4.6 Article

Sediment and particulate phosphorus characteristics in grassed waterways from row crop corn and alfalfa fields collected by manual University of Exeter samplers and automatic sampling

Journal

HYDROLOGICAL PROCESSES
Volume 25, Issue 15, Pages 2329-2338

Publisher

WILEY
DOI: 10.1002/hyp.7987

Keywords

runoff monitoring; particulate phosphorus; particle size; fine-grained sediment

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Phosphorus (P) export from agricultural lands above known threshold levels can result in adverse impacts to receiving water quality. Phosphorus loss occurs in dissolved and sediment-bound, or particulate phosphorous (PP), forms, with the latter often dominating losses from row-cropped systems. To target practices, land managers need good computer models and model developers need good monitoring data. Sediment monitoring data (e. g. radiometric finger printing and sediment P sorption capacity) can help identify sediment source areas and improve models, but require more sediment mass than is typically obtained by automatic sampling. This study compares a simple suspended sediment sampler developed at the University of Exeter (UE) with automatic sampling in intermittent channels draining corn and alfalfa fields. The corn field had a greater runoff coefficient (27%) than alfalfa (11%). No differences were found in enrichment ratios (sediment constituent/soil constituent) in PP (PPER) or percent loss on ignition (LOIER) between paired UE samplers on corn. The median LOIER for the UE samplers (1.9%) did not differ significantly (p > 0.13) from the automatic sampler (2.0%). The PPER from the UE samplers was on average 20% lower than the automatic samplers. A correlation (r(2) = 0.75) was found between sediment PP and % LOI from automatic samplers and UE samplers for particles < 50 mu m, while for > 50 mu m PP concentration did not change with changes in % LOI. Sediment ammonium-oxalate extractable metals were similarly related to LOI, with the strongest correlation for iron (r(2) = 0.71) and magnesium (r(2) = 0.70). Copyright (C) 2011 John Wiley & Sons, Ltd.

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