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New insight into the response and transport of nitrate in karst groundwater to rainfall events

地下水 硝酸盐 喀斯特 水文学(农业) 地表径流 环境科学 反硝化 地表水 自流含水层 地下水流 含水层 地质学 氮气 化学 环境工程 生态学 古生物学 岩土工程 有机化学 生物
作者
Zhongjun Wang,Fu‐Jun Yue,Lu Ji,Yuchun Wang,Caiqing Qin,Hu Ding,Lili Xue,Si‐Liang Li
出处
期刊:Science of The Total Environment [Elsevier BV]
卷期号:818: 151727-151727 被引量:29
标识
DOI:10.1016/j.scitotenv.2021.151727
摘要

Abstract Although numerous studies focused on nitrate source, transformation and transport of river water in karst area have been reported, it's still unclear in understanding nitrate main source and transformation in karst groundwater system and how nitrate transport from soil to water during rainfall events in karst critical zone. In order to explore the response and transport of nitrate in karst groundwater to rainfall events, different depths of well water before, during and after rainfall event were sampled, and hillslope runoff, surface runoff of different land-use types during rainfall event were sampled synchronously at a typical karst agricultural catchment in Southwest China. Results showed that fluctuations of EC, pH and DO in deep borehole well (W1) and artesian well (W2) were small, on the contrary, variations of EC and DO in shallow well (W3) were large during sampling period. The nitrate concentrations and isotopic values indicated that nitrate in karst groundwater mainly originated from chemical fertilizer (CF), and influenced by denitrification process. High intensity of denitrification was observed in deep groundwater (87%) and artesian well water (almost 100%). Extremely high dual nitrate isotope values up to 46.8 ± 1.5‰ and 24.7 ± 0.5‰ were found in the deep artesian well. The small variation of water chemistry (EC, DO and pH), nitrate concentration and dual nitrate isotope values in deep wells during sampling period suggested that newly supplied nitrogen in deep groundwater during rainfall events also comes from deep groundwater. Low nitrogen concentrations in hillslope subsurface flow and surface runoff suggests that nitrogen transport process leading to increase of water nitrogen content mainly occur in depression. Nitrogen in depression soil is mainly transported to groundwater through fissures, fractures and conduits, rather than through vertical migration processes in the soil during rainfall events.

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