奈曼旗农牧交错带地下水水化学形成机制 与背景值研究

展开
  • (1. 中国地质科学院水文地质环境地质研究所,河北 石家庄 050061;2. 河北省/中国地质调查局 地下水污染机理与修复重点实验室,河北 石家庄 050061;3. 奈曼旗水务局,内蒙古自治区, 通辽 028300;4. 奈曼旗自然资源局,内蒙古自治区,通辽市 028306)
鲁重生,助理研究员,主要从事水文地质、水文地球化学方面研究. E-mail:cugblcs4515@163.com
曹文庚,研究员,主要从事水文地质、水文地球化学方面研究. E-mail:caowengeng@mail.cgs.gov.cn

网络出版日期: 2025-09-17

基金资助

中国地质调查局水文地质调查项目(编号:DD20242500-1);中国地质科学院基本科研业务费专项(编号:SK202411)资助.

Study on the Formation Mechanism and Background Values of Groundwater Hydrochemistry in Farming-Pastoral Zone, Naiman Banner

Expand
  • (1. The Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geosciences, Shijiazhuang 050061, China; 2. Key Laboratory of Groundwater Contamination and Remediation of Hebei Province Hebei Province & China Geological Survey, Shijiazhuang 050061, China; 3. Water Affairs Bureau of Naiman Banner, Inner Mongolia, Tongliao 028000, China; 4. Natural Resources Bureau of Naiman Banner, Inner Mongolia, Tongliao 028306, China)
LU Chongsheng, assistant researcher, mainly engaged in hydrogeological and hydrogeochemical research. E-mail: cugblcs4515@163.com
CAO Wengeng, research fellow, mainly engaged in hydrogeological and hydrogeochemical research. E-mail: caowengeng@mail.cgs.gov.cn

Online published: 2025-09-17

Supported by

Project supported by the Hydrogeological survey project of China Geological Survey (Grant No. DD20242500-1); Chinese Academy of Geological Science Basal Research Fund (Grant No. SK202411).

摘要

奈曼旗农牧交错带地处科尔沁沙地腹地生态脆弱区,其地下水水化学形成机制与背景值 研究可支撑水资源配置及农牧业绿色发展。基于水文地质调查与水文地球化学分析,结合自组织 映射神经网络与K-means 聚类混合算法,揭示了地下水化学组成、主控过程及环境背景值。结果表 明:地下水化学组成空间差异性强,但水化学类型均以HCO3-Ca·Mg 为主,呈弱碱性;地下水化学演 化主要受碳酸盐矿物的溶解—沉淀以及硅酸盐矿物的风化溶解驱动,同时受控于正向阳离子交替 吸附作用;总铁、F-、TDS 和NO3-N是影响奈曼旗地下水质量的关键指标,通过水文地球化学图解 法、Grubbs 检验及自组织映射神经网络多方法联合估算其视背景值范围分别为0.42~0.56 mg/L、 0.34~0.38 mg/L、181~188 mg/L 和0.22~1.58 mg/L,其中,总铁的高背景可能与菱铁矿溶解有关,而 F-富集则受控于萤石溶解及正向阳离子交替吸附作用。这为区域水资源优化管理、污染防治及生 态保护提供了科学依据。

本文引用格式

鲁重生, 曹文庚, 庄海艳, 丛日辉, 仝艳龙, 任宇, 李祥志, 宋乐, 卢瑶, 郭记菊 . 奈曼旗农牧交错带地下水水化学形成机制 与背景值研究[J]. 地球科学进展, 0 : 1 . DOI: 10.11867/j.issn.1001-8166.2025.059

Abstract

Abstract:The farming-pastoral zone in Naiman Banner is located in the hinterland of of Horqin Sandy Land. The research on the formation mechanism and background value of groundwater hydrochemistry supports the allocation of water resources and the green development of agriculture and animal husbandry. Based on hydrogeological survey and hydrogeochemical analysis, combined with self-organizing map neural network (SOM) and K-means clustering hybrid algorithm, this study revealed the characteristics of groundwater chemical composition, main controlling factors and environmental background values. Results indicated significant spatial heterogeneity in groundwater chemistry, with HCO3-Ca·Mg as the predominant hydrochemical type and weakly alkaline characteristics. Groundwater chemical evolution is primarily driven by dissolution-precipitation of carbonate minerals and weathering of silicate minerals, and controlled by alternating positive cation adsorption. The apparent background values of Total Fe (TFe), F- , TDS and NO3-N, key indicators affecting the quality of groundwater in Naiman Banner, were 0.42~0.56 mg/L, 0.34~0.38 mg/L, 181~188 mg/L and 0.22~1.58 mg/L, respectively, which were estimated by using a coupled approach of hydrogeochemical graphic method, Grubbs test and SOM. The high background of TFe may be related to siderite dissolution, while the F- enrichment is controlled by fluorite dissolution and alternating positive cation adsorption. This research elucidates the groundwater background values and hydrochemical formation mechanisms in the farming-pastoral zone of Naiman Banner, providing scientific support for the optimization management of regional water resource, pollution prevention, and ecological conservation.
文章导航

/