H. Dutoit, L. Truche, F. V. Donzé, T. Wiersberg, M. L. Doan, J. Li, A. Greenwood, E. Caspari, N. Lefeuvre, J. Dominique, S. Auclair, L. Masci, G. Hetényi, M. Venier, O. Müntener, ICDP DIVE Science Team
{"title":"DIVE-1井眼连续实时探测H2、He、222Rn表明结晶岩深部裂缝流体运移","authors":"H. Dutoit, L. Truche, F. V. Donzé, T. Wiersberg, M. L. Doan, J. Li, A. Greenwood, E. Caspari, N. Lefeuvre, J. Dominique, S. Auclair, L. Masci, G. Hetényi, M. Venier, O. Müntener, ICDP DIVE Science Team","doi":"10.1029/2025GC012168","DOIUrl":null,"url":null,"abstract":"<p>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<sub>2</sub>) 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<sub>2</sub> 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<sub>2</sub>, N<sub>2</sub>, <sup>40</sup>Ar, <sup>38</sup>Ar, <sup>36</sup>Ar, CO<sub>2</sub>, CH<sub>4</sub>, H<sub>2</sub>, He, and <sup>222</sup>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<sub>2</sub> with CH<sub>4</sub> and CO<sub>2</sub> provides initial insights into their possible origins, making this method a promising tool for exploring H<sub>2</sub> and He gases in deep geological formations.</p>","PeriodicalId":50422,"journal":{"name":"Geochemistry Geophysics Geosystems","volume":"26 5","pages":""},"PeriodicalIF":2.9000,"publicationDate":"2025-05-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2025GC012168","citationCount":"0","resultStr":"{\"title\":\"Continuous Real-Time Detection of H2, He, and 222Rn While Drilling DIVE-1 Boreholes (ICDP) Indicates Deep Fracture Fluid Migration in Crystalline Rocks\",\"authors\":\"H. Dutoit, L. Truche, F. V. Donzé, T. Wiersberg, M. L. Doan, J. Li, A. Greenwood, E. Caspari, N. Lefeuvre, J. Dominique, S. Auclair, L. Masci, G. Hetényi, M. Venier, O. Müntener, ICDP DIVE Science Team\",\"doi\":\"10.1029/2025GC012168\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>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<sub>2</sub>) 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<sub>2</sub> 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<sub>2</sub>, N<sub>2</sub>, <sup>40</sup>Ar, <sup>38</sup>Ar, <sup>36</sup>Ar, CO<sub>2</sub>, CH<sub>4</sub>, H<sub>2</sub>, He, and <sup>222</sup>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. 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Continuous Real-Time Detection of H2, He, and 222Rn While Drilling DIVE-1 Boreholes (ICDP) Indicates Deep Fracture Fluid Migration in Crystalline Rocks
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 (H2) 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 H2 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 O2, N2, 40Ar, 38Ar, 36Ar, CO2, CH4, H2, He, and 222Rn 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 H2 with CH4 and CO2 provides initial insights into their possible origins, making this method a promising tool for exploring H2 and He gases in deep geological formations.
期刊介绍:
Geochemistry, Geophysics, Geosystems (G3) publishes research papers on Earth and planetary processes with a focus on understanding the Earth as a system. Observational, experimental, and theoretical investigations of the solid Earth, hydrosphere, atmosphere, biosphere, and solar system at all spatial and temporal scales are welcome. Articles should be of broad interest, and interdisciplinary approaches are encouraged.
Areas of interest for this peer-reviewed journal include, but are not limited to:
The physics and chemistry of the Earth, including its structure, composition, physical properties, dynamics, and evolution
Principles and applications of geochemical proxies to studies of Earth history
The physical properties, composition, and temporal evolution of the Earth''s major reservoirs and the coupling between them
The dynamics of geochemical and biogeochemical cycles at all spatial and temporal scales
Physical and cosmochemical constraints on the composition, origin, and evolution of the Earth and other terrestrial planets
The chemistry and physics of solar system materials that are relevant to the formation, evolution, and current state of the Earth and the planets
Advances in modeling, observation, and experimentation that are of widespread interest in the geosciences.