, Giovanni Farello, Roberta Romualdi, Anna Alisi, Alberto Eugenio Tozzi, Clara Balsano. Originally published in the Journal of Medical Internet Research (https://www.jmir.org), 13.01.2022.)
- Published
- 2022
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40. Estimating the viscosity of volcanic melts from the vibrational properties of their parental glasses.
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Cassetta M, Di Genova D, Zanatta M, Boffa Ballaran T, Kurnosov A, Giarola M, and Mariotto G
- Abstract
The numerical modelling of magma transport and volcanic eruptions requires accurate knowledge of the viscosity of magmatic liquids as a function of temperature and melt composition. However, there is growing evidence that volcanic melts can be prone to nanoscale modification and crystallization before and during viscosity measurements. This challenges the possibility of being able to quantify the crystal-free melt phase contribution to the measured viscosity. In an effort to establish an alternative route to derive the viscosity of volcanic melts based on the vibrational properties of their parental glasses, we have subjected volcanologically relevant anhydrous glasses to Brillouin and Raman spectroscopic analyses at ambient conditions. Here, we find that the ratio between bulk and shear moduli and the boson peak position embed the melt fragility. We show that these quantities allow an accurate estimation of volcanic melts at eruptive conditions, without the need for viscosity measurements. An extensive review of the literature data confirms that our result also holds for hydrous systems; this study thus provides fertile ground on which to develop new studies of the nanoscale dynamics of natural melts and its impact on the style of volcanic eruptions.
- Published
- 2021
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41. Natural Infection of Southern Highbush Blueberry ( Vaccinium corymbosum Interspecific Hybrids) by Xylella fastidiosa subsp. fastidiosa .
- Author
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Di Genova D, Lewis KJ, and Oliver JE
- Subjects
- Animals, Plant Diseases, Southeastern United States, Blueberry Plants, Infections, Xylella genetics
- Abstract
Xylella fastidiosa ( Xf ) is an emerging insect-vectored, xylem-limited bacterium that can cause disease on several economically important fruit and tree crops including almond, blueberry, citrus, grapevine, peach, and pecan. On blueberry, Xf causes bacterial leaf scorch (BLS), which is prevalent in the southeastern United States. This disease, previously reported to be caused by Xf subsp. multiplex ( Xfm ), can result in rapid plant decline and death of southern highbush (SHB) blueberry cultivars. In 2017, a survey of blueberry plantings in southern Georgia (U.S.A.) confirmed the presence of Xf -infected plants in eight of nine sites examined, and seven isolates were cultured from infected plants. Genetic characterization of these isolates through single-locus and multilocus sequence analysis revealed that three isolates from two sites belonged to Xf subsp. fastidiosa ( Xff ), with significant similarity to isolates from grapevine. After these three isolates were artificially inoculated onto greenhouse-grown SHB blueberries (cv. 'Rebel'), symptoms typical of BLS developed, and Xff infection was confirmed through genetic characterization and reisolation of the bacterium to fulfill Koch's postulates. Because all previously reported Xf isolates from blueberry have been characterized as Xfm , this is the first time that isolation of Xff has been reported from naturally infected blueberry plantings. The potential impact of Xff isolates on disease management in blueberry requires further exploration. Furthermore, given that isolates from both Xfm and Xff were obtained within a single naturally infected blueberry planting, blueberry in southern Georgia may provide opportunities for intersubspecific recombination between Xff and Xfm isolates.
- Published
- 2020
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42. In situ observation of nanolite growth in volcanic melt: A driving force for explosive eruptions.
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Di Genova D, Brooker RA, Mader HM, Drewitt JWE, Longo A, Deubener J, Neuville DR, Fanara S, Shebanova O, Anzellini S, Arzilli F, Bamber EC, Hennet L, La Spina G, and Miyajima N
- Abstract
Although gas exsolution is a major driving force behind explosive volcanic eruptions, viscosity is critical in controlling the escape of bubbles and switching between explosive and effusive behavior. Temperature and composition control melt viscosity, but crystallization above a critical volume (>30 volume %) can lock up the magma, triggering an explosion. Here, we present an alternative to this well-established paradigm by showing how an unexpectedly small volume of nano-sized crystals can cause a disproportionate increase in magma viscosity. Our in situ observations on a basaltic melt, rheological measurements in an analog system, and modeling demonstrate how just a few volume % of nanolites results in a marked increase in viscosity above the critical value needed for explosive fragmentation, even for a low-viscosity melt. Images of nanolites from low-viscosity explosive eruptions and an experimentally produced basaltic pumice show syn-eruptive growth, possibly nucleating a high bubble number density., (Copyright © 2020 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution License 4.0 (CC BY).)
- Published
- 2020
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43. Raman spectra of Martian glass analogues: A tool to approximate their chemical composition.
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Di Genova D, Kolzenburg S, Vona A, Chevrel MO, Hess KU, Neuville DR, Ertel-Ingrisch W, Romano C, and Dingwell DB
- Abstract
Raman spectrometers will form a key component of the analytical suite of future planetary rovers intended to investigate geological processes on Mars. In order to expand the applicability of these spectrometers and use them as analytical tools for the investigation of silicate glasses, a database correlating Raman spectra to glass composition is crucial. Here we investigate the effect of the chemical composition of reduced silicate glasses on their Raman spectra. A range of compositions was generated in a diffusion experiment between two distinct, iron-rich end-members (a basalt and a peralkaline rhyolite), which are representative of the anticipated compositions of Martian rocks. Our results show that for silica-poor (depolymerized) compositions the band intensity increases dramatically in the regions between 550-780 cm
-1 and 820-980 cm-1 . On the other hand, Raman spectra regions between 250-550 cm-1 and 1000-1250 cm-1 are well developed in silica-rich (highly polymerized) systems. Further, spectral intensity increases at ~965 cm-1 related to the high iron content of these glasses (~7-17 wt % of FeOtot ). Based on the acquired Raman spectra and an ideal mixing equation between the two end-members we present an empirical parameterization that enables the estimation of the chemical compositions of silicate glasses within this range. The model is validated using external samples for which chemical composition and Raman spectra were characterized independently. Applications of this model range from microanalysis of dry and hydrous silicate glasses (e.g., melt inclusions) to in situ field investigations and studies under extreme conditions such as extraterrestrial (i.e., Mars) and submarine volcanic environments.- Published
- 2016
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44. Approximate chemical analysis of volcanic glasses using Raman spectroscopy.
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Di Genova D, Morgavi D, Hess KU, Neuville DR, Borovkov N, Perugini D, and Dingwell DB
- Abstract
The effect of chemical composition on the Raman spectra of a series of natural calcalkaline silicate glasses has been quantified by performing electron microprobe analyses and obtaining Raman spectra on glassy filaments (~450 µm) derived from a magma mingling experiment. The results provide a robust compositionally-dependent database for the Raman spectra of natural silicate glasses along the calcalkaline series. An empirical model based on both the acquired Raman spectra and an ideal mixing equation between calcalkaline basaltic and rhyolitic end-members is constructed enabling the estimation of the chemical composition and degree of polymerization of silicate glasses using Raman spectra. The model is relatively insensitive to acquisition conditions and has been validated using the MPI-DING geochemical standard glasses1 as well as further samples. The methods and model developed here offer several advantages compared with other analytical and spectroscopic methods such as infrared spectroscopy, X-ray fluorescence spectroscopy, electron and ion microprobe analyses, inasmuch as Raman spectroscopy can be performed with a high spatial resolution (1 µm
2 ) without the need for any sample preparation as a nondestructive technique. This study represents an advance in efforts to provide the first database of Raman spectra for natural silicate glasses and yields a new approach for the treatment of Raman spectra, which allows us to extract approximate information about the chemical composition of natural silicate glasses using Raman spectroscopy. We anticipate its application in handheld in situ terrestrial field studies of silicate glasses under extreme conditions (e.g. extraterrestrial and submarine environments)., (© 2015 The Authors Journal of Raman Spectroscopy Published by John Wiley & Sons Ltd.)- Published
- 2015
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45. Hypoxia sustains glioblastoma radioresistance through ERKs/DNA-PKcs/HIF-1α functional interplay.
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Marampon F, Gravina GL, Zani BM, Popov VM, Fratticci A, Cerasani M, Di Genova D, Mancini M, Ciccarelli C, Ficorella C, Di Cesare E, and Festuccia C
- Subjects
- Benzamides pharmacology, Cell Hypoxia drug effects, Cell Hypoxia genetics, Cell Hypoxia radiation effects, Cell Line, Tumor, Gene Expression Regulation, Neoplastic drug effects, Gene Expression Regulation, Neoplastic radiation effects, Glioblastoma drug therapy, Glioblastoma radiotherapy, Humans, Hypoxia-Inducible Factor 1, alpha Subunit antagonists & inhibitors, Hypoxia-Inducible Factor 1, alpha Subunit genetics, MAP Kinase Signaling System drug effects, MAP Kinase Signaling System radiation effects, Radiation Tolerance drug effects, Butadienes pharmacology, Enzyme Inhibitors pharmacology, Glioblastoma pathology, Hypoxia-Inducible Factor 1, alpha Subunit metabolism, Nitriles pharmacology, Oxygen metabolism, Radiation Tolerance genetics
- Abstract
The molecular mechanisms by which glioblastoma multiforme (GBM) refracts and becomes resistant to radiotherapy treatment remains largely unknown. This radioresistance is partly due to the presence of hypoxic regions, which are frequently found in GBM tumors. We investigated the radiosensitizing effects of MEK/ERK inhibition on GBM cell lines under hypoxic conditions. Four human GBM cell lines, T98G, U87MG, U138MG and U251MG were treated with the MEK/ERK inhibitor U0126, the HIF-1α inhibitor FM19G11 or γ-irradiation either alone or in combination under hypoxic conditions. Immunoblot analysis of specific proteins was performed in order to define their anti‑oncogenic or radiosensitizing roles in the different experimental conditions. MEK/ERK inhibition by U0126 reverted the transformed phenotype and significantly enhanced the radiosensitivity of T98G, U87MG, U138MG cells but not of the U251MG cell line under hypoxic conditions. U0126 and ERK silencing by siRNA reduced the levels of DNA protein kinase catalytic subunit (DNA-PKcs), Ku70 and K80 proteins and clearly reduced HIF-1α activity and protein expression. Furthermore, DNA-PKcs siRNA-mediated silencing counteracted HIF-1α activity and downregulated protein expression suggesting that ERKs, DNA-PKcs and HIF-1α cooperate in radioprotection of GBM cells. Of note, HIF-1α inhibition under hypoxic conditions drastically radiosensitized all cell lines used. MEK/ERK signal transduction pathway, through the sustained expression of DNA-PKcs, positively regulates HIF-1α protein expression and activity, preserving GBM radioresistance in hypoxic condition.
- Published
- 2014
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46. Intravesical instillations with polydeoxyribonucleotides reduce symptoms of radiation-induced cystitis in patients treated with radiotherapy for pelvic cancer: a pilot study.
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Bonfili P, Franzese P, Marampon F, La Verghetta ME, Parente S, Cerasani M, Di Genova D, Mancini M, Vittorini F, Gravina GL, Ruggieri V, Di Staso M, Popov VM, Tombolini V, and Di Cesare E
- Subjects
- Administration, Intravesical, Aged, Female, Humans, Male, Middle Aged, Pelvis radiation effects, Pilot Projects, Cystitis drug therapy, Cystitis etiology, Pelvic Neoplasms radiotherapy, Polydeoxyribonucleotides administration & dosage, Radiation Injuries drug therapy, Radiation Injuries etiology
- Abstract
Purpose: Chronic radiation cystitis (CRC) is a serious complication that can arise in patients with pelvic malignancies treated with radiotherapy. Polydeoxyribonucleotides (PDRNs) are known to reduce inflammation and improve tissue perfusion and angiogenesis. In this manuscript, we describe our observational experience regarding intravesical instillation of PDRNs in improving symptoms of CRC in subjects unresponsiveness to conventional medical therapy., Methods: Eight patients with persistent and/or worsening CRC symptoms, despite conventional therapy, received biweekly intravesical instillation of PDRNs for two consecutive months. Symptoms were scored according to the Late Effects of Normal Tissues-Subjective, Objective, Management, Analytic (LENT-SOMA) scale, before, at the end, and after 4 months following the PDRNs treatment., Results: Four months after instillations, a significant improvement in the subjective perception of CRC symptoms was experienced by participants. The mean LENT-SOMA score was reduced from 1.16+0.26 before to 0.34+0.035 after 4 months from instillations (p<0.001). No adverse effect related to instillations was reported., Conclusions: Subjective perception of persistent and/or worsening CRC symptoms, despite conventional therapy, is improved after intravesical instillation with PDRNs without adverse events. Even though we deduced suggestive insights, the results need to be collected and verified from a large-scale study.
- Published
- 2014
- Full Text
- View/download PDF
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