% 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{Farid:22519,
      author       = {Farid, A. and Jadoon, K. and Akhter, G. and Iqbal, M.A.},
      title        = {{H}ydrostratigraphy and hydrogeology of the western part of
                      {M}aira area, {K}hyber {P}akhtunkhwa, {P}akistan: a case
                      study by using electrical resistivity},
      journal      = {Environmental monitoring and assessment},
      volume       = {185},
      number       = {3},
      issn         = {0167-6369},
      address      = {Dordrecht [u.a.]},
      publisher    = {Springer Science + Business Media B.V},
      reportid     = {PreJuSER-22519},
      pages        = {2407-2422},
      year         = {2012},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {Hydrostratigraphy and hydrogeology of the Maira vicinity is
                      important for the characterization of aquifer system and
                      developing numerical groundwater flow models to predict the
                      future availability of the water resource. Conventionally,
                      the aquifer parameters are obtained by the analysis of
                      pumping tests data which provide limited spatial information
                      and turn out to be costly and time consuming. Vertical
                      electrical soundings and pump testing of boreholes were
                      conducted to delineate the aquifer system at the western
                      part of the Maira area, Khyber Pakhtun Khwa, Pakistan.
                      Aquifer lithology in the eastern part of the study area is
                      dominated by coarse sand and gravel whereas the western part
                      is characterized by fine sand. An attempt has been made to
                      estimate the hydraulic conductivity of the aquifer system by
                      establishing a relationship between the pumping test results
                      and vertical electrical soundings by using regression
                      technique. The relationship is applied to the area along the
                      resistivity profiles where boreholes are not drilled. Our
                      findings show a good match between pumped hydraulic
                      conductivity and estimated hydraulic conductivity. In case
                      of sparse borehole data, regression technique is useful in
                      estimating hydraulic properties for aquifers with varying
                      lithology.},
      cin          = {IBG-3},
      ddc          = {333.7},
      cid          = {I:(DE-Juel1)IBG-3-20101118},
      pnm          = {Terrestrische Umwelt},
      pid          = {G:(DE-Juel1)FUEK407},
      typ          = {PUB:(DE-HGF)16},
      pubmed       = {pmid:22736209},
      UT           = {WOS:000314033300031},
      doi          = {10.1007/s10661-012-2720-z},
      url          = {https://juser.fz-juelich.de/record/22519},
}