Figure 5 - uploaded by Nabin Kharal
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... map in Figure 5 gives an overview of which method has been done where in the study are. Observation wells are shown as well. ...
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... 10 is an example on how an interpretation can be based on structures. We measured a 180 meters long profile along the road to the river passing beside the water works ( Fig 5). The last ~50 meters of the profile are parallel to the ERT and Seismic profiles. ...
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... locations were chosen for the Mariotte infiltration test. Location 1 is the end of the seismic line, whereas location 2 is roughly the end of the ERT line (Fig. ...
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... slug test is performed through various ways, in this case of study the Hvorlev's Method was used where water is added through a tube and measure amount of water decrease or water that get percolated inside the soil (Fig. 15). The following task were carried during this test: 1) Measure depth of water table before test 2) Fill a given volume of water in the well and measure h at increasing times (e.g. every 5 cm), h0 is the head value at time t = ...
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