A026 SOIL MOISTURE DYNAMICS WITH TIME LAPSE GPR J. SCHMALHOLZ 1 A. KEMNA 2 M. MÜLLER 1 H. STOFFEGEN 3 AND U. YARAMANCI 1 Introduction 1 Tracing the water content in the uppermost soil is of great interest for a variety of different scientific disciplines. Since many processes are linked to the volumetric water content and its dynamics the scale of interest ranges from kilometres to submetres. With the availability of shielded high frequency ground penetrating radar (GPR) antennas a non- respectively minimally invasive geophysical tool valuable information concerning the water content can be obtained with a spatial resolution in


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