Geophysical Methods as Support to Aquifer Recharge

AbstractIn the framework of WAter Re-BOrn Project a large pond in Mereto (upper Friuli plain) was chosen as artificial recharge test site. Several geophysical investigations (GPR, Electrical Resistivity Tomography and High Resolution Seismic) were carried out to study and to characterize the vadose zone of this large infiltration basin. These geophysical integrated methods supplied us many information to characterize the vadose zone and the unconfined aquifer in the study area. The geophysical information greatly reduces the hydrogeological knowledge gaps and was used to improve the three-dimensional Finite Element numerical model to predict the effect of the artificial recharge

Aquifer Characterization and Monitoring by Active and Passive Seismic Surveys

AbstractA 3D active and passive seismic survey was carried over an aquifer in Italy. We used 1-component vertical receivers in a fine areal grid of 100x100 m. Furthermore, two orthogonal linear profiles were acquired with 3-component receivers, recording the signal of a directional vibrator in the x, y and z direction, so getting a 9-component wave field. The data allow studying the elastic propagation effects of seismic waves in the aquifer, getting independent measurements of direct P, SH and SV arrivals. The elastic parameters they provide allow exploiting the Rayleigh wave velocities obtained by passive seismic for aquifer monitoring

Results of geophysical monitoring over a "leaking" natural analogue site in Italy

CO2 storage in the subsurface is becoming more and more attractive as a means to reduce CO2 emissions to the atmosphere and hence minimize human-induced global warming. The ability to monitor and verify these CO2 storage reservoirs is a key element for further implementation of other storage sites. Since the current sites fortunately do not appear to "leak" CO2, it is difficult to test the most suitable monitoring techniques for their ability to detect CO2 migration pathways. In this study different monitoring methods have been evaluated at a site in the Latera caldera (central Italy) where natural, thermo-metamorphically produced CO2 finds its way to the surface. The aim of the study is to identify which monitoring methods can detect the migrating CO2 and to gain understanding of the preferential migration pathways of the CO2. Different geophysical monitoring techniques have been deployed at a small, 200×500 m study area located in the centre of the caldera: 2D reflection seismics (testing different sources), 2D refraction seismics, multi-channel analysis of surface wave (MASW), ground penetrating radar (GPR), micro-gravity, magnetometer, self-potential (SP), 2D and 3D geo-electrical measurements and electro-magnetic (EM31 and EM34) measurements. Furthermore CO2 flux measurements were performed in a dense grid over the study area, and a limited number of soil gas samples collected along two profiles, to "ground-truth" the geophysical results. In general a good correlation has been observed between the different methods and the presence of CO2. Geophysical responses, especially those of the reflection seismic and magnetometer data, change markedly from one side of the proposed main fault to the other, probably linked to a sharp geological boundary. The observed fractures on the seismic data seem to correspond with the preferred migration pathways of the CO2. The GPR and resistivity measurements detect strong variations in conductivity induced by the presence of the CO2 up to about 2 and 20 m depth, respectively, as supported by the soil gas and flux measurements. © 2009 Elsevier Ltd. All rights reserved

Fast method to transform chirp envelope data into pseudo-seismic data

Chirp technology is an acoustic tool for imaging the shallow seabed with a high resolution, used for investigations of modern to Quaternary sedimentary structures and processes and more applied goals, such as hazard surveys for drilling, archeology, geology or engineering fields. In this paper, we present new methods that improve such imaging. During the standard acquisition, the Chirp waveforms are converted into analytic signals and only their envelope is preserved and interpreted, because the highly oscillating signal is otherwise difficult to be identified visually. Doing so, however, the phase information is lost, and the final processing is limited mainly to simple time-varying gain recovery or filtering. We present a work flow including a derivative step to transform the enveloped signal into a seismic-like waveform. In this way, we can apply processing tools as FX deconvolution and migration to improve the signal/noise ratio and reduce diffractions. This method allows reviving standard and legacy Chirp data where the full-waveform information is missing