Loading…
Insights gained from two decades of intensive monitoring: hydrology and nitrate export in a tile-drained agricultural catchment
Nitrate (NO 3 − ) export from agricultural land poses an ongoing threat to both inland and coastal waters. Experimental studies investigating the hydrology-NO 3 − -export mechanisms require long-term data to identify reliable causal relationships. In this study, utilizing a 23-year continuous datase...
Saved in:
Published in: | Frontiers in water 2024-04, Vol.6 |
---|---|
Main Authors: | , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites |
Online Access: | Get full text |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Summary: | Nitrate (NO
3
−
) export from agricultural land poses an ongoing threat to both inland and coastal waters. Experimental studies investigating the hydrology-NO
3
−
-export mechanisms require long-term data to identify reliable causal relationships. In this study, utilizing a 23-year continuous dataset with a high temporal resolution (daily to twice a week), we aim to identify potential drivers for NO
3
-losses and assess the impact of nitrogen (N) soil surface budgets on NO
3
-export. A drainage plot (4.2 ha) and a ditch catchment (179 ha) were fully equipped to register hydrological parameters, including water sample collection. Mean annual NO
3
−
-N concentrations (loads) for the drainage plot and the ditch catchment were 9.4 mg l
−1
(20.6 kg ha
−1
) and 6.0 mg L
−1
(20.9 kg ha
−1
), respectively. Annual discharge was closely positively correlated with annual NO
3
-losses, highlighting the significant influence of prevailing weather and, consequently, hydrologic conditions on NO
3
-export rates. The majority of the annual NO
3
−
-load was exported during winter (56% at the drainage plot, 51% at the ditch catchment), while the rest was exported during spring (28, 29%), summer (9, 9%) and fall (7, 11%). We could not find any direct relationships between N soil surface budgets and NO
3
-losses. Putting all results together, it can be concluded that agricultural activities for many decades resulted in high soil N stocks, which determined the general high NO
3
−
-N concentration levels. Nevertheless, temporal NO
3
-export dynamics during the last two decades were clearly driven by hydro-meteorological conditions, nearly independently of land management and N soil surface budgets on the fields. |
---|---|
ISSN: | 2624-9375 2624-9375 |
DOI: | 10.3389/frwa.2024.1369552 |