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EFFECTS OF SUBSURFACE DRAINAGE SYSTEMS ON WATER AND NITROGEN FOOTPRINTS SIMULATED WITH RZWQM2

机译:地下排水系统对RZWQM2模拟水和氮足迹的影响

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Developing drainage water management (DWM) systems in the Midwest to reduce nitrogen (N) transport to the northern Gulf of Mexico hypoxic zone requires understanding of the long-term performance of these systems. Few studies have evaluated long-term impacts of DWM, and the simulation of controlled drainage (CD) with the Root Zone Water Quality Model (RZWQM) is limited, while shallow drainage (SD) has not been examined. We tested RZWQM using nine years (2007-2015) of field data from southeast Iowa for CD, SD, conventional drainage (DD), and undrained (ND) systems and simulated the long-term (1971-2015) impacts. RZWQM accurately simulated N loss in subsurface drainage, and the simulations agreed with field data that CD and SD substantially reduced N loss to drainage. As indicated by the field data, the SD N concentration was predicted to be greater than DD and CD, likely due to reduced time of travel to shallower drains. The long-term simulations show that CD and SD reduced annual N lost via tile drainage by 26% and 40%, respectively. Annual reductions in N lost via tile drainage ranged from 28% in the driest years to 22% in the wettest years for CD and from 56% in the driest years to 35% in the wettest years for SD. Considering spring N loading for the purpose of addressing hypoxia in the Gulf of Mexico, CD was found to be less effective than SD, and in many years CD exported more N in the spring than DD. Spring N loading (April through June) was indicated by the EPA Science Advisory Board to have the greatest impact on hypoxia in the northern Gulf of Mexico. Therefore, improvement of CD systems within the months of April through June to reduce N loss via drainage across the upper Midwest landscape may be required. Limited research in the upper Midwest has addressed spring N loading under controlled drainage systems (CD). This research will help model developers, model users, and agricultural scientists more clearly understand N transport under different systems, including CD, SD, and ND, which will aid in developing the design and management of drainage systems to reduce N transport from tile-drained agriculture to surface waters.
机译:开发中西部地区的排水水管理(DWM)系统减少氮气(n)运输到墨西哥北湾缺氧区需要了解这些系统的长期性能。很少有研究评估了DWM的长期影响,并且控制引流(CD)的模拟与根区水质模型(RZWQM)有限,而浅排水(SD)尚未被检查。我们使用来自东南IOWA的九年(2007-2015)的RZWQM用于CD,SD,常规排水(DD)和未推迟(ND)系统的现场数据,并模拟长期(1971-2015)的影响。 RZWQM在地下排水中准确地模拟了N损失,并且模拟与CD和SD的现场数据同意,CD和SD显着降低了排水的损耗。如现场数据所示,预测SD N浓度大于DD和CD,可能由于行驶时间减少到较浅的漏斗。长期仿真显示CD和SD分别减少了通过瓷砖排水减少26%和40%。通过瓷砖排水的人数减少的年度减少在最干燥的年度达到28%,在最潮湿的岁月中达到22%,在最干燥的几年中56%到35%到35%的SD。考虑到春季N负载用于解决墨西哥湾的缺氧,发现CD比SD效果不那么有效,并且在许多年中,CD在春季比DD导出更多N. EPA科学咨询委员会指示春天(四月至6月)对墨西哥北部的缺氧产生最大的影响。因此,可能需要改善4月份的CD系统,以便通过跨越中西部景观的排水减少N损失。上下中西部的有限研究已经解决了控制排水系统(CD)下的弹簧N负载。该研究将有助于建模开发商,模型用户和农业科学家更清楚地了解不同系统的运输,包括CD,SD和ND,这将有助于开发排水系统的设计和管理,以减少从瓷砖排出的输送农业到地表水域。

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