2014
DOI: 10.1016/j.jhydrol.2014.10.058
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Investigating summer flow paths in a Dutch agricultural field using high frequency direct measurements

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Cited by 23 publications
(19 citation statements)
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“… (a) Precipitation and evapotranspiration (mm/d), (b–g) jointly conditioned model result (green, solid line denotes median, shaded area 5–95% prediction interval), heads‐only‐conditioned model result (black, solid line denotes median, shaded area 5–95% prediction interval), and observations (red) for: (b) head in piezometer 5a (for location see Figure 1), (c) head beneath ditch, (d) tile drain exfiltration, (e) ditch in/exfiltration, (f) EC25 of tile drain exfiltration, and (g) EC25 of ditch exfiltration. Shaded red areas around measured values in Figures 9e and 9g are the 25–75% percentiles of Monte Carlo uncertainty estimates [ Delsman et al ., ]. Note that the ditch exfiltration peak of 10 September 2013 was likely caused by infiltration‐excess overland flow [ Delsman et al ., ] and was therefore excluded from the conditioning process.…”
Section: Resultsmentioning
confidence: 99%
“… (a) Precipitation and evapotranspiration (mm/d), (b–g) jointly conditioned model result (green, solid line denotes median, shaded area 5–95% prediction interval), heads‐only‐conditioned model result (black, solid line denotes median, shaded area 5–95% prediction interval), and observations (red) for: (b) head in piezometer 5a (for location see Figure 1), (c) head beneath ditch, (d) tile drain exfiltration, (e) ditch in/exfiltration, (f) EC25 of tile drain exfiltration, and (g) EC25 of ditch exfiltration. Shaded red areas around measured values in Figures 9e and 9g are the 25–75% percentiles of Monte Carlo uncertainty estimates [ Delsman et al ., ]. Note that the ditch exfiltration peak of 10 September 2013 was likely caused by infiltration‐excess overland flow [ Delsman et al ., ] and was therefore excluded from the conditioning process.…”
Section: Resultsmentioning
confidence: 99%
“…Moreover, they concluded that the fresh/saline ratio of the drainage water will change from zero to the infiltration/upward seepage ratio. However, as shown by others (De Vos et al, 2002;Delsman et al, 2014;Eeman et al, 2012), seasonal variations of infiltration and plant root withdrawal of fresh water will cause temporal fluctuations of the thickness of the lenses and the fresh-saline ratio of the drainage water.…”
Section: Current Progressmentioning
confidence: 97%
“…study. On the other hand, the Schermer polder (surface level 4.14-3.86 m BSL, water depth average depth, water depth 5 m BSL, salinity concentration variation in the ditches 700-7700 g/m 3 (Delsman et al, 2014b)) is representative of polders where the main salinity input derives from shallow saline groundwater, viz. exfiltrating towards ditches and tile drains (Fig.…”
Section: Introductionmentioning
confidence: 99%