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ABSTRACT: <br /> <br /> <br /> <br /> <br /> The measurement of resistivity with the dipole dipole configuration in Ciemas region of Sukabumi Regency has been done in two lines, where the first line has a valley and slopes which is not too abrupt. In the other hand...
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id-itb.:64982017-09-27T10:39:01Z#TITLE_ALTERNATIVE# (NIM 12102022), Muhaemin Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/6498 ABSTRACT: <br /> <br /> <br /> <br /> <br /> The measurement of resistivity with the dipole dipole configuration in Ciemas region of Sukabumi Regency has been done in two lines, where the first line has a valley and slopes which is not too abrupt. In the other hand, the topography of the second line is a relatively flat enough. The measurement of resistivity were strongly influenced by the surface variation, the sensitivity factor, and the depth investigation. So it needs a special measurement technique to reduce the noise while the measurement take place. The main purpose of this methode is to obtain a subsurface physical properties from the resistivity data. For a better interpretation, it needs a field data such as test pit data. text |
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ABSTRACT: <br />
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The measurement of resistivity with the dipole dipole configuration in Ciemas region of Sukabumi Regency has been done in two lines, where the first line has a valley and slopes which is not too abrupt. In the other hand, the topography of the second line is a relatively flat enough. The measurement of resistivity were strongly influenced by the surface variation, the sensitivity factor, and the depth investigation. So it needs a special measurement technique to reduce the noise while the measurement take place. The main purpose of this methode is to obtain a subsurface physical properties from the resistivity data. For a better interpretation, it needs a field data such as test pit data. |
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