% 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{Grlich:189596,
      author       = {Görlich, Isa and Weigand, Susanne and Beuel, Sonja and
                      Bouchaou, Lhoussaine and Reichert, Barbara},
      title        = {{S}tatusanalyse von {M}eerwasserintrusionen und
                      {G}rundwasserhaushaltsmodellierung des oberen
                      {K}üstenaquifers in {A}gadir, {M}arokko{S}tatusanalysis and
                      groundwater storage model of the upper coastal aquifer in
                      {A}gadir, {M}orocco},
      journal      = {Grundwasser},
      volume       = {20},
      number       = {1},
      issn         = {1432-1165},
      address      = {Berlin},
      publisher    = {Springer},
      reportid     = {FZJ-2015-02734},
      pages        = {25 - 37},
      year         = {2015},
      abstract     = {In Agadir, a coastal town situated in the semi-arid
                      south-western part of Morocco, irrigated agriculture and
                      tourism are the primary economic activities. Both sectors
                      require high volumes of fresh water. Over the last few
                      decades, this constantly increasing demand has resulted in a
                      significant drawdown of the water table, accompanied by
                      seawater intrusion leading to a decrease in water quality. A
                      groundwater storage model has verified the extensive
                      drawdown. Positive terms in the flow balance equation are
                      represented by groundwater recharge from bankfiltration, and
                      by irrigation return flow. The negative terms are dominated
                      by groundwater removal for irrigation. A sensitivity
                      analysis reveals parameters which require further
                      investigation. A spatially and temporally variable seawater
                      intrusion front was identified using specific ion ratios,
                      chloride concentrations and groundwater salinity. The
                      intrusion front extends roughly from the northwest to the
                      southeast, following the coast. Compared to 2005, the
                      intrusion front had advanced further inland by 2010. In 2011
                      and 2012, the effects of seawater intrusion have tended to
                      diminish.},
      cin          = {IBG-3},
      ddc          = {690},
      cid          = {I:(DE-Juel1)IBG-3-20101118},
      pnm          = {255 - Terrestrial Systems: From Observation to Prediction
                      (POF3-255) / 255 - Terrestrial Systems: From Observation to
                      Prediction (POF3-255)},
      pid          = {G:(DE-HGF)POF3-255 / G:(DE-HGF)POF3-255},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000351399600004},
      doi          = {10.1007/s00767-014-0280-6},
      url          = {https://juser.fz-juelich.de/record/189596},
}