首页|洞庭湖湿地潜流带地下水中氮磷迁移转化过程及驱动机制分析

洞庭湖湿地潜流带地下水中氮磷迁移转化过程及驱动机制分析

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为了揭示洞庭湖湿地潜流带地下水中氮磷的迁移转化过程,以洞庭湖湘江入湖口附近湿地为研究区,定期采集地表水和地下水水样进行水化学参数测试,采用熵权指数法进行水质评价,运用相关性分析、结构方程模型等方法研究理化参数对氮磷迁移转化的驱动机制。结果表明:58。8%的地下水水样为Ⅳ类或Ⅴ类水,TN、NH4+和TP是主要的超标因子,氮的迁移转化主要受矿化作用、反硝化作用和硝酸盐异化还原成铵等反应控制,磷的迁移富集与Fe/Mn氧化物或氢氧化物的还原性溶解密切相关;地下水中氮磷组分含量在丰水期和枯水期表现出明显差异,受潜流交换作用影响,除NH4+、溶解有机氮和TN外,地下水中NO2-、NO3-、TP和溶解态活性磷含量随着河岸距离增加而减小;温度、氧化还原电位、溶解氧、总溶解固体和电导率均会影响微生物活性,是地下水中氮磷迁移转化的关键驱动因子。
Analysis of nitrogen and phosphorus migration and transformation and driving mechanism in hyporheic zone groundwater of Dongting Lake wetland
In order to reveal the migration and transformation process of nitrogen and phosphorus in groundwater in the hyporheic zone of wetland,the wetland near the entrance of the Xiang River to Dongting Lake was taken as the study area,and surface water and groundwater samples were collected and hydrochemical parameters were measured periodically.The entropy weight index method was used for water quality evaluation,and correlation analysis and structural equation modeling were applied to study the driving mechanism of physicochemical parameters on nitrogen and phosphorus migration and transformation.The results show that 58.8%of the groundwater samples are class Ⅳ or Ⅴ,and total nitrogen(TN),NH4+and total phosphorus(TP)are the main over-standard factors.The migration and transformation of nitrogen are mainly controlled by mineralization,denitrification,and dissimilatory nitrate reduction to ammonium,and the migration and enrichment of phosphorus are closely related to the reducing dissolution of Fe/Mn oxides or hydroxides.The contents of nitrogen and phosphorus components in the groundwater show obvious differences between the wet and the dry seasons.Under the influence of the hyporheic exchange,except for NH4,dissolved organic nitrogen and TN,the contents of NO2-,N03-,TP and soluble reactive phosphorus in the groundwater decrease with increasing distance from the riverbank.Temperature,redox potential,dissolved oxygen,total dissolved solids,and electrical conductivity can affect microbial activity and are key driving factors for nitrogen and phosphorus migration and transformation in groundwater.

hyporheic zonegroundwaternitrogen and phosphorus migration and transformationentropy weight index methodstructural equation modelDongting Lake wetland

陆帅帅、周念清、蔡奕、郭梦申、赵文刚、王在艾

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同济大学土木工程学院,上海 200092

湖南省水利水电科学研究院,湖南长沙 410007

潜流带 地下水 氮磷迁移转化 熵权指数法 结构方程模型 洞庭湖湿地

国家自然科学基金项目国家自然科学基金项目

4207717642272291

2024

水资源保护
河海大学 中国水利学会环境水利研究会

水资源保护

CSTPCD北大核心EI
影响因子:0.827
ISSN:1004-6933
年,卷(期):2024.40(5)