METODE POLARISASI TERINDUKSI DALAM KAWASAN WAKTU UNTUK IDENTIFIKASI MINERAL LOGAM PADA PEMODELAN FISIS TIME DOMAIN INDUCED POLARIZATION METHOD FOR BASE METAL IDENTIFICATION IN PHYSICAL MODELING

Budiarto, Dedik (2015) METODE POLARISASI TERINDUKSI DALAM KAWASAN WAKTU UNTUK IDENTIFIKASI MINERAL LOGAM PADA PEMODELAN FISIS TIME DOMAIN INDUCED POLARIZATION METHOD FOR BASE METAL IDENTIFICATION IN PHYSICAL MODELING. Masters thesis, UPN "VETERAN" YOGYAKARTA.

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Abstract

Metode polarisasi terinduksi kawasan waktu atau Time Domain Induced
Polarization (TDIP) merupakan salah satu metode geofisika yang digunakan untuk
identifikasi bawah permukaan terutama mineral logam. Metode TDIP memberikan
informasi sifat fisis batuan atau mineral dilihat dari sifat kelistrikan dan
polarisasinya, metode ini memberikan parameter-parameter resistivitas (ρ) dan
chargeabilitas (M). Studi eksperimental telah dilakukan untuk menguji respon
TDIP dari berbagai sampel model uji.
Sistem pengukuran menggunakan Syscal Junior Auto 568 sebagai alat untuk
merekam resistivitas dan chargeabilitas. Pengukuran dilakukan menggunakan
konfigurasi Dipole-Dipole dengan spasi a=10cm, panjang lintasan 180cm untuk
menguji respon dari model bola pejal berkadar besi (Fe) 0%, 10%, 20%, 30% dan
50% yang diletakkan pada kedalaman 15cm pada akuarium bermedium air.
Hasil pengukuran air menggunakan soil box memberikan respon resistivitas
sebesar 20.5Ωm. Hasil pengukuran menunjukkan nilai resistivitas semakin
mengecil dengan bertambahnya kadar besi (Fe) pada model bola pejal. Namun,
hasil respon chargeabilitas menunjukkan nilai semakin besar seiring bertambahnya
kadar besi (Fe) pada model bola pejal. Hasil sampel uji berupa bola pejal yang
memiliki kandungan besi (Fe) tidak menunjukan respon TDIP yang sempurna, hal
ini depengaruhi oleh perbedaan resistivitas yang sangat kecil antara model dan
medium air.
Kata kunci : Time Domain Induced Polarization (TDIP), Dipole-Dipole,
resistivitas, chargeabilitas, pemodelan 2D

Time Domain Induced Polarization (TDIP) method is one of geophysical
method used to identify subsurface mainly metallic minerals. TDIP method can
provide more information about physical properties of rocks or minerals views of
the electrical and polarization properties, these methods can give the parameters
of resistivity (ρ) and chargeability (M). An experimental study have been conducted
to test the TDIP response of the various samples model.
The measurement system is built with Syscal Junior Auto 568 as a device
for sampling resistivity and chargeability. Measurements using a dipole-dipole
configuration with a space (a) = 10cm, distance = 180cm to test the response of the
some models with iron (Fe) contains 0%, 10%, 20%, 30% and 50% were placed at
a depth of 15cm in medium water.
The results of measurement water using soil box can provide resistivity
response of 20.5Ωm. The measurement results indicate the value of the resistivity
has small with increasing levels of iron (Fe) contains in the model. However, the
results chargeability response indicate larger value with increasing levels of iron
(Fe) contains in the model. Result from sample of model with iron (Fe) contains did
not indicate a perfect TDIP response, it is influenced by a very small difference in
resistivity between the model and the medium of water.
Keywords: Time Domain Induced Polarization (TDIP), Dipole-Dipole, resistivity,
chargeability, 2D modelling

Item Type: Thesis (Masters)
Subjek: Q Science > QC Physics
Divisions: x. Faculty of Engineering, Science and Mathematics > School of Engineering Sciences
Depositing User: Bugel Suryanta
Date Deposited: 18 May 2016 04:03
Last Modified: 18 May 2016 04:03
URI: http://eprints.upnyk.ac.id/id/eprint/1395

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