2015
DOI: 10.1016/j.jhydrol.2015.09.060
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Uncertainty in nutrient loads from tile-drained landscapes: Effect of sampling frequency, calculation algorithm, and compositing strategy

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Cited by 94 publications
(60 citation statements)
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“…For both P forms monitored in drainage waters, no such differences were found. During the REs, a dilution of N-NO 3 in drainage waters usually prevailed, whilst for both P-PO 4 and P tot , the concentrations usually rose with elevated discharge, which is in accordance with many monitoring campaigns in tile-drained catchments [5,12,18,25,31]. The only exceptions were sites PD1 and PD2, with Cfw N-NO 3 higher in ESs than in RSs.…”
Section: Dynamics Of N and P Concentrationssupporting
confidence: 86%
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“…For both P forms monitored in drainage waters, no such differences were found. During the REs, a dilution of N-NO 3 in drainage waters usually prevailed, whilst for both P-PO 4 and P tot , the concentrations usually rose with elevated discharge, which is in accordance with many monitoring campaigns in tile-drained catchments [5,12,18,25,31]. The only exceptions were sites PD1 and PD2, with Cfw N-NO 3 higher in ESs than in RSs.…”
Section: Dynamics Of N and P Concentrationssupporting
confidence: 86%
“…M2 appeared to be quite a reasonable algorithm for the assessment of N-NO 3 loads, when only grab sampling (without continuous monitoring of discharge) was employed. However, it still gave large underestimations, especially for both phosphorus compounds, as the grab sampling rarely captured different REs with different P concentration values, as documented by [31][32][33][34].…”
Section: Comparison Of Load Assessment Methodsmentioning
confidence: 99%
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“…The resulting 10‐min concentration file was merged with the 10‐min discharge file to create a 10‐min loading file. This method has been shown to reduce the uncertainty associated with collecting both surface and subsurface samples for water quality loading in tile‐drained landscapes (Williams et al, 2015b). Loads were calculated as the product of the 10‐min concentrations and 10‐min discharges summed over the entire water year and the spring loading period.…”
Section: Methodsmentioning
confidence: 99%
“…Phosphorus loads were calculated by multiplying continuous discharge measurements with continuous concentration data that were constructed through linear interpolation between individual water samples. According to the findings of Harmel et al (2006) and Williams et al (2015b), P loads reported herein were likely within 5 to 20% of actual P loads, based on sampling strategy and frequency. Calculated P loads were aggregated to annual values, with data from the 40 fields totaling 112 site years.…”
Section: Discussionmentioning
confidence: 69%