Geology & Exploration

Susceptibility (seismic)

Susceptibility: Understanding the Magnetic Response of Rocks

In the realm of geology and geophysics, the term susceptibility (specifically magnetic susceptibility) plays a crucial role in understanding the magnetic properties of rocks. This property essentially measures how easily a rock can be magnetized when exposed to an external magnetic field. It's a fundamental concept used in various geological investigations, from exploring mineral deposits to unraveling Earth's magnetic history.

Defining Susceptibility: A Ratio of Magnetic Strength

Susceptibility is defined as the ratio of the intensity of magnetization (I) to the magnetic field (H) projected into the rock. This ratio, denoted by the letter k, essentially quantifies the rock's ability to respond to an external magnetic field.

k = I/H

A higher susceptibility value indicates that the rock is more easily magnetized, meaning it will have a stronger magnetization in the presence of a given magnetic field. Conversely, a lower susceptibility value suggests the rock is less susceptible to magnetization.

What Influences Rock Susceptibility?

Several factors influence a rock's susceptibility, including:

  • Mineral composition: The presence of magnetic minerals like magnetite, hematite, and pyrrhotite significantly influences a rock's susceptibility. These minerals are naturally magnetic and readily align themselves with an external field, increasing the overall magnetization.
  • Grain size and shape: The size and shape of magnetic mineral grains within a rock also play a role. Fine-grained minerals often exhibit higher susceptibility compared to coarse-grained ones.
  • Temperature: Susceptibility can change with temperature, as the alignment of magnetic domains within the minerals can be affected by heat.
  • Pressure: High pressure can also influence susceptibility, particularly in the case of rocks with highly magnetic minerals.

Applications of Susceptibility Measurements

Susceptibility measurements have numerous applications in geological research and exploration:

  • Mineral exploration: Identifying areas rich in magnetic minerals, which often correspond to valuable deposits.
  • Paleomagnetic studies: Investigating the Earth's magnetic field history by analyzing the magnetization of ancient rocks.
  • Environmental studies: Tracing the movement of sediments and pollutants based on their magnetic signatures.
  • Archaeological investigations: Dating and understanding the formation of archaeological sites based on magnetic properties of materials.
  • Geotechnical engineering: Assessing the magnetic properties of soil and rocks for construction purposes.

Tools and Techniques for Measuring Susceptibility

Various instruments are used to measure susceptibility in rocks, including:

  • Kappabridge: A portable device that measures susceptibility by measuring the magnetic field induced in a rock sample.
  • Magnetic susceptibility meter: A more sophisticated instrument that can measure susceptibility over a range of frequencies and temperatures.
  • Magnetic gradiometer: Used to detect changes in magnetic susceptibility over a larger area, useful for mapping geological features.

Conclusion

Susceptibility is a key property that allows us to understand the magnetic behavior of rocks and unlock valuable information about Earth's history, mineral resources, and environmental processes. By measuring and analyzing susceptibility, geologists can gain insights into the composition, formation, and magnetic properties of rocks, contributing to a wide range of scientific and practical applications.


Test Your Knowledge

Susceptibility Quiz:

Instructions: Choose the best answer for each question.

1. What is magnetic susceptibility?

a) The ability of a rock to resist magnetization.

Answer

Incorrect. This describes magnetic permeability, not susceptibility.

b) The ratio of the intensity of magnetization to the applied magnetic field.
Answer

Correct! This is the definition of magnetic susceptibility.

c) The strength of the magnetic field generated by a rock.
Answer

Incorrect. This describes the rock's magnetic moment, not susceptibility.

d) The temperature at which a rock becomes magnetic.
Answer

Incorrect. This describes the Curie temperature, not susceptibility.

2. Which of the following factors does NOT influence a rock's susceptibility?

a) Mineral composition

Answer

Incorrect. The presence of magnetic minerals greatly affects susceptibility.

b) Grain size and shape
Answer

Incorrect. Fine-grained minerals generally have higher susceptibility.

c) Density of the rock
Answer

Correct! Density itself doesn't directly affect susceptibility, although it might correlate with mineral content.

d) Temperature
Answer

Incorrect. Susceptibility can change with temperature due to changes in magnetic domain alignment.

3. Which of these minerals is NOT a major contributor to a rock's magnetic susceptibility?

a) Magnetite

Answer

Incorrect. Magnetite is highly magnetic and strongly influences susceptibility.

b) Hematite
Answer

Incorrect. Hematite can be magnetic, although its susceptibility is lower than magnetite.

c) Quartz
Answer

Correct! Quartz is non-magnetic and does not contribute significantly to rock susceptibility.

d) Pyrrhotite
Answer

Incorrect. Pyrrhotite is a magnetic mineral and influences susceptibility.

4. Magnetic susceptibility measurements can be used for which of the following applications?

a) Mapping underground geological structures.

Answer

Correct! Magnetic susceptibility variations can reveal buried features.

b) Dating archaeological artifacts.
Answer

Incorrect. While magnetic properties can be used for dating, susceptibility alone might not be sufficient.

c) Detecting mineral deposits.
Answer

Correct! Magnetic minerals often indicate the presence of valuable deposits.

d) Studying the history of Earth's magnetic field.
Answer

Correct! Paleomagnetic studies use susceptibility measurements of ancient rocks.

5. What is a Kappabridge used for?

a) Measuring the magnetic field strength of a rock.

Answer

Incorrect. A Kappabridge measures susceptibility, not field strength.

b) Determining the age of a rock.
Answer

Incorrect. Age determination requires other methods like radiometric dating.

c) Measuring the magnetic susceptibility of a rock sample.
Answer

Correct! This is the primary function of a Kappabridge.

d) Creating a magnetic map of a region.
Answer

Incorrect. While useful for mapping, a Kappabridge is typically used for point measurements.

Susceptibility Exercise:

Imagine you are a geologist studying a region with potential iron ore deposits. You are using a Kappabridge to measure the magnetic susceptibility of rock samples. You encounter two samples with the following results:

  • Sample A: Susceptibility value = 0.01 SI units
  • Sample B: Susceptibility value = 0.5 SI units

1. Which sample is more likely to contain a higher concentration of iron ore?

2. Explain your reasoning, considering the relationship between magnetic susceptibility and mineral composition.

Exercice Correction

**1. Sample B is more likely to contain a higher concentration of iron ore.**

**2. Reasoning:** * Iron ore primarily consists of magnetite, a highly magnetic mineral. * A higher magnetic susceptibility value indicates a stronger response to an external magnetic field, suggesting a higher concentration of magnetic minerals. * Therefore, Sample B with its significantly higher susceptibility value is more likely to contain a greater abundance of magnetic minerals, including magnetite, making it a promising indicator for iron ore deposits.


Books

  • "Magnetic Susceptibility of Rocks" by J. D. A. Piper (2003): A comprehensive text covering the theory, measurement, and interpretation of magnetic susceptibility in rocks.
  • "Geophysics for Geoscientists" by J. M. Reynolds (2011): A textbook that includes chapters on rock magnetism and paleomagnetism, offering insights into magnetic susceptibility and its applications.
  • "Earthquake Engineering: From Theory to Practice" by A. S. Papageorgiou and D. P. Abrahamson (2008): A detailed resource for earthquake engineering, focusing on seismic vulnerability and risk assessment.
  • "Principles of Engineering Geology" by A. R. Jumikis (1983): A classic textbook offering insights into the geological aspects of earthquake hazards and susceptibility.

Articles

  • "Magnetic Susceptibility as a Tool for Studying the Environment" by J. D. A. Piper (2002): Discusses the application of magnetic susceptibility in environmental studies, including sediment transport and pollution tracing.
  • "Paleomagnetism and the History of the Earth's Magnetic Field" by R. T. Merrill and M. W. McElhinny (1996): An article that delves into the use of paleomagnetism and magnetic susceptibility to understand Earth's magnetic history.
  • "Seismic Hazard Assessment: A Guide for Building Safer Communities" by U.S. Geological Survey (2014): A comprehensive guide on seismic hazard assessment, including methodologies for evaluating seismic susceptibility.
  • "Seismic Vulnerability of Buildings: A Review" by A. K. Chopra (2001): An article exploring the vulnerability of buildings to earthquakes, covering various aspects of seismic susceptibility.

Online Resources

  • Geomagnetism & Paleomagnetism, USGS: https://www.usgs.gov/science-support/geomagnetism-paleomagnetism - A detailed website by the U.S. Geological Survey focusing on geomagnetism and paleomagnetism, providing resources on magnetic susceptibility and its applications.
  • Earthquakes, USGS: https://www.usgs.gov/natural-hazards/earthquakes - A comprehensive website by the U.S. Geological Survey dedicated to earthquake information, including hazard assessment, seismic susceptibility, and vulnerability.
  • Seismic Hazard Maps, USGS: https://www.usgs.gov/natural-hazards/earthquakes/science/maps - A website offering access to interactive seismic hazard maps, providing insights into seismic susceptibility across the United States.

Search Tips

  • "Magnetic susceptibility rocks": To find information about the magnetic susceptibility of rocks, including measurement techniques and applications.
  • "Seismic vulnerability assessment": To discover resources on assessing the vulnerability of regions and structures to earthquakes.
  • "Earthquake hazards map": To access maps illustrating seismic hazards and susceptibility for specific locations.
  • "Paleomagnetism research papers": To find scientific papers exploring the use of paleomagnetism and magnetic susceptibility in understanding Earth's history.

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