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Electrical and Magnetic Properties

Electricity and magnetism are two expressions of a single force, called "electromagnetism". Two electrical properties that have important industrial and electronic applications are piezoelectricity and pyroelectricity, although these properties are not typically used in mineral identification.  These properties are shown by certain classes of minerals or synthetic crystalline materials that lack a center of symmetry.  Magnetism is an important diagnostic tool for a few minerals.  Radioactivity, or the spontaneous decay or disintegration of an unstable atomic nucleus accompanied by the emission of electromagnetic energy, can be detected in some minerals with a Geiger counter and for these minerals, it is a diagnostic property.

Smoky and Milky QuartzPiezoelectricity is the ability of a mineral or crystal to acquire opposing electrical charges on opposing surfaces when  mechanical stress (such as bending, stretching, or compression) is applied to the crystal. The piezoelectric effect is caused by the displacement of ionic charges within a crystal structure, and the magnitude of the charge generally is proportional to the amount of stress applied.  Removal of the stress reverses the effect.  This electrical charge can be converted into a voltage using a charge amplifier.

Of the minerals in the twenty crystal classes that lack a center of symmetry, only a few are piezoelectric to any significant degree.  Piezoelectricity was first discovered in quartz crystals.  This effect allows them to be used in certain sorts of radio tuners (first done in 1921, but now largely replaced by other types), in the timing mechanisms of quartz watches, and in the electronics industry.  Tourmaline, another strongly piezoelectric mineral, is used in gauges to measure transient blast pressures.

Tourmaline and CalcitePyroelectricity is the ability of a mineral or crystal to acquire opposing electrical charges on opposing surfaces as a result of heating.  Tourmaline was recognized as a distinct mineral with a highly variable composition because of  pyroelectricity.  The pyroelectric property of the tourmaline shown on the right made photographing it very difficult, because the heat of the lights that were used to illuminate it produced an electrical charge that attracted a heavy coating of dust.  The dust had to be removed before the photograph could be taken.  (quickly before more dust was attracted!)

PyrrhotiteMagnetism and electricity are closely related, and are regarded by physicists as two expressions of a single force, called "electromagnetism".  Although only minerals that are strongly attracted to a magnetic field are considered to be magnetic, all matter has some magnetic properties, even though it may be too small to be detectable.  This is because all matter is made up of moving charged particles (electrons and protons), whose motion sets up magnetic fields. 

The magnetic properties of atoms and molecules are primarily dependent on the spin of electrons in a substance.  Electrons can spin in one of two opposite directions and any two electrons in the same orbit are constrained to spin in opposing directions.  A spinning electron behaves as a small magnet and will produce a magnetic field while orbiting around the nucleus of an atom.  The opposing spins of two electrons in an orbital results in a net zero magnetic moment.  Diamagnetic substances have zero net magnetic moment because they have the same number of electrons of opposing spin.  Diamagnetic substances are actually slightly repelled by a magnetic field due to the negative charge of the electron clouds.  Quartz and calcite are diamagnetic.

A paramagnetic substance has a random arrangement of magnetic dipoles of the atoms in its structure until the material is placed within a magnetic field.  At that time the dipoles will align themselves with the external magnetic field.  Olivine and pyroxene are paramagnetic.

Ferromagnetic substances show strong magnetic attraction when subjected to a magnetic field and will remain magnetic after the removal of the magnetic field unless heated above their Curie temperatures.  Magnetism occurs because the magnetic dipoles of domains that make up a ferromagnetic substance align when in the presence of a magnetic field.   Metallic iron, nickel, cobalt, and numerous alloys of these transition metals are ferromagnetic.  Heating above the Curie temperature of a ferromagnetic substance causes the magnetic dipoles in the domains to randomly realign and the material will behave as a paramagnetic substance.  

Ferrimagnetic substances are characterized by strong permanent magnetic susceptibility caused by ionic spin moment that are antiparallel.  Magnetite and pyrrhotite are ferrimagnetic.

MetatorberniteRadioactivity is the spontaneous decay or disintegration of an unstable atomic nucleus of an atom of one element to produce one or more new nuclides and the emission of radiation (energy).  The radioactive  isotopes of potassium, strontium, thorium, uranium and samarium  (40K, 87Sr, 232Th, 238U, 235U,  247Sm) are geologically important for absolute age dating and as a diagnostic tool.  The radioactivity of some uranium- and thorium-rich minerals is great enough that it can be detected by a Geiger counter and is therefore a diagnostic property.  The radioactivity of these and other radioactive minerals may also pose a health risk.  

There are three mechanisms of radioactive decay: alpha decay, beta decay and electron capture.  Alpha decay results in the emission of an alpha particle.  The alpha particle (a) is identical to the nucleus of 4He (helium) atom and consists of two protons and two neutrons.  The decay of uranium-238 is an example of alpha decay.  Alpha decay reduces the mass number of the nucleus by four and the atomic number by two due to the loss of two protons and two neutrons from the parent isotope.

238 =>  234Th + a + g + Energy 

Beta decay results in the emission of a beta particle (b).  A beta particle is equivalent to a negatively charged electron.  The beta particle is formed through the decay of a neutral neutron particle into a positively charged proton.

87Rb => 87Sr + b- + Energy

Electron capture occurs when an orbital electron is captured by the nucleus.  The decay of potassium-40 to argon-4o occurs through electron capture.  The nuclear charge decreases by one without any significant change in mass.

40K + orbital e-  =>  40A + g + Energy


 

 

Frequently used abbreviations: NPL  Non-vertebrate Paleontology Laboratory | TNSC Texas Natural Science Center | UTDGS Department of Geological Sciences | BEG  Bureau of Economic Geology | VPL Vertebrate Paleontology Laboratory | JSG  Jackson School of Geosciences | SUPPORT | VOLUNTEER | GLOSSARY


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