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  2. Alkaline earth metal - Wikipedia

    en.wikipedia.org/wiki/Alkaline_earth_metal

    The heavier alkaline earth metals react more vigorously than the lighter ones. [2] The alkaline earth metals have the second-lowest first ionization energies in their respective periods of the periodic table [4] because of their somewhat low effective nuclear charges and the ability to attain a full outer shell configuration by losing just two ...

  3. Rare-earth mineral - Wikipedia

    en.wikipedia.org/wiki/Rare-earth_mineral

    [2] [3] Rare earth minerals are rare because rare earth elements have unique geochemical properties that prevent them from easily forming minerals, [4] and are therefore not normally found in deposits large or concentrated enough for mining. [4] This is the reason they are called "rare" earths.

  4. Alkaline earth octacarbonyl complex - Wikipedia

    en.wikipedia.org/wiki/Alkaline_earth_octa...

    Since full saturation of the occupied valence orbitals to form a closed shell species requires a total of 20 electrons, the magic number 20 is fulfilled. The resulting complex has the formula: [M(CO) 8] q, where M is either a transition metal or alkaline earth metal and q is the charge of the ion. For all alkaline earth metals, q is -2.

  5. Category:Alkaline earth metals - Wikipedia

    en.wikipedia.org/wiki/Category:Alkaline_earth_metals

    Pages in category "Alkaline earth metals" The following 12 pages are in this category, out of 12 total. This list may not reflect recent changes. ...

  6. Radium - Wikipedia

    en.wikipedia.org/wiki/Radium

    Because of its relative longevity, 226 Ra is the most common isotope of the element, making up about one part per trillion of the Earth's crust; essentially all natural radium is 226 Ra. [29] Thus, radium is found in tiny quantities in the uranium ore uraninite and various other uranium minerals, and in even tinier quantities in thorium minerals.

  7. Earth (historical chemistry) - Wikipedia

    en.wikipedia.org/wiki/Earth_(historical_chemistry)

    These rare-earth oxides are used as tracers to determine which parts of a watershed are eroding. Clockwise from top center: praseodymium, cerium, lanthanum, neodymium, samarium, and gadolinium. Earths were defined by the Ancient Greeks as "materials that could not be changed further by the sources of heat then available". [1]

  8. Rare-earth element - Wikipedia

    en.wikipedia.org/wiki/Rare-earth_element

    Scandium and yttrium are considered rare-earth elements because they tend to occur in the same ore deposits as the lanthanides and exhibit similar chemical properties, but have different electrical and magnetic properties. [2] [3] The term 'rare-earth' is a misnomer because they are not actually scarce, although historically it took a long time ...

  9. Organometallic chemistry - Wikipedia

    en.wikipedia.org/wiki/Organometallic_chemistry

    Organometallic chemistry is the study of organometallic compounds, chemical compounds containing at least one chemical bond between a carbon atom of an organic molecule and a metal, including alkali, alkaline earth, and transition metals, and sometimes broadened to include metalloids like boron, silicon, and selenium, as well.