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

IF 2.9 2区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
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
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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 (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.

Abstract Image

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
钻井过程中地流体的识别和实时监测对于安全钻井作业至关重要,可以为储层性质和流体运移提供有价值的见解。虽然泥浆气测井在油气勘探中已经建立了良好的基础,但最近对天然氢(H2)和氦(He)勘探的兴趣促使人们需要改进泥浆气测井技术,以便在结晶基岩中进行连续电缆取心。H2和He的检测在勘探这两种商品时特别有用,但也有助于识别深层流体运移,特别是在结晶基岩中。作为DIVE-ICDP项目的一部分,本研究展示了在Ivrea-Verbano地区(意大利北部)钻探的两个井(909.5和578.5 m深)中O2、N2、40Ar、38Ar、36Ar、CO2、CH4、H2、He和222Rn的泥浆气测井结果。与地球物理测井资料对比表明,气峰与井内流体物性变化具有良好的相关性,指示了流体的流入区域。事实证明,实时气体监测对于识别深层天然气运移和辅助决策是有价值的。尽管该技术潜力巨大,但也面临着一些挑战,比如区分地层衍生气体和钻井诱导气体。建议进行补充分析,包括同位素研究,以完善来源鉴定。然而,He和H2与CH4和CO2的相关性提供了对其可能起源的初步见解,使该方法成为探索深层地质构造中H2和He气体的有前途的工具。
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来源期刊
Geochemistry Geophysics Geosystems
Geochemistry Geophysics Geosystems 地学-地球化学与地球物理
CiteScore
5.90
自引率
11.40%
发文量
252
审稿时长
1 months
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.
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