Prediction of nitrate accumulation and leaching beneath groundwater irrigated corn fields in the Upper Platte basin under a future climate scenario

被引:22
作者
Akbariyeh, Simin [1 ]
Pena, Cesar Augusto Gomez [2 ]
Wang, Tiejun [3 ]
Mohebbi, Amin [4 ]
Bartelt-Hunt, Shannon [5 ]
Zhang, Jianmin [6 ]
Li, Yusong [5 ]
机构
[1] Calif Polytech State Univ San Luis Obispo, Dept Civil & Environm Engn, N Perimeter Rd, San Luis Obispo, CA 93405 USA
[2] Technol Univ Panama, Reg Ctr Chiriqui, Dept Civil Engn, Sixth West Ave, David Dist 0401, Chiriqui County, Panama
[3] Tianjin Univ, Inst Surface Earth Syst Sci, Weijin Rd Campus,92 Weijin Rd, Tianjin 300072, Peoples R China
[4] No Arizona Univ, Dept Civil Engn Construct Management & Environm E, 2112 S Huffer Ln, Flagstaff, AZ 86011 USA
[5] Univ Nebraska, Dept Civil Engn, 844 N 16th St, Lincoln, NE 68508 USA
[6] Sichuan Univ, State Key Lab Hydraul & Mt River Engn, 24 South Sect 1,Yihuan Rd, Chengdu 610065, Sichuan, Peoples R China
基金
美国农业部;
关键词
Climate change; Groundwater recharge; Nitrate-N accumulation; Vadose zone modeling; SOIL-MOISTURE DYNAMICS; PRINCE-EDWARD-ISLAND; HIGH-PLAINS AQUIFER; FEASIBILITY ANALYSIS; RECHARGE ESTIMATION; REGIONAL ESTIMATION; CROP PRODUCTION; WATER-BALANCE; IMPACT; EVAPOTRANSPIRATION;
D O I
10.1016/j.scitotenv.2019.05.417
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
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.
引用
收藏
页码:514 / 526
页数:13
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