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@PHDTHESIS{Piotrowski:911026,
      author       = {Piotrowski, Joseph},
      title        = {{E}ffects of salt precipitation during evaporation on
                      porosity and permeability of porous media},
      volume       = {587},
      school       = {Univ. Stuttgart},
      type         = {Dissertation},
      address      = {Jülich},
      publisher    = {Forschungszentrum Jülich GmbH Zentralbibliothek, Verlag},
      reportid     = {FZJ-2022-04352},
      isbn         = {978-3-95806-650-2},
      series       = {Schriften des Forschungszentrums Jülich Reihe Energie $\&$
                      Umwelt / Energy $\&$ Environment},
      pages        = {xxvii, 139},
      year         = {2022},
      note         = {Dissertation, Univ. Stuttgart, 2022},
      abstract     = {Salt precipitation from evaporation is a key factor for
                      soil degradation due to salinization in arid and semi-arid
                      regions. It also plays a key role in porous construction
                      material deterioration due to salt weathering.
                      Evaporation-induced water movement transports dissolved salt
                      ions to the surface of the porous medium where they
                      accumulate. When the solubility limit is reached, salt
                      starts to precipitate and forms crusts on top
                      (efflorescence) or inside (subflorescence) of the porous
                      medium depending on the type of solute in solution. For the
                      development of strategiesto treat salt-affected porous media
                      and to prevent precipitation, it is important to understand
                      the formation and the impact of the salt crusts on water
                      flow during evaporation. Salt crust formation depends on
                      ambient factors such as temperature, relative humidity, and
                      wind speedover the porous medium, and also on solution
                      properties, such as the type of dissolved ions and
                      viscosity. However, it is not known how the hydraulic
                      properties of the porous medium such as porosity,
                      permeability, and water retention affect evaporation and
                      crust formation in detail.In this context, the overall aim
                      of this thesis is to improve understanding of the impact of
                      salt crusts on evaporation with a focus on the porosity, the
                      intrinsic permeability, and the spatial and temporal
                      development of salt crusts.},
      cin          = {IBG-3},
      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)3 / PUB:(DE-HGF)11},
      urn          = {urn:nbn:de:0001-2022112304},
      url          = {https://juser.fz-juelich.de/record/911026},
}