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<div class=3DSection1>

<table class=3DMsoNormalTable border=3D0 cellpadding=3D0 width=3D"95%"
 style=3D'width:95.0%;mso-cellspacing:1.5pt;mso-padding-alt:3.75pt 3.75pt 3=
.75pt 3.75pt'>
 <tr style=3D'mso-yfti-irow:0;mso-yfti-firstrow:yes'>
  <td colspan=3D2 style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><b>Paper No. 32-0</b><o:p></o:p></p>
  </td>
 </tr>
<!--abstract-->
 <tr style=3D'mso-yfti-irow:1'>
  <td colspan=3D3 style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'><!--Interes=
tPaper32644-->
  <p class=3DMsoNormal><b><i><span style=3D'font-size:18.0pt;font-family:Ar=
ial'>&#8220;IN-HOUSE&#8221;
  AQUIFER MONITORING: A NEW LABORATORY INSTALLATION FOR MULTIDISCIPLINARY
  LEARNING</span></i></b><o:p></o:p></p>
  </td>
 </tr>
<!--/abstract-->
 <tr style=3D'mso-yfti-irow:2'>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'><!--abstract-->
  <p class=3DMsoNormal><b><a href=3D"mailto:pdoss@usi.edu">DOSS, Paul K.</a=
></b>,
  Geology, Univ. of Southern Indiana, 8600 University Blvd, Evansville, IN
  47712, pdoss@usi.edu. <o:p></o:p></p>
  <p>A nest of deep and shallow piezometers (<span class=3DGramE>ground-wat=
er</span>
  monitoring wells) was installed at the site of a new science-education
  building for the <st1:place w:st=3D"on"><st1:PlaceType w:st=3D"on">Univer=
sity</st1:PlaceType>
   of <st1:PlaceName w:st=3D"on">Southern Indiana</st1:PlaceName></st1:plac=
e> in
  November 2001. After completion of the building construction, these
  piezometers <span class=3DGramE>will be housed</span> in a ground-water
  monitoring laboratory on the ground floor within the building. This
  piezometer nest <span class=3DGramE>was designed and installed primarily =
for
  undergraduate teaching and research purposes within the Department of Geo=
logy</span>.
  This installation permits direct student access to a bedrock ground-water
  system used for local domestic supplies. The deep well <span class=3DGram=
E>was
  drilled</span> to a depth of 33.5 m (110 ft) and the shallow well was
  installed at a depth of 18.3 m (60 ft). Intact bedrock cores <span
  class=3DGramE>were recovered</span> from the piezometer screened interval=
s. The
  nest displays vertical hydraulic gradients and the geochemical signatures=
 of
  deep and shallow ground water are distinct. <!--/abstract--><!--abstract-=
->Results
  from this technology are directly applicable to curricular elements in hy=
drogeology,
  environmental geology, sedimentation and <span class=3DSpellE>stratigraph=
y</span>,
  and geochemistry. Moreover, natural water samples are available to studen=
ts
  and faculty in the chemistry department. This novel laboratory provides a
  controlled setting for understanding well installations and the use and
  application of water-quality monitoring instruments, environmental sampli=
ng
  equipment, aquifer testing, and digital recording devices. Drilling and w=
ell
  installation is a minor cost compared to other construction expenses and =
<span
  class=3DGramE>can be easily incorporated</span> into building plans durin=
g a
  design phase. Finish design includes stainless steel casings mounted thro=
ugh
  a laboratory bench and the infrastructure for monitoring, pumping, and
  sampling. <!--/abstract--><o:p></o:p></p>
  </td>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'><o:p>&nbsp;</o:p></=
span></p>
  </td>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'><o:p>&nbsp;</o:p></=
span></p>
  </td>
 </tr>
 <tr style=3D'mso-yfti-irow:3'>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><a
  href=3D"http://gsa.confex.com/gsa/2002NC/finalprogram/index.html">North-C=
entral
  Section (36th) and Southeastern Section (51st), GSA Joint Annual Meeting
  (April 3&#8211;5, 2002)</a> <o:p></o:p></p>
  </td>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'><o:p>&nbsp;</o:p></=
span></p>
  </td>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'><o:p>&nbsp;</o:p></=
span></p>
  </td>
 </tr>
 <tr style=3D'mso-yfti-irow:4'>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'><!--info-->
  <p class=3DMsoNormal>Session No. 32<br>
  <a href=3D"http://gsa.confex.com/gsa/2002NC/finalprogram/session_1892.htm=
">Technology
  for Inquiry-Based Earth Science Education</a><br>
  Hyatt Regency Hotel: Regency Ballroom Center<br>
  1:00 PM-3:00 PM, Thursday, April 4, 2002<o:p></o:p></p>
<!--/info--></td>
<!--hideinscheduler-->
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'><o:p>&nbsp;</o:p></=
span></p>
  </td>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'><o:p>&nbsp;</o:p></=
span></p>
  </td>
 </tr>
 <tr style=3D'mso-yfti-irow:5'>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal>&nbsp;<o:p></o:p></p>
  </td>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'><o:p>&nbsp;</o:p></=
span></p>
  </td>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'><o:p>&nbsp;</o:p></=
span></p>
  </td>
 </tr>
 <tr style=3D'mso-yfti-irow:6;mso-yfti-lastrow:yes'>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <div class=3DMsoNormal align=3Dcenter style=3D'text-align:center'>
  <hr size=3D2 width=3D"100%" align=3Dcenter>
  </div>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'>&copy; Copyright 20=
02 The
  Geological Society of <st1:country-region w:st=3D"on"><st1:place w:st=3D"=
on">America</st1:place></st1:country-region>
  (GSA), all rights reserved. Permission <span class=3DGramE>is hereby gran=
ted</span>
  to the author(s) of this abstract to reproduce and distribute it freely, =
for
  noncommercial purposes. Permission is hereby granted to any individual
  scientist to download a single copy of this electronic file and reproduce=
 up
  to 20 paper copies for noncommercial purposes advancing science and <span
  class=3DGramE>education, including classroom use, providing all reproduct=
ions
  include</span> the complete content shown here, including the author
  information. All other forms of reproduction and/or transmittal <span
  class=3DGramE>are prohibited</span> without written permission from GSA
  Copyright Permissions.</span> <o:p></o:p></p>
  <div class=3DMsoNormal align=3Dcenter style=3D'text-align:center'>
  <hr size=3D2 width=3D"100%" align=3Dcenter>
  </div>
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  </td>
<!--/hideinscheduler-->
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span></p>
  </td>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'><o:p>&nbsp;</o:p></=
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