Studi Pemodelan Distribusi Konduktivitas Bawah Permukaan 3-D Berbasis Data Resistivitas Menggunakan Program Aplikasi DCIP3D Versi 2.1

Nadhia Fairuz Syafira, Sitti Ahmiatri Saptari, Adhika Junara Karunianto
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Abstract

Human needs will increase in various aspects, including the need for content in the earth. In describing the distribution of physical properties beneath the earth's surface, 3-D modeling is the best way to find out the details of the subsurface content of the earth. To facilitate the making of 3-D models from the earth, the DCIP3D application program is used. DCIP3D develops a series of inversion algorithms to restore 3-D conductivity models. The research was conducted to optimize the use of DCIP3D version 2.1. The data used are secondary and synthetic data. Secondary data is resistivity geoelectric data consisting of four line of the results of the PTBGN-BATAN survey in the Ahu Mamuju, West Sulawesi, 2017. Data processing is done by making mesh cell size which is a discritization of the earth model. The variation of the mesh core size is done (5 × 5 × 5) m, (10 × 10 × 10) m and (15 × 15 × 15) m. By completing various input files for DCIP3D, the 3-D subsurface conductivity model was successfully restored. Adding topographic values to the model causes the model to look even more real. The best model that describes the conductivity of the secondary data survey area is a model with a core cell (10 × 10 × 10) m because it corresponds to the distance between the electrodes used during data acquisition.
基于电阻数据的三维表面导电性分布研究采用了DCIP3D版本2.1的应用程序
人类的需求将在各个方面增加,包括对地球物质的需求。在描述地表下物理性质分布时,三维建模是了解地表下物质细节的最佳方法。为了便于从地球制作三维模型,使用了DCIP3D应用程序。DCIP3D开发了一系列反演算法来恢复三维电导率模型。本研究旨在优化DCIP3D 2.1版的使用。所使用的数据是二手和综合数据。二次数据是2017年西苏拉威西Ahu Mamuju的PTBGN-BATAN调查结果的四条线的电阻率地电数据。数据处理是通过制作网格单元大小来完成的,网格单元大小是地球模型的一种区分。网格芯尺寸的变化分别为(5 × 5 × 5) m、(10 × 10 × 10) m和(15 × 15 × 15) m。通过完成DCIP3D的各种输入文件,成功恢复了三维地下电导率模型。在模型中添加地形值会使模型看起来更加真实。描述二次数据调查区域电导率的最佳模型是具有核心单元(10 × 10 × 10) m的模型,因为它对应于数据采集期间使用的电极之间的距离。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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