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

Citation
He. Andersen et al., Analysis of the hydrology and flow of nitrogen in 17 Danish catchments, WATER SCI T, 44(7), 2001, pp. 63-68
Citations number
12
Categorie Soggetti
Environment/Ecology
Journal title
WATER SCIENCE AND TECHNOLOGY
ISSN journal
02731223 → ACNP
Volume
44
Issue
7
Year of publication
2001
Pages
63 - 68
Database
ISI
SICI code
0273-1223(2001)44:7<63:AOTHAF>2.0.ZU;2-X
Abstract
In the search for tools for evaluating the effects of national action plans combating diffuse nutrient pollution causing eutrophication of surface wat ers, 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 o f 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 us ed for separating the hydrograph time-series into three runoff components: baseflow, interflow and overland flow. Large regional variations in net N i nput were found ranging from 62 kg N ha(-1) yr(-1) in the loamy eastern par t of the country dominated by cereal production to 137 kg N ha(-1) yr(-1) i n the western part characterised by less fertile sandy soils and dominated by animal husbandry. N leaching from the root zone showed a corresponding v ariation 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 re garding 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 tran sport to the stream. The hydrological modelling revealed that loamy catchme nts had a high proportion of quick flow (overland flow + interflow), wherea s baseflow dominated the sandy catchments. Further, a highly significant re lationship between N retention and proportion of quick flow was found empha sising the importance of understanding the hydrological pathways. This shou ld be taken into consideration when evaluating the N loading of surface wat ers resulting from a given agricultural practice and the effects of possibl e changes in this practice.