首页|期刊导航|生态环境学报|珠江口立沙岛地下水水化学特征与高氨地下水溯源分析

珠江口立沙岛地下水水化学特征与高氨地下水溯源分析OA

Hydrochemical Characteristics and Source Apportionment of High-Ammonium Groundwater in Lisha Island,Pearl River Estuary

中文摘要英文摘要

为阐明珠江口典型河口沙洲立沙岛复杂地下水系统的水化学特征、补给来源及高氨氮成因,于丰、枯水期系统采集了潜水与承压水样品,综合运用水化学、多同位素(δ2H、δ18O、3H、δ13C、14C、δ15N-NH4+)等环境示踪技术进行研究.结果表明,研究区地下水系统呈现清晰的"陆源-混合-海源"三元空间结构,水化学类型由陆源补给区的 HCO3-Ca 型向海源影响区的Cl-Na 型演化.氢氧同位素证实地下水均来源于大气降水,但经历了与海水的不同程度混合.3H与 14C(校正年龄为2 200 a BP)联合示踪确认,地下水咸化是全新世古海水残留与现代海水沿西南侧优势通道入侵共同作用的结果.高浓度氨氮是该区域的显著特征,其δ15N-NH4+值变化范围大(-2.7‰-+26.7‰),多数样品值远超有机质矿化(+2‰-+8‰)的典型范围,而极低的 NO3-含量排除了硝化作用导致 15N 富集的可能.高氨氮的物质来源是沉积物中天然有机质的降解,而 δ15N-NH4+值异常富集主要归因于微生物厌氧氨氧化(anammox)过程的同位素分馏效应.离子偏离分析进一步表明,NH4+浓度与Na+、K⁺、HCO3-的正向偏离呈显著正相关(p<0.05),与SO42-的负向偏离呈显著负相关(p<0.05).该研究可为立沙岛乃至类似河口岛屿地区的地下水资源开发及生态环境保护提供理论支持.

To elucidate the hydrochemical characteristics,recharge sources,and genesis of high-ammonium(NH4+)groundwater in the complex system of Lisha Island,a typical estuarine sandbar in the Pearl River Estuary,unconfined and confined groundwater samples were systematically collected during wet and dry seasons.A comprehensive study was conducted using hydrochemistry and multiple environmental isotope tracers(δ2H,δ18O,3H,δ13C,14C,and δ15 N-NH4+).The results indicate that the groundwater system exhibits a clear ternary spatial structure of"terrestrial source-mixing-marine source,"with hydrochemical facies evolving from HCO3-Ca type in the terrestrial recharge area to Cl-Na type in the marine-influenced area.Hydrogen and oxygen isotopes confirm that all groundwater originates from atmospheric precipitation but has experienced varying degrees of mixing with seawater.The combined use of 3H and 14C(corrected age 0 to 2 200 a BP)tracers confirms that groundwater salinization results from the combined effects of residual Holocene paleo-seawater and modern seawater intrusion along a preferential pathway on the southwest side.High NH4+concentration is a significant regional characteristic;its δ15N-NH4+values show a wide range(from-2.7‰ to+26.7‰),with most samples far exceeding the typical range(+2‰ to+8‰)for organic matter mineralization.The extremely low NO3-content rules out nitrification as the cause for the 15N enrichment.The material source of the high NH4+is the degradation of natural organic matter in sediments,while the anomalous enrichment in δ15N-NH4+is primarily attributed to the isotopic fractionation effect of the microbial anaerobic ammonium oxidation(anammox)process.Furthermore,analysis of ionic deviation from conservative mixing reveals that NH4+concentration is significantly positively correlated with the positive deviations of Na⁺,K⁺,and HCO3-(p<0.05),and negatively correlated with the negative deviation of SO42-(p<0.05).This study provides a scientific basis for the sustainable development of groundwater resources and the ecological protection of Lisha Island and similar estuarine islands.

李骏;李绍恒;陈建耀;江涛;蔡勋江;曾彩明;江锦锐;陈泽成;任坤

中山大学地理科学与规划学院,广东 广州 510006中山大学地理科学与规划学院,广东 广州 510006||嘉应学院地理科学与旅游学院,广东 梅州 514015中山大学地理科学与规划学院,广东 广州 510006中山大学地理科学与规划学院,广东 广州 510006广东省东莞生态环境监测站,广东 东莞 523000广东省东莞生态环境监测站,广东 东莞 523000广东省东莞生态环境监测站,广东 东莞 523000广东省东莞生态环境监测站,广东 东莞 523000中山大学地理科学与规划学院,广东 广州 510006||中国地质科学院岩溶地质研究所/国土资源部广西岩溶动力学重点实验室,广西 桂林 541004

资源环境

高氨氮地下水同位素示踪厌氧氨氧化水化学海水入侵珠江口

high-ammonium groundwaterisotope tracinganaerobic ammonium oxidationhydrochemistryseawater intrusionPearl River Estuary

《生态环境学报》 2026 (4)

586-597,12

国家重点研发计划项目(2023YFC3709002)中国地质科学院岩溶地质研究所基本科研业务费项目(2023018)

10.16258/j.cnki.1674-5906.2026.04.009

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