Insights gained from two decades of intensive monitoring: hydrology and nitrate export in a tile-drained agricultural catchment

Andreas Bauwe, Bernd Lennartz
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Abstract

Nitrate (NO3−) export from agricultural land poses an ongoing threat to both inland and coastal waters. Experimental studies investigating the hydrology-NO3−-export mechanisms require long-term data to identify reliable causal relationships. In this study, utilizing a 23-year continuous dataset with a high temporal resolution (daily to twice a week), we aim to identify potential drivers for NO3-losses and assess the impact of nitrogen (N) soil surface budgets on NO3-export. A drainage plot (4.2 ha) and a ditch catchment (179 ha) were fully equipped to register hydrological parameters, including water sample collection. Mean annual NO3−-N concentrations (loads) for the drainage plot and the ditch catchment were 9.4 mg l−1 (20.6 kg ha−1) and 6.0 mg L−1 (20.9 kg ha−1), respectively. Annual discharge was closely positively correlated with annual NO3-losses, highlighting the significant influence of prevailing weather and, consequently, hydrologic conditions on NO3-export rates. The majority of the annual NO3−-load was exported during winter (56% at the drainage plot, 51% at the ditch catchment), while the rest was exported during spring (28, 29%), summer (9, 9%) and fall (7, 11%). We could not find any direct relationships between N soil surface budgets and NO3-losses. Putting all results together, it can be concluded that agricultural activities for many decades resulted in high soil N stocks, which determined the general high NO3−-N concentration levels. Nevertheless, temporal NO3-export dynamics during the last two decades were clearly driven by hydro-meteorological conditions, nearly independently of land management and N soil surface budgets on the fields.
二十年密集监测的启示:瓦片排水农业集水区的水文和硝酸盐输出
农田排放的硝酸盐(NO3-)对内陆和沿海水域都构成了持续的威胁。调查水文-NO3-输出机制的实验研究需要长期数据来确定可靠的因果关系。在这项研究中,我们利用 23 年连续数据集和高时间分辨率(每天到每周两次),旨在确定 NO3 损失的潜在驱动因素,并评估氮(N)土壤表面预算对 NO3 排放的影响。一个排水小区(4.2 公顷)和一个沟渠集水区(179 公顷)配备了完整的水文参数登记设备,包括水样采集。排水地块和沟渠集水区的年平均 NO3-N 浓度(负荷)分别为 9.4 毫克/升(20.6 千克/公顷)和 6.0 毫克/升(20.9 千克/公顷)。年排放量与年 NO3 损失量呈密切的正相关关系,这突出表明了当时的天气以及水文条件对 NO3 出口率的重要影响。每年的 NO3 负荷大部分在冬季输出(56% 在排水地块,51% 在沟渠集水区),其余则在春季(28%,29%)、夏季(9%,9%)和秋季(7%,11%)输出。我们没有发现土壤表面氮含量与三氧化二氮流失量之间有任何直接关系。综合所有结果,我们可以得出结论:几十年来的农业活动导致土壤氮储量较高,这也决定了 NO3-N 浓度水平普遍较高。然而,在过去二十年中,氮氧化物的时间输出动态明显受水文气象条件的驱动,几乎与土地管理和田地的氮土壤表层预算无关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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