ISTerre - Institut des Sciences de la Terre

Publications

Svetlana BYRDINA — 2014-06-19T08:07:55Z

Torres, JL, S Byrdina, G Romero-Beltran, S Garambois, M Rivera, et al, Magma storage below Sabancaya volcano (Southern Peru) imaged by broad band magnetotellurics, ESS Open Archive, DOI : 10.22541/ESSoar.174491958.89031768/v1

Torres, J. L. S. Byrdina et al. (2024), Magma reservoir below Sabancaya volcano (Southern Peru) imaged by broadband magnetotellurics, Extended abstract, 26th EM Induction Workshop, Beppu, Japan, September 7-13, 2024

M. Byrdin and S. Byrdina, Impact of triplet state population on GFP-type fluorescence and photobleaching,
2025, Biology of the Cell 117(2):e2400076, DOI : 10.1111/boc.202400076

Dutoit,H., et al, 2024, Assessing the helium potential of Variscan batholiths : Insight from Corsica Island Geochemistry, Geophysics, Geosystems 25 (7), e2024GC011519

Budi-Santoso, F. Beauducel, I G. M. Nandaka, H. Humaida, F. Costa, C.Widiwijayanti, M. Iguchi, J.-P. Métaxian, I. Rudianto, M. Rozin, Sulistiyani, I. Nurdin, K. Kelfoun, S. Byrdina, V. Pinel, A. A. Fahmi, A. Laurin, M. H. Rizal, N. Dahamna, 2023, The Merapi volcano monitoring system, pp 409-436, in Merapi Volcano : geology, eruptive activity, and monitoring of a high-risk volcano, Springer International Publishing, doi:10.1007/978-3-031-15040-1_13

Girault, F., F Viveiros, C Silva, S Thapa, JE Pacheco, LB Adhikari, et al.,2022, Radon signature of CO2 flux constrains the depth of degassing : Furnas volcano (Azores, Portugal) versus Syabru-Bensi (Nepal Himalayas), Scientific Reports 12 (1), 10837, 13, https://doi.org/10.1038/s41598-022-14653-5

Miller, CA, BW Christenson, S Byrdina, J Vandemeulebrouck, et al., 2020, Snapshot of a magmatic/hydrothermal system from electrical resistivity tomography and fumarolic composition, Whakaari/White Island, New Zealand, Journal of Volcanology and Geothermal Research 400, 106909, https://doi.org/10.1016/j.jvolgeores.2020.106909

Yogeshwar, P., M Küpper, B Tezkan, V Rath, D Kiyan, S Byrdina, et al, 2020, Innovative boat-towed transient electromagnetics—Investigation of the Furnas volcanic lake hydrothermal system, Azores, Geophysics 85 (2), E41-E56, https://doi.org/10.1190/geo2019-0292.1

Hogg, C., D. Kiyan, V. Rath, S. Byrdina, J. Vandemeulebrouck, A. Revil, F. Viveiros, R. Carmo, C. Silva, T. Ferreira (2017) Three-Dimensional interpretation of short period magnetotelluric data at Furnas Volcano, Azores Islands, Geophys. J. Int. Vol. 213 Issue 1, p371-386. 16p. DOI : 10.1093/gji/ggx512

Byrdina, S., S. Friedel, J. Vandemeulebrouck, A. Budi-Santoso, Suhari, W. Suryanto, M. H. Rizal, E. Winata, Kusdaryanto, (2017). Geophysical image of the hydrothermal system of Merapi volcano., J. Volcanol. Geotherm. Res., 329,30-40

Gresse, M., J. Vandemeulebrouck, S. Byrdina, G. Chiodini, A. Revil, T. C. Johnson, T. Ricci, G. Vilardo, T. Lebourg, J. Grangeon, P. Bascou, and L. Metral, 3-D resistivity tomography of the Solfatara crater (Italy) : Implication for the multiphase flow structure of the shallow hydrothermal system, Journal of Geophysical
Research : Solid Earth, 122, 8749–8768. https://doi.org/10.1002/2017JB014389

Gresse, M., J. Vandemeulebrouck, S. Byrdina, G. Chiodini and P.P. Bruno (2016). Changes in CO2 diffuse degassing induced by the passing of seismic waves, J. Volcanol. Geotherm. Res., DOI : 10.1016/j.jvolgeores.2016.04.019

Brothelande E., J-F Lénat, M Chaput, L Gailler, A Finizola, S Dumont, A Peltier, P Bachèlery, S Barde-Cabusson, S Byrdina, E. Garaebiti et al, Structure and evolution of an active resurgent dome evidenced by geophysical investigations : The Yenkahe dome-Yasur volcano system (Siwi caldera, Vanuatu), Journal of Volcanology and Geothermal Research, 2015, doi:10.1016/j.jvolgeores.2015.08.021

Gresse M., J. Vandemeulebrouck, S.Byrdina, G. Chiodini, J.P. Bruno, Changes in CO2 diffuse degassing induced by the passing of seismic waves, Journal of Volcanology and Geothermal Research, 2015 320:12-18

Byrdina S., J. Vandemeulebrouck, C. Cardellini, A. Legaz, C. Camerlynck, G. Chiodini, T.Lebourg, M. Gresse, G. Motos, P. Bascou, A. Carrier, S. Caliro, 2014, Relations between electrical resistivity, carbon dioxide flux, and self-potential in the shallow hydrothermal system of Solfatara (Phlegrean Fields, Italy), , J. Volcanol. Geotherm. Res, 2014, 283, p. 172-182. ISSN 0377-0273

Revil A., M. Karaoulis, S. Srivastava and S. Byrdina, 2013, Joint inversion of self-potential and resistivity data to localize the burning front of underground coal fires, Geophysics, 78, 5, B259-B273.

Byrdina, S., D. Ramos, J. Vandemeulebrouck, P. Masias, A. Revil, A. Finizola, K. Gonzales Zuniga, V. Cruz, Y. Antayhua (2013) Influence of the regional topography on the remote emplacement of hydrothermal systems with examples of Ticsani and Ubinas volcanoes, Southern Peru, Earth Planet. Sci. Lett., 365, 152–164. pdf

Byrdina, S. C. Rücker, M. Zimmer, S. Friedel, U. Serfling, 2011, Self potential signals preceding variations of fumarole activity at Merapi volcano, Central Java, J. Volcanol. Geotherm. Res, doi:10.1016/j.jvolgeores.2011.12.002. pdf

Revil, A et al., Hydrogeology of Stromboli volcano, Aeolian Islands (Italy) from the interpretation of resistivity tomograms, self-potential, soil temperature and soil CO2 concentration measurements, 2011, Geophys. J. Int. 186, 1078–1094

Narteau C., Byrdina S., Shebalin P., Schorlemmer D. Common dependence on stress for the two fundamental laws of statistical seismology, 2009, Nature, 462, p. 642-645

Byrdina S., Revil A., Pant S. R., Koirala B. P., Shrestha P. L., Tiwari D. R., Gautam U. P., Shrestha K., Sapkota S. N., Contraires S., Perrier F. Dipolar self-potential anomaly associated with carbon dioxide and radon flux at Syabru-Bensi hot springs in central Nepal, 2009, Journal of Geophysical Research, 114, B10101.

Perrier F., P.Richon, S. Byrdina, S. Rajaure, C. France-Lanorde, A. Revil, S. Contraires, S. Bureau U.Gautam, B. Koirala, P. Shrestha, D.R. Tiwari, L. Bollinger, S. N. Sapkota, A direct evidence for high carbon dioxide and radon-222 gas exhalation at the Syabru-Bensi hot springs in Central Nepal, 2009, Earth and Planetary Science Letters, 278,198-207, doi:10.1016/j.epsl.2008.12.008

Crespy, A. Revil, A. Linde, N. Byrdina, S. Jardani, A. Boleve, A. Henry, P., Detection and localization of hydromechanical disturbances in a sandbox using the self-potential method, 2008, Journal of Geophysical Research, 113, B01205-B01300, DOI 10.1029/2007JB005042

Revil A. et al,, Inner structure of La Fossa di Vulcano (Vulcano Island, southern Tyrrhenian Sea, Italy) revealed by high-resolution electric resistivity tomography coupled with self-potential, temperature, and CO2 diffuse degassing measurements, 2007, Journal of Geophysical Research, 113, B07207

Byrdina, S., P. Shebalin, C. Narteau and J-L. Le Mouel, Temporal properties of seismicity and largest earthquakes in SE Carpathians, 2006, Nonlin. Processes Geophys. 13, 1-11

Friedel, S., Byrdina, S., Jacobs, F. and Zimmer, M., Self-potential and ground temperature at Merapi volcano prior to its crisis in the rainy season 2000-2001, 2004 Journal of Volcanology and Geothermal Research, N.134 149-168,

Byrdina, S., Friedel, S., Wassermann, J. and Zlotnicki, J., Self-potential variations associated with ultra-long-period seismic signals at Merapi volcano, 2003 Geophyical Research Letters, V 30, N 22, 2156

Projets

Svetlana BYRDINA — 2014-03-27T17:26:02Z

INSU 2020 - 2021 : "Développement de méthodes d'investigation et étude du couplage hydromécanique et de la sismicité induite pour la géothermie moyenne enthalpie" (responsable J.L. Got)

Pack Ambition Recherche de la région AURA 2022 - maintenant : "Méthodes passives d'estimation des ressources et des risques pour la géothermie moyenne enthalpie et le chauffage urbain" (responsable J.L. Got)

INSU SYSTER 2022-2024 « Modèle structural du volcan Krafla et de son système géothermal : contraintes fournies par l'imagerie magnétique par drone » (resp. C. Bouligand)

INSU 2022-2023 : "Études de la structure profonde de volcan Ubinas " (responsable S. Byrdina)

Structure et Dynamique des systèmes hydrothermaux

Jean VANDEMEULEBROUCK, Svetlana BYRDINA — 2013-03-12T10:49:37Z

Hydrothermal systems are found at most active volcanoes and their understanding is important for following reasons :

Variations in hydrothermal circulation reflect the temporal evolution of the volcanic activity like the reactivation of the magmatic processes or preparation of the volcanic crisis ;
Hydrothermal systems may interact with magma ascent leading to explosive hydro-magmatic eruptions ;
Their emplacement and geometry are controlled by principal geological structures, therefore the map of the hydrothermal system gives us an image of the buried ancient crater rims, faults or permeable zones ;
Long term hydrothermal circulation can contribute to destabilization of the edifice by weakening the stiffness of the rocks.

We study hydrothermal systems by geophysical methods like the electric self-potential and resistivity methods as well as the measurements of the ground temperature distribution or analysis of ambient seismic noise. Self-potential method allows ground flow systems to be detected and their geometries to be constrained (Figure 1). Knowledge of the ground temperature distribution allows us to couple the models of mass and heat transfer (Figure 2).

Figure 1. Fluid circulation at a shallow depth below Solfatara crater of Phlegreen Fields. 2-D Electrical resistivity cross-section along two intersecting profiles compared to a) Google Image draped over a digital elevation model of the area b) a ground temperature distribution. Resistive zones like those below the Bocca Grande fumarole correspond to an upward flow of the carbon dioxide/vapor mixture (dashed line), conductive zone below the Fangaia mud pool indicates the presence of the liquid water (solid line).

Cliquer sur l'image pour l'agrandir.

Figure 2. Influence of the regional topography on the geometry of the hydrothermal body. We build our study on field data of self-potential (a), spring temperature, and on the results of direct numerical simulation coupling mass and heat transfer inside the volcanic edifice (b). Our numerical results show a significant derivation of hydrothermal system due to gradient of regional topography. Byrdina et al., Earth Planet. Sci. Lett., 2013

Structure and dynamics of hydrothermal systems

Anaïs SCHNEIDER, Jean VANDEMEULEBROUCK, Svetlana BYRDINA — 2013-03-12T10:49:37Z

Hydrothermal systems are found at most active volcanoes and their understanding is important for following reasons :

Variations in hydrothermal circulation reflect the temporal evolution of the volcanic activity like the reactivation of the magmatic processes or preparation of the volcanic crisis ;
Hydrothermal systems may interact with magma ascent leading to explosive hydro-magmatic eruptions ;
Their emplacement and geometry are controlled by principal geological structures, therefore the map of the hydrothermal system gives us an image of the buried ancient crater rims, faults or permeable zones ;
Long term hydrothermal circulation can contribute to destabilization of the edifice by weakening the stiffness of the rocks.

Cliquer sur l'image pour l'agrandir.

CV

Svetlana BYRDINA — 2013-02-06T17:06:21Z

Éducation :

Doctorat de l'Institut de Physique du Globe de Paris en Géophysique interne ; 06/07/2004
Diplôme en géophysique (équivalent à DEA), Université technologique de Berlin ; 06/09/1999
Diplôme en Physique, Université Lomonossov de Moscou ; 31/10/1993

Expérience professionnelle :

Ingénieure de recherche à ISTerre en méthodes électromagnétiques, responsable d'instrumentation magneto-tellurique.
Ingénieur d'études IRD à OPG Clermont-Ferrand ; utilisation de données d'imagerie radar satellitaires : 2007-2009.
Stage post-doctoral à l'IPGP dans le cadre de projet européen E2C2 (extreme events, causes and consequences) : 2005-2007.

Recherche :

Études des fluides crustaux par les méthodes électromagnétiques
L'imagerie des systèmes hydrothermaux par les méthodes électriques (potentiel spontané et tomographie de la résistivité électrique) et thermiques.
Modélisation numérique de transport des fluides et de chaleur au sein des systèmes hydrothermaux

Participation aux projets :

INSU 2020 - 2021 : "Développement de méthodes d'investigation et étude du couplage hydromécanique et de la sismicité induite pour la géothermie moyenne enthalpie" (responsable J.L. Got)
Pack Ambition Recherche de la région AURA 2022 - maintenant : "Méthodes passives d'estimation des ressources et des risques pour la géothermie moyenne enthalpie et le chauffage urbain" (responsable J.L. Got)
INSU SYSTER 2022-2024 « Modèle structural du volcan Krafla et de son système géothermal : contraintes fournies par l'imagerie magnétique par drone » (resp. C. Bouligand)
INSU 2022-2023 : "Études de la structure profonde de volcan Ubinas " (responsable S. Byrdina)