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

被引:19
作者
Siebers, Nina [1 ]
Kruse, Jens [1 ,2 ]
Jia, Yunsheng [1 ]
Lennartz, Bernd [3 ]
Koch, Stefan [3 ]
机构
[1] Forschungszentrum Julich, Inst Bio & Geosci Agrosphere IBG 3, D-52425 Julich, Germany
[2] Univ Bonn, Inst Crop Sci & Resource Conservat INRES, Soil Sci & Soil Ecol, Nussallee 13, D-53115 Bonn, Germany
[3] Univ Rostock, Fac Agr & Environm Sci, Justus Von Liebig Weg 6, D-18051 Rostock, Germany
关键词
Phosphorus leaching; Colloid transport; Flow component separation; Lowland catchment; Asymmetric flow field-flow fractionation; NATURAL COLLOIDS; LOWLAND CATCHMENT; STREAM WATERS; TRANSPORT; SOIL; RIVER; FRACTIONATION; NANOPARTICLES; MOBILIZATION; SPECIATION;
D O I
10.1016/j.scitotenv.2023.161439
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
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.
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页数:11
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