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@ARTICLE{Eludoyin:837570,
      author       = {Eludoyin, Adebayo O. and Griffith, Bruce and Orr, Robert J.
                      and Bol, Roland and Quine, Timothy A. and Brazier, Richard
                      E.},
      title        = {{A}n evaluation of the hysteresis in chemical
                      concentration–discharge ( {C} – {Q} ) relationships from
                      drained, intensively managed grasslands in southwest
                      {E}ngland},
      journal      = {Hydrological sciences journal},
      volume       = {62},
      number       = {8},
      issn         = {2150-3435},
      address      = {Wallingford},
      publisher    = {IAHS Press},
      reportid     = {FZJ-2017-06458},
      pages        = {1243 - 1254},
      year         = {2017},
      abstract     = {This study examined the hysteresis exhibited in
                      concentration–discharge (C–Q) relationships in the
                      runoff from four hydrologically separated fields
                      (catchments) at an intensively managed grassland. The
                      objectives were to examine C–Q relationships constructed
                      from high-resolution time series of flow, temperature, pH,
                      conductivity, nitrate and turbidity, and their implications
                      for hydrological processes. High-resolution datasets from
                      the quality assured records of the Rothamsted Research North
                      Wyke Farm Platform in the UK were examined using a graphical
                      method and cross-correlation statistics. The study found
                      that storm events based C–Q hysteresis reflects the
                      cross-correlation that is generally hidden in time series
                      analysis of large datasets, and that although Q and water
                      quality variables can be effectively influenced by catchment
                      size, the C–Q relationship is less significantly
                      influenced. The dominant C–Q relationships of the water
                      variables in the study area reflect that saturated overland
                      flow was prevalent during the study period in the
                      catchments, while the CCF results indicate coupled transfer
                      of sediments and solute in the area at lag ≥ 0.},
      cin          = {IBG-3},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IBG-3-20101118},
      pnm          = {255 - Terrestrial Systems: From Observation to Prediction
                      (POF3-255)},
      pid          = {G:(DE-HGF)POF3-255},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000403800000005},
      doi          = {10.1080/02626667.2017.1313979},
      url          = {https://juser.fz-juelich.de/record/837570},
}