Using Sobol' sensitivity analysis to identify important model layers of a prediction model for simulating soil nitrogen transport in surface runoff and subsurface water

被引:0
作者
Zhang, Shiwei [1 ,2 ]
Tong, Juxiu [1 ,2 ]
Ye, Ming [3 ]
机构
[1] China Univ Geosci Beijing, MOE Key Lab Groundwater Circulat & Environm Evolut, Beijing 100083, Peoples R China
[2] China Univ Geosci Beijing, Sch Water Resources & Environm, Beijing 100083, Peoples R China
[3] Florida State Univ, Dept Earth Ocean & Atmospher Sci, Tallahassee, FL 32306 USA
基金
中国国家自然科学基金;
关键词
HYDRUS-1D; Sobol GSA; The prediction model of soil nitrogen transport; Model parameter; GLOBAL SENSITIVITY; HYDRAULIC CONDUCTIVITY; UNCERTAINTY ANALYSIS; CHEMICAL-TRANSPORT; SOLUTE-TRANSPORT; OVERLAND-FLOW; RAINFALL; DENITRIFICATION; NITRIFICATION; INFILTRATION;
D O I
10.1007/s00477-024-02894-x
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Due to complex soil conditions of farmlands, a model simulating soil nitrogen transport in surface runoff and subsurface water is subject to uncertainty not only in model parameters but also in representation of soil layers in model layers. This study presents a model of nitrogen transport with the following three layers: a ponding-runoff layer, a soil mixing layer, and a underlying soil layer, which have a total of nine parameters. The model simulates concentrations of urea, ammonia nitrogen, and nitrate nitrogen in surface water and at the depths of 2 cm and 32 cm below soil surface. The main focus of this study is to identify the most important model layer that is crucial for simulating soil nitrogen transport. The global sensitivity analysis method of Sobol' is used to examine importance of the three model layers, because the Sobol' method can consider impacts of individual parameters and parameters interactions on model simulations. Results show the following: (1) the soil mixing layer is the most important one for simulating urea transport in surface water, and the underlying soil layer is the most important one for simulating NH4+-N and NO3--N transport in surface water, (2) the underlying soil layer is the most important one for simulating nitrogen transport at the depths of 2 cm and 32 cm below soil surface, and (3) parameters interactions have a negligible impact on the simulations. These results can be used for improvement of the model and reduction of model prediction uncertainty, and provide a reference for subsequent studies on soil nitrogen transport to reduce agricultural non-point sources pollution.
引用
收藏
页码:747 / 763
页数:17
相关论文
共 57 条
[31]   Simulating soil conservation measures to control soil and nutrient losses in a small, vineyard dominated, basin [J].
Ramos, M. C. ;
Benito, C. ;
Martinez-Casasnovas, J. A. .
AGRICULTURE ECOSYSTEMS & ENVIRONMENT, 2015, 213 :194-208
[32]   Measuring and modeling ammonium adsorption by calcareous soils [J].
Ranjbar, F. ;
Jalali, M. .
ENVIRONMENTAL MONITORING AND ASSESSMENT, 2013, 185 (04) :3191-3199
[33]  
Rose C. W., 1985, Advances in Soil Science, USA, V2, P1
[34]   Solute Transfer from the Soil Surface to Overland Flow: A Review [J].
Shi, Xiaonan ;
Wu, Laosheng ;
Chen, Weiping ;
Wang, Quanjiu .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 2011, 75 (04) :1214-1225
[35]  
Simunek J., 2013, HYDRUS Software Series, V3, P342
[36]  
SNYDER JK, 1985, T ASAE, V28, P1450, DOI 10.13031/2013.32459
[37]  
Sobol I.M., 1993, MATH MODELING COMP E, V1, P407, DOI DOI 10.18287/0134-2452-2015-39-4-459-461
[38]   Global sensitivity analysis in hydrological modeling: Review of concepts, methods, theoretical framework, and applications [J].
Song, Xiaomeng ;
Zhang, Jianyun ;
Zhan, Chesheng ;
Xuan, Yunqing ;
Ye, Ming ;
Xu, Chonggang .
JOURNAL OF HYDROLOGY, 2015, 523 :739-757
[39]   PARAMETER UNCERTAINTY AND INTERACTION IN COMPLEX ENVIRONMENTAL-MODELS [J].
SPEAR, RC ;
GRIEB, TM ;
SHANG, N .
WATER RESOURCES RESEARCH, 1994, 30 (11) :3159-3169
[40]  
STEENHUIS TS, 1980, T ASAE, V23, P615, DOI 10.13031/2013.34634