University of Illinois at Urbana-Champaign, Champaign, IL 61801, USA.
Sci Total Environ. 2021 Mar 10;759:143502. doi: 10.1016/j.scitotenv.2020.143502. Epub 2020 Nov 11.
The use of nitrogen (N) fertilizer marked the start of modern agriculture that boosted food production to help alleviate food shortages across the globe but at the cost of severe environmental issues and critical stress to the agroecosystem. This paper was aimed at determining the fate and transport of nitrite and ammonia under future climate projections by adapting the recommended land management practices that are supposed to reduce nitrate N in surface water to state government target. To accomplish these objectives, a fully-distributed physical-based hydrologic model, MIKE SHE, and a hydrodynamic river model, MIKE 11, were coupled with MIKE ECO-Lab to simulate the fate and transport of different forms of N in the agro-ecosystem in the Upper Sangamon River Basin (USRB). Twelve (12) combinations of land management and climate projections were simulated to evaluate the N fate and transport in the USRB from 2020 to 2050. Under the current land management, the nitrate concentration in surface water was expected to exceed the EPA limit of 10 ppm up to 2.5% of the days in the simulation period. Regulating the fertilizer application rates to approximately 50% of the current rate will ensure this limit will not be exceeded in the future. Implementing cover cropping alone can potentially decrease nitrate N concentrations by 33% in surface water under dry climate and in the saturated zone under future projections. By combining the cover cropping and regulated application rate management, the nitrate N concentration in the saturated zone was expected to decrease by 67% compared with historic baseline. The modeling framework developed and used in this study can help evaluate the effectiveness of different management schemes aimed at reducing future nutrient load in our surface water and groundwater.
氮肥的使用标志着现代农业的开端,它提高了粮食产量,有助于缓解全球粮食短缺问题,但也带来了严重的环境问题和对农业生态系统的严重压力。本文旨在通过适应建议的土地管理实践,将地表水中硝酸盐氮减少到州政府的目标,来确定亚硝酸盐和氨在未来气候预测下的归宿和运移。为了实现这些目标,我们采用了完全分布式物理基础水文模型 MIKE SHE 和水动力河模型 MIKE 11,并与 MIKE ECO-Lab 耦合,以模拟农业生态系统中不同形式氮的归宿和运移。模拟了 12 种土地管理和气候预测组合,以评估从 2020 年到 2050 年美国桑加蒙河流域(USRB)的氮归宿和运移。在当前的土地管理下,预计地表水中的硝酸盐浓度将在模拟期内超过 EPA 限值 10 ppm 的天数高达 2.5%。将肥料施用量调节到目前用量的 50%左右,可确保未来不会超过这一限制。仅实行覆盖作物种植,在干旱气候下和未来预测中饱和带中,地表水中的硝酸盐氮浓度可能会降低 33%。通过结合覆盖作物种植和调控施用量管理,与历史基线相比,预计饱和带中的硝酸盐氮浓度将降低 67%。本研究中开发和使用的建模框架可用于评估不同管理方案的有效性,旨在减少未来我们地表水和地下水的养分负荷。