Tennessine

Tennessine sī chhiau-tāng (superheavy) jîn-chō goân-sò͘ chi̍t khoán, goân-chú-hoan 117, hû-hō Ts.

Tennessine,  ₁₁₇Ts

Ki-pún sèng-chit
Miâ, hû-hō	tennessine, Ts
Gōa-hêng	poàn-kim-sio̍k (ū-chhek)[1]
Tennessine tī chiu-kî-piáu lāi ê ūi-tì
At ↑ Ts ↓ (Usu) livermorium ← tennessine → oganesson
Goân-chú-hoan	117
Goân-chú-liōng	[294]
Goân-sò͘ lūi-pia̍t	boē tiāⁿ m̄-koh khó-lêng sī āu-kòe-tō͘ kim-sio̍k[2][3]
Cho̍k, hun-khu	17 cho̍k, p khu
Chiu-kî	tē 7 chiu-kî
Tiān-chú pâi-lia̍t	[Rn] 5f14 6d10 7s2 7p5 (ū-chhek)[4]
per shell	2, 8, 18, 32, 32, 18, 7 (ū-chhek)
Bu̍t-lí sèng-chit
Siòng	kò͘-siōng (ū-chhek)[4][5]
Iûⁿ-tiám	623–823 K ​(350–550 °C, ​662–1022 °F) (ū-chhek)[4]
Hut-tiám	883 K ​(610 °C, ​1130 °F) (ū-chhek)[4]
Bi̍t-tō͘  (sek-un)	7.1–7.3 g·cm−3 (extrapolated)[5]
Goân-chú sèng-chit
Sng-hòa-sò͘	−1, +1, +3, +5 ​(ū-chhek)[1][4]
Tiān-lī-lêng	1st: 742.9 kJ·mol−1 (ū-chhek)[4] 2nd: 1785.0–1920.1 kJ·mol−1 (extrapolated)[5]
Goân-chú pòaⁿ-kèng	empirical: 138 pm (ū-chhek)[5]
Kiōng-kè pòaⁿ-kèng	156–157 pm (extrapolated)[5]
Cha̍p-lio̍k
CAS teng-kì pian-hō	54101-14-3
Le̍k-sú
Hō-miâ	Tennessee
Hoat-hiān	Joint Institute for Nuclear Research kap Lawrence Livermore National Laboratory (2010)
Chòe ún-tēng ê tông-ūi-sò͘
Chú bûn-chiong: tennessine ê tông-ūi-sò͘
iso NA half-life DM DE (MeV) DP 294Ts[6] syn 51+41 −16 ms α 10.81 290Mc 293Ts[7] syn 22+8 −4 ms α 11.11, 11.00, 10.91 289Mc

Pún goân-sò͘ sī 2010 nî Lō͘-se-a kap Bí-kok ha̍p-chok ê gián-kiù ùi Dubna soan-pò͘--ê, kàu 2016 nî ûi-chí, sī siāng sin hoat-kiàn ê goân-sò͘. Hō-miâ ê lâi-goân sī Tennessee, Bí-kok ê chi̍t chiu.

Chham-khó

1. Fricke, B. (1975). "Superheavy elements: a prediction of their chemical and physical properties". Recent Impact of Physics on Inorganic Chemistry. 21: 89–144. doi:10.1007/BFb0116498. 4 October 2013 khòaⁿ--ê.
2. Royal Society of Chemistry (2016). "Ununseptium". rsc.org. Royal Society of Chemistry. 9 November 2016 khòaⁿ--ê. A highly radioactive metal, of which only a few atoms have ever been made.
3. GSI (14 December 2015). "Research Program – Highlights". superheavies.de. GSI. goân-loē-iông tī 2020-05-13 hőng khó͘-pih. 9 November 2016 khòaⁿ--ê. If this trend were followed, element 117 would likely be a rather volatile metal. Fully relativistic calculations agree with this expectation, however, they are in need of experimental confirmation.
4. Hoffman, D. C.; Lee, D. M.; Pershina, V. (2006). "Transactinides and the future elements". Chū Morss; Edelstein, N. M.; Fuger, J. The Chemistry of the Actinide and Transactinide Elements (3rd pán.). Springer Science+Business Media. pp. 1652–1752. ISBN 1-4020-3555-1.
5. Bonchev, D.; Kamenska, V. (1981). "Predicting the Properties of the 113–120 Transactinide Elements". Journal of Physical Chemistry. 85 (9): 1177–1186. doi:10.1021/j150609a021.
6. Oganessian, Yu. Ts.; et al. (2013). "Experimental studies of the ²⁴⁹Bk + ⁴⁸Ca reaction including decay properties and excitation function for isotopes of element 117, and discovery of the new isotope ²⁷⁷Mt". Physical Review C. 87 (5): 054621. Bibcode:2013PhRvC..87e4621O. doi:10.1103/PhysRevC.87.054621.
7. Khuyagbaatar, J.; Yakushev, A.; Düllmann, Ch. E.; et al. (2014). "⁴⁸Ca+²⁴⁹Bk Fusion Reaction Leading to Element Z=117: Long-Lived α-Decaying ²⁷⁰Db and Discovery of ²⁶⁶Lr". Physical Review Letters. 112 (17): 172501. doi:10.1103/PhysRevLett.112.172501.