Journalartikel

Loss of subsurface particulate and truly dissolved phosphorus during various flow conditions along a tile drain-ditch-brook continuum


AutorenlisteSiebers, Nina; Kruse, Jens; Jia, Yunsheng; Lennartz, Bernd; Koch, Stefan

Jahr der Veröffentlichung2023

ZeitschriftScience of the Total Environment

Bandnummer866

ISSN0048-9697

eISSN1879-1026

Open Access StatusHybrid

DOI Linkhttps://doi.org/10.1016/j.scitotenv.2023.161439

VerlagElsevier


Abstract
Subsurface losses of colloidal and truly dissolved phosphorus (P) from arable land can cause ecological damage to sur-face water. To gain deeper knowledge about subsurface particulate P transport from inland sources to brooks, we stud-ied an artificially drained lowland catchment (1550 ha) in north-eastern Germany. We took daily samples during the winter discharge period 2019/2020 at different locations, i.e., a drain outlet, ditch, and brook, and analyzed them for total P (TPunfiltered), particulate P >750 nm (TP>750 nm), colloidal P (TPcolloids), and truly dissolved P (truly DP) during baseflow conditions and high flow events. The majority of TPunfilteredin the tile drain, ditch, and brook was formed by TP>750 nm (54 to 59 %), followed by truly DP (34 to 38 %) and a small contribution of TPcolloids (5 to 6 %). During flow events, 63 to 66 % of TPunfiltered was present as particulate P (TP>750 nm + TPcolloids), whereas during baseflow the fig-ure was 97 to 99 %; thus, truly DP was almost negligible (1 to 3 % of TPunfiltered)during baseflow. We also found that colloids transported in the water samples have their origin in the water-extractable nanocolloids (0.66 to 20 nm) within the C horizon, which are mainly composed of clay minerals. Along the flow path there is an agglomeration of P-bearing nanocolloids from the soil, with an increasing importance of iron(III) (hydr)oxides over clay particles. Event flow facilitated the transport of greater amounts of larger particles (>750 nm) through the soil matrix. However, the discharge did not exhaust colloid mobilization and colloidal P was exported through the tile-drainage system during the complete runoff period, even under baseflow conditions. Therefore, it is essential that the impact of rainfall intensity and pattern on particulate P discharge be considered more closely so that drainage management can be adjusted to achieve a reduced P export from agricultural land.



Zitierstile

Harvard-ZitierstilSiebers, N., Kruse, J., Jia, Y., Lennartz, B. and Koch, S. (2023) Loss of subsurface particulate and truly dissolved phosphorus during various flow conditions along a tile drain-ditch-brook continuum, Science of the Total Environment, 866, Article 161439. https://doi.org/10.1016/j.scitotenv.2023.161439

APA-ZitierstilSiebers, N., Kruse, J., Jia, Y., Lennartz, B., & Koch, S. (2023). Loss of subsurface particulate and truly dissolved phosphorus during various flow conditions along a tile drain-ditch-brook continuum. Science of the Total Environment. 866, Article 161439. https://doi.org/10.1016/j.scitotenv.2023.161439



Schlagwörter


Colloid transportFlow component separationLOWLAND CATCHMENTmobilizationNATURAL COLLOIDSPhosphorus leachingSTREAM WATERS


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