Fig. 6From: Groundwater aquifer detection using the electrical resistivity method at Ito Campus, Kyushu University (Fukuoka, Japan)a Inverted section of data from Line 1 section A (0–200 m); b inverted section of data from Line 1 section B (120–240 m); c inverted section of data from Line 1 section C (240–360 m); d inverted section of data from Line 1 section D (360–480 m); e inverted section of Line 2, and f inverted section of Line 3Back to article page