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首页> 外文期刊>The Science of the Total Environment >Prediction of nitrate accumulation and leaching beneath groundwater irrigated corn fields in the Upper Platte basin under a future climate scenario
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Prediction of nitrate accumulation and leaching beneath groundwater irrigated corn fields in the Upper Platte basin under a future climate scenario

机译:在未来气候情景下上普拉特盆地地下水灌溉玉米田下硝酸盐累积和淋失的预测

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摘要

Understanding the impacts of future climate change on soil hydrological processes and solute transport is crucial to develop appropriate strategies to minimize the adverse impacts of agricultural activities on groundwater quality. To evaluate the direct effects of climate change on the transport and accumulation of nitrale-N, we developed an integrated modeling framework combining climatic change, nitrate-N infiltration in the unsaturated zone, and groundwater level fluctuations. The study was based on a center-pivot irrigated corn field at the Nebraska Management Systems Evaluation Area (MSEA) site. Future groundwater recharge (GR) and actual evapotranspiration (ETa) rates were predicted via an inverse vadose zone modeling approach by using climatic data generated by the Weather Research and Forecasting (WRF) climate model under the RCP 8.5 scenario, which was downscaled from the global CCSM4 model to a resolution of 24 km by 24 km. A groundwater flow model was first calibrated on the basis of historical groundwater table measurements and then applied to predict the future groundwater table in 2057-2060. Finally, the predicted future GR rate, ETa rate, and groundwater level, together with future precipitation data from the WRF climate model, were used in a three-dimensional (3D) model to predict nitrate-N concentrations in tire subsurface (saturated and unsaturated parts) from 2057 to 2060. The future GR was predicted to decrease in the study area, as compared with the average GR data from the literature. Correspondingly, the groundwater level was predicted to decrease (30 to 60 cm) over the 5 years of simulation in the future. The nitrate-N mass in the simulation domain was predicted to increase but at a slower rate than in the past. Sensitivity analysis indicated that the accumulation of nitrate-N is sensitive to groundwater table elevation changes and irrigation rates. (C) 2019 Elsevier B.V. All rights reserved.
机译:了解未来气候变化对土壤水文过程和溶质运移的影响,对于制定适当的策略以最小化农业活动对地下水质量的不利影响至关重要。为了评估气候变化对硝态氮的运输和积累的直接影响,我们开发了一个综合的建模框架,该框架结合了气候变化,非饱和区硝态氮的渗透和地下水位的波动。该研究基于内布拉斯加州管理系统评估区(MSEA)站点的中心枢轴灌溉玉米田。通过反渗流区建模方法,使用天气研究与预报(WRF)气候模型在RCP 8.5情景下生成的气候数据,通过反渗流区建模方法预测了未来的地下水补给(GR)和实际蒸散(ETa)速率,该数据已从全球范围缩减CCSM4模型的分辨率为24 km x 24 km。首先根据历史地下水位测量值对地下水流量模型进行校准,然后将其用于预测2057-2060年的未来地下水位。最后,将预测的未来GR率,ETa率和地下水位以及WRF气候模型的未来降水数据一起用于三维(3D)模型中,以预测轮胎地下(饱和和非饱和)中的硝酸盐氮浓度部分)从2057年到2060年。与文献中的平均GR数据相比,预计研究区域的未来GR将会减少。相应地,在未来的5年模拟中,预计地下水位将下降(30至60 cm)。预计模拟域中的硝态氮质量会增加,但增速会比过去慢。敏感性分析表明,硝态氮的积累对地下水位的高程变化和灌溉速率敏感。 (C)2019 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《The Science of the Total Environment 》 |2019年第1期| 514-526| 共13页
  • 作者单位

    Calif Polytech State Univ San Luis Obispo, Dept Civil & Environm Engn, N Perimeter Rd, San Luis Obispo, CA 93405 USA;

    Technol Univ Panama, Reg Ctr Chiriqui, Dept Civil Engn, Sixth West Ave, David Dist 0401, Chiriqui County, Panama;

    Tianjin Univ, Inst Surface Earth Syst Sci, Weijin Rd Campus,92 Weijin Rd, Tianjin 300072, Peoples R China;

    No Arizona Univ, Dept Civil Engn Construct Management & Environm E, 2112 S Huffer Ln, Flagstaff, AZ 86011 USA;

    Univ Nebraska, Dept Civil Engn, 844 N 16th St, Lincoln, NE 68508 USA;

    Sichuan Univ, State Key Lab Hydraul & Mt River Engn, 24 South Sect 1,Yihuan Rd, Chengdu 610065, Sichuan, Peoples R China;

    Univ Nebraska, Dept Civil Engn, 844 N 16th St, Lincoln, NE 68508 USA;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Climate change; Groundwater recharge; Nitrate-N accumulation; Vadose zone modeling;

    机译:气候变化;地下​​水补给;硝酸盐 - 氮积累;Vadose区建模;

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