Figure 4.(a) Measured MRS data and fit of the inversion. (b)–(d) Inversion results. Total water content and normalized permeability (product of total water content and mean decay time, normalized by its maximum value) are derived from the PWC distribution.
Figure 5.Results of measurements at Muravera, Sardinia. (a) Block inversion of direct current geoelectric measurements. (b) MRS inversion results including resistivity inversion.
Figure 6.Results from the combinable magnetic resonance (CMR) tool at well SWS 16. Leftmost column shows the partial water content for several decay-time classes (from pink, 0.3–30 ms to green, 80–300 ms).
Figure 8.Two-dimensional distribution of the total water content at the Nauen, Germany test site. A survey was conducted using four positions (P1-P4) and all useful combinations of transmitter and receiver loops at these positions. The loop diameter was 50 m. The lateral extent of the primary aquifer (blue = 25% water content) is clearly visible.
