University of Coimbra, CEMMPRE, Department of Civil Engineering, University of Coimbra, Polo 2, 3030-788, Coimbra, Portugal.
Department of Earth and Environmental Sciences, University of Waterloo, Waterloo, Ontario, N2L 3G1, Canada.
Environ Sci Pollut Res Int. 2022 Apr;29(16):23919-23935. doi: 10.1007/s11356-021-16725-x. Epub 2021 Nov 24.
Nitrogen (N) legacies have built up in anthropogenic landscapes over decades of agricultural intensification, and these legacies lead to time lags in water quality change measurable even beyond the moment of application of N. It is important to understand these legacies to quantify the relationship between N inputs and N concentrations in streams and implement best management practices for water quality improvement; however, little is known about the magnitude of legacies in various landscape elements like soils and groundwater. Here, we have used the ELEMeNT (Exploration of Long-tErM Nutrient Trajectories) model to explore the buildup and depletion of N legacies over a 216-year period, across the Mondego River Basin, a 6645-km watershed in Portugal, where human interventions have considerably changed the characteristics of the basin to prevent floods and improve farming conditions in recent decades. The results show that the increase in the amount of inorganic fertilizer applied was the main driver for the anthropogenic N loads in the watershed from 1950 until the beginning of the 1990s. The N inputs have been decreasing since then, but N loads in the river did not document any decrease till the 1990s; after which there was a decline. This time lag between the N inputs to the watershed and the N loads in the river (about two decades) is a function of accumulation of N legacy.
几十年来,农业集约化导致人为景观中氮(N)遗留物不断积累,这些遗留物导致水质变化的时间滞后,甚至在施加 N 之后仍可测量到。了解这些遗留物对于量化 N 输入与溪流中 N 浓度之间的关系以及实施改善水质的最佳管理实践非常重要;然而,对于土壤和地下水等各种景观要素中遗留物的程度知之甚少。在这里,我们使用 ELEMeNT(长期养分轨迹探索)模型,探索了 216 年来葡萄牙蒙德古河流域 6645 平方公里流域中氮遗留物的积累和消耗情况,在过去几十年中,人为干预极大地改变了流域的特征,以防止洪水和改善农业条件。结果表明,自 1950 年以来,无机化肥施用量的增加是流域人为氮负荷的主要驱动因素,直到 1990 年代初。此后,氮输入一直在减少,但直到 1990 年代,河流中的氮负荷并没有减少;此后出现了下降。这种氮输入到流域和河流中氮负荷之间的时间滞后(约二十年)是氮遗留物积累的函数。