% IMPORTANT: The following is UTF-8 encoded.  This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.

@ARTICLE{Missong:283057,
      author       = {Missong, Anna and Bol, Roland and Willbold, Sabine and
                      Klumpp, Erwin and Siemens, Jan},
      title        = {{P}hosphorus forms in forest soil colloids as revealed by
                      liquid-state 31{P}-{NMR}},
      journal      = {Journal of plant nutrition and soil science},
      volume       = {179},
      number       = {2},
      issn         = {0044-3263},
      address      = {Weinheim},
      publisher    = {Wiley-VCH},
      reportid     = {FZJ-2016-01739},
      pages        = {159–167},
      year         = {2016},
      abstract     = {Nanoparticles and colloids affect the storage and hence the
                      availability of P in forest ecosystems. We investigated the
                      fine colloids present in forest soils and their association
                      with inorganic and organic P. To differentiate between the
                      different P forms, we performed liquid-state 31P-nucelar
                      magnetic resonance (31P-NMR) measurements on forest bulk
                      soil extracts, on colloid extracts and on the electrolyte
                      phase of their soil suspensions. The 31P-NMR spectra
                      indicated that soil nanoparticles and colloids were more
                      enriched with organic than with inorganic P forms compared
                      to the electrolyte phase. The P concentration was enriched
                      in the colloidal fraction in comparison to the bulk soil and
                      the phosphate diesters were more dominant in the colloidal
                      fraction when compared to the bulk soil. The colloidal
                      P-diester to P-monoester ratios were 2 to 3 times higher in
                      the colloidal fraction than in the bulk soil. In contrast,
                      relatively large percentages of inorganic P were found in
                      the electrolyte phase},
      cin          = {IBG-3 / ZEA-3},
      ddc          = {570},
      cid          = {I:(DE-Juel1)IBG-3-20101118 / I:(DE-Juel1)ZEA-3-20090406},
      pnm          = {255 - Terrestrial Systems: From Observation to Prediction
                      (POF3-255)},
      pid          = {G:(DE-HGF)POF3-255},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000374035700004},
      doi          = {10.1002/jpln.201500119},
      url          = {https://juser.fz-juelich.de/record/283057},
}