Physics
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This article is about the field of science. For other uses, see Physics (disambiguation).
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Physics is one of the oldest academic disciplines, perhaps the oldest through its inclusion of astronomy.[6] Over the last two millennia, physics was a part of natural philosophy along with chemistry, certain branches of mathematics, and biology, but during the Scientific Revolution in the 17th century, the natural sciences emerged as unique research programs in their own right.[7] Physics intersects with many interdisciplinary areas of research, such as biophysics and quantum chemistry, and the boundaries of physics are not rigidly defined. New ideas in physics often explain the fundamental mechanisms of other sciences, while opening new avenues of research in areas such as mathematics and philosophy.
Physics also makes significant contributions through advances in new technologies that arise from theoretical breakthroughs. For example, advances in the understanding of electromagnetism or nuclear physics led directly to the development of new products which have dramatically transformed modern-day society, such as television, computers, domestic appliances, and nuclear weapons; advances in thermodynamics led to the development of industrialization; and advances in mechanics inspired the development of calculus.
History
Main article: History of physics
As noted below, the means used to understand the behavior of natural phenomena and their effects evolved from philosophy, progressively replaced by natural philosophy then natural science, to eventually arrive at the modern conception of physics.[citation needed]Natural philosophy has its origins in Greece during the Archaic period, (650 BCE – 480 BCE), when Pre-Socratic philosophers like Thales refused supernatural, religious or mythological explanations for natural phenomena and proclaimed that every event had a natural cause.[8] They proposed ideas verified by reason and observation and many of their hypotheses proved successful in experiment,[9] for example atomism.
Classical physics became a separate science when early modern Europeans used these experimental and quantitative methods to discover what are now considered to be the laws of physics.[10][11] Kepler, Galileo and more specifically Newton discovered and unified the different laws of motion.[12] Experimental physics had its debuts with experimentation concerning statics by medieval Muslim physicists like al-Biruni and Alhazen.[13][14] During the industrial revolution, as energy needs increased, so did research, which led to the discovery of new laws in thermodynamics, chemistry and electromagnetics.
Modern physics started with the works of Max Planck in quantum theory and Einstein in relativity, and continued in quantum mechanics pioneered by Heisenberg, Schrödinger and Paul Dirac.
Philosophy
Main article: Philosophy of physics
In many ways, physics stems from ancient Greek philosophy. From Thales' first attempt to characterize matter, to Democritus' deduction that matter ought to reduce to an invariant state, the Ptolemaic astronomy of a crystalline firmament, and Aristotle's book Physics (an early book on physics, which attempted to analyze and define motion from a philosophical point of view), various Greek philosophers advanced their own theories of nature. Physics was known as natural philosophy until the late 18th century.By the 19th century physics was realized as a discipline distinct from philosophy and the other sciences. Physics, as with the rest of science, relies on philosophy of science to give an adequate description of the scientific method.[15] The scientific method employs a priori reasoning as well as a posteriori reasoning and the use of Bayesian inference to measure the validity of a given theory.[16]
The development of physics has answered many questions of early philosophers, but has also raised new questions. Study of the philosophical issues surrounding physics, the philosophy of physics, involves issues such as the nature of space and time, determinism, and metaphysical outlooks such as empiricism, naturalism and realism.[17]
Many physicists have written about the philosophical implications of their work, for instance Laplace, who championed causal determinism,[18] and Erwin Schrödinger, who wrote on quantum mechanics.[19] The mathematical physicist Roger Penrose has been called a Platonist by Stephen Hawking,[20] a view Penrose discusses in his book, The Road to Reality.[21] Hawking refers to himself as an "unashamed reductionist" and takes issue with Penrose's views.[22]
Core theories
Further information: Branches of physics, Outline of physics
Though physics deals with a wide variety of systems, certain theories are used by all physicists. Each of these theories were experimentally tested numerous times and found correct as an approximation of nature (within a certain domain of validity). For instance, the theory of classical mechanics accurately describes the motion of objects, provided they are much larger than atoms and moving at much less than the speed of light. These theories continue to be areas of active research, and a remarkable aspect of classical mechanics known as chaos was discovered in the 20th century, three centuries after the original formulation of classical mechanics by Isaac Newton (1642–1727).These central theories are important tools for research into more specialized topics, and any physicist, regardless of his or her specialization, is expected to be literate in them. These include classical mechanics, quantum mechanics, thermodynamics and statistical mechanics, electromagnetism, and special relativity.
Classical physics
| Classical Physics |
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Main article: Classical physics
Classical physics includes the traditional branches and topics that were recognized and well-developed before the beginning of the 20th century—classical mechanics, acoustics, optics, thermodynamics, and electromagnetism. Classical mechanics) is concerned with bodies acted on by forces and bodies in motion and may be divided into statics (study of the forces on a body or bodies at rest), kinematics (study of motion without regard to its causes), and dynamics (study of motion and the forces that affect it); mechanics may also be divided into solid mechanics and fluid mechanics (known together as continuum mechanics), the latter including such branches as hydrostatics, hydrodynamics, aerodynamics, and pneumatics. Acoustics, the study of sound, is often considered a branch of mechanics because sound is due to the motions of the particles of air or other medium through which sound waves can travel and thus can be explained in terms of the laws of mechanics. Among the important modern branches of acoustics is ultrasonics, the study of sound waves of very high frequency beyond the range of human hearing. Optics, the study of light, is concerned not only with visible light but also with infrared and ultraviolet radiation, which exhibit all of the phenomena of visible light except visibility, e.g., reflection, refraction, interference, diffraction, dispersion, and polarization of light. Heat is a form of energy, the internal energy possessed by the particles of which a substance is composed; thermodynamics deals with the relationships between heat and other forms of energy. Electricity and magnetism have been studied as a single branch of physics since the intimate connection between them was discovered in the early 19th century; an electric current gives rise to a magnetic field and a changing magnetic field induces an electric current. Electrostatics deals with electric charges at rest, electrodynamics with moving charges, and magnetostatics with magnetic poles at rest.Modern physics
Main article: Modern physics
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| History of modern physics |
Solvay Conference of 1927, with prominent physicists such as Albert Einstein, Werner Heisenberg, Max Planck, Hendrik Lorentz, Niels Bohr, Marie Curie, Erwin Schrödinger and Paul Dirac.
The two chief theories of modern physics present a different picture of the concepts of space, time, and matter from that presented by classical physics. Quantum theory is concerned with the discrete, rather than continuous, nature of many phenomena at the atomic and subatomic level, and with the complementary aspects of particles and waves in the description of such phenomena. The theory of relativity is concerned with the description of phenomena that take place in a frame of reference that is in motion with respect to an observer; the special theory of relativity is concerned with relative uniform motion in a straight line and the general theory of relativity with accelerated motion and its connection with gravitation. Both quantum theory and the theory of relativity find applications in all areas of modern physics.
Difference between classical and modern physics
While physics aims to discover universal laws, its theories lie in explicit domains of applicability. Loosely speaking, the laws of classical physics accurately describe systems whose important length scales are greater than the atomic scale and whose motions are much slower than the speed of light. Outside of this domain, observations do not match their predictions. Albert Einstein contributed the framework of special relativity, which replaced notions of absolute time and space with spacetime and allowed an accurate description of systems whose components have speeds approaching the speed of light. Max Planck, Erwin Schrödinger, and others introduced quantum mechanics, a probabilistic notion of particles and interactions that allowed an accurate description of atomic and subatomic scales. Later, quantum field theory unified quantum mechanics and special relativity. General relativity allowed for a dynamical, curved spacetime, with which highly massive systems and the large-scale structure of the universe can be well-described. General relativity has not yet been unified with the other fundamental descriptions; several candidate theories of quantum gravity are being developed.Relation to other fields
This parabola-shaped lava flow illustrates the application of mathematics in physics—in this case, Galileo's law of falling bodies.
Prerequisites
Mathematics is the language used for compact description of the order in nature, especially the laws of physics. This was noted and advocated by Pythagoras,[23] Plato,[24] Galileo,[25] and Newton.Physics theories use mathematics[26] to obtain order and provide precise formulas, precise or estimated solutions, quantitative results and predictions. Experiment results in physics are numerical measurements. Technologies based on mathematics, like computation have made computational physics an active area of research.
The distinction is clear-cut, but not always obvious. For example, mathematical physics is the application of mathematics in physics. Its methods are mathematical, but its subject is physical.[27] The problems in this field start with a "math model of a physical situation" and a "math description of a physical law". Every math statement used for solution has a hard-to-find physical meaning. The final mathematical solution has an easier-to-find meaning, because it is what the solver is looking for.
Physics is a branch of fundamental science, not practical science.[28] Physics is also called "the fundamental science" because the subject of study of all branches of natural science like chemistry, astronomy, geology and biology are constrained by laws of physics.[29] For example, chemistry studies properties, structures, and reactions of matter (chemistry's focus on the atomic scale distinguishes it from physics). Structures are formed because particles exert electrical forces on each other, properties include physical characteristics of given substances, and reactions are bound by laws of physics, like conservation of energy, mass and charge.
Physics is applied in industries like engineering and medicine.
Application and influence
Main article: Applied physics
Applied physics is a general term for physics research which is intended for a particular use. An applied physics curriculum usually contains a few classes in an applied discipline, like geology or electrical engineering. It usually differs from engineering in that an applied physicist may not be designing something in particular, but rather is using physics or conducting physics research with the aim of developing new technologies or solving a problem.The approach is similar to that of applied mathematics. Applied physicists can also be interested in the use of physics for scientific research. For instance, people working on accelerator physics might seek to build better particle detectors for research in theoretical physics.
Physics is used heavily in engineering. For example, statics, a subfield of mechanics, is used in the building of bridges and other structures. The understanding and use of acoustics results in better concert halls; similarly, the use of optics creates better optical devices. An understanding of physics makes for more realistic flight simulators, video games, and movies, and is often critical in forensic investigations.
With the standard consensus that the laws of physics are universal and do not change with time, physics can be used to study things that would ordinarily be mired in uncertainty. For example, in the study of the origin of the earth, one can reasonably model earth's mass, temperature, and rate of rotation, over time. It also allows for simulations in engineering which drastically speed up the development of a new technology.
But there is also considerable interdisciplinarity in the physicist's methods and so many other important fields are influenced by physics, e.g. the fields of econophysics and sociophysics.
Research
Scientific method
Physicists use a scientific method to test the validity of a physical theory, using a methodical approach to compare the implications of the theory in question with the associated conclusions drawn from experiments and observations conducted to test it. Experiments and observations are collected and compared with the predictions and hypotheses made by a theory, thus aiding in the determination or the validity/invalidity of the theory.A scientific law is a concise verbal or mathematical statement of a relation that expresses a fundamental principle of a theory, like Newton's law of universal gravitation. [30]
Theory and experiment
Main articles: Theoretical physics and Experimental physics
Physicists who work at the interplay of theory and experiment are called phenomenologists. Phenomenologists look at the complex phenomena observed in experiment and work to relate them to fundamental theory.
Theoretical physics has historically taken inspiration from philosophy; electromagnetism was unified this way.[31] Beyond the known universe, the field of theoretical physics also deals with hypothetical issues,[32] such as parallel universes, a multiverse, and higher dimensions. Theorists invoke these ideas in hopes of solving particular problems with existing theories. They then explore the consequences of these ideas and work toward making testable predictions.
Experimental physics informs, and is informed by, engineering and technology. Experimental physicists involved in basic research design and perform experiments with equipment such as particle accelerators and lasers, whereas those involved in applied research often work in industry, developing technologies such as magnetic resonance imaging (MRI) and transistors. Feynman has noted that experimentalists may seek areas which are not well-explored by theorists.[33]
Scope and aims
For example, the ancient Chinese observed that certain rocks (lodestone) were attracted to one another by some invisible force. This effect was later called magnetism, and was first rigorously studied in the 17th century. A little earlier than the Chinese, the ancient Greeks knew of other objects such as amber, that when rubbed with fur would cause a similar invisible attraction between the two. This was also first studied rigorously in the 17th century, and came to be called electricity. Thus, physics had come to understand two observations of nature in terms of some root cause (electricity and magnetism). However, further work in the 19th century revealed that these two forces were just two different aspects of one force—electromagnetism. This process of "unifying" forces continues today, and electromagnetism and the weak nuclear force are now considered to be two aspects of the electroweak interaction. Physics hopes to find an ultimate reason (Theory of Everything) for why nature is as it is (see section Current research below for more information).
Research fields
Contemporary research in physics can be broadly divided into condensed matter physics; atomic, molecular, and optical physics; particle physics; astrophysics; geophysics and biophysics. Some physics departments also support research in Physics education.Since the 20th century, the individual fields of physics have become increasingly specialized, and today most physicists work in a single field for their entire careers. "Universalists" such as Albert Einstein (1879–1955) and Lev Landau (1908–1968), who worked in multiple fields of physics, are now very rare.[34]
Condensed matter
Main article: Condensed matter physics
Velocity-distribution data of a gas of rubidium atoms, confirming the discovery of a new phase of matter, the Bose–Einstein condensate
The most familiar examples of condensed phases are solids and liquids, which arise from the bonding and electromagnetic force between atoms. More exotic condensed phases include the superfluid and the Bose–Einstein condensate found in certain atomic systems at very low temperature, the superconducting phase exhibited by conduction electrons in certain materials, and the ferromagnetic and antiferromagnetic phases of spins on atomic lattices.
Condensed matter physics is by far the largest field of contemporary physics. Historically, condensed matter physics grew out of solid-state physics, which is now considered one of its main subfields. The term condensed matter physics was apparently coined by Philip Anderson when he renamed his research group—previously solid-state theory—in 1967.
In 1978, the Division of Solid State Physics at the American Physical Society was renamed as the Division of Condensed Matter Physics.[35] Condensed matter physics has a large overlap with chemistry, materials science, nanotechnology and engineering.
Atomic, molecular, and optical physics
Main article: Atomic, molecular, and optical physics
Atomic, molecular, and optical physics (AMO) is the study of matter–matter and light–matter interactions on the scale of single atoms and molecules. The three areas are grouped together because of their interrelationships, the similarity of methods used, and the commonality of the energy scales that are relevant. All three areas include both classical, semi-classical and quantum treatments; they can treat their subject from a microscopic view (in contrast to a macroscopic view).Atomic physics studies the electron shells of atoms. Current research focuses on activities in quantum control, cooling and trapping of atoms and ions,[citation needed] low-temperature collision dynamics and the effects of electron correlation on structure and dynamics. Atomic physics is influenced by the nucleus (see, e.g., hyperfine splitting), but intra-nuclear phenomena such as fission and fusion are considered part of high-energy physics.
Molecular physics focuses on multi-atomic structures and their internal and external interactions with matter and light. Optical physics is distinct from optics in that it tends to focus not on the control of classical light fields by macroscopic objects, but on the fundamental properties of optical fields and their interactions with matter in the microscopic realm.
High-energy physics (particle physics)
Main article: Particle physics
A simulated event in the CMS detector of the Large Hadron Collider, featuring a possible appearance of the Higgs boson.
Currently, the interactions of elementary particles are described by the Standard Model. The model accounts for the 12 known particles of matter (quarks and leptons) that interact via the strong, weak, and electromagnetic fundamental forces. Dynamics are described in terms of matter particles exchanging gauge bosons (gluons, W and Z bosons, and photons, respectively). The Standard Model also predicts a particle known as the Higgs boson, the existence of which has not yet been verified; as of 2010[update], searches for it are underway in the Tevatron at Fermilab and in the Large Hadron Collider at CERN.
Astrophysics
Main articles: Astrophysics and Physical cosmology
The discovery by Karl Jansky in 1931 that radio signals were emitted by celestial bodies initiated the science of radio astronomy. Most recently, the frontiers of astronomy have been expanded by space exploration. Perturbations and interference from the earth's atmosphere make space-based observations necessary for infrared, ultraviolet, gamma-ray, and X-ray astronomy.
Physical cosmology is the study of the formation and evolution of the universe on its largest scales. Albert Einstein's theory of relativity plays a central role in all modern cosmological theories. In the early 20th century, Hubble's discovery that the universe was expanding, as shown by the Hubble diagram, prompted rival explanations known as the steady state universe and the Big Bang.
The Big Bang was confirmed by the success of Big Bang nucleosynthesis and the discovery of the cosmic microwave background in 1964. The Big Bang model rests on two theoretical pillars: Albert Einstein's general relativity and the cosmological principle. Cosmologists have recently established the ΛCDM model of the evolution of the universe, which includes cosmic inflation, dark energy and dark matter.
Numerous possibilities and discoveries are anticipated to emerge from new data from the Fermi Gamma-ray Space Telescope over the upcoming decade and vastly revise or clarify existing models of the universe.[36][37] In particular, the potential for a tremendous discovery surrounding dark matter is possible over the next several years.[38] Fermi will search for evidence that dark matter is composed of weakly interacting massive particles, complementing similar experiments with the Large Hadron Collider and other underground detectors.
IBEX is already yielding new astrophysical discoveries: "No one knows what is creating the ENA (energetic neutral atoms) ribbon" along the termination shock of the solar wind, "but everyone agrees that it means the textbook picture of the heliosphere — in which the solar system's enveloping pocket filled with the solar wind's charged particles is plowing through the onrushing 'galactic wind' of the interstellar medium in the shape of a comet — is wrong."[39]
Current research
Further information: List of unsolved problems in physics
A typical event described by physics: a magnet levitating above a superconductor demonstrates the Meissner effect.
In condensed matter physics, an important unsolved theoretical problem is that of high-temperature superconductivity. Many condensed matter experiments are aiming to fabricate workable spintronics and quantum computers.
In particle physics, the first pieces of experimental evidence for physics beyond the Standard Model have begun to appear. Foremost among these are indications that neutrinos have non-zero mass. These experimental results appear to have solved the long-standing solar neutrino problem, and the physics of massive neutrinos remains an area of active theoretical and experimental research. Particle accelerators have begun probing energy scales in the TeV range, in which experimentalists are hoping to find evidence for the Higgs boson and supersymmetric particles.[40]
Theoretical attempts to unify quantum mechanics and general relativity into a single theory of quantum gravity, a program ongoing for over half a century, have not yet been decisively resolved. The current leading candidates are M-theory, superstring theory and loop quantum gravity.
Many astronomical and cosmological phenomena have yet to be satisfactorily explained, including the existence of ultra-high energy cosmic rays, the baryon asymmetry, the acceleration of the universe and the anomalous rotation rates of galaxies.
Although much progress has been made in high-energy, quantum, and astronomical physics, many everyday phenomena involving complexity, chaos, or turbulence are still poorly understood.[citation needed] Complex problems that seem like they could be solved by a clever application of dynamics and mechanics remain unsolved; examples include the formation of sandpiles, nodes in trickling water, the shape of water droplets, mechanisms of surface tension catastrophes, and self-sorting in shaken heterogeneous collections.[citation needed]
These complex phenomena have received growing attention since the 1970s for several reasons, including the availability of modern mathematical methods and computers, which enabled complex systems to be modeled in new ways. Complex physics has become part of increasingly interdisciplinary research, as exemplified by the study of turbulence in aerodynamics and the observation of pattern formation in biological systems. In 1932, Horace Lamb said:[41]I am an old man now, and when I die and go to heaven there are two matters on which I hope for enlightenment. One is quantum electrodynamics, and the other is the turbulent motion of
What is Mineral Physics?
Mineral physics is the science of materials that compose the Earth and other planets. Mineral physicists do not always study minerals or use only physics; they employ the principles and techniques from chemistry, physics, materials science and biology to address mineralogical problems and processes within planetary interiors.Why Teach Mineral Physics?
Research in mineral physics is essential in interpreting observational data from many of the disciplines in the Earth sciences, including geodynamics, seismology, geochemistry, petrology, geomagnetism, and planetary science, as well as materials science and even climate studies, as illustrated in the figure on the right (click on the image to see a larger version).All of the natural sciences devote a great deal of their focus on processes that occur on the Earth's surface. Our understanding of these processes can be enriched by insight into how the Earth's surface and atmosphere have developed and continue to evolve over time. Much of this evolution is the result of surface manifestations of deep Earth phenomena. Mineral Physics helps us understand the properties of materials that are involved in these deep Earth phenomena, which include:
Digital relief map of the North Atlantic. Image by the National Geophysical Data Center
- Propagation of seismic waves
- Earth's gravitational field
- Earth's magnetic field
- Plate tectonics
- Mantle convection
- Eruptions of kimberlites
- Volcanism
- Hot spots
- Evolution of the Earth's interior
- Release of gases from the Earth's interior into the atmosphere.
- Superconductivity
- Optical properties
- Magnetic properties
- Potential for generating, storing, conducting, and releasing energy
- Potential for information storage
- Chemical properties
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Teaching Activities Related to Mineral Physics
From the On the Cutting Edge Teaching Mineralogy, Petrology and Geochemistry collections.Elasticity and sound wave velocities
- Mineral Physics Activity Sets – J. Michael Brown and Anastasia Chopelas, University of Washington
High-pressure behavior
- Crystal Structures as Geobarometers – Kent Ratajeski, Montana State University
- Calculating Pressures and Temperatures of Petrologic Events: Geothermobarometry – Donna L. Whitney, University of Minnesota
- Progressive Metamorphism of Pelitic Rocks: A Lab Assignment to Facilitate Translation from AFM Space to P-T Space – Jane Selverstone, University of New Mexico
- Working with Electron Microprobe Data from a High Pressure Experiment - Calculating Mineral Formulas, Unit Cell Content, and Geothermometry – Brandon Schwab, Humboldt State University
- Sodium: Stony Brook's Artem Oganov Explains Discoveries - This 16-minute Youtube video explains how sodium changes its properties under pressure.
X-ray diffraction and scattering
- Single Crystal X-Ray Diffraction Tutorial – Christine Clark and Barb Dutrow, Eastern Michigan University and Louisiana State University
- X-ray Powder Diffraction (XRD) -Barbara L. Dutrow and Christine M. Clark, Louisiana State University and Eastern Michigan University
- Mineral Synthesis and X-Ray Diffraction Experiments – Dexter Perkins and Paul Sorensen, University of North Dakota
- Determination of Chemical Composition, State of Order, Molar Volume, and Density of a Monoclinic Alkali Feldspar Using X-Ray Diffraction – Guy L. Horvis, Lafayette College
- Better Living Through Minerals:X-Ray Diffraction of Household Products – Barb Dutrow, Louisiana State University
- Synthetic Alkali Halides - Dexter Perkins, University of North Dakota
- Making Solid Solutions with Alkali Halides (and Breaking them) – John Brady, Smith College
Phase transitions in minerals
- Phase Fun with Feldspars : Simple Experiments to Change Chemical Composition, State of Order, and Crystal System – Guy L. Hovis, Lafayette College
- Synthetic Alkali Halides - Dexter Perkins, University of North Dakota
- Making Solid Solutions with Alkali Halides (and Breaking them) – John Brady, Smith College
- Sodium: Stony Brook's Artem Oganov Explains Discoveries - This 16-minute Youtube video explains how sodium changes its properties under pressure.
- Stony Brook's Oganov on New Superhard Phase of Boron – This 8-minute YouTube video explains the discovery of a new superhard phase of boron, a major advance described in Nature. Led by Oganov, a research team has discovered a new phase that shows charge transfer from the B2 to the B12 clusters, which thus play the same roles as cations and anions in normal ionic salts.
Phase Equilibria and Phase Diagrams
- Teaching Phase Equilibria Tutorial from Integrating Research and Education – Dave Mogk and Dexter Perkins (editors), Montana State University and University of North Dakota
- Thermodynamics "Crash Course" by Alex Navrotsky, UC Davis, including Outline (Microsoft Word 25kB Jun16 09), and Powerpoint presentations on Fundamentals (PowerPoint 9.4MB Jun18 09), Partial Molar Qualities (PowerPoint 2.7MB Jun18 09), Complex Solid Solutions (PowerPoint 5.9MB Jun18 09), and Phase Diagrams (PowerPoint 5.3MB Jun18 09)
- Phase Equilibria - Dexter Perkins, University of North Dakota
- Plagioclase Phase Diagram - Dexter Perkins, University of North Dakota
- Crystallization and Melting of Diopside - Anorthite - Dexter Perkins, University of North Dakota
- Phase Diagrams in Vivo - Erich U. Peterson, University of Utah
- Phase Diagrams - Dexter Perkins, University of North Dakota
- Useful Phase Diagrams - John Brady, Smith College
- Phase diagrams From Kitchen Chemistry - John Brady, Smith College
- Binary Eutectic In-class Exercise (Di-An) - Allen Glazner, Univ. North Carolina
- Constructing a Two Component Phase diagram Using Experimental Data in the Hypothetical System A-B - R.K. Smith, Univ. Texas San Antonio
- Ternary System: Determination of Crystal-Liquid and Crystal-Crystal Proportions Using the Lever and Tangent Rules - R.K. Smith, Univ. Texas San Antonio
- The use of visualization and sketches of thin sections to encourage a better understanding of phase diagrams: Binary and ternary phase diagram exercises - Jennifer M. Wenner and Drew S. Coleman, University of Wisconsin Oshkosh and University of North Carolina
- Calculating a Simple Phase Diagram: Diamond=Graphite - Dexter Perkins, University of North Dakota
Defects
- From 2D to 3D: Escher Drawings, Crystallography, Crystal Chemistry, and Crystal "Defects" - Peter Buseck, Arizona State University
Hot Spots
Computer model of mantle plumes originating from the core-mantle boundary. Details
- Is Yellowstone Volcanism Formed by a Deep-Seated Mantle Plume -- Kent Ratajeski, Montana State University
- The Cretaceous Superplume -- Kent Ratajeski, Montana State University
- Testing the Fixed-Hotpsot Moving-Plate Model -- Sara Harris, University of British Columbia
- Hot Spot Lesson--Mantle Plumes -- from the ERESE project.
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Additional Mineral Physics Topics
We are interested in expanding our resource collection in the following areas. If you have a teaching activity, website, article, or course syllabus related to any of these topics, please contribute it using a form on the Mineralogy contribute a resource page.- Anelasticity (attenuation and dispersion)
- Electrical properties
- Equations of state
- Fracture and flow
- Instruments and techniques:
- Diamond-anvil, high-pressure apparatus
- Multi-anvil, high-pressure apparatus
- Magnetic properties
- Neutron diffraction and scattering
- Neutron sources
- NMR, Mossbauer spectroscopy, and other magnetic techniques
- Optical, infrared, and Raman spectroscopy
- Physical thermodynamics
- Plasticity, diffusion, and creep
- Synchrotron X-radiation sources
- Shock wave experiments
- Surfaces and interfaces
- Thermal expansivity
- Thermal properties
- Transport properties
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Instructional Modules We'd Like to See Developed!
Phase Transitions
What types (displacive, reconstructive, order-disorder)? Why are they important? Changes in crystal structure, unit cell volume results in density changes... What are the impacts--e.g. seismic structure of crust/mantle.... How can these be used to interpret Earth (e.g. structure state of alkali feldspars as thermometer; aluminosilicates in interpreting metamorphic conditions; SiO2 polymorphs, alpha, beta quartz, cristobalite, coesite....impact and deep crustal burial .... olivine-beta phase and seismic discontinuities...)Bulk Modulus
What is it, and why is it important? The bulk modulus (K) of a substance is a quantification of its resistance to uniform compression. It can be defined as the change in pressure necessary to cause a specified relative change in volume.K = -V * ∂p/∂V
where:
- V = volume
- p = pressure
Crystal defects
What are the different types of defects: omission, substitution, Frenkel; point defects, dislocations, etc.; How do these affect physical and chemical processes in Earth? Melting--application in igneous petrology; Deformation mechanisms--application in structural geology, etc....)Synchrotron Experiments
We'd like to create a "primer" on the theory and use of the X-ray Synchrotron developed as part of our project on Geochemical Instruments and Techniques. This "primer" would include information on the method, instrument components, theory of how it works, typical applications, strengths and limitations, links to other resources....Description of recent advances e.g. micro XRF and XRD, XANES and EXAFS, etc. Applications in environmental geochemistry (structure state of bad elements, sorption properties etc.)Diamond Anvil Experiments
We'd like to develop a similar "primer" on diamond anvil apparatus for our project on Geochemical Instruments and Techniques. Includes info on what is the method, instrument components, theory of how it works, typical applications, strengths and limitations, links to other resources....Description of recent advances e.g High pressure XRay experiments, etc. Barophilic microbes; Turning peanut butter into diamonds....New Frontiers (Exciting new Research Results)
What are the really "hot topics" emerging in the field of mineral physics? What is the importance and implications of discovery of post-perovskite on the structure of mantle, coupling with outer core and relation to Earth's magnetic field, electrical conductivity? We would like to encourage development of teaching activities that derive from the primary scientific literature, and demonstrate how data and data products are used to replicate or simulate authentic research results.Back to Top
Contribute a Resource
Please use the following links to contribute a mineralogy resource:- Contribute a teaching activity: problem sets, laboratory exercises, etc.
- Contribute a URL: links to URLS that contain useful information such as related webpages (e.g. facilities, government agencies, faculty course we bpages), PowerPoints, tutorials, etc.
- Contribute an article: that are recommended for class use; independent study reading, group discussions and presentations....
- Contribute a course syllabus
About this project
Developed as a collaboration between the On the Cutting Edge geoscience faculty professional development program (NSF DUE 06-18482) and the COMPRES program (NSF EAR 06-49658).Back to Top
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