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    全球天然氢气成因机理、分布规律与地球物理勘探技术进展

    Natural hydrogen: Advances in genesis mechanisms, global distribution, and geophysical exploration

    • 摘要: 天然氢气作为零碳清洁能源,其高效勘探与开发对全球能源低碳转型具有重要意义。厘清氢气成因机理、主控因素与分布规律,是实现天然氢资源规模化利用的基础。通过系统梳理了近年来有关氢气成因机理研究进展,构建了完整的成因分类体系,并通过汇总世界范围内不同成因氢气藏数据与全球岩性地图、活动断层、各类型盆地相互叠合,总结了不同成因氢气的主控因素与空间分布规律,主要取得以下认识:(1)氢气成因可划分为无机、有机及混合成因三大类。无机成因包括蛇纹石化、断层活动、前寒武基底滞留氢等水岩反应,水和有机质的电离辐射作用,原生与次生地球深部脱气;有机成因包括沉积有机质热演化与甲烷裂解成氢的有机质热解、氢化酶/固氮酶的微生物作用;混合成因则为多机制耦合作用的结果。(2)氢气富集受断裂、岩性组合、盆地类型的控制作用。断裂因兼具生氢场所、运移通道与储集条件的三重作用,为氢气的生成、聚集和保存提供了有利条件;变质岩、深成侵入岩与火山岩是氢气富集的有利岩性背景;天然氢气多发育于各类含油气盆地中。(3)空间分布上,无机成因氢气主要分布于构造活动带及前寒武纪稳定区;有机成因氢气集中于富有机质沉积区;混合成因氢气则常见于构造复杂、多源叠合区域。我国天然氢资源显示广泛,但分布较为分散。当前,天然氢气研究在多来源贡献的精确甄别以及全球资源潜力的系统预测等方面仍面临挑战,未来需深化氢气成因理论、发展深部探测技术并构建预测模型,以支撑规模天然氢气的资源评价与勘探突破。该研究为天然氢气成因机理与富集规律提供了系统理论依据,有助于富氢区预测与勘探目标优选,对推进能源转型与实现“双碳”目标具有重要科学意义。

       

      Abstract: Natural hydrogen, as a zero-carbon clean energy source, is of great significance for the global energy transition to low-carbon development through its efficient exploration and exploitation. Clarifying the genesis mechanisms, key controlling factors, and distribution patterns of hydrogen is fundamental to achieving large-scale utilization of natural hydrogen resources. Recent advances in hydrogen genesis research are systematically reviewed, a comprehensive genesis classification system is established, and global hydrogen reservoir data with lithological maps, active faults, and basin types are integrated. Summarized are the key controlling factors and spatial distribution patterns of hydrogen reservoirs of different origins, yielding the following insights: (1) Hydrogen genesis can be categorized into three major types: inorganic, organic, and mixed. Inorganic genesis encompasses water-rock reactions such as serpentinization, fault activity, and trapped hydrogen in the Precambrian basement; ionizing radiation effects on water and organic matter; and primary and secondary deep degassing. Organic genesis involves organic matter pyrolysis through the thermal evolution of sedimentary organic matter and methane cracking for hydrogen production, and microbial processes mediated by hydrogenases/nitrogenases. Mixed genesis results from the coupling of multiple mechanisms. (2) Hydrogen enrichment is controlled by faults, lithological assemblages, and basin types. Faults provide triple functions as hydrogen generation sites, migration pathways, and storage conditions, facilitating hydrogen generation, accumulation, and preservation. Metamorphic rocks, plutonic intrusions, and volcanic rocks form favorable lithological backgrounds for hydrogen enrichment. Natural hydrogen predominantly develops within various petroliferous basins. (3) Spatially, inorganic hydrogen is predominantly distributed in tectonically active belts and Precambrian stable zones; organic hydrogen is concentrated in organic-rich sedimentary areas; while mixed-origin hydrogen is commonly found in tectonically complex regions with multiple source superimpositions. China has extensive natural hydrogen resources, though their distribution remains relatively dispersed. Current research on natural hydrogen faces challenges in precisely distinguishing contributions from multiple sources and systematically predicting global resource potential. Future efforts should deepen hydrogen genesis theories, advance deep detection technologies, and develop predictive models to support the evaluation of large-scale natural hydrogen resources and exploration breakthroughs. The study provides a systematic theoretical basis for natural hydrogen genesis mechanisms and enrichment patterns, facilitating the prediction of hydrogen-rich zones and the optimization of exploration targets. These findings hold significant scientific importance for advancing energy transition and achieving the dual carbon goals.

       

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