| 注册
首页|期刊导航|水文地质工程地质|地质成因高铵地下水研究进展

地质成因高铵地下水研究进展

杜尧 熊耀劲 邓娅敏 王焰新

水文地质工程地质2025,Vol.52Issue(1):23-31,9.
水文地质工程地质2025,Vol.52Issue(1):23-31,9.DOI:10.16030/j.cnki.issn.1000-3665.202409031

地质成因高铵地下水研究进展

Research progress on geogenic-contaminated high ammonium groundwater

杜尧 1熊耀劲 1邓娅敏 1王焰新1

作者信息

  • 1. 地下水质与健康教育部重点实验室,湖北 武汉 430078||中国地质大学(武汉)环境学院,湖北 武汉 430078
  • 折叠

摘要

Abstract

Groundwater nitrogen contamination is one of the most prevalent water environment problems worldwide.For a long time,the high concentration of ammonium in groundwater has been attributed to inputs from various human activities.However,the natural ammonium anomalies in groundwater have been neglected in previous studies.This paper reviewed the potential sources of ammonium in groundwater systems from anthropogenic sources including domestic and industrial wastewater discharges,domestic landfills,fertilizer and pesticide applications,sewage irrigation,and geological sources of natural organic matter mineralization.The global distribution of geogenic high-ammonium groundwater was also summarized.From the perspectives of depositional and hydrogeochemical environments,it is summarized that the occurrence characteristics of geogenic ammonium in groundwater systems were organic matter-rich,stagnant,confined,and reducing conditions.Based on two typical case studies,it is clarified that the evolution of macroscopic depositional environments controls the abundance/bio-availability of buried organic matter and thus results in the formation of high-ammonium groundwater through mineralization,whereas the molecular composition of natural organic matter and its degradation pathway at the microscale play a major role in controlling the transport and enrichment of ammonium in groundwater.The direction of future research on high ammonium groundwater that should be deepened and expanded was proposed,mainly including the combination of macro-model and micro-mechanism,the control of the organic carbon age,and the influence of high ammonium groundwater discharge on the nutrient status of surface water.

关键词

地下水/铵氮/地质成因/沉积演化/有机质降解

Key words

groundwater/ammonium/geogenic/sedimentary evolution/organic matter degradation

分类

天文与地球科学

引用本文复制引用

杜尧,熊耀劲,邓娅敏,王焰新..地质成因高铵地下水研究进展[J].水文地质工程地质,2025,52(1):23-31,9.

基金项目

国家自然科学基金项目(42177181) (42177181)

水文地质工程地质

OA北大核心

1000-3665

访问量0
|
下载量0
段落导航相关论文