Tectonic and Anthropogenic Microseismic Activity While Drilling Toward Supercritical Conditions in the Larderello‐Travale Geothermal Field, Italy

Abstract

This study investigates the seismic activity occurring at the Larderello‐Travale geothermal field, central Italy, from June 2017 to January 2018. We deployed a network composed of nine broadband stations around the Venelle 2 well drilling for supercritical fluids. During the experiment, we recognize two types of seismic events (type 1 and type 2). Type‐1 events have clear P and S wave arrivals and occur in clusters both above and below the K‐horizon, which is a seismic reflector marking a debated transition zone at depth. The distribution and evolution of the seismic sequences suggest that the K‐horizon could be interpreted as a fluid‐rich region at near‐lithostatic pressures. Type‐2 events usually occur in swarms and show a periodic pattern, a narrow frequency band, and almost identical waveforms. Their source is estimated to be located near the well, and their occurrence ceases after about 3 weeks from the conclusion of the drilling. We propose a causal link with the drilling operations where pressure fronts inside the well may promote phase changes and fluid flow across the drilled formations. Our study sheds light on the fluid‐driven tectonic and anthropogenic seismic activity at the Larderello‐Travale geothermal field. More generally, we show that microseismic activity occurring during drilling in high‐pressure and high‐temperature conditions can remain at low magnitudes and that geothermal wells targeting geothermal fluids in such systems may be handled safely despite the critical conditions encountered at depth. The drilling of the Venelle 2 well is an encouraging example for the development of geothermal energy in critical conditions.

Distribution of geothermal arsenic in relation to geothermal play types: A global review and case study from the Anatolian plate (Turkey)

“…In contrast to shallow circulating surface waters, geothermal fluid circulates to deeper depths (nearly 3000 m; Minetto et al, 2020) for a longer time in the geothermal system and water-rock interaction time becomes longer. Lower dissolved oxygen ratio, higher pH values, high temperatures and more reduced redox conditions represent deeper aquifer environments with geothermal fluids (Ayotte, 1999).…”