Thermal released mercury: a new exploration technology for natural gas hydrate exploration in Tibetan Plateau permafrost area

The occurrence environment and fundamental characteristics of natural gas hydrate (NGH) in the permafrost regions of the Tibetan Plateau are highly complex. A significant barrier to advancements in NGH exploration within these areas is the lack of effective exploration methods. The Juhugeng mining a...

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Main Authors: Chaoqing Zhao, Yu Tang, Shouji Pang, Shunyao Zhang, Fugui Zhang
Format: Article
Language:English
Published: Frontiers Media S.A. 2025-03-01
Series:Frontiers in Energy Research
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Online Access:https://www.frontiersin.org/articles/10.3389/fenrg.2025.1505654/full
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author Chaoqing Zhao
Yu Tang
Shouji Pang
Shunyao Zhang
Fugui Zhang
Fugui Zhang
author_facet Chaoqing Zhao
Yu Tang
Shouji Pang
Shunyao Zhang
Fugui Zhang
Fugui Zhang
author_sort Chaoqing Zhao
collection DOAJ
description The occurrence environment and fundamental characteristics of natural gas hydrate (NGH) in the permafrost regions of the Tibetan Plateau are highly complex. A significant barrier to advancements in NGH exploration within these areas is the lack of effective exploration methods. The Juhugeng mining area represents the sole location in China’s permafrost zone where NGH has been identified. In this study, we conducted a thermal released mercury (TRM) exploration experiment in the Juhugeng area, covering an area of 11.75 km2 with a sampling density of 16 points per square kilometer. Soil samples were collected to a depth of 60 cm, totaling 163 samples, which were analyzed for TRM using the XG-7Z Zeeman mercury analyzer. The experimental results indicate that high-value anomalies of TRM occur at the boundaries of NGH deposits, while lower values are observed directly above the hydrates, forming an annular anomaly pattern. The maximum value of TRM recorded was 127.37 ngg−1, with an average value of 32.59 ngg−1, and the lower limit of the anomaly was established at 39.24 ngg−1. By analyzing the spatial relationship between TRM anomalies and hydrocarbon anomalies, this study proposes a geogas migration mechanism for the formation of TRM anomalies. The anomalies are closely linked to NGH deposits, suggesting that TRM analysis is an effective auxiliary exploration technology for NGH in permafrost regions.
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publisher Frontiers Media S.A.
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spelling doaj-art-df90eadb457740ec837e61e09e5fa9d42025-08-20T02:46:28ZengFrontiers Media S.A.Frontiers in Energy Research2296-598X2025-03-011310.3389/fenrg.2025.15056541505654Thermal released mercury: a new exploration technology for natural gas hydrate exploration in Tibetan Plateau permafrost areaChaoqing Zhao0Yu Tang1Shouji Pang2Shunyao Zhang3Fugui Zhang4Fugui Zhang5China Liaocheng Bureau of Natural Resources and Planning, Liaocheng, ChinaInstitute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang, ChinaObservation and Research Station of Gas Hydrate and Permafrost Environment in Muli Town, Ministry of Natural Resources, Beijing, Qinghai, ChinaInstitute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang, ChinaInstitute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang, ChinaObservation and Research Station of Gas Hydrate and Permafrost Environment in Muli Town, Ministry of Natural Resources, Beijing, Qinghai, ChinaThe occurrence environment and fundamental characteristics of natural gas hydrate (NGH) in the permafrost regions of the Tibetan Plateau are highly complex. A significant barrier to advancements in NGH exploration within these areas is the lack of effective exploration methods. The Juhugeng mining area represents the sole location in China’s permafrost zone where NGH has been identified. In this study, we conducted a thermal released mercury (TRM) exploration experiment in the Juhugeng area, covering an area of 11.75 km2 with a sampling density of 16 points per square kilometer. Soil samples were collected to a depth of 60 cm, totaling 163 samples, which were analyzed for TRM using the XG-7Z Zeeman mercury analyzer. The experimental results indicate that high-value anomalies of TRM occur at the boundaries of NGH deposits, while lower values are observed directly above the hydrates, forming an annular anomaly pattern. The maximum value of TRM recorded was 127.37 ngg−1, with an average value of 32.59 ngg−1, and the lower limit of the anomaly was established at 39.24 ngg−1. By analyzing the spatial relationship between TRM anomalies and hydrocarbon anomalies, this study proposes a geogas migration mechanism for the formation of TRM anomalies. The anomalies are closely linked to NGH deposits, suggesting that TRM analysis is an effective auxiliary exploration technology for NGH in permafrost regions.https://www.frontiersin.org/articles/10.3389/fenrg.2025.1505654/fullthermal released mercurynatural gas hydrateexploration technologypermafrost regionTibetan plateau
spellingShingle Chaoqing Zhao
Yu Tang
Shouji Pang
Shunyao Zhang
Fugui Zhang
Fugui Zhang
Thermal released mercury: a new exploration technology for natural gas hydrate exploration in Tibetan Plateau permafrost area
Frontiers in Energy Research
thermal released mercury
natural gas hydrate
exploration technology
permafrost region
Tibetan plateau
title Thermal released mercury: a new exploration technology for natural gas hydrate exploration in Tibetan Plateau permafrost area
title_full Thermal released mercury: a new exploration technology for natural gas hydrate exploration in Tibetan Plateau permafrost area
title_fullStr Thermal released mercury: a new exploration technology for natural gas hydrate exploration in Tibetan Plateau permafrost area
title_full_unstemmed Thermal released mercury: a new exploration technology for natural gas hydrate exploration in Tibetan Plateau permafrost area
title_short Thermal released mercury: a new exploration technology for natural gas hydrate exploration in Tibetan Plateau permafrost area
title_sort thermal released mercury a new exploration technology for natural gas hydrate exploration in tibetan plateau permafrost area
topic thermal released mercury
natural gas hydrate
exploration technology
permafrost region
Tibetan plateau
url https://www.frontiersin.org/articles/10.3389/fenrg.2025.1505654/full
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