| Atomic Mass | 88.90584 |
|---|---|
| Configuración de electrones | [Kr]5s24d1 |
| Estados de oxidación | +3 |
| Año Descubrido | 1794 |
| Atomic Mass | 88.90584 |
|---|---|
| Configuración de electrones | [Kr]5s24d1 |
| Estados de oxidación | +3 |
| Año Descubrido | 1794 |
| Element Name | Yttrium |
|---|---|
| Element Symbol | Y |
| InChI | InChI=1S/Y |
| InChIKey | VWQVUPCCIRVNHF-UHFFFAOYSA-N |
| Atomic Weight |
88.905 838(2) 88.90584 88.91 88.90584(2) |
|---|---|
| Electron Configuration |
[Kr]5s24d1 |
| Atomic Radius |
Van der Waals Atomic Radius : 219 pm (Van der Waals) Empirical Atomic Radius : 180pm (Empirical) Covalent Atomic Radius : 190(7) pm (Covalent) |
| Oxidation States |
+3 3, 2, 1 (a weakly basic oxide) |
| Ground Level |
2D3/2 |
| Ionization Energy |
6.217 eV 6.21726 ± 0.00010 eV |
| Electronegativity |
Pauling Scale Electronegativity : 1.22(Pauling Scale) Allen Scale Electronegativity : 1.12(Allen Scale) |
| Electron Affinity |
0.307eV -0.4eV |
| Atomic Spectra |
Lines Holdings Levels Holdings |
| Physical Description |
Solid |
| Element Classification |
Metal |
| Element Period Number |
5 |
| Element Group Number |
3 |
| Density |
4.47 grams per cubic centimeter |
| Melting Point |
1795 K (1522°C or 2772°F) 1526°C |
| Boiling Point |
3618 K (3345°C or 6053°F) 2930°C |
| Estimated Crustal Abundance |
3.3×101 milligrams per kilogram |
| Estimated Oceanic Abundance |
1.3×10-5 milligrams per liter |
The name derives from the Swedish village of Ytterby where the mineral gadolinite was found. In 1794, the Finnish chemist Johan Gadolin discovered yttrium in the mineral ytterbite, which was later renamed gadolinite for Gadolin. Gadolin originally called the element ytterbium after ytterbite. The name was subsequently shortened to yttrium, and later another element was given the name ytterbium.
Yttrium was discovered by Johan Gadolin, a Finnish chemist, while analyzing the composition of the mineral gadolinite ((Ce, La, Nd, Y)2FeBe2Si2O10) in 1789. Gadolinite, which was named for Johan Gadolin, was discovered several years earlier in a quarry near the town of Ytterby, Sweden. Today, yttrium is primarily obtained through an ion exchange process from monazite sand ((Ce, La, Th, Nd, Y)PO4), a material rich in rare earth elements.
Namded after Ytterby, a village in Sweden near Vauxholm. Yttria earth containing yttrium was discovered by Gadolin in 1794. Ytterby is the site of a quarry which yielded many unusual minerals containing rare earths and other elements. This small town, near Stockholm, bears the honor of giving names to erbium, terbium, and ytterbium as well as yttrium.
In 1843 Mosander showed that yttira could be resolved into the oxides (or earths) of three elements. The name yttria was reserved for the most basic one; the others were named erbia and terbia.
| Year | Atomic Weight (uncertainty) [u] | Reference |
|---|---|---|
| 2021 | 88.905 838(2) | https://doi.org/10.1515/pac-2019-0603 |
| 2017 | 88.905 84(1) | https://doi.org/10.1515/pac-2019-0603 |
| 2013 | 88.905 84(2) | https://doi.org/10.1515/pac-2015-0305 |
| 1985 | 88.905 85(2) | https://doi.org/10.1351/pac198658121677 |
| 1969 | 88.9059(1) | https://doi.org/10.1351/pac197021010091 |
| 1961 | 88.905 | https://doi.org/10.1021/ja00881a001 |
| 1931 | 88.92 | https://doi.org/10.1039/JR9310001617 |
| 1925 | 88.9 | https://doi.org/10.1039/CT9252700913 |
| 1920 | 89.33 | https://doi.org/10.1021/ja02233a600 |
| 1903 | 89.0 | https://doi.org/10.1021/ja02003a001 |
| 1902 | 89 | https://doi.org/10.1007/BF01370337 |
| Year | Isotope | Abundance (uncertainty) | Reference |
|---|
| 1975, 89Y, 1, doi:10.1351/pac197647010075 |
Yttrium has a silver-metallic luster and is relatively stable in air. Turnings of the metal, however, ignite in air if their temperature exceeds 400°C. Finely divided yttrium is very unstable in air.
Although metallic yttrium is not widely used, several of its compounds are. Yttrium oxide (Y2O3) and yttrium orthovanadate (YVO4) are both combined with europium to produce the red phosphor used in color televisions. Garnets made from yttrium and iron (Y3Fe5O12) are used as microwave filters in microwave communications equipment. Garnets made from yttrium and aluminum (Y3Al5O12) are used in jewelry as simulated diamond.
Yttrium oxide is one of the most important compounds of yttrium and accounts for the largest use. It is widely used in making YVO4 europium, and Y2O3 europium phosphors to give the red color in color television tubes. Hundreds of thousands of pounds are now used in this application.
Yttrium oxide also is used to produce yttrium-iron-garnets, which are very effective microwave filters.
Yttrium iron, aluminum, and gadolinium garnets, with formulas such as Y3Fe5O12 and Y3Al5O12, have interesting magnetic properties. Yttrium iron garnet is also exceptionally efficient as both a transmitter and transducer of acoustic energy. Yttrium aluminum garnet, with a hardness of 8.5, is also finding use as a gemstone (simulated diamond).
Small amounts of yttrium (0.1 to 0.2%) can be used to reduce the grain size in chromium, molybdenum, zirconium, and titanium, and to increase strength of aluminum and magnesium alloys.
Alloys with other useful properties can be obtained by using yttrium as an additive. The metal can be used as a deoxidizer for vanadium and other nonferrous metals. The metal has a low cross section for nuclear capture. 90Y, one of the isotopes of yttrium, exists in equilibrium with its parent 90Sr, a product of nuclear explosions. Yttrium has been considered for use as a nodulizer for producing nodular cast iron, in which the graphite forms compact nodules instead of the usual flakes. Such iron has increased ductility.
Yttrium also can be used in laser systems and as a catalyst for ethylene polymerization reactions.
It also has potential use in ceramic and glass formulas, as the oxide has a high melting point and imparts shock resistance and low expansion characteristics to glass.
Yttrium occurs in nearly all of the rare-earth minerals. Analysis of lunar rock samples obtained during the Apollo missions show a relatively high yttrium content.
It is recovered commercially from monazite sand, which contains about 3%, and from bastnasite, which contains about 0.2%. Wohler obtained the impure element in 1828 by reduction of the anhydrous chloride with potassium. The metal is now produced commercially by reduction of the fluoride with calcium metal. It can also be prepared by other techniques.
See more information at the Yttrium compound page.
| CID | Name | Formula | SMILES | Molecular Weight |
|---|---|---|---|---|
| 23993 | yttrium | Y | [Y] | 88.90584 |
| 104760 | yttrium-90 | Y | [90Y] | 89.907142 |
| 168049 | yttrium(3+) | Y+3 | [Y+3] | 88.90584 |
| 104964 | yttrium-91 | Y | [91Y] | 90.90730 |
| 105173 | yttrium-88 | Y | [88Y] | 87.90950 |
| 177472 | yttrium-86 | Y | [86Y] | 85.9149 |
| 178178 | yttrium-87 | Y | [87Y] | 86.91088 |
| 9877337 | yttrium-89 | Y | [89Y] | 88.905838 |
| 167219 | yttrium-93 | Y | [93Y] | 92.9096 |
| 167364 | yttrium-92 | Y | [92Y] | 91.90895 |
| 177601 | yttrium-95 | Y | [95Y] | 94.91282 |
| 181089 | yttrium-94 | Y | [94Y] | 93.91159 |
| 42624151 | yttrium-90(3+) | Y+3 | [90Y+3] | 89.907142 |
| 9877336 | yttrium-89(3+) | Y+3 | [89Y+3] | 88.905838 |
| 42628832 | yttrium-99 | Y | [99Y] | 98.92416 |
| 46830028 | yttrium-86(3+) | Y+3 | [86Y+3] | 85.9149 |
| Stable Isotope Count | 1 |
|---|---|
| Summary | Natural yttrium contains one isotope, 89Y. Nineteen other unstable isotopes have been characterized. |
Carbon nanotubes (CNT), which are nano-scaled carbon tubes, are being examined in nanobiotechnology research studies because it has been discovered that CNTs labeled with 86Y (with a half-life of 0.6 day) are soluble when they are injected into mice. This discovery was made after mice were given an intravenous or intraperitoneal (directly into a body cavity) injection with the 86Y CNT and then were examined using positron emission tomography (PET) scans to observe whether the 86Y had been flushed from their systems. The PET scan determined that accumulation of 86Y occurred in the liver, kidney, and spleen with very rapid blood clearance. This has broad implications for developing drug treatments [303]. Radiomicrosphere therapy (RT) that uses 90Y (with a half-life of 64 h) microspheres is a proven therapy that helps treat hepatic (liver) cancer (Fig. IUPAC.39.1) [304]. 90Y is also used in radiosynovectomy to reduce joint pain [305].
![Fig. IUPAC.39.1: Ultrapure ⁹⁰Y. (Photo Source: Pacific Northwest National Laboratory) [306].](https://pubchem.ncbi.nlm.nih.gov/images/iupac/j_pac-2015-0703_fig_059.jpg)
| Isotope | Atomic Mass (uncertainty) [u] | Abundance (uncertainty) |
|---|---|---|
| 89Y | 88.905 838(2) | 1 |
| Isotope | Atomic Mass (uncertainty) [u] | Abundance (uncertainty) |
|---|---|---|
| 89Y | 88.9058403(24) | 1 |
| Nuclide | Atomic Mass and Uncertainty [u] | Half Life and Uncertainty | Discovery Year | Decay Modes, Intensities and Uncertainties [%] |
|---|---|---|---|---|
| 75Y | 74.965840 ± 0.000322 [Estimated] | 100 us [Estimated] | β+ ?; β+p ?; p ? | |
| 76Y | 75.958937 ± 0.000322 [Estimated] | 28 ms ± 9 | 2001 | β+ ?; p ?; β+p ? |
| 77Y | 76.950146 ± 0.000218 [Estimated] | 63 ms ± 17 | 1999 | β+≈100%; β+p ?; p ? |
| 78Y | 77.943990 ± 0.00032 [Estimated] | 54 ms ± 5 | 1992 | β+=100%; β+p ? |
| 78Ym | 77.943990 ± 0.00032 [Estimated] | 5.8 s ± 0.6 | 1998 | β+=100%; β+p ? |
| 79Y | 78.937946000 ± 0.000086 | 14.8 s ± 0.6 | 1992 | β+=100% |
| 80Y | 79.934354750 ± 0.000006701 | 30.1 s ± 0.5 | 1981 | β+=100% |
| 80Ym | 79.934354750 ± 0.000006701 | 4.8 s ± 0.3 | 1998 | IT=81±0.2%; β+=19±0.2% |
| 80Yn | 79.934354750 ± 0.000006701 | 4.7 us ± 0.3 | 1997 | IT=100% |
| 81Y | 80.929454283 ± 0.000005802 | 70.4 s ± 1.0 | 1981 | β+=100% |
| 82Y | 81.926930189 ± 0.000005902 | 8.30 s ± 0.20 | 1980 | β+=100% |
| 82Ym | 81.926930189 ± 0.000005902 | 258 ns ± 22 | 1994 | IT=100% |
| 82Yn | 81.926930189 ± 0.000005902 | 148 ns ± 6 | 1994 | IT=100% |
| 83Y | 82.922484026 ± 0.00002 | 7.08 m ± 0.08 | 1962 | β+=100% |
| 83Ym | 82.922484026 ± 0.00002 | 2.85 m ± 0.02 | 1972 | β+=60±0.5%; IT=40±0.5% |
| 84Y | 83.920671060 ± 0.000004615 | 39.5 m ± 0.8 | 1962 | β+=100% |
| 84Ym | 83.920671060 ± 0.000004615 | 4.6 s ± 0.2 | 1976 | β+=100% |
| 84Yn | 83.920671060 ± 0.000004615 | 292 ns ± 10 | 2005 | IT=100% |
| 85Y | 84.916433039 ± 0.00002036 | 2.68 h ± 0.05 | 1952 | β+=100% |
| 85Ym | 84.916433039 ± 0.00002036 | 4.86 h ± 0.20 | 1952 | β+≈100%; IT ? |
| 85Yn | 84.916433039 ± 0.00002036 | 178 ns ± 7 | 1977 | IT=100% |
| 86Y | 85.914886095 ± 0.000015182 | 14.74 h ± 0.02 | 1951 | β+=100% |
| 86Ym | 85.914886095 ± 0.000015182 | 47.4 m ± 0.4 | 1962 | IT=99.31±0.4%; β+=0.69±0.4% |
| 86Yn | 85.914886095 ± 0.000015182 | 125.3 ns ± 5.5 | 2000 | IT=100% |
| 87Y | 86.910876100 ± 0.00000121 | 79.8 h ± 0.3 | 1940 | β+=100% |
| 87Ym | 86.910876100 ± 0.00000121 | 13.37 h ± 0.03 | 1940 | IT=98.43±1.1%; β+=1.57±1.1% |
| 88Y | 87.909501274 ± 0.00000161 | 106.629 d ± 0.024 | 1948 | β+=100% |
| 88Ym | 87.909501274 ± 0.00000161 | 301 us ± 3 | 1955 | IT=100% |
| 88Yn | 87.909501274 ± 0.00000161 | 13.98 ms ± 0.17 | 1962 | IT=100% |
| 89Y | 88.905838156 ± 0.000000363 | Stable | 1923 | IS=100% |
| 89Ym | 88.905838156 ± 0.000000363 | 15.663 s ± 0.005 | 1951 | IT=100% |
| 90Y | 89.907141749 ± 0.000000379 | 64.05 h ± 0.05 | 1937 | β-=100% |
| 90Ym | 89.907141749 ± 0.000000379 | 3.226 h ± 0.011 | 1961 | IT=99.9982±0.2%; β-=0.0018±0.2% |
| 91Y | 90.907298048 ± 0.000001978 | 58.51 d ± 0.06 | 1943 | β-=100% |
| 91Ym | 90.907298048 ± 0.000001978 | 49.71 m ± 0.04 | 1953 | IT≈100%; β- ? |
| 92Y | 91.908945752 ± 0.000009798 | 3.54 h ± 0.01 | 1940 | β-=100% |
| 92Ym | 91.908945752 ± 0.000009798 | 3.7 us ± 0.5 | 2009 | IT=100% |
| 93Y | 92.909578434 ± 0.000011259 | 10.18 h ± 0.08 | 1948 | β-=100% |
| 93Ym | 92.909578434 ± 0.000011259 | 820 ms ± 40 | 1974 | IT=100% |
| 94Y | 93.911592062 ± 0.000006849 | 18.7 m ± 0.1 | 1948 | β-=100% |
| 94Ym | 93.911592062 ± 0.000006849 | 1.304 us ± 0.012 | 1999 | IT=100% |
| 95Y | 94.912819697 ± 0.000007277 | 10.3 m ± 0.1 | 1959 | β-=100% |
| 95Ym | 94.912819697 ± 0.000007277 | 48.6 us ± 0.5 | 1981 | IT=100% |
| 96Y | 95.915909305 ± 0.000006521 | 5.34 s ± 0.05 | 1975 | β-=100% |
| 96Ym | 95.915909305 ± 0.000006521 | 9.6 s ± 0.2 | 1974 | β-=100% |
| 96Yn | 95.915909305 ± 0.000006521 | 181 ns ± 9 | 2017 | IT=100% |
| 97Y | 96.918286702 ± 0.000007201 | 3.75 s ± 0.03 | 1970 | β-=100%; β-n=0.055±0.4% |
| 97Ym | 96.918286702 ± 0.000007201 | 1.17 s ± 0.03 | 1970 | β->99.3%; IT<0.7%; β-n=0.11±0.3% |
| 97Yn | 96.918286702 ± 0.000007201 | 142 ms ± 8 | 1986 | IT=94.8±0.9%; β-=5.2±0.9% |
| 98Y | 97.922394841 ± 0.000008501 | 548 ms ± 2 | 1970 | β-=100%; β-n=0.33±0.3% |
| 98Ym | 97.922394841 ± 0.000008501 | 615 ns ± 8 | 1972 | IT=100% |
| 98Yn | 97.922394841 ± 0.000008501 | 2.32 s ± 0.08 | 1977 | β-≈100%; IT ?; β-n=3.44±9.5% |
| 98Yp | 97.922394841 ± 0.000008501 | 6.90 us ± 0.054 | 1970 | IT=100% |
| 98Yq | 97.922394841 ± 0.000008501 | 180 ns ± 7 | 2017 | IT=100% |
| 98Yr | 97.922394841 ± 0.000008501 | 450 ns ± 150 | 2017 | IT=100% |
| 98Yx | 97.922394841 ± 0.000008501 | 762 ns ± 14 | 1972 | IT=100% |
| 99Y | 98.924160839 ± 0.000007101 | 1.484 s ± 0.007 | 1975 | β-=100%; β-n=1.77±1.9% |
| 99Ym | 98.924160839 ± 0.000007101 | 8.2 us ± 0.4 | 1985 | IT=100% |
| 100Y | 99.927727678 ± 0.000012 | 940 ms ± 30 | 1977 | β-=100%; β-n ? |
| 100Ym | 99.927727678 ± 0.000012 | 727 ms ± 6 | 1977 | β-=100%; β-n=1.08±0.6% |
| 101Y | 100.930160817 ± 0.000007601 | 426 ms ± 20 | 1983 | β-=100%; β-n=2.3±0.8% |
| 101Ym | 100.930160817 ± 0.000007601 | 870 ns ± 90 | 2009 | IT=100% |
| 102Y | 101.934328471 ± 0.000004381 | 360 ms ± 40 | 1980 | β-=100%; β-n<2.6% |
| 102Ym | 101.934328471 ± 0.000004381 | 300 ms ± 100 | 1983 | β-=100%; β-n<2.6%; IT ? |
| 103Y | 102.937243796 ± 0.000012029 | 239 ms ± 12 | 1994 | β-=100%; β-n=8.0±1.7% |
| 104Y | 103.941943 ± 0.000215 [Estimated] | 197 ms ± 4 | 1994 | β-=100%; β-n=34±1%; β-2n ? |
| 105Y | 104.945711 ± 0.000429 [Estimated] | 95 ms ± 9 | 1994 | β-=100%; β-n<82%; β-2n ? |
| 106Y | 105.950842 ± 0.000537 [Estimated] | 75 ms ± 6 | 1997 | β-=100%; β-n ?; β-2n ? |
| 107Y | 106.954943 ± 0.000537 [Estimated] | 33.5 ms ± 0.3 | 1997 | β-=100%; β-n ?; β-2n ? |
| 108Y | 107.960515 ± 0.000644 [Estimated] | 30 ms ± 5 | 2010 | β-=100%; β-n ?; β-2n ? |
| 109Y | 108.965131 ± 0.000751 [Estimated] | 25 ms ± 5 | 2010 | β-=100%; β-n ?; β-2n ? |
