Oganesson (Og)
noble-gasExpected to be a Gas
मानक परमाणु भार
[294]इलेक्ट्रॉन विन्यास
[Rn] 7s2 7p6 5f14 6d10 (पूर्वानुमानित)गलनांक
उपलब्ध नहींक्वथनांक
-243.15 °Cघनत्व
7000 kg/m³ऑक्सीकरण अवस्थाएँ
−1, 0, +1, +2, +4, +6विद्युतऋणात्मकता (पॉलिंग)
उपलब्ध नहींआयनन ऊर्जा (प्रथम)
उपलब्ध नहींखोज का वर्ष
2006परमाणु त्रिज्या
उपलब्ध नहींविवरण
Oganesson is a synthetic element at the end of period 7 and is placed in group 18 with the noble gases. It has been made only atom by atom in heavy-ion fusion experiments, with the best-established isotope, ²⁹⁴Og, decaying in about a millisecond. Its chemistry has not been observed directly. Relativistic calculations suggest that it may be far less inert than lighter noble gases.
Oganesson does not occur naturally in the Earth’s crust. The name oganesson and symbol Og are the accepted ones for element 118. The name is in line with the tradition of honoring a scientist and recognizes Prof. Yuri Oganessian (Fig. IUPAC.118.1; born 1933) for his pioneering contribution to trans-actinoid element research. His many achievements include the discovery of super-heavy elements and significant advances in the nuclear physics of super-heavy nuclei, including experimental evidence for the “island of stability.”
In 2005, experiments were performed in Dubna’s U-400 cyclotron, where 48Ca bombarded a spinning target of 249Cf at nearly 3×104 km/s to produce oganesson. With the success of creating oganesson, scientists from Livermore and Joint Institute for Nuclear Research (JINR) are starting experiments to create element 120 by bombarding a 244Pu target with a beam of 58Fe [680], [681], [682], [683]. Oganesson has no known isotopic applications aside from scientific research.
On October 16, 2006, scientists working at the Joint Institute for Nuclear Research in Dubna, Russia, along with scientists from the U.S. Department of Energy's Lawrence Livermore National Laboratory, announced the creation of oganesson. They produced oganesson by bombarding atoms of californium-249 with ions of calcium-48. This produced oganesson-294, an isotope with a half-life of about 0.89 milliseconds (0.00089 seconds), and three free neutrons. The californium target was irradiated with a total of 1.6*1019 calcium ions over the course of 1080 hours, resulting in the production of three atoms of oganesson. Oganesson's most stable isotope, oganesson-294, has a half-life of about 0.89 milliseconds. It decays into livermorium-290 through alpha decay.
On Novemer 28th, 2016, element 118 was named Oganesson with the symbol (Og). The name was proposed by the Joint Institute for Nuclear Research, Dubna (Russia) and Lawrence Livermore National Laboratory (USA). It honors Professor Yuri Oganessian (born 1933) for his pioneering contributions to transactinoid elements research.
No macroscopic sample of oganesson has ever existed, so its appearance, density, melting point, and boiling point are not experimentally known. Predictions often treat it as a condensed, highly polarizable substance under ordinary conditions, but this remains theoretical.
Oganesson has no practical, commercial, medical, or industrial use. Its value is confined to nuclear research, where a few atoms can test models of superheavy nuclei, alpha decay, spontaneous fission, and the limits of the periodic table. The element cannot be stored or accumulated in useful quantities because its known nuclei decay almost immediately after formation.
Since only a few atoms of oganesson have ever been produced, it currently has no uses outside of basic scientific research.
No compound of oganesson has been experimentally prepared or characterized. Its possible chemistry is inferred from relativistic quantum calculations, which predict unusually strong spin-orbit effects and high polarizability for a group 18 element. Hypothetical species such as oganesson difluoride (OgF₂), oganesson tetrafluoride (OgF₄), and oxides have been discussed, but their stability, structures, and oxidation states are not established by experiment.
See more information at the Oganesson compound page.
The immediate hazard of oganesson is radiological rather than chemical. Known atoms decay by alpha emission and through radioactive daughter nuclei on extremely short timescales. Because only a few atoms are produced in shielded accelerator targets, ordinary chemical exposure is not a realistic scenario. Target materials and reaction products require standard controls for radioactive heavy-element experiments.
Oganesson has no confirmed natural occurrence and no known environmental cycle. Any atoms made in laboratories decay long before they could disperse as a chemical contaminant. Environmental considerations are therefore associated with accelerator operations, irradiated targets, and radioactive residues, not with persistent oganesson itself.
Oganesson has no commodity market, no industrial supply chain, and no recoverable stock. It is produced only in specialized nuclear laboratories by bombarding rare actinide targets, notably californium-249 (²⁴⁹Cf), with calcium-48 (⁴⁸Ca) ions. Production depends on scarce target isotopes, long accelerator runs, and detection of individual decay chains. Substitution and recycling are not meaningful concepts for the element itself.
Made by bombarding californium-249 with calcium-48.
Oganesson is not expected to be a persistent cosmic element because its known nuclei are far too unstable. Superheavy nuclei may be formed transiently in extreme nucleosynthetic environments, but no natural or extraterrestrial oganesson has been confirmed. Its relevance to astrophysics is mainly through theoretical work on nuclear stability at very high atomic number.
- Oganesson is the heaviest element with an officially approved name.
- Its placement under radon does not mean its chemistry is known to resemble radon closely.
- The name honors nuclear physicist Yuri Oganessian.
- Individual oganesson atoms are identified through correlated decay chains, not by weighing or isolating the element.
- Relativistic effects are expected to be central to any real oganesson chemistry.
चित्र
गुण
भौतिक
- घनत्व
- 7000 kg/m³ सभी तत्वों की घनत्व की तुलना करें →
- STP पर प्रावस्था
- गैस सभी तत्वों की STP पर प्रावस्था की तुलना करें →
- क्वथनांक
- -243.15 °C सभी तत्वों की क्वथनांक की तुलना करें →
रासायनिक
- इलेक्ट्रॉन बंधुता
- 0.056 eV
- ऑक्सीकरण अवस्थाएँ
- −1, 0, +1, +2, +4, +6 सभी तत्वों की ऑक्सीकरण अवस्थाएँ की तुलना करें →
- संयोजकता इलेक्ट्रॉन
- 8 सभी तत्वों की संयोजकता इलेक्ट्रॉन की तुलना करें →
- इलेक्ट्रॉन विन्यास
- [Rn] 7s2 7p6 5f14 6d10 (पूर्वानुमानित)
ऊष्मागतिक
उपलब्ध नहीं
नाभिकीय
- प्रोटॉन
- 118 सभी तत्वों की प्रोटॉन की तुलना करें →
- न्यूट्रॉन
- 175 सभी तत्वों की न्यूट्रॉन की तुलना करें →
- ज्ञात समस्थानिक
- 2 सभी तत्वों की ज्ञात समस्थानिक की तुलना करें →
- स्थिर समस्थानिक
- 0 सभी तत्वों की स्थिर समस्थानिक की तुलना करें →
- द्रव्यमान संख्या (सबसे स्थिर)
- 294
- सबसे स्थिर समस्थानिक
- Og-293
- खोज का वर्ष
- 2006
प्रचुरता
उपलब्ध नहीं
क्रिस्टल संरचना
उपलब्ध नहीं
इलेक्ट्रॉनिक संरचना
- प्रति कोश इलेक्ट्रॉन
- 14, 10, 8 सभी तत्वों की प्रति कोश इलेक्ट्रॉन की तुलना करें →
पहचानकर्ता
- CAS संख्या
- 54144-19-3 सभी तत्वों की CAS संख्या की तुलना करें →
- InChI
- InChI=1S/Og
- InChI कुंजी
- GOANEQIZDYDFCO-UHFFFAOYSA-N
इलेक्ट्रॉन विन्यास पूर्वानुमानित
——इस आयन के लिए इलेक्ट्रॉन विन्यास का डेटा उपलब्ध नहीं है।
परमाणु मॉडल
समस्थानिक न्यूट्रॉन की संख्या, द्रव्यमान और स्थिरता बदलते हैं — उदासीन परमाणु का इलेक्ट्रॉन विन्यास नहीं।
उपलब्ध नहीं
सांकेतिक परमाणु मॉडल, वास्तविक अनुपात में नहीं।
परमाणु पहचान-चिह्न
उत्सर्जन / अवशोषण स्पेक्ट्रम
समस्थानिक वितरण
कोई स्थिर समस्थानिक नहीं है।
| द्रव्यमान संख्या | परमाणु द्रव्यमान (u) | प्राकृतिक प्रचुरता | अर्धायु |
|---|---|---|---|
| 293 रेडियोधर्मी | 293.21356 ± 0.00078 | उपलब्ध नहीं | 1 ms |
| 294 रेडियोधर्मी | 294.21392 ± 0.00071 | उपलब्ध नहीं | 0.7 ms |
प्रावस्था / अवस्था
कारण: क्वथनांक (-243.15 °C) से 268.1 °C अधिक
सांकेतिक, वास्तविक अनुपात में नहीं
प्रावस्था संक्रमण बिंदु
घनत्व
मानक परिस्थितियों में
वर्तमान T पर आदर्श गैस नियम से अनुमानित
ठोस प्रावस्था के लिए क्रिस्टल संरचना का डेटा उपलब्ध नहीं है
समस्थानिक (2)
| द्रव्यमान संख्या | परमाणु द्रव्यमान (u) | प्राकृतिक प्रचुरता | अर्धायु | क्षय का प्रकार | |
|---|---|---|---|---|---|
| 293 रेडियोधर्मी | 293.21356 ± 0.00078 | उपलब्ध नहीं | 1 ms | α ? | |
| 294 रेडियोधर्मी | 294.21392 ± 0.00071 | उपलब्ध नहीं | 0.7 ms | α ≈100%SF ? |
विस्तृत गुण
सहसंयोजक त्रिज्याएँ (विस्तृत)
- सहसंयोजक त्रिज्या (प्यूक्को)
- 157 pm
संख्यांकन मापक्रम
- Mendeleev
- 118
ध्रुवणीयता और परिक्षेपण
- द्विध्रुव ध्रुवणीयता
- 58 a.u.
- द्विध्रुव ध्रुवणीयता (अनिश्चितता)
- 6 a.u.
उत्कृष्ट गैसों के गुण
ऑक्सीकरण अवस्था की श्रेणियाँ
उन्नत संदर्भ डेटा
समस्थानिक क्षय के प्रकार (3)
| समस्थानिक | मोड | तीव्रता |
|---|---|---|
| 293 | A | — |
| 294 | A | 100% |
| 294 | SF | — |
अतिरिक्त डेटा
Estimated Crustal Abundance
The estimated element abundance in the earth's crust.
Not Applicable
संदर्भ (1)
- [5] Oganesson https://education.jlab.org/itselemental/ele118.html
Estimated Oceanic Abundance
The estimated element abundance in the earth's oceans.
Not Applicable
संदर्भ (1)
- [5] Oganesson https://education.jlab.org/itselemental/ele118.html
संदर्भ
(8)
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.
This section provides all form of data related to element Oganesson.