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TDEM (Time Domain electomagnetic) or sometimes referred to TEM (transient <br /> <br /> <br /> electromagnetic) is a method that measures the electromagnetic transient voltage <br /> <br /> <br /> decay as a function of time. The results of the measurements us...
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id-itb.:206132017-09-27T11:45:17Z#TITLE_ALTERNATIVE# MEIRISKA NIM :102 10 092, WIDYA Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/20613 TDEM (Time Domain electomagnetic) or sometimes referred to TEM (transient <br /> <br /> <br /> electromagnetic) is a method that measures the electromagnetic transient voltage <br /> <br /> <br /> decay as a function of time. The results of the measurements using this TDEM <br /> <br /> <br /> method can then be interpreted using some software. One of the software that can be <br /> <br /> <br /> used is Interpex IX1D. This interpretation is done by using data from a field in the <br /> <br /> <br /> region x. The data field consists of 23 point soundings, which have been measured <br /> <br /> <br /> using a Geonics Protem with with 3 variations of different frequencies. Later after <br /> <br /> <br /> interpreted using this software, it can be predicted value of resistivity of each layer <br /> <br /> <br /> below the surface. And when it is linked to the prediction of geological data also <br /> <br /> <br /> types of materials that are below the surface. text |
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TDEM (Time Domain electomagnetic) or sometimes referred to TEM (transient <br />
<br />
<br />
electromagnetic) is a method that measures the electromagnetic transient voltage <br />
<br />
<br />
decay as a function of time. The results of the measurements using this TDEM <br />
<br />
<br />
method can then be interpreted using some software. One of the software that can be <br />
<br />
<br />
used is Interpex IX1D. This interpretation is done by using data from a field in the <br />
<br />
<br />
region x. The data field consists of 23 point soundings, which have been measured <br />
<br />
<br />
using a Geonics Protem with with 3 variations of different frequencies. Later after <br />
<br />
<br />
interpreted using this software, it can be predicted value of resistivity of each layer <br />
<br />
<br />
below the surface. And when it is linked to the prediction of geological data also <br />
<br />
<br />
types of materials that are below the surface. |
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Final Project |
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MEIRISKA NIM :102 10 092, WIDYA |
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MEIRISKA NIM :102 10 092, WIDYA #TITLE_ALTERNATIVE# |
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MEIRISKA NIM :102 10 092, WIDYA |
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MEIRISKA NIM :102 10 092, WIDYA |
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https://digilib.itb.ac.id/gdl/view/20613 |
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1821120210832195584 |