Rutherfordium: Béda antara owahan

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'''Rutherfordium''' ({{pronEng|ˌrʌðɚˈfɔrdiəm}}) kuwi sawijining [[unsur kimia]] jroning [[Tabel périodik]] kanthi simbul '''Rf''' lan [[nomer atom]] [[104]].
'''Rutherfordium''' ({{pronEng|ˌrʌðɚˈfɔrdiəm}}) iku sawijining [[unsur kimia]] jroning [[Tabel périodik]] kanthi simbul '''Rf''' lan [[nomer atom]] [[104]].
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{{Listen|filename=rutherfordium.ogg|title=Rutherfordium|description=Common English pronunciation of rutherfordium|format=[[Ogg]]}}
This is a [[radioactive]] [[synthetic element]] whose most stable known [[isotope]] is <sup>267</sup>Rf with a [[half-life]] of approximately 1.3 hours. Chemistry experiments have confirmed that rutherfordium behaves as the heavier homologue to hafnium in group 4 (see below).
This is a [[radioactive]] [[synthetic element]] whose most stable known [[isotope]] is <sup>267</sup>Rf with a [[half-life]] of approximately 1.3 hours. Chemistry experiments have confirmed that rutherfordium behaves as the heavier homologue to hafnium in group 4 (see below).


==Official discovery==
==Official discovery==
Element 104 was reportedly [[discovery of the chemical elements|first detected]] in 1966 at the [[JINR|Joint Institute of Nuclear Research ]] at [[Dubna]] ([[U.S.S.R.]]). Researchers there bombarded <sup>242</sup>[[plutonium|Pu]] with accelerated <sup>22</sup>[[neon|Ne]] [[ion]]s and separated the reaction products by gradient thermochromatography after conversion to chlorides by interaction with ZrCl<sub>4</sub>. The team identified a [[spontaneous fission]] activity contained within a volatile chloride portraying eka-hafnium properties. Although a half-life was not accurately determined, later calculations indicated that the product was most likely <sup>259</sup>Rf:<ref name=93TWG>[http://www.iupac.org/publications/pac/1993/pdf/6508x1757.pdf "DISCOVERY OF THE TRANSFERMIUM ELEMENTS"], '''IUPAC/IUPAP Technial Report''', ''Pure & Appl. Chem.'', Vol. 65, No. 8, pp. 1757-1814,1993. Retrieved on [[2008-03-04]]</ref>
Element 104 was reportedly [[discovery of the chemical elements|first detected]] in 1966 at the [[JINR|Joint Institute of Nuclear Research ]] at [[Dubna]] ([[U.S.S.R.]]). Researchers there bombarded <sup>242</sup>[[plutonium|Pu]] with accelerated <sup>22</sup>[[neon|Ne]] [[ion]]s and separated the reaction products by gradient thermochromatography after conversion to chlorides by interaction with ZrCl<sub>4</sub>. The team identified a [[spontaneous fission]] activity contained within a volatile chloride portraying eka-hafnium properties. Although a half-life was not accurately determined, later calculations indicated that the product was most likely <sup>259</sup>Rf:<ref name=93TWG>[http://www.iupac.org/publications/pac/1993/pdf/6508x1757.pdf "DISCOVERY OF THE TRANSFERMIUM ELEMENTS"], '''IUPAC/IUPAP Technial Report''', ''Pure & Appl. Chem.'', Vol. 65, No. 8, pp. 1757-1814,1993. Retrieved on [[2008-03-04]]</ref>


:<math>\, ^{242}_{94}\mathrm{Pu} + \, ^{22}_{10}\mathrm{Ne} \to \, ^{264-x}_{104}\mathrm{Rf}\to \,^{264-x}_{104}\mathrm{RfCl}_{4}</math>
:<math>\, ^{242}_{94}\mathrm{Pu} + \, ^{22}_{10}\mathrm{Ne} \to \, ^{264-x}_{104}\mathrm{Rf}\to \,^{264-x}_{104}\mathrm{RfCl}_{4}</math>
Larik 87: Larik 86:
===Chemistry===
===Chemistry===
In an analogous manner to zirconium and hafnium, rutherfordium is projected to form a very stable, high melting point oxide, RfO<sub>2</sub>. It should also react with halogens to form tetrahalides, RfX<sub>4</sub>, which hydrolyse on contact with water to form oxyhalides RfOX<sub>2</sub>. The tetrahalides should be volatile solids existing as monomeric tetrahedral molecules in the vapour phase.
In an analogous manner to zirconium and hafnium, rutherfordium is projected to form a very stable, high melting point oxide, RfO<sub>2</sub>. It should also react with halogens to form tetrahalides, RfX<sub>4</sub>, which hydrolyse on contact with water to form oxyhalides RfOX<sub>2</sub>. The tetrahalides should be volatile solids existing as monomeric tetrahedral molecules in the vapour phase.
In the aqueous phase, the Rf<sup>4+</sup> ion should hydrolyse less than titanium(IV) and to a similar extent to zirconium and hafnium, thus leading to the rutherfordyl oxyion, RfO<sub>2</sub><sup>2+</sup>. Treatment of the halides with halide ions promotes the formation of complex ions. The use of chloride and bromide ion should form the hexahalide complexes RfCl<sub>6</sub><sup>2-</sup> and RfBr<sub>6</sub><sup>2-</sup>. For the fluoride complexes, [[zirconium]] and [[hafnium]] tend to form hepta- and octa- complexes. Thus, for the larger rutherfordium ion, the complexes RfF<sub>6</sub><sup>2-</sup>, RfF<sub>7</sub><sup>3-</sup> and RfF<sub>8</sub><sup>4-</sup> are possible.
In the aqueous phase, the Rf<sup>4+</sup> ion should hydrolyse less than titanium(IV) and to a similar extent to zirconium and hafnium, thus leading to the rutherfordyl oxyion, RfO<sub>2</sub><sup>2+</sup>. Treatment of the halides with halide ions promotes the formation of complex ions. The use of chloride and bromide ion should form the hexahalide complexes RfCl<sub>6</sub><sup>2-</sup> and RfBr<sub>6</sub><sup>2-</sup>. For the fluoride complexes, [[zirconium]] and [[hafnium]] tend to form hepta- and octa- complexes. Thus, for the larger rutherfordium ion, the complexes RfF<sub>6</sub><sup>2-</sup>, RfF<sub>7</sub><sup>3-</sup> and RfF<sub>8</sub><sup>4-</sup> are possible.


==Experimental chemistry==
==Experimental chemistry==
Larik 141: Larik 140:
<ref>[http://www.springerlink.com/content/m87v320736564810/ "Experiments on the synthesis of neutron-deficient isotopes of kurchatovium in reactions with accelerated <sup>50</sup>Ti ions"], '''Oganesyan et al'''., ''Nucl. Phys. A.'', 1975, 36, 6. Retrieved on [[2008-02-29]]</ref>
<ref>[http://www.springerlink.com/content/m87v320736564810/ "Experiments on the synthesis of neutron-deficient isotopes of kurchatovium in reactions with accelerated <sup>50</sup>Ti ions"], '''Oganesyan et al'''., ''Nucl. Phys. A.'', 1975, 36, 6. Retrieved on [[2008-02-29]]</ref>
The reaction was further studied in 1985 by the GSI team who measured the decay properties of the isotopes <sup>257</sup>Rf and <sup>256</sup>Rf. The team were able to determine some initial spectroscopic properties of <sup>257</sup>Rf and found that the alpha decay pattern was very complicated.
The reaction was further studied in 1985 by the GSI team who measured the decay properties of the isotopes <sup>257</sup>Rf and <sup>256</sup>Rf. The team were able to determine some initial spectroscopic properties of <sup>257</sup>Rf and found that the alpha decay pattern was very complicated.
<ref>[http://www.springerlink.com/content/g721435j48022485/ "Study of evaporation residues produced in reactions of <sup>207</sup>,<sup>208</sup>Pb with <sup>50</sup>Ti"], '''Hessberger et al.''', ''Z. Physik'' ,1984, 316, 19-26. Retrieved on [[2008-02-29]]</ref>
<ref>[http://www.springerlink.com/content/g721435j48022485/ "Study of evaporation residues produced in reactions of <sup>207</sup>,<sup>208</sup>Pb with <sup>50</sup>Ti"], '''Hessberger et al.''', ''Z. Physik'' ,1984, 316, 19-26. Retrieved on [[2008-02-29]]</ref>


After an upgrade of their facilities, they repeated the reaction in 1994 with much higher sensitivity and detected some 1100 atoms of <sup>257</sup>Rf and 1900 atoms of <sup>256</sup>Rf along with <sup>255</sup>Rf in the measurement of the 1n,2n and 3n excitation functions. The large amount of decay data for <sup>257</sup>Rf allowed the detection of an isomeric level and the construction of a partial decay level structure which confirmed the very complicated alpha decay pattern. They also found evidence for an isomeric level in <sup>255</sup>Rf.
After an upgrade of their facilities, they repeated the reaction in 1994 with much higher sensitivity and detected some 1100 atoms of <sup>257</sup>Rf and 1900 atoms of <sup>256</sup>Rf along with <sup>255</sup>Rf in the measurement of the 1n,2n and 3n excitation functions. The large amount of decay data for <sup>257</sup>Rf allowed the detection of an isomeric level and the construction of a partial decay level structure which confirmed the very complicated alpha decay pattern. They also found evidence for an isomeric level in <sup>255</sup>Rf.
Larik 151: Larik 150:
===<sup>207</sup>Pb(<sup>50</sup>Ti,xn)<sup>257-x</sup>Rf (x=2)===
===<sup>207</sup>Pb(<sup>50</sup>Ti,xn)<sup>257-x</sup>Rf (x=2)===
This reaction was first studied in 1974 by the team at Dubna. They measured a spontaneous fission activity assigned to <sup>255</sup>Rf. The reaction was further studied in 1985 by the GSI team who measured the decay properties of the isotope <sup>255</sup>Rf. A further spectroscopic study was reported in 2000 which led to a first decay level scheme for the isotope.<ref>[http://www.edpsciences.org/articles/epja/abs/2001/09/epja1103/epja1103.html "Decay properties of neutron-deficient isotopes <sup>256,257</sup>Db, <sup>255</sup>Rf, <sup>252,253</sup>Lr"], '''Hessberger et al.''', ''Eur. Phys. J.'', A 12, 57-67 (2001). Retrieved on [[2008-02-29]]</ref> The isomeric level proposed in 1994 was not found. In 2006, the spectroscopy was continued and the decay scheme was confirmed and improved.
This reaction was first studied in 1974 by the team at Dubna. They measured a spontaneous fission activity assigned to <sup>255</sup>Rf. The reaction was further studied in 1985 by the GSI team who measured the decay properties of the isotope <sup>255</sup>Rf. A further spectroscopic study was reported in 2000 which led to a first decay level scheme for the isotope.<ref>[http://www.edpsciences.org/articles/epja/abs/2001/09/epja1103/epja1103.html "Decay properties of neutron-deficient isotopes <sup>256,257</sup>Db, <sup>255</sup>Rf, <sup>252,253</sup>Lr"], '''Hessberger et al.''', ''Eur. Phys. J.'', A 12, 57-67 (2001). Retrieved on [[2008-02-29]]</ref> The isomeric level proposed in 1994 was not found. In 2006, the spectroscopy was continued and the decay scheme was confirmed and improved.
<ref>[http://www.edpsciences.org/articles/epja/abs/2006/15/10050_2006_Article_100239/10050_2006_Article_100239.html "Alpha-gamma decay studies of <sup>255</sup>Rf, <sup>251</sup>No and <sup>247</sup>Fm"], '''Hessberger et al'''., ''Eur. Phys. J. A 30'', 561-569 (2006). Retrieved on [[2008-03-04]]</ref>
<ref>[http://www.edpsciences.org/articles/epja/abs/2006/15/10050_2006_Article_100239/10050_2006_Article_100239.html "Alpha-gamma decay studies of <sup>255</sup>Rf, <sup>251</sup>No and <sup>247</sup>Fm"], '''Hessberger et al'''., ''Eur. Phys. J. A 30'', 561-569 (2006). Retrieved on [[2008-03-04]]</ref>


===<sup>206</sup>Pb(<sup>50</sup>Ti,xn)<sup>256-x</sup>Rf (x=1,2)===
===<sup>206</sup>Pb(<sup>50</sup>Ti,xn)<sup>256-x</sup>Rf (x=1,2)===
Larik 179: Larik 178:
The reaction was further studied in 2000 by Yuri Lazarev and the team at Dubna. They were able to observe 69 alpha decays from <sup>261</sup>Rf and [[spontaneous fission]] of <sup>262</sup>Rf.
The reaction was further studied in 2000 by Yuri Lazarev and the team at Dubna. They were able to observe 69 alpha decays from <sup>261</sup>Rf and [[spontaneous fission]] of <sup>262</sup>Rf.
<ref>[http://prola.aps.org/abstract/PRC/v62/i6/e064307 "Decay properties of <sup>257</sup>No, <sup>261</sup>Rf, and <sup>262</sup>Rf"], '''Lazarev et al.''', ''Phys. Rev. C 62'', 064307 (2000). Retrieved on [[2008-03-04]]</ref>
<ref>[http://prola.aps.org/abstract/PRC/v62/i6/e064307 "Decay properties of <sup>257</sup>No, <sup>261</sup>Rf, and <sup>262</sup>Rf"], '''Lazarev et al.''', ''Phys. Rev. C 62'', 064307 (2000). Retrieved on [[2008-03-04]]</ref>
Later work on [[hassium]] has allowed a reassignment of the 5n product to <sup>261m</sup>Rf.
Later work on [[hassium]] has allowed a reassignment of the 5n product to <sup>261m</sup>Rf.


===<sup>242</sup>Pu(<sup>22</sup>Ne,xn)<sup>264-x</sup>Rf (x=3,4?,5?)===
===<sup>242</sup>Pu(<sup>22</sup>Ne,xn)<sup>264-x</sup>Rf (x=3,4?,5?)===
Larik 208: Larik 207:


===<sup>248</sup>Cm(<sup>16</sup>O,xn)<sup>264-x</sup>Rf (x=4)===
===<sup>248</sup>Cm(<sup>16</sup>O,xn)<sup>264-x</sup>Rf (x=4)===
This reaction was studied in 1969 by Albert Ghiorso at the University of California. The aim was to detect the 0.1-0.3 s SF activity reported at Dubna, assigned to <sup>260</sup>104. They were unable to do so, only observing a 10-30 ms SF activity, correctly assigned to <sup>260</sup>104. The failure to observe the 0.3 s SF activity identified by Dubna gave the Americans the incentive to name this element ''rutherfordium''.<ref name=93TWG/>
This reaction was studied in 1969 by Albert Ghiorso at the University of California. The aim was to detect the 0.1-0.3 s SF activity reported at Dubna, assigned to <sup>260</sup>104. They were unable to do so, only observing a 10-30 ms SF activity, correctly assigned to <sup>260</sup>104. The failure to observe the 0.3 s SF activity identified by Dubna gave the Americans the incentive to name this element ''rutherfordium''.<ref name=93TWG/>


===<sup>246</sup>Cm(<sup>18</sup>O,xn)<sup>264-x</sup>Rf===
===<sup>246</sup>Cm(<sup>18</sup>O,xn)<sup>264-x</sup>Rf===
In an attempt to unravel the properties of [[spontaneous fission]] activities in the formation of rutherfordium isotopes, this reaction was performed in 1976 by the FLNR. They observed an 80 ms SF activity. Subsequent work led to the complete retraction of the 0.3s - 0.1s - 80 ms SF activities observed by the Dubna team and associated with background signals.<ref name=93TWG/>
In an attempt to unravel the properties of [[spontaneous fission]] activities in the formation of rutherfordium isotopes, this reaction was performed in 1976 by the FLNR. They observed an 80 ms SF activity. Subsequent work led to the complete retraction of the 0.3s - 0.1s - 80 ms SF activities observed by the Dubna team and associated with background signals.<ref name=93TWG/>


===<sup>249</sup>Bk(<sup>15</sup>N,xn)<sup>264-x</sup>Rf (x=4)===
===<sup>249</sup>Bk(<sup>15</sup>N,xn)<sup>264-x</sup>Rf (x=4)===
This reaction was studied in 1977 by the team in Dubna. They were able to confirm the detection of a 76 ms SF activity. The assignment to rutherfordium isotopes was later retracted.
This reaction was studied in 1977 by the team in Dubna. They were able to confirm the detection of a 76 ms SF activity. The assignment to rutherfordium isotopes was later retracted.
The LBNL re-studied the reaction in 1980 and in 1981 they reported that they were unable to confirm the ~80 ms SF activity. The Dubna team were able to measure a 28 ms SF activity in 1985 and assigned the isotope correctly to <sup>260</sup>104.<ref name=93TWG/>
The LBNL re-studied the reaction in 1980 and in 1981 they reported that they were unable to confirm the ~80 ms SF activity. The Dubna team were able to measure a 28 ms SF activity in 1985 and assigned the isotope correctly to <sup>260</sup>104.<ref name=93TWG/>


===<sup>249</sup>Cf(<sup>13</sup>C,xn)<sup>262-x</sup>Rf (x=4)===
===<sup>249</sup>Cf(<sup>13</sup>C,xn)<sup>262-x</sup>Rf (x=4)===
This use of californium-249 as a target was first studied by Albert Ghiorso and the team at the University of California in 1969. They were able to observe a 11 ms SF activity which they correctly assigned to <sup>258</sup>104.<ref name=69Gh01/>
This use of californium-249 as a target was first studied by Albert Ghiorso and the team at the University of California in 1969. They were able to observe a 11 ms SF activity which they correctly assigned to <sup>258</sup>104.<ref name=69Gh01/>


===<sup>249</sup>Cf(<sup>12</sup>C,xn)<sup>261-x</sup>Rf (x=3,4)===
===<sup>249</sup>Cf(<sup>12</sup>C,xn)<sup>261-x</sup>Rf (x=3,4)===
Larik 370: Larik 369:
===<sup>268</sup>Rf===
===<sup>268</sup>Rf===
In the synthesis of [[ununpentium]], the isotope <sup>288</sup>115 has been observed to decay to <sup>268</sup>Db which undergoes [[spontaneous fission]] with a half life of 29 hours. Given that the [[electron capture]] of <sup>268</sup>Db cannot be detected, these SF events may in fact be due to the SF of <sup>268</sup>Rf, in which case the half-life of this isotope cannot be extracted.
In the synthesis of [[ununpentium]], the isotope <sup>288</sup>115 has been observed to decay to <sup>268</sup>Db which undergoes [[spontaneous fission]] with a half life of 29 hours. Given that the [[electron capture]] of <sup>268</sup>Db cannot be detected, these SF events may in fact be due to the SF of <sup>268</sup>Rf, in which case the half-life of this isotope cannot be extracted.
<ref name=E115ref/>
<ref name=E115ref/>


===<sup>266</sup>Rf===
===<sup>266</sup>Rf===
Larik 378: Larik 377:
==Retracted isotopes==
==Retracted isotopes==
===<sup>265</sup>Rf===
===<sup>265</sup>Rf===
In 1999, American scientists at the University of California, Berkeley, announced that they has succeeded in synthesizing three atoms of <sup>293</sup>118. These parent nuclei successively emitted seven alpha particles to form <sup>265</sup>Rf nuclei. Their claim was retracted in 2001. As such, this rutherfordium isotope is unconfirmed or unknown.<ref>see [[ununoctium]]</ref>
In 1999, American scientists at the University of California, Berkeley, announced that they has succeeded in synthesizing three atoms of <sup>293</sup>118. These parent nuclei successively emitted seven alpha particles to form <sup>265</sup>Rf nuclei. Their claim was retracted in 2001. As such, this rutherfordium isotope is unconfirmed or unknown.<ref>see [[ununoctium]]</ref>


===<sup>255m</sup>Rf===
===<sup>255m</sup>Rf===
Larik 484: Larik 483:
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{{Tabel périodik unsur kimia}}
{{Tabel périodik unsur kimia}}
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Révisi kala 29 Fèbruari 2016 13.16

104 lawrenciumrutherfordiumdubnium
Hf

Rf

(Upq)
Katrangan Umum Unsur
Jeneng, Lambang, Nomer atom rutherfordium, Rf, 104
Dhèrèt kimia logam transisi
Golongan, Période, Blok 4, 7, d
Massa atom [267] g/mol
Konfigurasi elektron [Rn] 5f14 6d2 7s2
Cacahing èlèktron saben kulit 2, 8, 18, 32, 32, 10, 2
Ciri-ciri fisik
Fase presumably a padhet
Massa jenis (watara suhu kamar) ora dimangertèni g/cm³
Ciri-ciri atom
Struktur kristal ora dimangertèni
Bilangan oksidasi 4
Energi ionisasi pertama: ora dimangertèni kJ/mol
Jari-jari atom (terhitung) ora dimangertèni pm
Jari-jari kovalen ora dimangertèni pm
Lain-lain
Nomor CAS 53850-36-5
Isotop
iso NA waktu paruh DM DE (MeV) DP
267Rf syn 1.3 h SF
263mRf syn ~15 m SF
α 7.90 ?
263gRf syn 8 s SF
262Rf syn 2.1 s SF
261mRf syn 1.1 m α 8.28 257No
261gRf syn 3.7 s 83% SF
17% α 8.52 257No
260Rf syn 20 ms SF
259Rf syn 3.1 s 93% α 8.87,8.77 255No
7% SF
258Rf syn 13 ms SF
257mRf syn 4.0 s α 9.02,8.97 253No
257gRf syn 3.5 s 89% α 8.90,8.78,8.52,8.28 253No
11% ε 257Lr
256Rf syn 6.2 ms 99.7% SF
0.3% α 8.79 252No
255Rf syn 1.8 s ~50% α 8.81,8.77,8.74,8.71 251No
~50% SF
254Rf syn 0.022 ms SF
253Rf syn 0.048 ms SF
Referensi

Rutherfordium (uniné /ˌrʌðɚˈfɔrdiəm/) iku sawijining unsur kimia jroning Tabel périodik kanthi simbul Rf lan nomer atom 104.

Sintesis isotop minangka produk turunan (decay)

Sisa/residu Evaporasi Isotop Rf kang katon
288115 268Rf (manawa EC saka 268Db)
291116 , 287114 , 283112 267Rf
282113 266Rf (EC of 266Db)
271Hs 263gRf
263Db 263mRf (EC of 263Db)
266Sg (possibly 266mSg) 262Rf (possibly 262mRf)
277112 , 273Ds , 269Hs , 265Sg 261mRf , 261Rf
271Ds , 267Hs , 263Sg 259Rf
269Ds , 265Hs , 261Sg 257Rf
264Hs , 260Sg 256Rf
259Sg 255Rf

Kronologi temon isotop

Isotop Taun ditemokaké reaksi
253Rf 1994 204Pb(50Ti,n) [1]
254Rf 1994 206Pb(50Ti,2n) [1]
255Rf 1974? 1985 207Pb(50Ti,2n)
256Rf 1974? 1985 208Pb(50Ti,2n)
257Rfg,m 1969 249Cf(12C,4n) [2]
258Rf 1969 249Cf(13C,4n) [2]
259Rf 1969 249Cf(13C,3n) [2]
260Rf 1969 248Cm(16O,4n)
261Rfm 1970 248Cm(18O,5n) [3]
261Rfg 1996 208Pb(70Zn,n) [4]
262Rf 1996 244Pu(22Ne,4n) [5]
263Rfm 1990? 248Cm(18O,3n)
263Rfg 2004 248Cm(26Mg,3n) [6]
264Rf unknown
265Rf unknown
266Rf 2006? 237Np(48Ca,3n) [7]
267Rf 2003/2004 238U(48Ca,3n) [4]
268Rf 2003? 243Am(48Ca,3n) [8]

Kasil kimia saka isotop

Fusi adhem

Proyektil Target CN 1n 2n 3n
50Ti 208Pb 258Rf 38.0 nb , 17.0 MeV 12.3 nb , 21.5 MeV 660 pb , 29.0 MeV
50Ti 207Pb 257Rf 4.8 nb
50Ti 206Pb 256Rf 800 pb , 21.5 MeV 2.4 nb , 21.5 MeV
50Ti 204Pb 254Rf 190 pb , 15.6 MeV
48Ti 208Pb 256Rf 380 pb , 17.0 MeV

Fusi panas

Proyektil Target CN 3n 4n 5n
26Mg 238U 264Rf 240 pb 1.1 nb
22Ne 244Pu 266Rf + 4.0 nb
18O 248Cm 266Rf + 13.0 nb

Rujukan

  1. a b Masalah sitiran: Tenger <ref> ora trep; ora ana tèks tumrap refs kanthi jeneng 97He01
  2. a b c Masalah sitiran: Tenger <ref> ora trep; ora ana tèks tumrap refs kanthi jeneng 69Gh01
  3. Masalah sitiran: Tenger <ref> ora trep; ora ana tèks tumrap refs kanthi jeneng 70Gh01
  4. a b see ununbium
  5. Masalah sitiran: Tenger <ref> ora trep; ora ana tèks tumrap refs kanthi jeneng 96La01
  6. see hassium
  7. see ununtrium
  8. see ununpentium

Pranala njaba

Golongan → 1 2
3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18
Période ↓
1 1
H

2
He
2 3
Li
4
Be


5
B
6
C
7
N
8
O
9
F
10
Ne
3 11
Na
12
Mg


13
Al
14
Si
15
P
16
S
17
Cl
18
Ar
4 19
K
20
Ca

21
Sc
22
Ti
23
V
24
Cr
25
Mn
26
Fe
27
Co
28
Ni
29
Cu
30
Zn
31
Ga
32
Ge
33
As
34
Se
35
Br
36
Kr
5 37
Rb
38
Sr

39
Y
40
Zr
41
Nb
42
Mo
43
Tc
44
Ru
45
Rh
46
Pd
47
Ag
48
Cd
49
In
50
Sn
51
Sb
52
Te
53
I
54
Xe
6 55
Cs
56
Ba
*
71
Lu
72
Hf
73
Ta
74
W
75
Re
76
Os
77
Ir
78
Pt
79
Au
80
Hg
81
Tl
82
Pb
83
Bi
84
Po
85
At
86
Rn
7 87
 Fr 
88
Ra
**
103
Lr
104
Rf
105
Db
106
Sg
107
Bh
108
Hs
109
Mt
110
Ds
111
Rg
112
Cn
113
Nh
114
Fl
115
Mc
116
Lv
117
Ts
118
Og

* Lantanida 57
La
58
Ce
59
Pr
60
Nd
61
Pm
62
Sm
63
Eu
64
Gd
65
Tb
66
Dy
67
Ho
68
Er
69
Tm
70
Yb
** Aktinida 89
Ac
90
Th
91
Pa
92
U
93
Np
94
Pu
95
Am
96
Cm
97
Bk
98
Cf
99
Es
100
Fm
101
Md
102
No
Seri Kimia saka Tabel Périodik
Logam alkali Alkali tanah Lantanida Aktinida Logam transisi
Logam Metaloid Nonlogam Halogen Gas mulia