A drone-based prototype technique for monitoring soil degassing at active volcanic craters

TL;DR

A drone-based system was developed to safely measure soil gas emissions at active volcanoes, offering a safer and more comprehensive way to monitor volcanic activity.

Contribution

The novel contribution is a drone-based method for soil degassing measurements in hazardous volcanic environments.

Findings

The drone system successfully collected CO2 and H2O flux data at multiple sites around Poás Volcano.

Site 1 showed the highest CO2 and H2O fluxes, suggesting active gas release linked to structural features.

The method demonstrated operational success at one site but faced challenges like sealing issues and telemetry interruptions.

Abstract

Developing techniques to monitor volcanic activity from safe distances is crucial for advancing scientific knowledge while protecting the safety of field personnel. One of the most demanding tasks in this context is the measurement of soil gas emissions, which offer valuable insights into fluid migration through the shallow crust and act as an early indicator of volcanic unrest and potential eruptive activity. Traditional soil degassing measurements commonly require two operators to be physically present with the instrument, sometimes exposing them to hazardous conditions. In this study, we present a new method for performing soil degassing measurements from a safe distance, using a customized Remotely Piloted Aircraft System (RPAS). This drone-based approach was designed to carry out accumulation chamber measurements in hazardous or otherwise inaccessible areas. We tested the system at four locations around the active crater of Poás Volcano in Costa Rica, where we collected data on CO2 and H2O fluxes, along with soil temperature and moisture. Our results reveal spatial variability in gas emissions and surface conditions across the study sites. A site located on the crater rim (Site 1) showed the highest CO2 and H2O fluxes, indicating active gas release possibly associated with structural features. A second site, located within the crater (Site 2), exhibited elevated H2O flux without detectable CO2, suggesting localized processes related to moisture transport. Our experiment on another crater site (Site 3) produced a complete and high-quality dataset, demonstrating the operational success of the method. In contrast, measurements at the last crater site (Site 4) were affected by chamber sealing issues and potentially by the influence of volcanic gas plumes. While the experiment faced several challenges, including imperfect ground-sensor contact as well as occasional telemetry interruptions, it successfully demonstrated the feasibility of using drones for soil degassing surveys. Based on these findings, we identify specific areas for improvement and propose future directions to enhance the system reliability and performance. Overall, this method offers a promising tool for extending soil gas measurements to hazardous or hard-to-reach environments, contributing to safer and more comprehensive monitoring of active volcanic systems.

The online version contains supplementary material available at 10.1186/s40623-025-02303-9.

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