Self-potential distribution on active volcano controlled by three-dimensional resistivity structure in Izu-Oshima, Japan

Abstract

S U M M A R YA self-potential (SP) survey is conducted in Izu-Oshima volcano to reveal subsurface fluid flows during a dormant period. At the southwestern slope outside the caldera, terrain-related SP is observed. Higher potentials are observed in the southern caldera, where fumarolic and thermal activities are found. Contrarily, lower potentials are observed in the northern caldera. This region coincides with an area where lavas pile thicker than that on the outside. 3-D simulations of the groundwater flow due to meteoric water infiltration and induced SP are performed with a heterogeneous electrical resistivity model, to understand the fundamental groundwater flow regime and causes of the observed SP. The observed SP variation is strongly affected by the subsurface resistivity structure and streaming potential within the unsaturated zone, and an overall pattern of the observed SP is reproduced without including an effect of thermally driven upward flows. The terrain-related SP at the southwestern slope is caused by the downward flow of the meteoric water in the unsaturated zone as proposed by previous researchers. The primary cause of the high SP observed in the southern caldera is shallow conductors connecting with a lower conductive layer. Contribution from the upward fluid flows due to the thermal activities, which was believed to be the main cause of the high SP at active areas, is thought to be smaller. The lower potential at the northern caldera is interpreted by the greater streaming potential as compared to that of the surroundings. This can be caused by the difference in the electrical and/or hydraulic parameters of lavas compared with those of pyroclastic rocks. One of the probable reasons of the greater streaming potential is the greater magnitude of zeta potentials of lavas. Probably, lower vertical permeabilities of lavas also lead to the greater streaming potential.

Hydrogeology of Stromboli volcano, Aeolian Islands (Italy) from the interpretation of resistivity tomograms, self-potential, soil temperature and soil CO2 concentration measurements

“…There are several models that link self‐potential signals to the depth (or the elevation) of the water table (see Jackson & Kauahikaua 1987; Aubert & Atangana 1996 for early investigations and Aizawa et al . 2009; Onizawa et al . 2009; Ball et al .…”

Changes in Electrokinetic Coupling Coefficients of Granite under Triaxial Deformation

“…International Journal of Geophysics The S w dependence of the coupling coefficients is important also for modeling of field self-potential data related to unsaturated flow in volcanic areas (e.g., [49,50]) and shallow groundwater systems. We need further study to clarify the S w change during dilatancy stage and its effect on the coupling coefficients of low-permeability rocks such as granite used in this study.…”

Influence of water pressure dynamics and fluid flow on the streaming‐potential response for unsaturated conditions

“…) and to detect electrical disturbances induced by magmatic intrusions (Onizawa et al . ; Mauri, Williams‐Jones, and Saracco, ). Self‐potential observations have been proposed as an approach to estimate hydraulic diffusivity (Maineult et al .…”

“…Some applications have been developed for the selfpotential anomaly mapping of a copper mine and for geothermal fields (Sindirgi, Pamukçu, andÖzyalin, 2008;Jouniaux and Ishido, 2012). Electrokinetics has been used to detect contaminant leachates (Canton et al 2010) and to detect electrical disturbances induced by magmatic intrusions (Onizawa et al 2009;Mauri, Williams-Jones, and Saracco, 2010). Selfpotential observations have been proposed as an approach to estimate hydraulic diffusivity (Maineult et al 2008) and permeability (Jouniaux, 2011).…”