Podcast
Questions and Answers
What is the relationship between the electric vector of light and the direction of light propagation?
What is the relationship between the electric vector of light and the direction of light propagation?
The electric vector is perpendicular to the direction in which the light is propagating.
How do changes in velocity affect the wavelength of light in optical mineralogy?
How do changes in velocity affect the wavelength of light in optical mineralogy?
If the velocity of light changes, then the wavelength must change to maintain a constant frequency (F).
Define wave front and wave normal in the context of light waves.
Define wave front and wave normal in the context of light waves.
A wave front is a parallel surface connecting equivalent points on adjacent waves, while a wave normal is a line perpendicular to the wave front, indicating the direction of wave movement.
Explain why frequency (F) is considered constant in optical mineralogy, regardless of the material light travels through.
Explain why frequency (F) is considered constant in optical mineralogy, regardless of the material light travels through.
What does a light ray represent in the context of light behavior and mineralogy?
What does a light ray represent in the context of light behavior and mineralogy?
What is the significance of light in optical mineralogy?
What is the significance of light in optical mineralogy?
Define visible light and its wavelength range.
Define visible light and its wavelength range.
How does light behave when passing through minerals?
How does light behave when passing through minerals?
What role does the petrographic microscope play in mineral identification?
What role does the petrographic microscope play in mineral identification?
Explain the concept of the electromagnetic spectrum in relation to light.
Explain the concept of the electromagnetic spectrum in relation to light.
Flashcards
Light in Optical Mineralogy
Light in Optical Mineralogy
Light interacts with minerals' atomic structure, helping identify minerals in rocks using a microscope.
Electromagnetic Spectrum
Electromagnetic Spectrum
A continuous range of radiation, from cosmic rays to radio waves, with visible light as a small portion.
Visible Light Wavelengths
Visible Light Wavelengths
Visible light ranges from 390 nm to 770 nm.
Optical Mineralogy Principle
Optical Mineralogy Principle
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Petrographic Microscope
Petrographic Microscope
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Electric Vector
Electric Vector
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Light and Minerals
Light and Minerals
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Constant Frequency
Constant Frequency
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Wave Front
Wave Front
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Wave Normal
Wave Normal
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Study Notes
Optical Mineralogy Course (801202)
- Course offered during the first semester of 2024/2025
- Instructor: Dr. Sanaa Al-Zyoud
- Department: Applied Earth and Environmental Sciences
- Faculty: Earth and Environmental Sciences
- University: Al al-Bayt University
Course Description
- Aims to study optical properties of rock-forming minerals
- Includes light properties and light theories
- Covers plane polarized light and its properties
- Focuses on minerals under polarized light (PPL and XPL)
- Relevant for later study units on igneous, metamorphic, and sedimentary rocks.
- Students gain basic knowledge, data analysis, and interpretation skills.
- Training provided on instruments and techniques, with the scientific way of thinking.
Course Outcomes
- Students will be able to distinguish between different types of light interactions.
- Students will understand the link between light properties and the physical properties of minerals.
- Students will be able to evaluate mineral properties optically.
- Students will be able to distinguish minerals optically
Textbook Information
- Title: Introduction to Optical Mineralogy
- Author: William D. Nesse
- Publisher: Oxford University Press, Inc.
- Year: 1991
- Edition: Second Edition
- Website: https://www.amazon.com/Introduction-Optical-Mineralogy-William- Nesse/dp/0195060245
Course Content (by week)
- Week 1: Introduction, Nature of Light, Electromagnetic Radiation Phase, Perception of Color, Interaction of Light and Matter, Plane Polarized Light
- Week 2: Petrographic Microscope, Illuminator, Substage Assembly, Microscope Stage, Objective Lenses, Upper Polar, Bertrand Lens
- Week 3: Refractometry, Relief, Becke Line Method
- Week 5: Optics of Isotropic Materials, Isotropic Indicatrix, Distinguishing Between Isotropic & Anisotropic Minerals, Identification of Isotropic Minerals
- Week 6: Optics of Anisotropic Minerals, Introduction, Interference Phenomena, Determining Thickness of a Sample
- Week 7: Determining Birefringence from Color Chart, Recognizing Different Orders of Interference Colors.
- Week 8: Mid-Term Exam
- Week 9: Extinction. Use of the Accessory Plates, Sign of Elongation, Relief, Pleochroism, Uniaxial Optics, Optic Sign, Crystallographic Considerations, Uniaxial Indicatrix
- Week 10: Birefringence, and Interference Colors, Extinction, Pleochroism, Interference Figure, Selecting Grains, Determining Indices of Refraction
- Week 11: Biaxial Optics, Biaxial Indicatrix, Crystallographic Orientation, Biaxial Interference Figures
- Week 12: Identification of Minerals – Descriptive Features, Cleavage, Twinning, Alteration, Association, Tactics, Opaque Minerals, Non-minerals (selected topics).
- Week 13: Optical Properties of Non-silicate (Selected topics),
- Week 14: Optical Properties of Silicate (Selected topics)
- Week 15: Final Exam
Additional Topics
- Light (in relation to mineralogy): Light as a tool, light as energy, its nature, properties, and how light interacts with minerals. Types of polarization, generating polarized light, polarization by absorption, reflection, scattering.
- Quantum Electrodynamics and Light: Relationship between wave and particle duality, how light interacts with matter, describing light as being composed of photons.
- Minerals properties in PPL: A fundamental principle that most minerals can transmit light if they are thin enough, using the petrographic microscope. How to prepare mineral thin sections.
- Minerals Color: How color is used for mineral identification. Opaque & non-opaque mineral differences.
- Relief: The degree to which a mineral's grain stands out from the mounting medium, determining if relief is strong, moderate, or low.
- Optic axis: Direction in a crystal where light is either not refracted or polarized.
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