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@ARTICLE{Gottselig:840068,
      author       = {Gottselig, N. and Amelung, Wulf and Kirchner, J. W. and
                      Bol, R. and Eugster, W. and Granger, S. J. and
                      Hernández-Crespo, C. and Herrmann, F. and Keizer, J. J. and
                      Korkiakoski, M. and Laudon, H. and Lehner, I. and Löfgren,
                      S. and Lohila, A. and Macleod, C. J. A. and Mölder, M. and
                      Müller, C. and Nasta, P. and Nischwitz, V. and
                      Paul-Limoges, E. and Pierret, M. C. and Pilegaard, K. and
                      Romano, N. and Sebastià, M. T. and Stähli, M. and Voltz,
                      M. and Vereecken, H. and Siemens, J. and Klumpp, E.},
      title        = {{E}lemental {C}omposition of {N}atural {N}anoparticles and
                      {F}ine {C}olloids in {E}uropean {F}orest {S}tream {W}aters
                      and {T}heir {R}ole as {P}hosphorus {C}arriers},
      journal      = {Global biogeochemical cycles},
      volume       = {31},
      number       = {10},
      issn         = {0886-6236},
      address      = {Hoboken, NJ},
      publisher    = {Wiley},
      reportid     = {FZJ-2017-07632},
      pages        = {1592 - 1607},
      year         = {2017},
      abstract     = {Biogeochemical cycling of elements largely occurs in
                      dissolved state, but many elements may also be bound to
                      natural nanoparticles (NNP, 1–100 nm) and fine colloids
                      (100–450 nm). We examined the hypothesis that the size and
                      composition of stream water NNP and colloids vary
                      systematically across Europe. To test this hypothesis, 96
                      stream water samples were simultaneously collected in 26
                      forested headwater catchments along two transects across
                      Europe. Three size fractions (~1–20 nm, >20–60 nm, and
                      >60 nm) of NNP and fine colloids were identified with Field
                      Flow Fractionation coupled to inductively coupled plasma
                      mass spectrometry and an organic carbon detector. The
                      results showed that NNP and fine colloids constituted
                      between 2 ± $5\%$ (Si) and 53 ± $21\%$ (Fe; mean ± SD) of
                      total element concentrations, indicating a substantial
                      contribution of particles to element transport in these
                      European streams, especially for P and Fe. The particulate
                      contents of Fe, Al, and organic C were correlated to their
                      total element concentrations, but those of particulate Si,
                      Mn, P, and Ca were not. The fine colloidal fractions >60 nm
                      were dominated by clay minerals across all sites. The
                      resulting element patterns of NNP <60 nm changed from North
                      to South Europe from Fe- to Ca-dominated particles, along
                      with associated changes in acidity, forest type, and
                      dominant lithology.},
      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:000416625200010},
      doi          = {10.1002/2017GB005657},
      url          = {https://juser.fz-juelich.de/record/840068},
}