ISSN 1000-3665 CN 11-2202/P

    江汉平原东部农业区浅层地下水无机氮素分布特征及成因分析

    Distribution characteristics and migration mechanism of inorganic nitrogen in shallow groundwater in the agricultural area of the eastern Jianghan Plain

    • 摘要: 地下水无机氮素污染是江汉平原较为普遍的水环境问题之一,农业活动是地下水中无机氮的重要来源。然而,在河网密集的农业区,受降水和地表水补给的浅层地下水中无机氮素的污染来源和迁移转化机制的研究尚有所欠缺。研究以江汉平原东部河网密集的农业区为研究对象,采用水化学结合氢氧同位素和锶同位素的方法,分析了地表水和地下水的化学特征、无机氮素的来源及其迁移转化机制。结果表明:(1)研究区地表水和地下水阳离子以Ca2+和Na+为主,阴离子以\mathrmHCO_3^- 为主,水化学类型主要为HCO3—Ca•Na和HCO3—Ca型;(2)地表水和地下水中的无机氮素均是以硝酸盐为主,地下水无机氮素的浓度明显高于地表水,硝酸盐浓度较高的地下水样主要分布于北部和南部城镇周边,氨氮浓度较高的水样分布较为零散;(3)地表水和地下水的主要补给来源是大气降水,其水化学特征主要受硅酸盐和蒸发岩风化作用的控制,且受到了人类活动的影响;(4)地表水中极低浓度的无机氮主要来源于大气降水,地下水中相对较高浓度的无机氮主要来源于农业地区的生活污水和粪便;(5)氧化还原条件影响了无机氮组分的相互转化,表层的污染源无机氮素以氨氮为主,地下水氨氮浓度较高,随着大气降水向下的运移伴随着硝化反应的发生,硝酸盐逐渐富集。研究成果有助于了解水网密集农业区地下水无机氮富集的成因和迁移转化机制,可为江汉平原的地下水污染防控提供重要科学依据。

       

      Abstract: Groundwater inorganic nitrogen contamination is one of the most widespread water environmental issues in the Jianghan Plain. Agricultural activities constitute an important source of inorganic nitrogen in groundwater. However, in agricultural regions characterized by dense river networks, the sources, migration pathways, and transformation mechanisms of inorganic nitrogen in shallow groundwater recharged by precipitation and surface water remain insufficiently understood. Taking the agricultural area of the eastern Jianghan Plain as a case study, the chemical characteristics, the source of inorganic nitrogen, and its migration and transformation mechanism of surface water and groundwater were analyzed by hydrochemistry combined with hydrogen-oxygen and strontium isotopes. The results show that the cations of surface water and groundwater samples in the study area were dominated by Ca2+ and Na+, and the anions were dominated by \mathrmHCO_3^- .The water chemical type was dominated by HCO3–Ca•Na and HCO3–Ca. The inorganic nitrogen in surface water and groundwater was mainly nitrate, and the concentration of inorganic nitrogen in groundwater was significantly higher than that in surface water. The groundwater with high nitrate concentration was mainly distributed around the northern and southern towns, and the distribution of ammonia nitrogen with high concentration was scattered. Precipitation was the primary source of surface water and groundwater recharge in the region. The chemical characteristics of surface water and groundwater were mainly controlled by silicate and evaporite weathering, and were obviously affected by human activities. The surface water with extreme low concentration of inorganic nitrogen was mainly from atmospheric precipitation, while the groundwater with relatively high concentration of inorganic nitrogen was mainly from domestic sewage and feces in agricultural areas. The mutual transformation of inorganic nitrogen components was affected by the redox conditions. The inorganic nitrogen of the pollution source in the surface layer was mainly ammonia nitrogen, and the concentration of ammonia nitrogen in groundwater is high. Nitrate was gradually enriched by nitrification, accompanied by the downward migration of atmospheric precipitation. This study is of great significance for understanding the causes and migration and transformation mechanism of inorganic nitrogen enrichment in groundwater in agricultural areas with dense water networks, and for the prevention and control of groundwater pollution in Jianghan Plain.

       

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