MRI observation of oxygen-supersaturated water transport in a geological matrix.
The oxygen content of groundwater is a crucial property for many geochemical and biogeochemical processes including environmental remediation measures. In this contribution, we present results of a direct MRI observation of the propagation of a locally administered oxygen supersaturation through a water saturated sediment column.
Nestle
Nikolaus
N
Institute of Hydrochemistry, Technische Universität München, Marchioninistrasse 17, D-81377 München, Germany. nikolaus.nestle@ch.tum.de
Baumann
Thomas
T
Wunderlich
Arthur
A
Niessner
Reinhard
R
D019015:Geologic Sediments / Q000737:chemistry*; D008279:Magnetic Resonance Imaging / Q000379:methods*; D010100:Oxygen / Q000032:analysis*; D014867:Water / Q000737:chemistry*; D014881:Water Supply
D014867:Water; D010100:Oxygen