Open AccessHydrology is the key factor for nitrogen export from tile-drained catchments under consistent land-management
Author(s) -
Andreas Bauwe,
Petra Kahle,
Bärbel Tiemeyer,
Bernd Lennartz
Publication year - 2020
Publication title -
environmental research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.37
H-Index - 124
ISSN - 1748-9326
DOI - 10.1088/1748-9326/aba580
Subject(s) - tile drainage , environmental science , hydrology (agriculture) , drainage basin , surface runoff , land use , drainage , land management , ditch , climate change , precipitation , discharge , agricultural land , soil water , soil science , geography , ecology , geotechnical engineering , engineering , cartography , biology , meteorology
In this study, 14 years of climate, stream flow, land management, nitrate-nitrogen (NO 3 – N) load and concentration data were analyzed to identify potential drivers for NO 3 – N losses at two tile-drained catchments under cropland use in northeastern Germany. Mean (±standard deviation) annual NO 3 – N concentrations were 9.7 ± 2.9 (drainage plot) and 6.8 ± 2.4 mg l −1 (ditch catchment), while mean annual NO 3 – N loads amounted to 22 ± 16 and 20 ± 16 kg ha −1 , respectively. Significant positive relationships between annual discharge and annual NO 3 – N losses underlined the importance of hydrologic conditions on NO 3 – N export mechanisms. No direct relationships were found between N soil surface surpluses and NO 3 – N losses. Any possible impact of N soil surface surpluses on NO 3 – N export rates was overridden by the hydro-meteorological conditions in the catchment. Positive correlations between the climatic water balance and NO 3 – N losses suggest that agricultural catchments with similar characteristics as ours may face—without countermeasures—increased N losses in the future as regional climate projections predict wetter winters in the coming decades. Our analysis has further shown that effects of land management strategies aiming at reducing N losses into surface waters might only become visible with a delay of years or even decades.