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@ARTICLE{Bauke:916702,
      author       = {Bauke, Sara L. and Amelung, Wulf and Bol, Roland and
                      Brandt, Luise and Brüggemann, Nicolas and Kandeler, Ellen
                      and Meyer, Nele and Or, Dani and Schnepf, Andrea and
                      Schloter, Michael and Schulz, Stefanie and Siebers, Nina and
                      von Sperber, Christian and Vereecken, Harry},
      title        = {{S}oil water status shapes nutrient cycling in
                      agroecosystems from micrometer to landscape scales},
      journal      = {Journal of plant nutrition and soil science},
      volume       = {185},
      number       = {6},
      issn         = {0932-6979},
      address      = {Weinheim},
      publisher    = {Wiley-VCH},
      reportid     = {FZJ-2023-00042},
      pages        = {773 - 792},
      year         = {2022},
      abstract     = {Soil water status, which refers to the wetness or dryness
                      of soils, is crucial for the productivity of agroecosystems,
                      as it determines nutrient cycling and uptake physically via
                      transport, biologically via the moisture-dependent activity
                      of soil flora, fauna, and plants, and chemically via
                      specific hydrolyses and redox reactions. Here, we focus on
                      the dynamics of nitrogen (N), phosphorus (P), and sulfur (S)
                      and review how soil water is coupled to the cycling of these
                      elements and related stoichiometric controls across
                      different scales within agroecosystems. These scales span
                      processes at the molecular level, where nutrients and water
                      are consumed, to processes in the soil pore system, within a
                      soil profile and across the landscape. We highlight that
                      with increasing mobility of the nutrients in water,
                      water-based nutrient flux may alleviate or even exacerbate
                      imbalances in nutrient supply within soils, for example, by
                      transport of mobile nutrients towards previously depleted
                      microsites (alleviating imbalances), or by selective loss of
                      mobile nutrients from microsites (increasing imbalances).
                      These imbalances can be modulated by biological activity,
                      especially by fungal hyphae and roots, which contribute to
                      nutrient redistribution within soils, and which are
                      themselves dependent on specific, optimal water
                      availability. At larger scales, such small-scale effects
                      converge with nutrient inputs from atmospheric (wet
                      deposition) or nonlocal sources and with nutrient losses
                      from the soil system towards aquifers. Hence, water acts as
                      a major control in nutrient cycling across scales in
                      agroecosystems and may either exacerbate or remove spatial
                      disparities in the availability of the individual nutrients
                      (N, P, S) required for biological activity.},
      cin          = {IBG-3},
      ddc          = {640},
      cid          = {I:(DE-Juel1)IBG-3-20101118},
      pnm          = {2173 - Agro-biogeosystems: controls, feedbacks and impact
                      (POF4-217)},
      pid          = {G:(DE-HGF)POF4-2173},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000888991800001},
      doi          = {10.1002/jpln.202200357},
      url          = {https://juser.fz-juelich.de/record/916702},
}