Minerals/Metals/Alkaline earths

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This is a visual image of a forsterite crystal. Credit: Azuncha.

The alkaline earth metals are the elements in Group 2 of the Periodic Table: beryllium (Be), magnesium (Mg), calcium (Ca), strontium (Sr), barium (Ba), and radium (Ra).

Their minerals usually contain more than 25 atomic % of these elements.

Berylliums[edit]

This is a beryllium-chromium phase diagram. Credit: M. Venkatraman and J.P. Neumann.

Beryllium occurs in a hexgonal close-packed (hcp) crystal structure at room temperature (α-Be).

As indicated in the phase diagram on the left beryllium occurs as (β-Be) which is bcc at higher temperatures up to melting.

Native beryllium is not known to occur on the surface of the Earth, but may eventually be found among beryllium-bearing minerals in small amounts.

Bromellites[edit]

Agregate of large cm-size transparent, colourless and slightly yellowish crystals of bromellite cemented by white, granular, sugar-like phenakite masse. Credit: Pavel M. Kartashov.{{free media}}

Bromellite is BeO, with 50 at % beryllium.[1]

Magnesiums[edit]

This portion of the iron-magnesium phase diagram is concentrated on the magnesium-rich end. Credit: A.A. Nayeb-Hashemi, J.B. Clark and L.J. Swartzendruber.

Magnesium has a hcp structure from room temperature up to melting. No other phases occur as is shown in the magnesium-end of the iron-magnesium phase diagram on the left.

Native magnesium is unlikely to occur on the surface of the Earth and is not known to occur.

Chloromagnesites[edit]

Chloromagnesite, or chlormagnesite, has the formula MgCl2, with 33.3 at % magnesium.[1]

Forsterites[edit]

Forsterite is the big tabular and colorless crystal on sanidine (little colorless crystals). Credit: Fred Kruijen.

Mg2SiO4 is the formula for forsterite, with 28.6 at % magnesium.[1]

Forsterite is a member of the olivine group of minerals.[1]

Calciums[edit]

This is an Aluminum-Calcium phase diagram. Credit: The ESA IMPRESS Team.

Calcium has a face-centered cubic (fcc) crystal structure at room temperature.

As shown in the phase diagram on the left, it does not change structure up to melting.

Native calcium is not known to occur on the surface of the Earth.

Fluorites[edit]

Violet fluorite on feldspar is from Strzegom, a rare locality for fluorites. Credit: Spirifer Minerals.

Fluorite has the formula CaF2 with 33.3 at % calcium.[1] Fluorites are also halogen minerals.

Bredigites[edit]

Bredigite is α-Ca2SiO4, with 28.5 at % calcium.[1]

γ-dicalcium silicates[edit]

γ-dicalcium silicate has the formula γ-Ca2SiO4, with 28.5 at % calcium.[1]

Strontiums[edit]

This is a magnesium-strontium phase diagram. Credit: A.A. Nayeb-Hashemi and J.B. Clark.

Strontium at room temperature crystallizes in a fcc structure (α-Sr).

According to the phase diagram on the left, α-Sr transforms to γ-Sr (bcc) at 547°C.

Native strontium does not appear to occur on the surface of the Earth.

Bariums[edit]

This is a pressure-temperature phase diagram for barium. Credit: David A. Young, ERDA.

Barium is bcc (α-Ba) at room temperature as the phase diagram on the left indicates. It does change to an hcp structure at high pressures and temperatures.

Native barium is not known to occur on the surface of the Earth.

Radiums[edit]

"Solid radium is bcc at room temperature. Radium melts at 973 K.63"[2]

Hypotheses[edit]

  1. Native alkaline earths may require very arid and reducing environments to occur.

See also[edit]

References[edit]

  1. 1.0 1.1 1.2 1.3 1.4 1.5 1.6 Willard Lincoln Roberts, George Robert Rapp, Jr., and Julius Weber (1974). Encyclopedia of Minerals. 450 West 33rd Street, New York, New York 10001 USA: Van Nostrand Reinhold Company. p. 693. ISBN 0-442-26820-3. |access-date= requires |url= (help)CS1 maint: Multiple names: authors list (link)
  2. David A. Young (11 September 1975). Phase Diagrams of the Elements (PDF). University of California, Livermore, California USA: Lawrence Livermore Laboratory. p. 70. Retrieved 2015-08-26.

External links[edit]