Geomorphologic and sedimentary features dominate the nitrogen accumulation and leaching in the deep vadose zone from a catchment viewpoint

IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL
Kangda Tan , Shiqin Wang , Wenbo Zheng , Zhixiong Zhang , Bingxia Liu
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Abstract

Although the application of nitrogen fertilizer increases grain yield, it also raises the risk of nitrogen leaching to groundwater. Not much work has been done on nitrogen accumulation and leaching at a watershed level, especially for deep vadose zone of alluvial-proluvial sediments. Here, nitrate (NO3) accumulation and leaching were investigated in the deep vadose zone (20 m below ground level (b.g.l.)) across Baiyangdian watershed in the North China Plain (NCP). The study area is rich in sedimentary deposits of varying geomorphologic features. Results of the study showed that watershed geomorphologic and sedimentary features control not only soil water flux, but also nitrate accumulation and leaching in the deep vadose zone. Nitrate leaching was highest (252.0 kg·N·ha−1·y−1) and accumulation lowest (352.7 kg·N·ha−1) in regions of the study area with highly permeable sandy alluvial-proluvial fan. In contrast, nitrate accumulation was highest (3276.7 kg·N·ha−1) and leaching lowest (9.8 kg·N·ha−1·y−1) in thick silty/clay flood plains and lake depressions areas. The nitrate flux was primarily driven by vertical infiltration in flood plains and lake depressions. Also, Nitrogen fertilizer (N-fertilizer) input and irrigation affect nitrogen leaching into the deeper vadose zone and groundwater in the study area. It was inferred that, rising of water table under extreme precipitation events could trigger the release accumulated soil nitrogen, the shorten nitrogen leaching lag-time, and increase risk of groundwater pollution. This finding could guide policy decisions given the sensitivity and vulnerability of groundwater to the risk of pollution in the study area.

Abstract Image

从集水区的角度看,深渗透带的氮富集和淋滤主要由地貌和沉积特征决定
虽然氮肥的施用增加了粮食产量,但也增加了氮渗入地下水的风险。在流域水平上,特别是冲积-洪积沉积物的深渗透带,对氮的积累和淋滤的研究还不多。以华北平原白洋淀流域为研究对象,研究了该流域深层渗流带(地下20 m)中硝态氮(NO3 -)的富集和淋溶过程。研究区富含多种地貌特征的沉积矿床。研究结果表明,流域地貌和沉积特征不仅控制着土壤水通量,而且还控制着深层渗透带中硝酸盐的积累和淋滤。高渗透性砂质冲积扇区域的硝态氮淋出量最高(252.0 kg·N·ha−1·y−1),累积量最低(352.7 kg·N·ha−1)。在厚粉质/粘土冲积平原和湖泊洼地,硝态氮积累量最高(3276.7 kg·N·ha - 1),淋滤量最低(9.8 kg·N·ha - 1·y - 1)。河漫滩和湖泊洼地的硝酸盐通量主要由垂直入渗驱动。此外,氮肥的输入和灌溉对研究区深层渗透带和地下水的氮淋滤也有影响。由此推断,极端降水事件下的地下水位上升会触发累积土壤氮的释放,缩短氮淋溶滞后时间,增加地下水污染风险。考虑到研究区域地下水对污染风险的敏感性和脆弱性,这一发现可以指导政策决策。
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来源期刊
Journal of Hydrology
Journal of Hydrology 地学-地球科学综合
CiteScore
11.00
自引率
12.50%
发文量
1309
审稿时长
7.5 months
期刊介绍: The Journal of Hydrology publishes original research papers and comprehensive reviews in all the subfields of the hydrological sciences including water based management and policy issues that impact on economics and society. These comprise, but are not limited to the physical, chemical, biogeochemical, stochastic and systems aspects of surface and groundwater hydrology, hydrometeorology and hydrogeology. Relevant topics incorporating the insights and methodologies of disciplines such as climatology, water resource systems, hydraulics, agrohydrology, geomorphology, soil science, instrumentation and remote sensing, civil and environmental engineering are included. Social science perspectives on hydrological problems such as resource and ecological economics, environmental sociology, psychology and behavioural science, management and policy analysis are also invited. Multi-and interdisciplinary analyses of hydrological problems are within scope. The science published in the Journal of Hydrology is relevant to catchment scales rather than exclusively to a local scale or site.
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