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GPS readings from different locations of the study area were used for further ground checking.
The geographical locations of the study sites and their depths at high and low tides are shown in Table 1.
A total 20 groundwater samples were collected from different locations of the study area (Fig. 1) from shallow tubewells.
For correlation purposes, disturbed and undisturbed soil samples were collected from twenty-two lofathenstudythe study area.
Vertical electrical sounding (VES) was carried out in 37 locations of the study area to understand the geology and also to verify the extent of weathering.
Groundwater samples were collected from 24 locations of the study area using Global Positioning System (GPS) during the month of June 2013 and February 2014.
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First of all, such temperature difference is related to different locations of the studied process.
Fig. 1 Locality map. a The Japan Islands, showing the plate configuration and the locations of the studied areas.
Figure 1 Location of the study site.
Figure 1 Location of the study area.
Fig. 1 Location of the study area.
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