Neon (Ne)
noble-gasGas
標準原子量
20.1797 u電子配置
[He] 2s2 2p6融点
-248.59 °C沸点
-246.05 °C密度
0.8999 kg/m³酸化数
0電気陰性度（Pauling）
データなし第1イオン化エネルギー
21.564541 eV発見年
1898原子半径
160 pm詳細
Neon is a noble gas and the second lightest member of group 18. It is monatomic, colorless, and chemically very inert under ordinary conditions because its outer electron shell is closed. In the atmosphere it is present only as a minor constituent, but it is readily recognized by the intense reddish-orange light emitted in low-pressure electrical discharges. Its technological importance rests mainly on this optical behavior and on its cryogenic properties.
Colourless gaseous element of group 18 on the periodic table (noble gases). Neon occurs in the atmosphere, and comprises 0.0018% of the volume of the atmosphere. It has a distinct reddish glow when used in discharge tubes and neon based lamps. It forms almost no chemical compounds. Neon was discovered in 1898 by Sir William Ramsey and M.W. Travers.
The name derives from the Greek neos for "new". It was discovered from its bright orange spectral lines by the Scottish chemist William Ramsay and the English chemist Morris William Travers in 1898 from a liquefied air sample.
Neon was discovered by Sir William Ramsay, a Scottish chemist, and Morris M. Travers, an English chemist, shortly after their discovery of the element krypton in 1898. Like krypton, neon was discovered through the study of liquefied air. Although neon is the fourth most abundant element in the universe, only 0.0018% of the earth's atmosphere is neon.
From the Greek word neos, new. Discovered by Ramsay and Travers in 1898. Neon is a rare gaseous element present in the atmosphere to the extent of 1 part in 65,000 of air. It is obtained by liquefaction of air and separated from the other gases by fractional distillation.
Pure neon is a colorless, odorless, monatomic gas at ordinary temperature and pressure. When cooled below its boiling point it becomes a colorless cryogenic liquid, and at still lower temperature a solid. In a discharge tube it emits a bright red-orange glow from atomic emission lines.
Neon is best known for luminous advertising signs, indicator lamps, and decorative discharge tubes, where low-pressure neon gives a distinctive red-orange emission. Other gases or phosphors are used for many colors often called “neon” in commerce. Neon is also used in some high-voltage indicators, gas lasers such as helium-neon lasers, and specialized cryogenic applications. Liquid neon has a high refrigeration capacity per unit volume, but its cost limits broad use.
The largest use for neon gas is in advertising signs. Neon is also used to make high voltage indicators and is combined with helium to make helium-neon lasers. Liquid neon is used as a cryogenic refrigerant. Neon is highly inert and forms no known compounds, although there is some evidence that it could form a compound with fluorine.
Although neon advertising signs account for the bulk of its use, neon also functions in high-voltage indicators, lightning arrestors, wave meter tubes, and TV tubes. Neon and helium are used in making gas lasers. Liquid neon is now commercially available and is finding important application as an economical cryogenic refrigerant.
Isotopes in Earth/Planetary Science
Neon is subject to stable isotopic fractionation by physical processes, such as exchange between gas, liquid, and solid phases. Small variations in the isotope-amount ratio n(22Ne)/n(20Ne) have been used to examine gas-liquid exchange processes during groundwater recharge (water moving downward from the surface) and discharge [29] M. Ozima, F. A. Podosek. Noble Gas Geochemistry: 2nd Edition, p. 286, Cambridge University Press, Cambridge, UK (2002)., [101] Noble Gases in Geochemistry and Cosmochemistry: Reviews in Mineralogy and Geochemistry, D. Porcelli, C. J. Ballentine, and R. Wieler (Eds.), p. 844, Mineralogical Society of America and the Geochemical Society, Washington, DC (2002)., [102] F. Peeters, U. Beyerle, W. Aeschbach-Hertig, J. Holocher, M. S. Brennwald, R. Kipfer. Geochim. Cosmochim. Acta.67, 587 (2003)..
Isotopes in Geochronology
Some 21Ne and 22Ne form naturally in the Earth’s crust largely by reactions of 18O and 19F in minerals with neutrons and alpha particles emitted from uranium and thorium decay, called nucleogenic neon isotopes [29] M. Ozima, F. A. Podosek. Noble Gas Geochemistry: 2nd Edition, p. 286, Cambridge University Press, Cambridge, UK (2002)., [101] Noble Gases in Geochemistry and Cosmochemistry: Reviews in Mineralogy and Geochemistry, D. Porcelli, C. J. Ballentine, and R. Wieler (Eds.), p. 844, Mineralogical Society of America and the Geochemical Society, Washington, DC (2002).. In addition, neon isotopes can form at the surface of the Earth and in extraterrestrial bodies by cosmic-ray-induced spallation reactions on magnesium, silicon, aluminum, and sodium [103] T. E. Cerling, H. Craig. Annu. Rev. Earth Planet. Sci.22, 273 (1994)., [104] D. Lal, B. Peters. “Cosmic ray produced radioactivity on the earth”, in Cosmic Rays II, K. Sitte (Ed.), Springer-Verlag, New York (1967).. Analyses of all three stable neon isotopes may be used to distinguish these sources from primordial neon. The relative amounts of atmospheric neon and crustal nucleogenic neon isotopes in deep groundwaters and natural gases have been used in studies of solid-water-gas interactions and migration (Fig. IUPAC.10.1). The cosmogenic component is mainly detected in 21Ne and can be used to determine cosmic-ray exposure ages of rock samples, including meteorites exposed during travel through space and boulders exposed by melting of glacial ice (Fig. IUPAC.10.1).
Isotopes in Industry
Masers (Microwave Amplification by Stimulated Emission of Radiation) containing 20Ne have been used to study quantum physics. 21Ne may also play a role in maser studies of quantum physics [106] W. R. Bennett. Phys. Rev.126, 580 (1962)..
Isotopes Used as a Source of Radioactive Isotope(s)
22Ne is used to produce the radioisotope 22Na via the reaction 22Ne (p, n) 22Na [107] R. Policroniades, E. Moreno, A. Varela, G. Murillo, A. Huerta, M. E. Ortiz, E. Chávez. Rev. Mex. Fis. S.54, 46 (2008).. 20Ne has been used to produce the radioisotope 18F via the reaction 20Ne (d, 4He) 18F [107] R. Policroniades, E. Moreno, A. Varela, G. Murillo, A. Huerta, M. E. Ortiz, E. Chávez. Rev. Mex. Fis. S.54, 46 (2008)..
Neon has no stable neutral compounds known under ordinary chemical conditions. Its very high ionization energy and negligible electron affinity make conventional oxidation states chemically inaccessible. Laboratory studies have identified transient ionic or weakly bound species such as NeH⁺ and van der Waals complexes at low temperature or in plasmas, but these are not isolable bulk compounds. Neon clathrate hydrates have been reported only under suitable low-temperature, high-pressure conditions, where neon is physically trapped rather than chemically bonded.
Neon is a very inert element, however, it has been reported to form a compound with fluorine. It is still questionable if true compounds of neon exist, but evidence is mounting in favor of their existence. The ions, Ne+, (NeAr)+, (NeH)+, and (HeNe+) are known from optical and mass spectrometric studies. Neon also forms an unstable hydrate.
See more information at the Neon compound page.
Neon is not toxic and is not chemically reactive in normal use. The main hazards are physical: compressed gas cylinders can rupture if mishandled, and released gas can displace oxygen in confined spaces. Liquid neon and cold equipment can cause cryogenic burns and embrittle some materials. Discharge devices also involve electrical hazards and, in some cases, fragile glass under reduced pressure.
Atmospheric neon is chemically persistent and does not participate significantly in biological or geochemical reactions. It enters the air mainly from primordial atmospheric inventory and minor natural releases from rocks and waters; it is lost only slowly by atmospheric escape processes. Because it is inert, dilute, and nonbioaccumulative, neon has no known essential biological role and little direct ecological activity.
Commercial neon is obtained by fractional distillation of liquefied air, usually as a minor by-product of large oxygen and nitrogen production. Its low atmospheric abundance makes recovery more specialized than for argon, and purification requires separation from helium, hydrogen, and other light gases. Demand is concentrated in signage, electronics, lasers, and niche cryogenic uses. Recycling is possible from closed systems but is uncommon for small lamps and signs, so supply depends strongly on industrial gas infrastructure.
Obtained from production of liquid air as a byproduct of producing liquid oxygen and nitrogen.
Neon is a cosmically abundant light noble gas made chiefly during stellar nucleosynthesis in massive stars, especially through carbon and oxygen burning stages. It is found in the Sun, stellar atmospheres, nebulae, and planetary atmospheres, although its abundance in rocky planets is reduced by volatility and atmospheric loss. Several stable isotopes occur naturally, with ²⁰Ne dominant on Earth.
- The familiar red-orange sign color is produced by neon itself, not by a coating.
- Many commercial “neon” signs of other colors contain argon, mercury vapor, or phosphors instead.
- Neon was discovered through the fractional distillation of liquid air.
- Liquid neon is denser than liquid helium but boils at a much higher temperature.
- Neon has no known stable neutral compound at ambient conditions.
- The name comes from a Greek word meaning “new.”
画像
性質
物理的性質
- 原子半径（経験値）
- 160 pm 全元素の原子半径（経験値）を比較 →
- 共有結合半径
- 58 pm 全元素の共有結合半径を比較 →
- ファンデルワールス半径
- 154 pm 全元素のファンデルワールス半径を比較 →
- 密度
- 0.8999 kg/m³ 全元素の密度を比較 →
- モル体積
- 0.0168 L/mol
- 標準温度・圧力（STP）での相
- 気体 全元素の標準温度・圧力（STP）での相を比較 →
- 融点
- -248.59 °C 全元素の融点を比較 →
- 沸点
- -246.05 °C 全元素の沸点を比較 →
- 比熱容量
- 1.03 J/(g·K) 全元素の比熱容量を比較 →
- モル熱容量
- 20.786 J/(mol·K) 全元素のモル熱容量を比較 →
- 結晶構造
- 面心立方構造 全元素の結晶構造を比較 →
化学的性質
- 電気陰性度（Allen）
- 4.787
- 電子親和力
- -1.2 eV (負の値—この原子は電子を取り込まないと予測される)
- 第1イオン化エネルギー
- 21.564541 eV 全元素の第1イオン化エネルギーを比較 →
- 第2イオン化エネルギー
- 40.963111 eV 全元素の第2イオン化エネルギーを比較 →
- 第3イオン化エネルギー
- 63.423518 eV 全元素の第3イオン化エネルギーを比較 →
- 第4イオン化エネルギー
- 97.190335 eV 全元素の第4イオン化エネルギーを比較 →
- 第5イオン化エネルギー
- 126.247435 eV 全元素の第5イオン化エネルギーを比較 →
- 酸化数
- 0 全元素の酸化数を比較 →
- 価電子
- 8 全元素の価電子を比較 →
- 電子配置
- [He] 2s2 2p6
熱力学的性質
- 三重点（温度）
- -248.59 °C
- 三重点（圧力）
- 4.34e+4 Pa
- 臨界点（温度）
- -228.658 °C
- 臨界点（圧力）
- 2.6786e+6 Pa
- 融解熱
- 0.00347204 eV 全元素の融解熱を比較 →
- 蒸発熱
- 0.01772296 eV 全元素の蒸発熱を比較 →
- 原子化熱
- 0 eV
原子核
- 陽子数
- 10 全元素の陽子数を比較 →
- 中性子数
- 10 全元素の中性子数を比較 →
- 既知の同位体
- 20 全元素の既知の同位体を比較 →
- 安定同位体
- 3 全元素の安定同位体を比較 →
- 最も安定な同位体
- Ne-20
- 発見年
- 1898
存在度
- 存在度（地殻）
- 0.005 mg/kg 全元素の存在度（地殻）を比較 →
- 存在度（海洋）
- 1.2 × 10−4 mg/L 全元素の存在度（海洋）を比較 →
結晶構造
- 格子定数a
- 443 pm
電子構造
- 各電子殻の電子数
- 2, 8 全元素の各電子殻の電子数を比較 →
識別子
- CAS登録番号
- 7440-01-9 全元素のCAS登録番号を比較 →
- 項記号
- 1S0
- InChI
- InChI=1S/Ne
- InChI Key
- GKAOGPIIYCISHV-UHFFFAOYSA-N
電子配置 測定値
Ne: 2s² 2p⁶[He] 2s² 2p⁶1s² 2s² 2p⁶原子モデル
同位体によって中性子数、質量、安定性は変わりますが、中性原子の電子配置は変わりません。
模式的な原子モデルです。実際の縮尺とは異なります。
原子の指紋
発光／吸収スペクトル
同位体分布
| 質量数 | 原子質量（u） | 天然存在比 | 半減期 |
|---|---|---|---|
| 20 安定 | 19.9924401762 ± 0.0000000017 | 90.4800% | 安定 |
| 21 安定 | 20.993846685 ± 0.000000041 | 0.2700% | 安定 |
| 22 安定 | 21.991385114 ± 0.000000018 | 9.2500% | 安定 |
相／状態
理由: 沸点（-246.05 °C）より271.1 °C高い
模式図、実際の縮尺とは異なります
相転移点
相転移エネルギー
融点で1 molを融解させるのに必要なエネルギー
沸点で1 molを蒸発させるのに必要なエネルギー
密度
標準条件下
現在の温度Tにおいて理想気体の状態方程式で推定
詳細
原子スペクトル
スペクトル線データの収録状況 ?
| イオン | 電荷 | スペクトル線の総数 | 遷移確率 | 準位の表記 |
|---|---|---|---|---|
| Ne I | 0 | 1597 | 533 | 1597 |
| Ne II | +1 | 1914 | 233 | 1912 |
| Ne III | +2 | 910 | 637 | 910 |
| Ne IV | +3 | 643 | 72 | 643 |
| Ne V | +4 | 374 | 139 | 374 |
| Ne VI | +5 | 515 | 449 | 515 |
| Ne VII | +6 | 661 | 442 | 661 |
| Ne VIII | +7 | 745 | 540 | 745 |
| Ne IX | +8 | 229 | 228 | 229 |
| Ne X | +9 | 137 | 137 | 137 |
準位データの収録状況 ?
| イオン | 電荷 | 準位 |
|---|---|---|
| Ne I | 0 | 375 |
| Ne II | +1 | 385 |
| Ne III | +2 | 283 |
| Ne IV | +3 | 215 |
| Ne V | +4 | 161 |
| Ne VI | +5 | 135 |
| Ne VII | +6 | 208 |
| Ne VIII | +7 | 178 |
| Ne IX | +8 | 110 |
| Ne X | +9 | 149 |
化合物
同位体 (3)
Natural neon is a mixture of three isotopes. Six other unstable isotopes are known.
| 質量数 | 原子質量（u） | 天然存在比 | 半減期 | 崩壊形式 | |
|---|---|---|---|---|---|
| 20 安定 | 19.9924401762 ± 0.0000000017 | 90.4800% ± 0.0300% | 安定 | stable | |
| 21 安定 | 20.993846685 ± 0.000000041 | 0.2700% ± 0.0100% | 安定 | stable | |
| 22 安定 | 21.991385114 ± 0.000000018 | 9.2500% ± 0.0300% | 安定 | stable |
スペクトル線
全1087件中50件を表示しています。 初期設定では、強度の測定値があるスペクトル線のみを表示します。
| 波長（nm） | 強度 | 電離段階 | 種類 | 遷移 | 精度 | 出典 | |
|---|---|---|---|---|---|---|---|
| 692.94673 nm | 100000 | Ne I | emission | 2s2.2p5.(2P*<1/2>).3s 2[1/2]* → 2s2.2p5.(2P*<3/2>).3p 2[3/2] | 測定値 | NIST | |
| 703.24131 nm | 85000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3s 2[3/2]* → 2s2.2p5.(2P*<3/2>).3p 2[1/2] | 測定値 | NIST | |
| 717.39381 nm | 77000 | Ne I | emission | 2s2.2p5.(2P*<1/2>).3s 2[1/2]* → 2s2.2p5.(2P*<3/2>).3p 2[5/2] | 測定値 | NIST | |
| 724.51666 nm | 77000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3s 2[3/2]* → 2s2.2p5.(2P*<3/2>).3p 2[1/2] | 測定値 | NIST | |
| 743.88984 nm | 60000 | Ne I | emission | 2s2.2p5.(2P*<1/2>).3s 2[1/2]* → 2s2.2p5.(2P*<3/2>).3p 2[1/2] | 測定値 | NIST | |
| 702.40504 nm | 34000 | Ne I | emission | 2s2.2p5.(2P*<1/2>).3s 2[1/2]* → 2s2.2p5.(2P*<3/2>).3p 2[3/2] | 測定値 | NIST | |
| 748.88712 nm | 32000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[1/2] → 2s2.2p5.(2P*<3/2>).3d 2[3/2]* | 測定値 | NIST | |
| 540.05618 nm | 20000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3s 2[3/2]* → 2s2.2p5.(2P*<1/2>).3p 2[1/2] | 測定値 | NIST | |
| 585.24879 nm | 20000 | Ne I | emission | 2s2.2p5.(2P*<1/2>).3s 2[1/2]* → 2s2.2p5.(2P*<1/2>).3p 2[1/2] | 測定値 | NIST | |
| 640.22472 nm | 20000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3s 2[3/2]* → 2s2.2p5.(2P*<3/2>).3p 2[5/2] | 測定値 | NIST | |
| 470.43948 nm | 15000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[1/2] → 2s2.2p5.(2P*<3/2>).5d 2[3/2]* | 測定値 | NIST | |
| 471.20625 nm | 15000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[5/2] → 2s2.2p5.(2P*<3/2>).6d 2[5/2]* | 測定値 | NIST | |
| 471.53441 nm | 15000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[5/2] → 2s2.2p5.(2P*<3/2>).6d 2[7/2]* | 測定値 | NIST | |
| 650.65281 nm | 15000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3s 2[3/2]* → 2s2.2p5.(2P*<3/2>).3p 2[5/2] | 測定値 | NIST | |
| 470.88584 nm | 12000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[1/2] → 2s2.2p5.(2P*<3/2>).5d 2[1/2]* | 測定値 | NIST | |
| 453.77551 nm | 10000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[1/2] → 2s2.2p5.(2P*<1/2>).5d 2[3/2]* | 測定値 | NIST | |
| 471.00638 nm | 10000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[1/2] → 2s2.2p5.(2P*<3/2>).5d 2[1/2]* | 測定値 | NIST | |
| 478.89249 nm | 10000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[5/2] → 2s2.2p5.(2P*<3/2>).7s 2[3/2]* | 測定値 | NIST | |
| 482.73382 nm | 10000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[1/2] → 2s2.2p5.(2P*<3/2>).6s 2[3/2]* | 測定値 | NIST | |
| 488.49181 nm | 10000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[5/2] → 2s2.2p5.(2P*<1/2>).5d 2[5/2]* | 測定値 | NIST | |
| 495.70324 nm | 10000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[3/2] → 2s2.2p5.(2P*<1/2>).5d 2[5/2]* | 測定値 | NIST | |
| 534.10932 nm | 10000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[1/2] → 2s2.2p5.(2P*<3/2>).4d 2[1/2]* | 測定値 | NIST | |
| 588.18952 nm | 10000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3s 2[3/2]* → 2s2.2p5.(2P*<1/2>).3p 2[1/2] | 測定値 | NIST | |
| 602.99969 nm | 10000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3s 2[3/2]* → 2s2.2p5.(2P*<1/2>).3p 2[1/2] | 測定値 | NIST | |
| 607.43377 nm | 10000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3s 2[3/2]* → 2s2.2p5.(2P*<3/2>).3p 2[1/2] | 測定値 | NIST | |
| 614.30626 nm | 10000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3s 2[3/2]* → 2s2.2p5.(2P*<3/2>).3p 2[3/2] | 測定値 | NIST | |
| 616.35939 nm | 10000 | Ne I | emission | 2s2.2p5.(2P*<1/2>).3s 2[1/2]* → 2s2.2p5.(2P*<1/2>).3p 2[1/2] | 測定値 | NIST | |
| 621.72812 nm | 10000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3s 2[3/2]* → 2s2.2p5.(2P*<3/2>).3p 2[3/2] | 測定値 | NIST | |
| 626.6495 nm | 10000 | Ne I | emission | 2s2.2p5.(2P*<1/2>).3s 2[1/2]* → 2s2.2p5.(2P*<1/2>).3p 2[3/2] | 測定値 | NIST | |
| 633.44278 nm | 10000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3s 2[3/2]* → 2s2.2p5.(2P*<3/2>).3p 2[5/2] | 測定値 | NIST | |
| 638.29917 nm | 10000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3s 2[3/2]* → 2s2.2p5.(2P*<3/2>).3p 2[3/2] | 測定値 | NIST | |
| 659.89529 nm | 10000 | Ne I | emission | 2s2.2p5.(2P*<1/2>).3s 2[1/2]* → 2s2.2p5.(2P*<1/2>).3p 2[1/2] | 測定値 | NIST | |
| 705.91074 nm | 10000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[1/2] → 2s2.2p5.(2P*<1/2>).3d 2[3/2]* | 測定値 | NIST | |
| 576.44189 nm | 7000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[5/2] → 2s2.2p5.(2P*<3/2>).4d 2[7/2]* | 測定値 | NIST | |
| 533.07771 nm | 6000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[1/2] → 2s2.2p5.(2P*<3/2>).4d 2[3/2]* | 測定値 | NIST | |
| 534.3282 nm | 6000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[1/2] → 2s2.2p5.(2P*<3/2>).4d 2[1/2]* | 測定値 | NIST | |
| 597.5534 nm | 6000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3s 2[3/2]* → 2s2.2p5.(2P*<1/2>).3p 2[3/2] | 測定値 | NIST | |
| 475.27311 nm | 5000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[5/2] → 2s2.2p5.(2P*<3/2>).6d 2[7/2]* | 測定値 | NIST | |
| 479.02171 nm | 5000 | Ne I | emission | 2s2.2p5.(2P*<1/2>).3p 2[3/2] → 2s2.2p5.(2P*<1/2>).6d 2[5/2]* | 測定値 | NIST | |
| 483.73128 nm | 5000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[1/2] → 2s2.2p5.(2P*<3/2>).6s 2[3/2]* | 測定値 | NIST | |
| 489.20896 nm | 5000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[3/2] → 2s2.2p5.(2P*<3/2>).7s 2[3/2]* | 測定値 | NIST | |
| 500.51582 nm | 5000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[3/2] → 2s2.2p5.(2P*<1/2>).5d 2[5/2]* | 測定値 | NIST | |
| 503.77504 nm | 5000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[5/2] → 2s2.2p5.(2P*<3/2>).5d 2[7/2]* | 測定値 | NIST | |
| 514.49371 nm | 5000 | Ne I | emission | 2s2.2p5.(2P*<1/2>).3p 2[3/2] → 2s2.2p5.(2P*<1/2>).5d 2[5/2]* | 測定値 | NIST | |
| 514.50308 nm | 5000 | Ne I | emission | 2s2.2p5.(2P*<1/2>).3p 2[3/2] → 2s2.2p5.(2P*<1/2>).5d 2[5/2]* | 測定値 | NIST | |
| 556.27668 nm | 5000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[5/2] → 2s2.2p5.(2P*<1/2>).4d 2[5/2]* | 測定値 | NIST | |
| 565.66578 nm | 5000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[3/2] → 2s2.2p5.(2P*<1/2>).4d 2[5/2]* | 測定値 | NIST | |
| 571.92256 nm | 5000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[3/2] → 2s2.2p5.(2P*<1/2>).4d 2[5/2]* | 測定値 | NIST | |
| 574.82979 nm | 5000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[5/2] → 2s2.2p5.(2P*<3/2>).4d 2[5/2]* | 測定値 | NIST | |
| 580.44496 nm | 5000 | Ne I | emission | 2s2.2p5.(2P*<3/2>).3p 2[5/2] → 2s2.2p5.(2P*<3/2>).4d 2[5/2]* | 測定値 | NIST |
詳細な性質
共有結合半径（詳細）
- 共有結合半径（Pyykkö）
- 67 pm
- 共有結合半径（Pyykkö、二重結合）
- 96 pm
ファンデルワールス半径
- Bondi
- 154 pm
- Alvarez
- 158 pm
- UFF
- 324.3 pm
- MM3
- 160 pm
原子半径と金属半径
- 原子半径（Rahm）
- 156 pm
番号付けの尺度
- Mendeleev
- 113
- Pettifor
- 2
- Glawe
- 2
電気陰性度の尺度
- Ghosh
- 0
- Gunnarsson–Lundqvist
- 7
- Robles–Bartolotti
- 7
分極率と分散
- 双極子分極率
- 2.6611 a.u.
- 双極子分極率（不確かさ）
- 0 a.u.
- C₆
- 6.2 Ha·Bohr6
- C₆ (Gould–Bučko)
- 6.91 Ha·Bohr6
化学親和力
- プロトン親和力
- 198.8 kJ/mol
- 気相塩基性
- 174.4 kJ/mol
希ガスの性質
相転移と同素体
| 融点 | 24.56 K |
| 沸点 | 27.1 K |
| 臨界点（温度） | 44.49 K |
| 臨界点（圧力） | 2.68 MPa |
| 三重点（温度） | 24.56 K |
| 三重点（圧力） | 43.37 kPa |
専門参考データ
遮蔽定数 (3)
| n | 軌道 | σ |
|---|---|---|
| 1 | s | 0.3579 |
| 2 | p | 4.2416 |
| 2 | s | 4.2416 |
同位体の崩壊形式 (35)
| 同位体 | モード | 強度 |
|---|---|---|
| 15 | 2p | 100% |
| 16 | 2p | 100% |
| 17 | B+ | 100% |
| 17 | B+p | 94.4% |
| 17 | B+A | 3.5% |
| 17 | B+pA | 0% |
| 18 | B+ | 100% |
| 19 | B+ | 100% |
| 23 | B- | 100% |
| 24 | B- | 100% |
X線散乱因子 (503)
| エネルギー (eV) | f₁ | f₂ |
|---|---|---|
| 10 | — | 0 |
| 10.1617 | — | 0 |
| 10.3261 | — | 0 |
| 10.4931 | — | 0 |
| 10.6628 | — | 0 |
| 10.8353 | — | 0 |
| 11.0106 | — | 0 |
| 11.1886 | — | 0 |
| 11.3696 | — | 0 |
| 11.5535 | — | 0 |
追加データ
Estimated Crustal Abundance
The estimated element abundance in the earth's crust.
5×10-3 milligrams per kilogram
参考文献 (1)
Estimated Oceanic Abundance
The estimated element abundance in the earth's oceans.
1.2×10-4 milligrams per liter
参考文献 (1)
参考文献
(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 Neon.
The element property data was retrieved from publications.