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

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.

Automated summary

Subsurface losses of colloidal and truly dissolved phosphorus (P) from arable land can cause ecological damage to surface water. We studied a drained lowland catchment in Germany to investigate the transport of subsurface particulate P from inland sources to brooks. Our results showed that particulate P and truly dissolved P were the main forms of P in the samples, with colloidal P contributing a smaller proportion. During flow events, particulate P was the dominant form of P, while during baseflow conditions, truly dissolved P was almost negligible. We also found that the transported colloids originated from water-extractable nanocolloids in the C horizon, which were mainly composed of clay minerals.