Analysis of the hydrology and flow of nitrogen in 17 Danish catchments

被引:19
作者
Andersen, HE [1 ]
Pedersen, ML [1 ]
Jorgensen, O [1 ]
Kronvang, B [1 ]
机构
[1] Natl Environm Res Inst, Dept Streams & Riparian Areas, DK-8600 Silkeborg, Denmark
关键词
hydrologic modelling; hydrologic pathways; nitrogen leaching; subsurface nitrogen removal;
D O I
10.2166/wst.2001.0390
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In the search for tools for evaluating the effects of national action plans combating diffuse nutrient pollution causing eutrophication of surface waters, a study of the nitrogen (N) flow in 17 Danish agricultural catchments was carried out. Data on N input and IN harvest for the agricultural year of 1993/1994 was obtained from questionnaire surveys facilitating the set up of N balances. Net export of N from the catchments measured at the outlet was obtained from time-series of stream water chemistry and discharge from 1993-1997. N leaching from the root zone of each field was calculated using an empirical model. A physically based lumped rainfall-runoff model was used for separating the hydrograph time-series into three runoff components: baseflow, interflow and overland flow. Large regional variations in net N input were found ranging from 62 kg N ha(-1) yr(-1) in the loamy eastern part of the country dominated by cereal production to 137 kg N ha(-1) yr(-1) in the western part characterised by less fertile sandy soils and dominated by animal husbandry. N leaching from the root zone showed a corresponding variation with regional averages ranging from 34.5 kg N ha(-1) yr(-1) to 90.9 kg N ha(-1) yr(-1). No similar regional pattern could however be found regarding net N export, and no relationship could be established between net IN export and root zone N leaching. This finding was ascribed to a varying and in some catchments very high (> 80%) N retention during subsurface transport to the stream. The hydrological modelling revealed that loamy catchments had a high proportion of quick flow (overland flow + interflow), whereas baseflow dominated the sandy catchments. Further, a highly significant relationship between N retention and proportion of quick flow was found emphasising the importance of understanding the hydrological pathways. This should be taken into consideration when evaluating the N loading of surface waters resulting from a given agricultural practice and the effects of possible changes in this practice.
引用
收藏
页码:63 / 68
页数:6
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