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河套灌区不同时期地下水氮磷时空分布特征与影响因素研究OA

Study on the Spatiotemporal Distribution Characteristics and Influencing Factors of Nitrogen and Phosphorus in Groundwater in the Hetao Irrigation Area During Different Periods

中文摘要英文摘要

内蒙古河套灌区是中国三个特大型灌区之一,区域内浅层地下水存在不同程度的氮磷污染,威胁区域饮水安全与农业可持续发展.以河套灌区最大灌域—义长灌域为研究区,于2024年8月和10月各布设76个监测点进行实地采样,分析了氮磷的时空特征以及水化学类型,同时结合氢氧同位素联合贝叶斯混合模型(MixSIAR)解析补给来源,并采用主成分分析和Pearson相关揭示主要影响因素.结果表明:时间上,10月地下水总氮(TN)浓度(平均14.7 mg/L)高于8月TN浓度(平均12.6 mg/L),10月总磷(TP)浓度(平均0.074 mg/L)低于8月TP浓度(平均0.127 mg/L);空间上,TN沿总排干呈点状高值分布,高浓度区集中于大型村落及养殖场周边,TP高值区主要集中在排水干沟上游及排水干沟转弯沉积处.水化学分析表明地下水以 Cl-Na 型为主,氢氧同位素与MixSIAR模型表明其补给主要源于沟渠水入渗(贡献率>92%).影响因素分析指出,农业施肥、养殖粪便及农村生活污水排放是核心污染源,水文地球化学过程(如高Cl-竞争吸附促进磷的迁移、高 HCO3-促进磷的沉淀等)以及降雨事件共同塑造了氮磷污染的时空格局.该结果为灌区地下水污染管控与农业可持续管理提供了科学依据.

The Hetao Irrigation District in Inner Mongolia stands as one of China's three large-scale irrigation districts.The shallow groundwater within this region is subjected to varying degrees of nitrogen and phosphorus contamination,posing threats to both local drinking water security and sustainable agricultural development.This study focuses on the largest irrigation area within the Hetao Irrigation District—the Yichang Irrigation Area.In August and October 2024,a total of 76 monitoring points were established for field sampling.The spatiotemporal characteristics of nitrogen and phosphorus,as well as hydrochemical types,were analyzed.Additionally,hydrogen and oxygen isotopes combined with the Bayesian mixing model(MixSIAR)were used to identify recharge sources,while principal component analysis(PCA)and Pearson correlation were employed to reveal the main influencing factors.The results indicate that temporally the mean groundwater total nitrogen(TN)concentration was higher in October(14.7 mg/L)than in August(12.6 mg/L),while the mean total phosphorus(TP)concentration was lower in October(0.074 mg/L)compared to August(0.127 mg/L).Spatially,TN exhibited a punctate high-value distribution along the main drainage ditch,with high-concentration areas concentrated around large villages and breeding farms.High TP values were mainly found in the upstream sections of the main drainage channels and at sedimentation points where the channels bend.Hydrochemical analysis showed that groundwater is predominantly of the Cl-Na type.Hydrogen and oxygen isotopes,along with the MixSIAR model,indicated that recharge primarily originates from canal water infiltration(contribution rate>92%).Analysis of influencing factors revealed that agricultural fertilization,livestock manure,and rural domestic wastewater discharge are the core pollution sources.Hydrogeochemical processes(such as high Cl-competitive adsorption promoting phosphorus migration and high HCO3-facilitating phosphorus precipitation)and rainfall events collectively shape the spatiotemporal patterns of nitrogen and phosphorus pollution.These findings provide a scientific basis for groundwater pollution control and sustainable agricultural management in irrigation districts.

陈光宇;柴猛;曹倡铭;刘芮宏;岳卫峰;李卫平;屈忠义

内蒙古科技大学能源与环境学院,内蒙古 包头 014010||黄河流域内蒙古段生态保护与综合利用自治区协同创新中心,内蒙古 包头 014010内蒙古科技大学能源与环境学院,内蒙古 包头 014010||黄河流域内蒙古段生态保护与综合利用自治区协同创新中心,内蒙古 包头 014010北京师范大学水科学研究院,北京 100875内蒙古科技大学能源与环境学院,内蒙古 包头 014010北京师范大学水科学研究院,北京 100875内蒙古科技大学能源与环境学院,内蒙古 包头 014010||黄河流域内蒙古段生态保护与综合利用自治区协同创新中心,内蒙古 包头 014010内蒙古科技大学能源与环境学院,内蒙古 包头 014010||黄河流域内蒙古段生态保护与综合利用自治区协同创新中心,内蒙古 包头 014010

农业科技

河套灌区地下水氮磷水化学成分氢氧同位素影响因素

Hetao Irrigation Areagroundwaternitrogen and phosphorushydrochemistryhydrogen and oxygen isotopesinfluencing factors

《节水灌溉》 2026 (5)

24-31,8

国家自然科学基金项目(52179032).

10.12396/jsgg.2025427

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