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VOOZH | about |
| General Properties | |
|---|---|
| Symbol: | La |
| Atomic Number: | 57 |
| Standard atomic weight (Ar): | 138.90547(7) |
| Electron configuration: | [Xe] 5d1 6s2 |
| Photos | ||
|---|---|---|
1.5 grams pure lanthanum |
| Atomic Properties | |
|---|---|
| Electronegativity (Pauling scale): | 1.1 |
| Atomic Radius: | 169 pm |
| Ionic Radius: | 103.2 pm (+3) |
| 1st Ionization energy: | 538 kJ/mol |
| 1st Electron affinity: | -48 kJ/mol |
| Oxidation States: | 2,3 |
| Physical Properties | |
|---|---|
| Standard State: | solid |
| Bonding Type: | metallic |
| Melting Point: | 1193 K |
| Boiling Point: | 3737 K |
| Density: | 6.15 g/cm3 |
| Metal/Non-Metal: | lanthanoid |
| Main isotopes of Lanthanum | ||||
|---|---|---|---|---|
| Isotope | % in Nature | Half Life | Decay type | Decay product |
| 137La | synthetic | 6×104y | ε | 137Ba |
| 138La | 0.090% | 1.05×1011y | ε | 138Ba |
| β− | 138Ce | |||
| 139La | 99.910% | - | Spontaneous fission ? | |
| Main ions of Lanthanum | ||||
|---|---|---|---|---|
| Name | Ion | Example minerals | ||
| lanthanum(II) | La2+ | |||
| lanthanum(III) | La3+ | Monazite-(La), Rhabdophane-(La) | ||
| Other Information | |
|---|---|
| Year Discovered: | 1838 |
| Discovered By: | |
| Named For: | From Greek: lanthanein - "to lie (hidden)" |
| CPK color coding: | #70D4FF |
| External Links: | WikipediaWebElementsLos Alamos National LaboratoryTheodore Gray's PeriodicTable.com |
| Simple Compounds and Mineral Names | ||||
|---|---|---|---|---|
| Sulfides | lanthanum sulphide | LaS | +2 | |
| dilanthanum trisulphide | La2S3 | +3 | ||
| Selenides | lanthanum selenide | LaSe | +2 | |
| Tellurides | lanthanum telluride | LaTe | +2 | |
| Hydrides | lanthanum dihydride | LaH2 | +2 | |
| lanthanum trihydride | LaH3 | +3 | ||
| Fluorides | lanthanum trifluoride | LaF3 | +3 | Fluocerite-(La) |
| Chlorides | lanthanum trichloride trihydrate | LaCl3 · 3H2O | +3 | |
| lanthanum trichloride | LaCl3 | +3 | ||
| Bromides | lanthanum tribromide | LaBr3 | +3 | |
| Iodides | lanthanum triiodide | LaI3 | +3 | |
| Oxides | dilanthanum trioxide | La2O3 | +3 | |
| Carbonates | lanthanum carbonate | La2(CO3)3 | +3 | |
| lanthanum carbonate octahydrate | La2(CO3)3 · 8H2O | +3 | Lanthanite-(La) | |
| basic lanthanum carbonate | LaCO3OH | +3 | , Kozoite-(La) | |
| Phosphates | lanthanum phosphate | LaPO4 | +3 | Monazite-(La) |
| lanthanum phosphate monohydrate | LaPO4 · H2O | +3 | Rhabdophane-(La) | |
| Vanadates | lanthanum vanadate | LaVO4 | +3 | Wakefieldite-(La) |
| Mineral Diversity of Lanthanum | |
|---|---|
| 3. Halides | 2 valid mineral species |
| 4. Oxides | 3 valid mineral species |
| 5. Carbonates | 14 valid mineral species |
| 8. Phosphates, Arsenates, Vanadates | 12 valid mineral species |
| 9. Silicates | 28 valid mineral species |
| Total: | 59 valid species containing essential Lanthanum |
| Minerals with the greatest weight % of Lanthanum | ||
|---|---|---|
| Håleniusite-(La) | (La,Ce)OF | 79.88 % |
| Fluocerite-(La) | LaF3 | 70.91 % |
| Kozoite-(La) | La(CO3)(OH) | 64.33 % |
| Hydroxylbastnäsite-(La) | (La,Nd,Ce)(CO3)(OH,F) | 64.33 % |
| Bastnäsite-(La) | La(CO3)F | 63.74 % |
| Percleveite-(La) | La2Si2O7 | 62.29 % |
| Monazite-(La) | La(PO4) | 59.39 % |
| Rhabdophane-(La) | La(PO4)·H2O | 55.14 % |
| Törnebohmite-(La) | La2Al(SiO4)2(OH) | 54.91 % |
| Wakefieldite-(La) | La(VO4) | 54.72 % |
| Geochemistry of Lanthanum | |
|---|---|
| Goldschmidt classification: | Lithophile |
| La3+ was one of the ions least depleted from the mantle in the formation of the crust. | |
| La3+ is enriched in Ca-Al-rich inclusions in meteorites relative to the composition of the solar system. | |
| La3+ is concentrated in residual soils and sediments (less certainty.) | |
| Elemental Abundance for Lanthanum | ||
|---|---|---|
| Crust (CRC Handbook) | 3.9 x 10-5 | mass fraction, kg/kg |
| Crust (Kaye & Laby) | 5.0 x 10-5 | mass fraction, kg/kg |
| Crust (Greenwood) | 3.5 x 10-5 | mass fraction, kg/kg |
| Crust (Ahrens/Taylor) | 1.6000 x 10-5 | mass fraction, kg/kg |
| Crust (Ahrens/Wänke) | 2.9000 x 10-5 | mass fraction, kg/kg |
| Crust (Ahrens/Weaver) | 2.8000 x 10-5 | mass fraction, kg/kg |
| Upper Crust (Ahrens/Taylor) | 3.0000 x 10-5 | mass fraction, kg/kg |
| Upper Crust (Ahrens/Shaw) | 3.200 x 10-6 | mass fraction, kg/kg |
| Sea Water (CRC Handbook) | 3.4 x 10-12 | mass per volume fraction, kg/L |
| Sea Water (Kaye & Laby) | 3.4 x 10-12 | mass per volume fraction, kg/L |
| The Sun (Kaye & Laby) | 5.0 x 10-7 | atom mole fraction relative to Si=1 |
| Solar System (Kaye & Laby) | 4.4 x 10-7 | atom mole fraction relative to Si=1 |
| Solar System (Ahrens) | 4.46 x 10-7 (2.0%) | atom mole fraction relative to Si=1 (% uncertainty) |
| Element association of Lanthanum in the Mineral World | |||
|---|---|---|---|
| This table compares the known valid mineral species listed listed with Lanthanum and the other elements listed based on the official IMA formula. Note that unlike other sections on this page this includes non-essential elements. The first data column contains the total number of minerals listed with Lanthanum and the element listed for that row. The second data column lists this number as a percentage of all minerals listed with Lanthanum. The final data column compares this percentage against the percentage of all minerals that contain the element listed in each row. Click on a heading to sort. |
| Periodic Table | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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Default Categories CPK Electronegativity Atomic Radius Lowest Oxidation Highest Oxidation Crustal Abundance Goldschmidt Mineral Species Minerals with La Relative Frequency | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| Barium << Lanthanum >> Cerium |
| Most widespread minerals containing Lanthanum |
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| This list of minerals containing Lanthanum is built from the mindat.org locality database. This is based on the number of localities entered for mineral species and is therefore slanted towards minerals interesting to collectors with less coverage of common rock-forming-minerals so it does not give an undistorted distribution of Lanthanum mineral species. It is more useful when comparing rare species rather than common species. |
| Name | Formula | Crystal System | Mindat Localities |
|---|---|---|---|
| Monazite-(La) | La(PO4) | Monoclinic | 63 |
| Agardite-(La) | LaCu6(AsO4)3(OH)6 · 3H2O | Hexagonal | 42 |
| Bastnäsite-(La) | La(CO3)F | Hexagonal | 40 |
| Allanite-(La) | (CaLa)(AlAlFe2+)O[Si2O7][SiO4](OH) | Monoclinic | 33 |
| Davidite-(La) | La(Y,U)Fe2(Ti,Fe,Cr,V)18(O,OH,F)38 | Trigonal | 33 |
| Rhabdophane-(La) | La(PO4) · H2O | Hexagonal | 28 |
| Ancylite-(La) | LaSr(CO3)2(OH) · H2O | Orthorhombic | 27 |
| Lanthanite-(La) | La2(CO3)3 · 8H2O | Orthorhombic | 16 |
| Florencite-(La) | LaAl3(PO4)2(OH)6 | Trigonal | 15 |
| Hydroxylbastnäsite-(La) | (La,Nd,Ce)(CO3)(OH,F) | Hexagonal | 11 |
| Photos |
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| Localities with greatest number of different Lanthanum mineral species |
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