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@ARTICLE{Harris:857180,
      author       = {Harris, P. and Bol, R. and Evans, J. and Hawkins, J. M. B.
                      and Dixon, E. R. and Wolf, K. and Dungait, J. A. J. and
                      Griffith, B. and Herbst, Michael and Dhanoa, M. S. and
                      Beaumont, D. A. and Dunn, R. M. and Wiesenberg, G. L. B.},
      title        = {{E}ffect of long-term drainage on plant community, soil
                      carbon and nitrogen contents and stable isotopic ( δ 13
                      {C}, δ 15 {N}) composition of a permanent grassland},
      journal      = {European journal of soil science},
      volume       = {69},
      number       = {1},
      issn         = {1351-0754},
      address      = {Oxford [u.a.]},
      publisher    = {Wiley-Blackwell},
      reportid     = {FZJ-2018-06417},
      pages        = {48 - 68},
      year         = {2018},
      abstract     = {This study compares data statistically that were collected
                      from both long‐term drained and undrained plots to test
                      hypotheses concerning the effect of drainage on plant
                      community, soil total nitrogen (TN), soil total carbon (TC)
                      and stable isotopic (δ15N, δ13C) contents in a permanent
                      grassland. In addition, the effects of soil depth,
                      topography (elevation, slope, aspect and compound
                      topographic index (CTI)) and spatial autocorrelation were
                      taken into account. Data were collected in 2010 at Rowden
                      Moor, North Wyke, Devon, UK, where, for the plots of this
                      study, subsurface drainage was introduced in 1987. The
                      results of a set of six linear mixed models showed that: (i)
                      plant community did not depend on drainage, but on elevation
                      and spatial effects, (ii) both TN and TC not only depended
                      on drainage, but also topography and sample depth, (iii) the
                      TC to TN ratio did not depend on drainage, but on elevation,
                      CTI and sample depth only, (iv) δ15N values did not depend
                      on drainage, but on topography and sample depth and (v)
                      δ13C values depended on drainage together with topography
                      and sample depth. Thus, drainage represented a significant
                      effect for only TN, TC and δ13C. Furthermore, changes in
                      soil physicochemical conditions, following the introduction
                      of drainage in the clay soil 24 years previously, induced a
                      shift in the plant community from a Lolium perenne L.
                      dominated grassland with numerous patches of Juncus species,
                      towards one with Lolium perenne and Trifolium repens L.},
      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:000427881900009},
      doi          = {10.1111/ejss.12504},
      url          = {https://juser.fz-juelich.de/record/857180},
}