Gravity profiles interpretation applying a metaheuristic particle optimization algorithm of mineralized bodies
Khalid S Essa1,2, Eid R Abo-Ezz3, Yves Géraud2
1Geophysics Department, Faculty of Science, Cairo University, Giza, P.O. 12613, Egypt.
Heliyon
|May 29, 2024
Summary
Particle optimization algorithm accurately interprets gravity anomalies for mineral exploration. This method effectively identifies subsurface targets, even with noisy data, proving reliable for geological surveys.
Area of Science:
- Geophysics
- Mineral Exploration
- Computational Methods
Background:
- Gravity anomaly interpretation is key for identifying subsurface mineralized targets.
- Understanding density variations is crucial for distinguishing targets from surrounding structures.
- Simple geometric bodies are often used to model ore and mineral targets.
Purpose of the Study:
- To apply the particle optimization algorithm for interpreting gravity anomalies.
- To determine parameters of buried bodies modeled as finite vertical cylinders.
- To assess the algorithm's effectiveness in mineral exploration contexts.
Main Methods:
- Utilized particle optimization algorithm, a global metaheuristic method.
- Inferred gravity anomaly profiles to determine body parameters (e.g., depth, length).
- Evaluated performance on synthetic data with varying noise levels (0%, 5%, 10%) and a real Canadian mineral exploration dataset.
Main Results:
- The particle optimization algorithm demonstrated stability and accuracy.
- Performance was unaffected by noise and multi-model scenarios.
- Results from a Canadian mineral exploration case study aligned with existing geological and borehole data.
Conclusions:
- The particle optimization algorithm is a robust tool for gravity data analysis in mineral exploration.
- The method reliably identifies subsurface targets, even in the presence of noise.
- The algorithm's findings are consistent with established geological information and prior research.
Related Concept Videos
Gravimetry: Overview
5.6K
Gravimetric analysis is a quantitative method where the analyte is isolated and weighed directly or after conversion into a substance of known composition. Gravimetric analysis can be classified as precipitation, electrogravimetry, volatilization, and particulate gravimetry, based on the method used to isolate the analyte.
In precipitation gravimetry, the analyte is converted into a precipitate and weighed. For example, the silver content in a sample can be estimated by precipitating and...
In precipitation gravimetry, the analyte is converted into a precipitate and weighed. For example, the silver content in a sample can be estimated by precipitating and...
5.6K
Mechanistic Models: Compartment Models in Algorithms for Numerical Problem Solving
50
Mechanistic models play a crucial role in algorithms for numerical problem-solving, particularly in nonlinear mixed effects modeling (NMEM). These models aim to minimize specific objective functions by evaluating various parameter estimates, leading to the development of systematic algorithms. In some cases, linearization techniques approximate the model using linear equations.
In individual population analyses, different algorithms are employed, such as Cauchy's method, which uses a...
In individual population analyses, different algorithms are employed, such as Cauchy's method, which uses a...
50
The Principle of Superposition and the Gravitational Field
1.3K
The principle of superposition applies to gravitational forces of objects that are sufficiently far apart. It states that the net gravitational force on a point object is the vector sum of the gravitational forces on it due to various objects. The principle helps calculate the force by listing the individual forces and then vectorially summing them up. However, it should be noted that the principle of superposition is not always apparent. In the presence of a second force, the first force could...
1.3K
Gravitational Potential Energy for Extended Objects
1.4K
Consider a system comprising several point masses. The coordinates of the center of mass for this system can be expressed as the summation of the product of each mass and its position vector divided by the total mass:
1.4K


