Neodymium (Nd)
lanthanideSolid
Bobot Atom Standar
144,242 uKonfigurasi elektron
[Xe] 6s2 4f4Titik lebur
1020,85 °CTitik didih
3073,85 °CMassa jenis
7010 kg/m³Bilangan oksidasi
0, +2, +3, +4Keelektronegatifan (Pauling)
1,14Energi ionisasi (ke-1)
5,52475 eVTahun penemuan
1841Jari-jari atom
185 pmDetail
Neodymium is a light lanthanide metal and one of the more abundant rare-earth elements. It occurs in minerals with other lanthanides rather than as a native element. Its chemistry is dominated by the trivalent ion Nd³⁺, which gives many salts and glasses a pink to violet color. Technologically, neodymium is most important in high-strength permanent magnets and in optically active glasses and crystals.
The metal has a bright silvery metallic luster, Neodymium is one of the more reactive rare-earth metals and quickly tarnishes in air, forming an oxide that spalls off and exposes metal to oxidation. The metal, therefore, should be kept under light mineral oil or sealed in a plastic material. Neodymium exists in two allotropic forms, with a transformation from a double hexagonal to a body-centered cubic structure taking place at 863°C.
The name derives from the Greek neos for "new" and didymos for "twin". It was discovered by the Swedish surgeon and chemist Carl Gustav Mosander in 1841, who called it didymium (or twin) because of its similarity to lanthanum, which he had previously discovered two years earlier. In 1885, the Austrian chemist Carl Auer (Baron von Welsbach) separated didymium into two elements, one of which he called neodymium (or new twin).
Neodymium was discovered by Carl F. Auer von Welsbach, an Austrian chemist, in 1885. He separated neodymium, as well as the element praseodymium, from a material known as didymium. Today, neodymium is primarily obtained from through an ion exchange process monazite sand ((Ce, La, Th, Nd, Y)PO4), a material rich in rare earth elements.
From the Greek word neos meaning new, and didymos, twin. In 1841, Mosander, extracted a rose-colored oxide from cerite , which he believed contained a new element. He named the element didymium, as it was an inseparable twin brother of lanthanum. In 1885 von Welsbach separated didymium into two new elemental components, neodymia and praseodymia, by repeated fractionation of ammonium didymium nitrate. While the free metal is in misch metal, long known and used as a pyrophoric alloy for light flints, the element was not isolated in relatively pure form until 1925. Neodymium is present in misch metal to the extent of about 18%. It is present in the minerals monazite and bastnasite, which are principal sources of rare-earth metals.
Pure neodymium is a bright, silvery metal when freshly cut, but it tarnishes in air as an oxide layer forms. It is relatively soft and can be cut with a knife. The metal slowly reacts with moisture and oxidizes more rapidly when finely divided or heated.
The largest use of neodymium is in neodymium-iron-boron permanent magnets, commonly based on the Nd₂Fe₁₄B phase. These magnets are used in electric motors, generators, hard-disk drives, loudspeakers, sensors, and magnetic couplings. Neodymium-doped yttrium aluminium garnet, Nd:Y₃Al₅O₁₂, is a major solid-state laser material. Neodymium compounds are also used to color and filter glass, including didymium-type eyewear for glassworking.
Neodymium makes up about 18% of Misch metal, a material that is used to make flints for lighters. Neodymium is also a component of didymium glass, which is used to make certain types of welder's and glass blower's goggles. Neodymium is added to glass to remove the green color caused by iron contaminants. It can also be added to glass to create violet, red or gray colors. Some types of glass containing neodymium are used by astronomers to calibrate devices called spectrometers and other types are used to create artificial rubies for lasers. Some neodymium salts are used to color enamels and glazes.
Didymium, of which neodymium is a component, is used for coloring glass to make welders goggles. By itself, neodymium colors glass delicate shades ranging from pure violet through wine-red and warm gray. Light transmitted through such glass shows unusually sharp absorption bands. The glass has been used in astronomical work to produce sharp bands by which spectral lines may be calibrated. Glass containing neodymium can be used as a laser material to produce coherent light. Neodymium salts are also used as a colorant for enamels.
Isotopes in Geochronology
143Nd is a radiogenic isotope produced by decay of 147Sm, with a half-life of 1.06×1011 years. Thus, the isotope-amount ratio n(143Nd)/n(144Nd) can be used for dating rocks on long time scales and as a chemical tracer in geochemistry (Fig. IUPAC.60.1) [427] M. T. McCullocha, M. R. Perfita. Earth. Planet. Sci. Lett.56, 167 (1981)., [428] R. Eichhorn, R. Höll, E. Jagoutz, U. Schärer. Geochim. Cosmochim. Acta61, 5005 (1997).. The very small accumulation of 142Nd in billion-year-old metamorphosed rocks from Greenland [from the relatively short-lived (about 68×106 years) alpha decay of 146Sm] provided evidence that the crust of the Earth formed before the young planet was more than 100×106 years old. This is because only a short amount of time could have elapse to incorporate the 146Sm parent radionuclide into the ancient Greenland minerals before it decayed [429] M. G. Jackson, S. R. Hart, A. A. P. Koppers, H. Staudigel, J. Konter, J. Blusztajn, M. Kurz, J. A. Russell. Nature448, 684 (2007)., [430] G. Caro, B. Bourdon, J. L. Birck, S. Moorbath. Nature423, 428 (2003)..
Isotopes Used as a Source of Radioactive Isotope(s)
146Nd has been used in the production of 147Pm (with a half-life of 2.6 years), via the reaction 146Nd (n, γ) 147Nd, which is followed by a subsequent electron decay reaction, 147Nd→ 147Pm+β - reaction. 147Pm is a radioactive power-generation source [431] C. S. Lee, Y. M. Wang, W. L. Cheng, G. Ting. J. Radioanal. Nucl. Chem.130, 21 (1988)..
Neodymium most commonly forms compounds in the +3 oxidation state, and Nd³⁺ salts are typically pale pink, rose, lavender, or violet depending on ligand and hydration. Important compounds include neodymium(III) oxide, Nd₂O₃, neodymium(III) chloride, NdCl₃, and neodymium(III) fluoride, NdF₃. The oxide is a common intermediate in separation and materials production. Divalent neodymium is known in some solid-state compounds, but it is much less stable and far less common than Nd³⁺ chemistry.
See more information at the Neodymium compound page.
Bulk neodymium metal has low acute toxicity but is reactive as a fine powder and can present a fire hazard. Dusts and soluble salts should be handled as industrial chemical hazards because rare-earth compounds can irritate the eyes, skin, and respiratory tract. Strong neodymium magnets create mechanical hazards: they can pinch skin, shatter on impact, damage magnetic media, and interfere with some implanted medical devices.
Neodymium has a low-to-moderate acute toxic rating. As with other rare earths, neodymium should be handled with care.
Neodymium is widely dispersed in the crust, mainly in rare-earth minerals such as monazite and bastnäsite. In natural waters it is present at very low concentrations and tends to bind to particles, phosphates, carbonates, and organic matter rather than remain as a free ion. Mining and processing can disturb soils and generate waste streams containing other rare earths, thorium, uranium, acids, or salts, depending on the ore and process.
Neodymium is produced by mining rare-earth ores, separating mixed lanthanides through solvent extraction or ion-exchange processes, and reducing suitable halides or oxides to metal when needed. Demand is strongly tied to Nd-Fe-B magnets, often with praseodymium partly substituting for neodymium and dysprosium or terbium added for high-temperature performance. Supply is constrained by the difficulty of separating similar lanthanides and by the environmental controls needed for ore processing. Recycling from magnets is technically possible and increasing, but collection and separation remain limiting factors.
Made from electrolysis of its halide salts, which are made from monazite sand.
Neodymium is produced mainly by neutron-capture nucleosynthesis in evolved stars and stellar explosions, with contributions from both slow and rapid neutron-capture processes. It is less abundant than lighter elements but is a normal trace constituent of the Solar System. Meteorites and planetary rocks contain neodymium in rare-earth patterns useful for geochemical and isotopic studies.
- The name neodymium means “new twin,” reflecting its separation from didymium.
- Natural neodymium consists of several stable isotopes and very long-lived radioactive ¹⁴⁴Nd and ¹⁵⁰Nd.
- Neodymium glass can appear different colors under different lighting because of sharp f-electron absorption bands.
- Nd-Fe-B magnets are usually coated because the alloy corrodes readily.
- Samarium-cobalt magnets tolerate heat better, but Nd-Fe-B magnets usually provide stronger fields for their size.
Gambar
Sifat
Fisika
- Jari-jari atom (empiris)
- 185 pm Bandingkan Jari-jari atom (empiris) semua unsur →
- Jari-jari kovalen
- 201 pm Bandingkan Jari-jari kovalen semua unsur →
- Jari-jari van der Waals
- 229 pm Bandingkan Jari-jari van der Waals semua unsur →
- Massa jenis
- 7010 kg/m³ Bandingkan Massa jenis semua unsur →
- Volume molar
- 0,0206 L/mol
- Fase pada STP
- Padat Bandingkan Fase pada STP semua unsur →
- Titik lebur
- 1020,85 °C Bandingkan Titik lebur semua unsur →
- Titik didih
- 3073,85 °C Bandingkan Titik didih semua unsur →
- Kapasitas kalor spesifik
- 0,19 J/(g·K) Bandingkan Kapasitas kalor spesifik semua unsur →
- Kapasitas kalor molar
- 27,45 J/(mol·K) Bandingkan Kapasitas kalor molar semua unsur →
- Struktur kristal
- Heksagonal susunan rapat Bandingkan Struktur kristal semua unsur →
Kimia
- Keelektronegatifan (Pauling)
- 1,14 Bandingkan Keelektronegatifan (Pauling) semua unsur →
- Afinitas elektron
- 1,913 eV
- Energi ionisasi (ke-1)
- 5,52475 eV Bandingkan Energi ionisasi (ke-1) semua unsur →
- Energi ionisasi (ke-2)
- 10,783037 eV Bandingkan Energi ionisasi (ke-2) semua unsur →
- Energi ionisasi (ke-3)
- 22,090076 eV Bandingkan Energi ionisasi (ke-3) semua unsur →
- Energi ionisasi (ke-4)
- 40,60014 eV Bandingkan Energi ionisasi (ke-4) semua unsur →
- Energi ionisasi (ke-5)
- 60,000207 eV Bandingkan Energi ionisasi (ke-5) semua unsur →
- Bilangan oksidasi
- 0, +2, +3, +4 Bandingkan Bilangan oksidasi semua unsur →
- Elektron valensi
- 3 Bandingkan Elektron valensi semua unsur →
- Konfigurasi elektron
- [Xe] 6s2 4f4
Termodinamika
- Kalor peleburan
- 0,07400114 eV Bandingkan Kalor peleburan semua unsur →
- Kalor penguapan
- 2,829455 eV Bandingkan Kalor penguapan semua unsur →
- Kalor sublimasi
- 2,995284 eV
- Kalor atomisasi
- 2,995284 eV
- Entalpi atomisasi
- 3,388091 eV
Nuklir
- Proton
- 60 Bandingkan Proton semua unsur →
- Neutron
- 82 Bandingkan Neutron semua unsur →
- Isotop yang diketahui
- 40 Bandingkan Isotop yang diketahui semua unsur →
- Isotop stabil
- 1 Bandingkan Isotop stabil semua unsur →
- Isotop paling stabil
- Nd-142
- Tahun penemuan
- 1841
Kelimpahan
- Kelimpahan (kerak Bumi)
- 41,5 mg/kg Bandingkan Kelimpahan (kerak Bumi) semua unsur →
- Kelimpahan (samudra)
- 2,8 × 10−6 mg/L Bandingkan Kelimpahan (samudra) semua unsur →
Struktur Kristal
- Konstanta kisi a
- 366 pm
Struktur Elektronik
- Elektron per kulit
- 2, 8, 18, 22, 8, 2 Bandingkan Elektron per kulit semua unsur →
Pengenal
- Nomor CAS
- 7440-00-8 Bandingkan Nomor CAS semua unsur →
- Simbol term
- 5I4
- InChI
- InChI=1S/Nd
- Kunci InChI
- QEFYFXOXNSNQGX-UHFFFAOYSA-N
Konfigurasi Elektron Diukur
Nd: 4f⁴ 6s²[Xe] 4f⁴ 6s²1s² 2s² 2p⁶ 3s² 3p⁶ 3d¹⁰ 4s² 4p⁶ 4d¹⁰ 5s² 5p⁶ 4f⁴ 6s²Model atom
Isotop mengubah jumlah neutron, massa, dan kestabilan — bukan konfigurasi elektron atom netral.
Model atom skematis, tidak sesuai skala.
Sidik Jari Atom
Spektrum Emisi / Absorpsi
Distribusi Isotop
| Nomor massa | Massa atom (u) | Kelimpahan alami | Waktu paruh |
|---|---|---|---|
| 142 Stabil | 141,907729 ± 0,000002 | 27,1520% | Stabil |
Fase / Wujud
Alasan: 995,9 °C di bawah titik lebur (1020,85 °C)
Skematis, tidak sesuai skala
Titik transisi fase
Energi transisi
Energi yang diperlukan untuk meleburkan 1 mol pada titik lebur
Energi yang diperlukan untuk menguapkan 1 mol pada titik didih
Energi yang diperlukan untuk menyublimkan 1 mol pada titik sublimasi
Massa jenis
Pada kondisi standar
Pada kondisi standar
Spektrum Atom
Menampilkan 10 dari 60. Diurutkan berdasarkan muatan ion (menaik).
Data Garis Spektrum ?
| Ion | Muatan | Total garis | Probabilitas transisi | Penamaan tingkat energi |
|---|---|---|---|---|
| Nd I | 0 | 118 | 9 | 9 |
| Nd II | +1 | 617 | 255 | 600 |
Data Tingkat Energi ?
| Ion | Muatan | Tingkat energi |
|---|---|---|
| Nd I | 0 | 739 |
| Nd II | +1 | 840 |
| Nd III | +2 | 31 |
| Nd IV | +3 | 19 |
| Nd V | +4 | 2 |
| Nd VI | +5 | 2 |
| Nd VII | +6 | 2 |
| Nd VIII | +7 | 2 |
| Nd IX | +8 | 2 |
| Nd X | +9 | 2 |
Jari-jari Ion
| Muatan | Koordinasi | Spin | Jari-jari |
|---|---|---|---|
| +2 | 8 | Tidak tersedia | 129 pm |
| +2 | 9 | Tidak tersedia | 135 pm |
| +3 | 6 | Tidak tersedia | 98.3 pm |
| +3 | 8 | Tidak tersedia | 110.9 pm |
| +3 | 9 | Tidak tersedia | 116.3 pm |
| +3 | 12 | Tidak tersedia | 127 pm |
Senyawa
Isotop (1)
Natural neodymium is a mixture of seven stable isotopes. Fourteen other radioactive isotopes are recognized.
| Nomor massa | Massa atom (u) | Kelimpahan alami | Waktu paruh | Mode peluruhan | |
|---|---|---|---|---|---|
| 142 Stabil | 141,907729 ± 0,000002 | 27,1520% ± 0,0400% | Stabil | stable |
Sifat Lanjutan
Jari-jari Kovalen (Lanjutan)
- Jari-jari kovalen (Pyykkö)
- 174 pm
- Jari-jari kovalen (Pyykkö, ikatan rangkap dua)
- 137 pm
Jari-jari van der Waals
- Alvarez
- 295 pm
- UFF
- 357,5 pm
- MM3
- 273 pm
Jari-jari Atom & Logam
- Jari-jari atom (Rahm)
- 284 pm
Skala Penomoran
- Mendeleev
- 19
- Pettifor
- 30
- Glawe
- 29
Skala Keelektronegatifan
- Ghosh
- 0
- Miedema
- 3
- Gunnarsson–Lundqvist
- 5
- Robles–Bartolotti
- 4
Polarizabilitas & Dispersi
- Polarizabilitas dipol
- 208 a.u.
- Polarizabilitas dipol (ketidakpastian)
- 20 a.u.
- C₆ (Gould–Bučko)
- 3560 Ha·Bohr6
Parameter Miedema
- Volume molar Miedema
- 20,58 cm3/mol
- Kerapatan elektron Miedema
- 2
Risiko Pasokan & Ekonomi
- Konsentrasi produksi
- 97
- Risiko pasokan relatif
- 10
- Distribusi cadangan
- 50
- Stabilitas politik (produsen terbesar)
- 24
- Stabilitas politik (pemilik cadangan terbesar)
- 24
Transisi Fase & Alotrop
| Titik lebur | 1289,15 K |
| Titik didih | 3347,15 K |
Kategori Bilangan Oksidasi
Data Referensi Lanjutan
Konstanta Pemerisaian (13)
| n | Orbital | σ |
|---|---|---|
| 1 | s | 1,1868 |
| 2 | p | 4,2434 |
| 2 | s | 15,7838 |
| 3 | d | 13,8432 |
| 3 | p | 19,311 |
| 3 | s | 19,6572 |
| 4 | d | 33,1908 |
| 4 | f | 37,734 |
| 4 | p | 29,986 |
| 4 | s | 29,0136 |
Detail Jari-jari Kristal (6)
| Muatan | CN | Spin | rcrystal (pm) | Asal |
|---|---|---|---|---|
| 2 | VIII | 143 | ||
| 2 | IX | 149 | ||
| 3 | VI | 112,3 | from r^3 vs V plots, | |
| 3 | VIII | 124,9 | from r^3 vs V plots, | |
| 3 | IX | 130,3 | from r^3 vs V plots, | |
| 3 | XII | 141 | estimated, |
Mode Peluruhan Isotop (52)
| Isotop | Mode | Intensitas |
|---|---|---|
| 124 | B+ | — |
| 124 | B+p | — |
| 125 | B+ | 100% |
| 125 | B+p | 0% |
| 126 | B+ | — |
| 126 | B+p | — |
| 127 | B+ | 100% |
| 127 | B+p | — |
| 128 | B+ | — |
| 129 | B+ | 100% |
Faktor Hamburan Sinar-X (508)
| Energi (eV) | f₁ | f₂ |
|---|---|---|
| 10 | — | 0,24448 |
| 10,1617 | — | 0,25177 |
| 10,3261 | — | 0,25926 |
| 10,4931 | — | 0,26698 |
| 10,6628 | — | 0,27494 |
| 10,8353 | — | 0,28312 |
| 11,0106 | — | 0,29156 |
| 11,1886 | — | 0,30024 |
| 11,3696 | — | 0,30918 |
| 11,5535 | — | 0,31839 |
Data Tambahan
Estimated Crustal Abundance
The estimated element abundance in the earth's crust.
4.15×101 milligrams per kilogram
Referensi (1)
- [5] Neodymium https://education.jlab.org/itselemental/ele060.html
Estimated Oceanic Abundance
The estimated element abundance in the earth's oceans.
2.8×10-6 milligrams per liter
Referensi (1)
- [5] Neodymium https://education.jlab.org/itselemental/ele060.html
Production
Production of this element (from raw materials or other compounds containing the element).
The element may be obtained by separating neodymium salts from other rare earths by ion-exchange or solvent extraction techniques, and by reducing anhydrous halides such as NdF3 with calcium metal. Other separation techniques are possible.
Referensi (1)
- [6] Neodymium https://periodic.lanl.gov/60.shtml
Referensi
(9)
Data deposited in or computed by PubChem
The half-life and atomic mass data was provided by the Atomic Mass Data Center at the International Atomic Energy Agency.
Element data are cited from the Atomic weights of the elements (an IUPAC Technical Report). The IUPAC periodic table of elements can be found at https://iupac.org/what-we-do/periodic-table-of-elements/. Additional information can be found within IUPAC publication doi:10.1515/pac-2015-0703 Copyright © 2020 International Union of Pure and Applied Chemistry.
The information are cited from Pure Appl. Chem. 2018; 90(12): 1833-2092, https://doi.org/10.1515/pac-2015-0703.
Thomas Jefferson National Accelerator Facility (Jefferson Lab) is one of 17 national laboratories funded by the U.S. Department of Energy. The lab's primary mission is to conduct basic research of the atom's nucleus using the lab's unique particle accelerator, known as the Continuous Electron Beam Accelerator Facility (CEBAF). For more information visit https://www.jlab.org/
The periodic table at the LANL (Los Alamos National Laboratory) contains basic element information together with the history, source, properties, use, handling and more. The provenance data may be found from the link under the source name.
The periodic table contains NIST's critically-evaluated data on atomic properties of the elements. The provenance data that include data for atomic spectroscopy, X-ray and gamma ray, radiation dosimetry, nuclear physics, and condensed matter physics may be found from the link under the source name. Ref: https://www.nist.gov/pml/atomic-spectra-database
This section provides all form of data related to element Neodymium.
The element property data was retrieved from publications.