Research on Topographic Effects of the Time-Domain Induced Polarization Method in Mineral Exploration

Time-domain induced polarization (TDIP) is a widely adopted geophysical technique for metallic mineral exploration. Field surveys are frequently carried out under complex topographic conditions such as slopes and valleys. Topographic undulation distorts TDIP responses and may bias the interpretation of ore-related subsurface anomalies. In this work, an unstructured finite-element forward modeling framework for TDIP is constructed using tetrahedral meshes generated by TetGen1.5.1, and the preconditioned conjugate gradient (PCG) solver is employed to solve large sparse linear systems. A spherical model with an analytical solution is adopted to verify the reliability of the algorithm. Numerical experiments are designed for flat, slope and valley terrain conditions to quantitatively evaluate mesh performance and topographic effects. Numerical results indicate that mesh quality acts as a dominant factor controlling simulation accuracy. Local adaptive mesh refinement can effectively reduce relative numerical errors and achieve a good balance between computational accuracy and cost. This study reproduces topographic effects that have been documented in the existing literature: the apparent chargeability exhibits asymmetric distribution over slopes, with attenuated anomaly amplitude and shifted anomaly position as the dip angle increases; current convergence in valleys amplifies secondary IP signals and alters anomaly patterns. Synthetic inversion tests demonstrate that neglecting topographic relief can induce inversion artifacts and misposition the target geological bodies. A field TDIP dataset from a mountainous polymetallic deposit further shows that terrain-constrained inversion facilitates the identification and discrimination of anomalies. The core advancement of this study lies in the establishment of an adaptive meshing workflow for TDIP forward modeling under complex terrain and its systematic quantitative evaluation. The proposed framework provides reliable technical support for high-precision TDIP data interpretation in mountainous mining areas.

Authors

Institutions

Publication Details

Journal
Minerals
Published
2026-11-11
DOI
https://doi.org/10.3390/min16111179
Primary Topic
Geophysical and Geoelectrical Methods
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
NOV
article

Research on Topographic Effects of the Time-Domain Induced Polarization Method in Mineral Exploration

Daiming Hu, Jianhua Cai
Minerals
Geophysical and Geoelectrical Methods
article

Research on Topographic Effects of the Time-Domain Induced Polarization Method in Mineral Exploration

Daiming Hu, Jianhua Cai
article en

Abstract

Time-domain induced polarization (TDIP) is a widely adopted geophysical technique for metallic mineral exploration. Field surveys are frequently carried out under complex topographic conditions such as slopes and valleys. Topographic undulation distorts TDIP responses and may bias the interpretation of ore-related subsurface anomalies. In this work, an unstructured finite-element forward modeling framework for TDIP is constructed using tetrahedral meshes generated by TetGen1.5.1, and the preconditioned conjugate gradient (PCG) solver is employed to solve large sparse linear systems. A spherical model with an analytical solution is adopted to verify the reliability of the algorithm. Numerical experiments are designed for flat, slope and valley terrain conditions to quantitatively evaluate mesh performance and topographic effects. Numerical results indicate that mesh quality acts as a dominant factor controlling simulation accuracy. Local adaptive mesh refinement can effectively reduce relative numerical errors and achieve a good balance between computational accuracy and cost. This study reproduces topographic effects that have been documented in the existing literature: the apparent chargeability exhibits asymmetric distribution over slopes, with attenuated anomaly amplitude and shifted anomaly position as the dip angle increases; current convergence in valleys amplifies secondary IP signals and alters anomaly patterns. Synthetic inversion tests demonstrate that neglecting topographic relief can induce inversion artifacts and misposition the target geological bodies. A field TDIP dataset from a mountainous polymetallic deposit further shows that terrain-constrained inversion facilitates the identification and discrimination of anomalies. The core advancement of this study lies in the establishment of an adaptive meshing workflow for TDIP forward modeling under complex terrain and its systematic quantitative evaluation. The proposed framework provides reliable technical support for high-precision TDIP data interpretation in mountainous mining areas.

MineralsVol. 16(11)
University of Science and Technology of China (CN), Hunan University of Arts and Science (CN)
Geophysical and Geoelectrical Methods
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.

Laika access coming soon