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@ARTICLE{Scotti:141815,
      author       = {Scotti, Ricardo and Conte, Pellegrino and Berns, Anne E.
                      and Alonzo, Giuseppe and Rao, Maria},
      title        = {{E}ffect of {O}rganic {A}mendments on the {E}volution of
                      {S}oil {O}rganic {M}atter in {S}oils {S}tressed by
                      {I}ntensive {A}gricultural {P}ractices},
      journal      = {Current organic chemistry},
      volume       = {17},
      number       = {24},
      issn         = {1385-2728},
      address      = {Hilversum [u.a.]},
      publisher    = {Bentham Science Publ.},
      reportid     = {FZJ-2014-00155},
      pages        = {2998-3005},
      year         = {2013},
      abstract     = {Losses of soil organic carbon often occur because of
                      intensive agricultural practices that lead to removal of
                      organic carbon following harvest production and to
                      insufficient inputs. Organic amendments can be very
                      appropriate for enhancing organic carbon content in very
                      stressed agricultural soils. By enhancing soil organic
                      matter, they generally play an important role in
                      environmental matrices due to their capacity in retaining
                      water and in enhancing nutrient availability to plants.
                      Therefore, understanding the mechanisms by which organic
                      amendments interact with other chemicals in the environment
                      is of paramount importance. The attention was focused on
                      farms near Sele river (Campania region, Italy), an area
                      characterized by intensive agriculture. Two farms, with
                      contrasting geopedologic properties (clay vs. sandy), were
                      selected in order to study the effect of different doses of
                      organic amendments containing compost from municipal solid
                      wastes and wood-wastes (scraps of poplars pruning) at
                      different ratios. The organic fractions were extracted from
                      soil, after one and twelve months from amendment, and were
                      analysed in order to establish their elemental composition
                      and properties by FTIR, CPMAS 13C NMR spectroscopy and
                      FFC-NMR relaxometry. Results showed an important role of
                      soil geopedologic characteristics and experimental time in
                      the evolution of humic acids. In less aerobic conditions as
                      occurs in clay soils, organic matter was more stable, rich
                      in carbonyl groups belonging to aldehydes and ketones,
                      whereas under more aerobic conditions, occurring in sandy
                      soils, organic matter had undergone a faster degradation,
                      due to oxidative conditions and more intensive microbial
                      activity.},
      cin          = {IBG-3},
      ddc          = {540},
      cid          = {I:(DE-Juel1)IBG-3-20101118},
      pnm          = {245 - Chemicals in the Environment (POF2-245)},
      pid          = {G:(DE-HGF)POF2-245},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000328902400006},
      url          = {https://juser.fz-juelich.de/record/141815},
}