Alfaninata, Yeshia (2025) Pemrosesan Data Magnetotellurik Menggunakan Fungsi Transfer Antarstasiun dan Inversi 2D untuk Estimasi Lapisan Clay Cap Pada Lapangan Panas Bumi "AFD". Other thesis, Institut Teknologi Sepuluh Nopember.
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Abstract
Metode Magnetotellurik (MT) telah terbukti efektif untuk memetakan distribusi resistivitas bawah permukaan pada sistem panas bumi, tetapi keandalannya sering terhambat oleh gangguan noise, terutama pada frekuensi rendah dan di wilayah padat penduduk seperti di Indonesia. Salah satu pendekatan yang dapat digunakan untuk mengurangi noise adalah penerapan fungsi transfer antarstasiun dan metode remote reference. Penelitian ini bertujuan untuk mengevaluasi efektivitas fungsi transfer antarstasiun dalam meningkatkan kualitas data MT, serta mengidentifikasi pola distribusi resistivitas bawah permukaan di Lapangan Panas Bumi “AFD”. Data yang digunakan merupakan data sekunder dari 28 stasiun MT hasil akuisisi tahun 2010, 2013, dan 2019, dengan 10 stasiun di antaranya diolah menggunakan metode antarstasiun. Selain itu, digunakan juga metode TDEM (Time Domain Electromagnetic) sebagai acuan untuk koreksi static shift guna mengurangi pengaruh distorsi galvanik akibat kondisi topografi atau variasi resistivitas lateral dangkal. Proses pengolahan dilanjutkan dengan inversi 2D pada tiga lintasan utama untuk memperoleh model resistivitas bawah permukaan. Hasil penelitian menunjukkan bahwa penggunaan fungsi transfer antarstasiun dapat meningkatkan kestabilan kurva impedansi, khususnya pada stasiun dengan kualitas medan magnet lokal yang kurang baik. Hasil inversi berhasil mengidentifikasi zona resistivitas rendah (2–10 ohm.m) yang diinterpretasikan sebagai lapisan clay cap pada elevasi 2000 hingga -1000 mdpl dengan ketebalan bervariasi antara 1000 hingga 2500 meter.
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The Magnetotelluric (MT) method has proven effective for mapping subsurface resistivity distribution in geothermal systems; however, its reliability is often hindered by noise, especially at low frequencies and in densely populated areas such as Indonesia. One approach to mitigate noise is the application of cross-station transfer functions and the remote reference method. This study aims to evaluate the effectiveness of cross-station transfer functions in improving MT data quality and to identify subsurface resistivity distribution patterns in the “AFD” Geothermal Field. The data used are secondary MT data from 28 stations acquired in 2010, 2013, and 2019, with 10 stations processed using cross-station methods. In addition, the Time Domain Electromagnetic (TDEM) method is used as a reference for static shift correction to minimize the effects of galvanic distortion caused by shallow lateral resistivity variations and surface topography. The processing continues with 2D inversion along three main survey lines to obtain a detailed subsurface resistivity model. The results show that applying cross-station transfer functions can enhance the stability of the impedance response curves, especially at stations with poor local magnetic field quality. The inversion results successfully identify a low-resistivity zone (2–10 ohm.m) interpreted as a clay cap at elevations ranging from 2000 to -1000 meters above sea level, with thicknesses varying between 1000 and 2500 meters.
Item Type: | Thesis (Other) |
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Uncontrolled Keywords: | Clay cap, Fungsi Transfer Antarstasiun, Magnetotellurik, Medan Magnet, Panas bumi, Interstation Transfer Function, Magnetotelluric, Magnetic Field, Geothermal |
Subjects: | Q Science > QC Physics > QC20.7.F67 Fourier transformations Q Science > QC Physics > QC610.3 Electric conductivity |
Divisions: | Faculty of Civil, Planning, and Geo Engineering (CIVPLAN) > Geophysics Engineering > 33201-(S1) Undergraduate Thesis |
Depositing User: | Yeshia Alfaninata |
Date Deposited: | 31 Jul 2025 05:51 |
Last Modified: | 31 Jul 2025 05:51 |
URI: | http://repository.its.ac.id/id/eprint/124042 |
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