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instr.html
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<!DOCTYPE html>
<html>
<head>
<title>Geomicrobiology Tuebingen</title>
<link rel="stylesheet" type="text/css" href="index.css">
</head>
<!-- Below is the main title script -->
<body>
<ul class="topmenu_ul">
<li class="topmenu_ul"><img src="images/logo.jpg" alt="Geomicrobiology Tuebingen" style="height:100px; vertical-align:middle;"></li>
<li class="topmenu_ul"><a class="title" href="index.html">Home</a></li>
<li class="topmenu_ul"><a class="title" href="research.html">Research</a></li>
<li class="topmenu_ul"><a class="title" href="about.html">People</a></li>
<li class="topmenu_ul"><a class="title" href="pubs.html">Publications</a></li>
<li class="topmenu_ul"><a class="title" href="instr.html">Instrumentation</a></li>
<li class="topmenu_ul"><a class="title" href="photos.html">Photos</a></li>
<li class="topmenu_ul"><a class="title" href="field.html">Field Sites</a></li>
<li class="topmenu_ul"><a class="title" href="jobs.html">Jobs</a></li>
</ul>
<img src="images/02.jpg" alt="Raublanch" style="width:100%; height:130px; margin-top:130px; z-index:0;">
<ul class="sidemenu_ul">
<li><a class="sidemenu" href="#head">Early Earth</a></li>
<li><a class="sidemenu" href="#senior">Iron Cycling</a></li>
<li><a class="sidemenu" href="#postdoc">Biochar</a></li>
<li><a class="sidemenu" href="#phd">Remediation</a></li>
<li><a class="sidemenu" href="#msc">Magnetic Nanoparticles</a></li>
<li><a class="sidemenu" href="#tech">Technicians</a></li>
<li><a class="sidemenu" href="#tech">Administative support</a></li>
<li><a class="sidemenu" href="#alumni">Alumni</a></li>
</ul>
<!-- Do not change anything above this line -->
<div class="maincontent">
<table class="maincontent" style="width:75%">
<tr><td colspan="2"><h2>Mössbauer spectroscopy</h2></td></tr>
<tr><td colspan="2">Banded Iron Formations</td></tr>
<tr>
<td><img src="images/bif.jpg" style="height:100px; width=100px;"></td>
<td>Banded Iron Formations (BIF's) form one of the most incredible sources of determining the Earth's history. Through the investigation of the different layering within the minerals, we can see microfossils of iron embedded with Si
</td>
</tr>
<tr><td colspan="2"><h2>Iron Cycling</h2></td></tr>
<tr><td colspan="2">Magnetite as a biogeobattery</td></tr>
<tr>
<td><img src="images/magnetite.jpg" style="height:150px; width=100px;"></td>
<td>Magneitite is the best mineral in the world
</td>
</tr>
<tr><td colspan="2">Oxidation profiles</td></tr>
<tr>
<td><img src="images/cores.jpg" style="height:100px; width=100px;"></td>
<td>We probe oxygen profiles with electrodes for some reason
</td>
</tr>
<tr><td colspan="2"><h2>Bichar</h2></td></tr>
<tr><td colspan="2">Banded Iron Formations</td></tr>
<tr>
<td><img src="images/bif.jpg" style="height:100px; width=100px;"></td>
<td>Banded Iron Formations (BIF's) form one of the most incredible sources of determining the Earth's history. Through the investigation of the different layering within the minerals, we can see microfossils of iron embedded with Si
</td>
</tr>
</table></td>
</tr>
</table>
</div>
</body>
</html>