Yuhzong Liao , Guiling Wang , Wei Zhang , Hanxiong Zhang , Jiyun Liang , Yufei Xi
{"title":"机器学习在郴州和惠州地区断控地热系统勘探中的应用","authors":"Yuhzong Liao , Guiling Wang , Wei Zhang , Hanxiong Zhang , Jiyun Liang , Yufei Xi","doi":"10.1016/j.geothermics.2025.103507","DOIUrl":null,"url":null,"abstract":"<div><div>This study investigates fault-controlled geothermal systems in southeastern China, focusing on representative regions in Hunan, Guangdong, and Jiangxi provinces. A machine learning approach—non-negative matrix factorization with k-means clustering (NMF<em>k</em>)—was applied to classify geothermal water types and delineate favorable exploration zones based on hydrochemical composition, flow rate, heat flow, and fault proximity. Geothermal waters were classified into three types with distinct geochemical and geological attributes: Type A, Type B, and Type C. Representative geothermal fields—Nuanshui (Type A), Longmen and Reshui (Type B), and Chengkou (Type C)—were selected to validate the classification and analyze reservoir characteristics and genetic mechanisms. Type B geothermal water exhibits the highest exploration potential, characterized by deep circulation (1900–5300 m), high reservoir temperatures (66–143 °C), strong confinement, and enrichment in Na⁺ and Li⁺. Its formation is primarily controlled by NW-trending faults and high heat-producing granites. Type C geothermal water shows moderate potential, with the highest heat flow (83 mW/m²), deep circulation (3500–5400 m), and elevated temperatures (109–127 °C), despite lower flow rates. It is hosted in granitic reservoirs associated with NE–N-trending faults. In contrast, Type A demonstrates the lowest geothermal potential, featuring shallow circulation (900–2100 m), lower temperatures (42–75 °C), high flow rates, and enrichment in Mg²⁺, Ca²⁺, and Sr²⁺, reflecting strong meteoric recharge and limited geochemical evolution. A conceptual model is proposed in which meteoric water infiltrates through fault zones, absorbs heat during deep circulation within granitic or carbonate rocks, and ascends to form geothermal reservoirs or surface springs. The classification results align well with spatial patterns of geothermal favorability, offering a robust framework for geothermal resource assessment and supporting sustainable development strategies in southeastern China.</div></div>","PeriodicalId":55095,"journal":{"name":"Geothermics","volume":"134 ","pages":"Article 103507"},"PeriodicalIF":3.9000,"publicationDate":"2025-10-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Machine learning for fault-controlled geothermal systems exploration in Chenzhou and Huizhou region, Southeast China\",\"authors\":\"Yuhzong Liao , Guiling Wang , Wei Zhang , Hanxiong Zhang , Jiyun Liang , Yufei Xi\",\"doi\":\"10.1016/j.geothermics.2025.103507\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>This study investigates fault-controlled geothermal systems in southeastern China, focusing on representative regions in Hunan, Guangdong, and Jiangxi provinces. A machine learning approach—non-negative matrix factorization with k-means clustering (NMF<em>k</em>)—was applied to classify geothermal water types and delineate favorable exploration zones based on hydrochemical composition, flow rate, heat flow, and fault proximity. Geothermal waters were classified into three types with distinct geochemical and geological attributes: Type A, Type B, and Type C. Representative geothermal fields—Nuanshui (Type A), Longmen and Reshui (Type B), and Chengkou (Type C)—were selected to validate the classification and analyze reservoir characteristics and genetic mechanisms. Type B geothermal water exhibits the highest exploration potential, characterized by deep circulation (1900–5300 m), high reservoir temperatures (66–143 °C), strong confinement, and enrichment in Na⁺ and Li⁺. Its formation is primarily controlled by NW-trending faults and high heat-producing granites. Type C geothermal water shows moderate potential, with the highest heat flow (83 mW/m²), deep circulation (3500–5400 m), and elevated temperatures (109–127 °C), despite lower flow rates. It is hosted in granitic reservoirs associated with NE–N-trending faults. In contrast, Type A demonstrates the lowest geothermal potential, featuring shallow circulation (900–2100 m), lower temperatures (42–75 °C), high flow rates, and enrichment in Mg²⁺, Ca²⁺, and Sr²⁺, reflecting strong meteoric recharge and limited geochemical evolution. A conceptual model is proposed in which meteoric water infiltrates through fault zones, absorbs heat during deep circulation within granitic or carbonate rocks, and ascends to form geothermal reservoirs or surface springs. The classification results align well with spatial patterns of geothermal favorability, offering a robust framework for geothermal resource assessment and supporting sustainable development strategies in southeastern China.</div></div>\",\"PeriodicalId\":55095,\"journal\":{\"name\":\"Geothermics\",\"volume\":\"134 \",\"pages\":\"Article 103507\"},\"PeriodicalIF\":3.9000,\"publicationDate\":\"2025-10-10\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geothermics\",\"FirstCategoryId\":\"5\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0375650525002585\",\"RegionNum\":2,\"RegionCategory\":\"工程技术\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"ENERGY & FUELS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geothermics","FirstCategoryId":"5","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0375650525002585","RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"ENERGY & FUELS","Score":null,"Total":0}
Machine learning for fault-controlled geothermal systems exploration in Chenzhou and Huizhou region, Southeast China
This study investigates fault-controlled geothermal systems in southeastern China, focusing on representative regions in Hunan, Guangdong, and Jiangxi provinces. A machine learning approach—non-negative matrix factorization with k-means clustering (NMFk)—was applied to classify geothermal water types and delineate favorable exploration zones based on hydrochemical composition, flow rate, heat flow, and fault proximity. Geothermal waters were classified into three types with distinct geochemical and geological attributes: Type A, Type B, and Type C. Representative geothermal fields—Nuanshui (Type A), Longmen and Reshui (Type B), and Chengkou (Type C)—were selected to validate the classification and analyze reservoir characteristics and genetic mechanisms. Type B geothermal water exhibits the highest exploration potential, characterized by deep circulation (1900–5300 m), high reservoir temperatures (66–143 °C), strong confinement, and enrichment in Na⁺ and Li⁺. Its formation is primarily controlled by NW-trending faults and high heat-producing granites. Type C geothermal water shows moderate potential, with the highest heat flow (83 mW/m²), deep circulation (3500–5400 m), and elevated temperatures (109–127 °C), despite lower flow rates. It is hosted in granitic reservoirs associated with NE–N-trending faults. In contrast, Type A demonstrates the lowest geothermal potential, featuring shallow circulation (900–2100 m), lower temperatures (42–75 °C), high flow rates, and enrichment in Mg²⁺, Ca²⁺, and Sr²⁺, reflecting strong meteoric recharge and limited geochemical evolution. A conceptual model is proposed in which meteoric water infiltrates through fault zones, absorbs heat during deep circulation within granitic or carbonate rocks, and ascends to form geothermal reservoirs or surface springs. The classification results align well with spatial patterns of geothermal favorability, offering a robust framework for geothermal resource assessment and supporting sustainable development strategies in southeastern China.
期刊介绍:
Geothermics is an international journal devoted to the research and development of geothermal energy. The International Board of Editors of Geothermics, which comprises specialists in the various aspects of geothermal resources, exploration and development, guarantees the balanced, comprehensive view of scientific and technological developments in this promising energy field.
It promulgates the state of the art and science of geothermal energy, its exploration and exploitation through a regular exchange of information from all parts of the world. The journal publishes articles dealing with the theory, exploration techniques and all aspects of the utilization of geothermal resources. Geothermics serves as the scientific house, or exchange medium, through which the growing community of geothermal specialists can provide and receive information.