Continuous Real‐Time Detection of H<sub>2</sub>, He, and <sup>222</sup>Rn While Drilling DIVE‐1 Boreholes (ICDP) Indicates Deep Fracture Fluid Migration in Crystalline Rocks

Abstract The identification and real‐time monitoring of geofluids during drilling is crucial for safe drilling operations and can provide valuable insights into reservoir properties and fluid migration. While mud gas logging is well established in oil and gas exploration, recent interest in natural hydrogen (H 2 ) and helium (He) exploration has prompted the need for improved mud gas logging techniques for continuous wireline coring in crystalline bedrock. The detection of both H 2 and He is particularly useful when exploring these two commodities but also for identifying deep fluid migration notably in crystalline bedrock. This study presents the results of mud gas logging of O 2 , N 2 , 40 Ar, 38 Ar, 36 Ar, CO 2 , CH 4 , H 2 , He, and 222 Rn from two boreholes (909.5 and 578.5 m deep) drilled in the Ivrea‐Verbano Zone (Northern Italy) as part of the DIVE‐ICDP project. Comparison with data from geophysical logging showed that gas peaks correlate well with variations in the physical characteristics of the well fluid, indicating zones of fluid inflow. Real‐time gas monitoring proved to be valuable for identifying deep gas migration and aiding decision‐making. Despite its potential, this technique faces challenges, such as distinguishing between formation‐derived and drilling‐induced gases. Complementary analyses, including isotopic studies, are recommended to refine source identification. Nevertheless, the correlation of He and H 2 with CH 4 and CO 2 provides initial insights into their possible origins, making this method a promising tool for exploring H 2 and He gases in deep geological formations.

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Publication Details

Journal
Geochemistry Geophysics Geosystems
Published
2025-05-01
DOI
https://doi.org/10.1029/2025gc012168
Citations
2
Primary Topic
earthquake and tectonic studies
Type
article
Field-Weighted Citation Impact
3.73

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article

Continuous Real‐Time Detection of H2, He, and 222Rn While Drilling DIVE‐1 Boreholes (ICDP) Indicates Deep Fracture Fluid Migration in Crystalline Rocks

J. Li, Mai‐Linh Doan, Hugo Dutoit, Thomas Wiersberg et al.
2 citations
Geochemistry Geophysics Geosystems
earthquake and tectonic studies
3.73
article

Continuous Real‐Time Detection of H2, He, and 222Rn While Drilling DIVE‐1 Boreholes (ICDP) Indicates Deep Fracture Fluid Migration in Crystalline Rocks

J. Li, Mai‐Linh Doan, Hugo Dutoit, Thomas Wiersberg, György Hetényi, Laurent Truche, Othmar Müntener, Frédéric‐Victor Donzé, Simon Auclair, Eva Caspari, Andrew Greenwood, Nicolas Lefeuvre, Jessy Dominique, Marta Venier, Lorella Masci
article en
2 citations

Abstract

Abstract The identification and real‐time monitoring of geofluids during drilling is crucial for safe drilling operations and can provide valuable insights into reservoir properties and fluid migration. While mud gas logging is well established in oil and gas exploration, recent interest in natural hydrogen (H 2 ) and helium (He) exploration has prompted the need for improved mud gas logging techniques for continuous wireline coring in crystalline bedrock. The detection of both H 2 and He is particularly useful when exploring these two commodities but also for identifying deep fluid migration notably in crystalline bedrock. This study presents the results of mud gas logging of O 2 , N 2 , 40 Ar, 38 Ar, 36 Ar, CO 2 , CH 4 , H 2 , He, and 222 Rn from two boreholes (909.5 and 578.5 m deep) drilled in the Ivrea‐Verbano Zone (Northern Italy) as part of the DIVE‐ICDP project. Comparison with data from geophysical logging showed that gas peaks correlate well with variations in the physical characteristics of the well fluid, indicating zones of fluid inflow. Real‐time gas monitoring proved to be valuable for identifying deep gas migration and aiding decision‐making. Despite its potential, this technique faces challenges, such as distinguishing between formation‐derived and drilling‐induced gases. Complementary analyses, including isotopic studies, are recommended to refine source identification. Nevertheless, the correlation of He and H 2 with CH 4 and CO 2 provides initial insights into their possible origins, making this method a promising tool for exploring H 2 and He gases in deep geological formations.

Geochemistry Geophysics GeosystemsVol. 26(5)
Centre National de la Recherche Scientifique (FR), Université de Pau et des Pays de l'Adour (FR), Montanuniversität Leoben (AT), Johannes Gutenberg University Mainz (DE), Université Clermont Auvergne (FR), Institut des Sciences de la Terre (FR), Laboratoire Magmas et Volcans (FR), GFZ Helmholtz Centre for Geosciences (DE), Université Gustave Eiffel (FR), Institut de Recherche pour le Développement (FR), Université Grenoble Alpes (FR), University of Lausanne (CH)
Ministère de l'Enseignement supérieur, de la Recherche et de l'Innovation, Agence Nationale de la Recherche, Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung, Institut Universitaire de France, Université de Lausanne
Openalex Percentile: Top 8%
earthquake and tectonic studies
3.73
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