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Nitrate concentrations and specific conductance measured during a depth profile indicated that the water column was generally homogeneous as expected for this karst environment, but changes were observed in the most productive zone of the aquifer that might indicate some heterogeneity within the complex network of flow paths.
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Articulation nodes can be detected during a depth-first traversal of the graph, by calculating the "lowpoint" values of every node (cf. [ 48]).
DNAPL was detected in one borehole during coring at a depth of 27 m.
The maximum spatial variability (for more than 50% of map cells in the vicinity of hypocenter) is observed with positive disturbances (DfoF2p) for the earthquakes that occurred during daytime at a depth of 70 300 km.
However, it is difficult to explain the observed increase in resistivity during March 2012 at a depth of 0.1 km; this depth roughly corresponds to the depth of low-temperature hot-spring waters in the site ASY area (Fig. 6).
These records were obtained during an event with a depth of 11 km and an M J of 4.9.
Figure 12 displays an example of the records obtained during an event with a depth of 13 km and an M J of 4.1 at KC01 KC04 in Kumamoto city with some stations in Mashiki town for comparison.
A confocal pinhole with 250 μm diameter was applied during measurement to enable a depth resolution of 2 to 3 μm.
Surveys were conducted on the reef flat during February and May 2016, at a depth of ~2 m.
Furthermore, geodetic surveys found the pressure source during the 1990 1995 eruption at a depth of about 1.5 3 km beneath the summit (Geodetic Survey Group, Joint Observation by National Universities, 1991; Ishihara, 1993; Hendrasto et al., 1997; Kohno et al., 2008).
This was integrated by a major shallowing upwards cycle during the Early Maastrichtian from a depth of 800 m to less than 10 m in the Late Maastrichtian, where a rudist ramp developed and then became zero at the Maastrichtian/Danian boundary.
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