Erbium: the essentials
pure erbium metal is soft and malleable and has a bright, silvery, metallic lustre. As with other rare-earth metals, its properties depend to a certain extent on impurities present. The metal is fairly stable in air and does not oxidise as rapidly as some of the other rare-earth metals.
Erbium was discovered by Carl G. Mosander at 1842 in Sweden. Origin of
name: named after the village of "Ytterby" near Vaxholm in
Sweden
In 1842 Gustav Mosander
separated "yttria", found in the mineral gadolinite, into three fractions
which he called yttria, erbia, and terbia. The names erbia and terbia became
confused in this early period. After 1860, Mosander's terbia was known as
erbia, and after 1877, the earlier known erbia became terbia. The erbia of
this period was later shown to consist of five oxides, now known as erbia,
scandia, holmia, thulia and ytterbia. Klemm and Bommer first produced
reasonably pure erbium metal in 1934 by reducing the anhydrous chloride with
potassium vapour.
Table: basic information about and classifications of erbium.
- Name: Erbium
- Symbol: Er
- Atomic number: 68
- Atomic weight: 167.259 (3)
- Standard state: solid at 298 K
- CAS Registry ID: 7440-52-0
|
- Group in periodic table:
- Group name: Lanthanoid
- Period in periodic table: 6 (lanthanoid)
- Block in periodic table: f-block
- Colour: silvery white
- Classification: Metallic
|

This sample is from The Elements Collection, an attractive and safely packaged collection of the 92 naturally occurring elements that is available for sale.
Isolation
erbium metal is available commercially so it is not normally necessary to make it in the laboratory, which is just as well as it is difficult to isolate as the pure metal. This is largely because of the way it is found in nature. The lanthanoids are found in nature in a number of minerals. The most important are xenotime, monazite, and bastnaesite. The first two are orthophosphate minerals LnPO4 (Ln deonotes a mixture of all the lanthanoids except promethium which is vanishingly rare) and the third is a fluoride carbonate LnCO3F. Lanthanoids with even atomic numbers are more common. The most comon lanthanoids in these minerals are, in order, cerium, lanthanum, neodymium, and praseodymium. Monazite also contains thorium and ytrrium which makes handling difficult since thorium and its decomposition products are radioactive.
For many purposes it is not particularly necessary to separate the metals, but if separation into individual metals is required, the process is complex. Initially, the metals are extracted as salts from the ores by extraction with sulphuric acid (H2SO4), hydrochloric acid (HCl), and sodium hydroxide (NaOH). Modern purification techniques for these lanthanoid salt mixtures are ingenious and involve selective complexation techniques, solvent extractions, and ion exchange chromatography.
Pure erbium is available through the reduction of ErF3 with calcium metal.
2ErF3 + 3Ca → 2Er + 3CaF2
This would work for the other calcium halides as well but the product CaF2 is easier to handle under the reaction conditions (heat to 50°C above the melting point of the element in an argon atmosphere). Excess calcium is removed from the reaction mixture under vacuum.
Neutral radii
The size of neutral atoms depends upon the way in which
the measurement is made and the environment. Follow the appropriate
hyperlinks for definitions of each radius type. The term "atomic radius" is
not particularly helpful although its use is widespread. The problem is its
meaning, which is clearly very different in different sources and books. Two
values are given here, one is based upon calculations and the other upon
observation - follow the appropriate link for further details.
- Atomic radius (empirical): 175 pm
- Atomic radius (calculated): 226 pm
- Covalent radius (2008 values): 189 pm
Ionic radii
This table gives some ionic radii. In this table,
geometry refers to the arrangment of the ion's nearest neighbours. Size
does depend upon geometry and environment. For electronic configurations,
where it matters, the values given for octahedral species are low spin
unless stated to be high spin. The terms low spin and high spin
refer to the electronic configurations of particular geomtries of certain
d-block metal ions. Further information is available in inorganic
chemistry textbooks, usually at Level 1 or First Year University level. For
definitions of ionic radius and further information, follow the hypertext
link.
| Ion |
Coordination type |
Radius / pm |
| Er(III) |
6-coordinate, octahedral |
103.0 |
| Er(III) |
8-coordinate |
114.4 |
The electron affinity of erbium is 50 kJ mol-1.
Ionisation Energies
This section includes ionisation energies of erbium.
| Ionisation energy number |
Enthalpy /kJ mol-1 |
| 1st |
589.3 |
| 2nd |
1150 |
| 3rd |
2194 |
| 4th |
4120 |
Electronic configuration
The following represents the electronic configuration and
its associated term symbol for the ground state neutral gaseous atom.
The configuration associated with erbium in its compounds is not necessarily
the same.
- Ground state electron configuration: [Xe].4f12.6s2
- Shell structure: 2.8.18.30.8.2
- Term symbol: 3H6
Reaction of erbium with air
Erbium metal tarnishes slowly in air and burns readily to
form erbium (III) oxide, Er2O3.
4Er + 3O2 → 2Er2O3
Reaction of erbium with water
The silvery white metal erbium is quite electropositive
and reacts slowly with cold water and quite quickly with hot water to form
erbium hydroxide, Er(OH)3, and hydrogen gas (H2).
2Er(s) + 6H2O(g) → 2Er(OH)3(aq) +
3H2(g)
Reaction of erbium with the halogens
Erbium metal reacts with all
the halogens to form erbium(III) halides. So, it reacts with fluorine, F2,
chlorine, Cl2, bromine, I2, and iodine, I2,
to form respectively erbium(III) bromide, ErF3, erbium(III)
chloride, ErCl3, erbium(III) bromide, ErBr3, and
erbium(III) iodide, ErI3.
2Er(s) + 3F2(g) → 2ErF3(s) [pink]
2Er(s) + 3Cl2(g) → 2ErCl3(s)
[violet]
2Er(s) + 3Br2(g) → 2ErBr3(s)
[violet]
2Er(s) + 3I2(g) → 2ErI3(s)
[violet]
Reaction of erbium with acids
Erbium metal dissolves
readily in dilute sulphuric acid to form solutions containing the yellow
aquated Er(III) ion together with hydrogen gas, H2. It is quite
likely that Er3+(aq) exists as largely the complex ion [Er(OH2)9]3+
2Er(s) + 3H2SO4(aq) → 2Er3+(aq)
+ 3SO42-(aq) + 3H2(g)
Here is some information
about the crystal structure of erbium.
- Space group: P63/mmc (Space group number: 194)
- Structure: hcp (hexagonal close-packed)
- Cell parameters:
- a: 355.88 pm
- b: 355.88 pm
- c: 558.74 pm
- α: 90.000°
- β: 90.000°
- γ: 120.000°
The most used definition of
electronegativity is that an element's
electronegativity is the power of an atom when in a molecule to
attract electron density to itself. The electronegativity depends upon a
number of factors and in particuler as the other atoms in the molecule. The
first scale of electronegativity was developed by Linus Pauling and on his
scale erbium has a value of 1.24 on a
scale running from from about 0.7 (an estimate for francium) to 2.20 (for
hydrogen) to 3.98 (fluorine). Electronegativity has no units but "Pauling
units" are often used when indicating values mapped on to the Pauling scale.
On the interactive plot below you may find the "Ball chart" and "Shaded
table" styles most useful.
Table of Different types of
electronegativity for erbium. Use the links in the "Electronegativity"
column for definitions, literature sources, and visual representations
in many different styles (one of which is shown below). All values are
quoted on the Pauling scale.
| Electronegativity |
Value in Pauling units |
| Pauling electronegativity |
1.24 |
| Sanderson electronegativity |
no data |
| Allred Rochow electronegativity |
1.11 |
Erbium is never found in
nature as the free element. Erbium is found in the ores monazite sand [(Ce,
La, etc.)PO4] and bastn°site [(Ce, La, etc.)(CO3)F],
ores containing small amounts of all the rare earth metals. It is difficult
to separate from other rare earth elements.
Abundances of erbium in various environments
In this table of abundances,
values are given in units of ppb (parts per billion; 1 billion = 109),
both in terms of weight and in terms of numbers of atoms. Values for
abundances are difficult to determine with certainty, so all values should
be treated with some caution, especially so for the less common elements.
Local concentrations of any element can vary from those given here an orders
of magnitude or so and values in various literature sources for less common
elements do seem to vary considerably.
Abundances for erbium in a number of different
environments. Use the links in the location column for definitions,
literature sources, and visual representations in many different styles
(one of which is shown below)
| Location |
ppb by weight |
ppb by atoms |
| Universe |
2 |
0.01 |
| Sun |
1 |
0.01 |
| Meteorite (carbonaceous) |
180 |
20 |
| Crustal rocks |
3000 |
370 |
| Sea water |
0.0009 |
0.000033 |
| Stream |
0.05 |
0.0003 |
Erbium has six stable
isotopes but only Er-168 appears to have a well established application.
Er-168 is used for the production of Er-169 which is used in form of citrate
for the treatment of rheumatoid arthritis. Erbium isotopes can be obtained
from Trace Sciences International.
Naturally occurring isotopes
| Isotope |
Atomic mass (ma/u) |
Natural abundance (atom %) |
Nuclear spin (I) |
Magnetic moment (μ/μN) |
| 162Er |
161.928775 (4) |
0.14 (1) |
0 |
|
| 164Er |
163.929198 (4) |
1.61 (3) |
0 |
|
| 166Er |
165.930290 (4) |
33.61 (35) |
0 |
|
| 167Er |
166.932046 (4) |
22.93 (17) |
7/2 |
-0.5665 |
| 168Er |
167.932368 (4) |
26.78 (26) |
0 |
|
| 170Er |
169.935461 (4) |
14.93 (27) |
0 |
|
Radiosotope data
| Isotope |
Mass |
Half-life |
Mode of decay |
Nuclear spin |
Nuclear magnetic moment |
| 160Er |
159.92908 |
1.19 d |
EC to 160Ho |
0 |
|
| 161Er |
160.9300 |
3.21 h |
EC to 161Ho |
3/2 |
-0.37 |
| 163Er |
162.93003 |
1.25 h |
EC to 163Ho |
5/2 |
0.557 |
| 165Er |
164.930723 |
10.36 h |
EC to 165Ho |
5/2 |
0.643 |
| 169Er |
168.934588 |
9.40 d |
β- to 169Tm |
1/2 |
0.515 |
| 171Er |
170.938026 |
7.52 h |
β- to 171Tm |
5/2 |
0.66 |
| 172Er |
171.939352 |
2.05 d |
β- to 172Tm |
|
|
Chlorides
- ErCl3:
- thermochemical cycle: (no value) kJ mol-1
- calculated: 4527 kJ mol-1
Oxides
- Er2O3:
- thermochemical cycle: (no value) kJ mol-1
- calculated: 13263 kJ mol-1
Common reference compound: .
Table of NMR-active nucleus propeties of erbium
| |
Isotope 1 |
Isotope 2 |
Isotope 3 |
| Isotope |
167Er |
|
|
| Natural
abundance /% |
22.95 |
|
|
| Spin (I) |
7/2 |
|
|
| Frequency
relative to 1H = 100 (MHz) |
about 2.88 |
|
|
| Receptivity,
DP, relative to 1H = 1.00 |
- |
|
|
| Receptivity,
DC, relative to 13C = 1.00 |
- |
|
|
| Magnetogyric ratio, γ (107 rad T-1 s-1) |
-0.77157 |
|
|
| Magnetic moment, μ
(μN) |
-0.63935 |
|
|
|
Nuclear quadrupole moment, Q (barn) |
3.57 |
|
|
| Line width
factor, 1056l (m4) |
|
|
Valence shell orbital radii
The following are calculated values of valence shell
orbital radii, Rmax
Table: valence shell orbital radii for erbium.
| Orbital |
Radius [/pm] |
Radius [/AU] |
| s orbital |
203.1 |
3.83742 |
| f orbital |
26.8 |
0.505998 |
Effective Nuclear Charges
The following are "Clementi-Raimondi" effective nuclear
charges, Zeff. Follow the hyperlinks for more details
and for graphs in various formats.
Table: effective nuclear charges for erbium
| 1s |
66.67 |
|
| 2s |
50.20 |
2p |
63.65 |
|
| 3s |
47.08 |
3p |
47.61 |
3d |
54.36 |
|
| 4s |
36.23 |
4p |
35.11 |
4d |
32.27 |
4f |
27.98 |
| 5s |
19.72 |
5p |
17.47 |
5d |
no data |
|
| 6s |
8.48 |
Electron binding energies
This table contains electron binding energies for erbium.
| Label |
Orbital |
eV [literature reference] |
| K |
1s |
57486 [1] |
| L I |
2s |
9751 [1] |
| L II |
2p1/2 |
9264 [1] |
| L III |
2p3/2 |
8358 [1] |
| M I |
3s |
2206 [1] |
| M II |
3p1/2 |
2006 [1] |
| M III |
3p3/2 |
1812 [1] |
| M IV |
3d3/2 |
1453 [1] |
| M V |
3d5/2 |
1409 [1] |
| N I |
4s |
449.8 [2] |
| N II |
4p1/2 |
366.2 [1] |
| N III |
4p3/2 |
320.2 [2] |
| N IV |
4d3/2 |
167.6 [2] |
| N V |
4d5/2 |
167.6 [2] |
| N VI |
4f5/2 |
- |
| N VII |
4f7/2 |
4.7 [2] |
| O I |
5s |
50.6 [2] |
| O II |
5p1/2 |
31.4 [2] |
| O III |
5p3/2 |
24.7 [2] |
Temperatures
-
Melting point: 1770 [or 1497 °C (2727 °F)] K
-
Boiling point: 3141 [or 2868 °C (5194 °F)] K (liquid range: 1371 K
Expansion and conduction properties
-
Thermal conductivity: 15 W m-1 K-1
-
Coefficient of linear thermal expansion: 12.2 x 10-6 K-1
Bulk properties
-
Density of solid: 9066 kg m-3
-
Molar volume: 18.46 cm3
-
Velocity of sound: 2830 m s-1
Elastic properties
-
Youngs modulus: 70 GPa
-
Rigidity modulus: 28 GPa
-
Bulk modulus: 44 GPa
-
Poissons ratio: 0.24 (no units)
Hardnesses
-
Brinell hardness: 814 MN m-2
- Vickers hardness: 589 MN m-2
Electrical properties
- Electrical resistivity: 86 10-8 Ω m; or mΩ cm
Enthalpies
- Enthalpy of fusion: 19.9 kJ mol-1
- Enthalpy of vaporisation: 285 kJ mol-1
- Enthalpy of atomisation: 317 kJ mol-1
Thermodynamic data
Table: thermodynamic data for erbium.
| State |
ΔfH° |
ΔfG° |
S° |
CpH |
H°298.15-H°0 |
| Units |
kJ mol-1 |
kJ mol-1 |
J K-1 mol-1 |
J K-1 mol-1 |
kJ mol-1 |
| Solid |
0 |
0 |
73.2 |
28.1 |
7.38 |
| Gas |
317 |
281 |
195.5 |
20.8 |
6.2 |
The following
uses for erbium are gathered from a number of
sources as well as from anecdotal comments. I'd be delighted to receive
corrections as well as additional referenced uses (please use the
feedback mechanism to add uses).
- nuclear industry
- metallurgical uses. Added to vanadium, for example, erbium lowers
hardness and improves workability
- erbium oxide is pink and is a colourant in glasses and porcelain
enamel glazes
- photographic filter