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Untrioctium
138Uto
-

Uto

Uoo
untriseptiumuntrioctiumuntriennium
Appearance
unknown
General properties
Name, symbol, number untrioctium, Uto, 138
Pronunciation /ntrˈɒktiəm/
Element category superactinides
Group, period, block N/A, 8, g
Mass number not applicable[1]
Electron configuration [Uuo] 5g126f37d18s28p2
(predicted)[2]
2, 8, 18, 32, 44, 21, 9, 4
(predicted)[2]
138
Physical properties
unknown
Atomic properties
unknown
Most stable isotopes
Main article: Isotopes of untrioctium
iso NA half-life DM DE (MeV) DP
366Uto
(predicted)[1]
syn
vter

Untrioctium, Uto, is the temporary name for element 138. Isotopes are predicted in the bands 451Uto to 395Uto, 371Uto to 365Uto, and 359Uto. There may be isotopes in the band from the neutron dripline to 452Uto, but it is not possible to predict which ones are possible. Reported half-lives are all less than 1 hr, and most are under 1 sec. Forty isotopes in the bands 451Uto to 434Uto and 423Uto to 402Uto are predicted to form. Four predicted isotopes, 438Uto and 436Uto through 434Uto, may persist for up to 2 days after the event which led to their formation. All other isotopes will last less than 1000 sec.

Uto may be proton-magic.

NUCLEAR PROPERTIES[]

INFORMATION SOURCES[]

While studies addressing specific issues have been carried out to very high N(1). and to moderate Z(2), (Z,N) or (Z,A) maps predicting half-lives and decay modes are almost completely limited to the region below Z = 130 and N = 220. There appears to be only one such map which extends beyond that region and is accessible(3).

(Z,N) maps for half-life and decay mode in Ref. 3 extend as high as Z = 175 and N = 333. Half-lives are reported as bands 3 orders of magnitude wide (0.001 - 1 sec, for example), and should be considered accurate only to within +/- orders of magnitude (presumably from band center. (A nuclide reported to be in the 0.001 - 1 sec band should be considered to have a possible half-life between 10-4.5 sec and 101.5 sec.) Decay modes are limited alpha emission, beta emission, proton emission, and fission; and to the principal one for each nuclide. There are areas where two modes (or more) may be important, meaning that small uncertainties is model parameters could have produced different results. It is also possible that cluster decay may become important above the neutron shell closures at N = 228 and 308.

Ref. 3 does have two significant weakness in the way data are presented. Nuclides which are beta-stable are identified by black squares, overwriting decay mode and half-life information. In addition, nuclides having half-lives less than 10-09 sec are not reported, which obscures the distinction between nuclides having half-lives in the 10-09 and 10-14 sec band and nuclear drops whose half-life is under 10-14 sec.

Above Z around 126, predictions in Ref. 3 may not reach the neutron dripline. This can be an important limitation because the only processes which can form nuclei at more than atoms / star quantity generate very neutron-rich nuclei. It is possible to to make a crude, but conservative (high N) guess for the dripline's location by averaging predicted values for even-N nuclei.{See "The Final Element" (this wiki).} It is also possible to guess at regions of the (Z,N) or (Z,A) plane in which a fission barrier high enough to permit nuclides exists by using a first-order, liquid drop model. {See "Nuclear Guesswork" (this wiki).} Specific numbers are reported for these guesses, not with the expectation that they are accurate, but because they are consistent from element to element. They allow construction of a map which at least hints at where in the (Z,A) plane nuclides may be found.

GUESSED PROPERTIES[]

Properties at high A: A simple liquid-drop picture indicates that 492Uto to 452Uto are unlikely to decay by neutron emission and are stable enough against fission to allow beta decay. Between 471Uto and 452Uto, Ref. 3 probably makes no predictions, but extrapolation from higher Z indicates that it would predict mainly short-lived, fission-decaying nuclides. Nuclear properties above 451Uto are highly uncertain, but it is possible that some relatively long-lived, beta-decaying isotopes of Uto are possible. It is possible to state that half-lives longer than 1 sec are implausible between the neutron dripline (nominally 492Uto) and 452Uto.

Properties Near N = 258: Ref. 3 indicates a weak shell closure at N = 258. Some other models, constructed to study rapid neutron capture processes, indicate a strong closure at N = 258(citation needed). No predictions, however, exist for decay properties of nuclides near 396Uto. Based on similarities to closures at N = 184, 228, and 308/318, the effect of a strong shell closure at N = 258 would be to stabilize a band from 400Uto down to 388Uto against fission, allowing decay by beta or alpha emission and half-lives in excess of 0.001 sec. Estimating from 293Cn, 354Ubh, and 472Uhq, and from its predicted stability against beta decay, 396Uto itself is expected to decay by alpha emission and might, optimistically, have a half-life on the order of 1 year. Some other nuclides in the 400Uto - 388Uto band will probably have half-lives exceeding 1000 sec, whether they decay by alpha or beta emission.

PREDICTED PROPERTIES[]

Isotopes in the band 451Uto - 439Uto are predicted to decay by beta emission. Predicted half-lives are in the 0.001 - 1 sec range. Actual half-lives are probably a few milliseconds and increase with declining N as the number of decays required to reach beta stability falls.

Isotopes in the band 438Uto - 430Uto are predicted to decay by fission. It appears to be possible for structure to destabilize a nuclide(4), so the data reported appear to be realistic, At the upper end of this band, though, half-lives are unrealistically high, since partial half-lives against beta emission should be on the order of milliseconds this far from beta stability(5). Half-lives decline as N falls, which is expected.

Isotopes in the band 429Uto - 403Uto are predicted to decay by beta emission. Half-lives are predicted to lie between 0.001 and 1 sec. Partial half-lives for beta decay should increase as N declines and the number of beta decays required to reach beta stability declines.

Between 402Uto and 398Uto, odd-N isotopes are predicted to decay by beta emission with 0.001 - 1 sec half-lives, and even-N isotopes are predicted to decay by fission with short - and declining - half-lives,

Isotopes in the band 397Uto to 395Uto have half-lives greater than expected, and decay via modes which are somewhat confusing. It is likely some predictions are artifacts.

There is a gap from 394Uto to 372Uto in which properties are not reported. These may be short lived nuclides or nuclear drops whose half-life is less than 10-14 sec. It appears to be the expected destabilized region above N = 228.

Between 371Uto and 365Uto drops are predicted to last long enough to be nuclides, but half-lives are microsecond-scale or shorter. Fission is predicted to dominate throughout this band.

Another gap is predicted between 364Uto and 360Uto. This may indicated very short lived nuclides or nuclear drops which don't last long enough to qualify as nuclides.

359Uto is predicted to decay by fission with a short half-life. This appears to be a nuclide which popped above the 10-09 sec model threshold.

N = 258 CLOSURE

The model used to predict decay properties of Uto isotopes has a relatively weak neutron shell closure at N = 258. Some neutron-dripline studies have indicated a strong closure at N = 258. If that closure is strong, one or more isotopes in the band 396Uto to 377Uto may even have half-lives exceeding 1000 sec. Note that the group included doubly-magic 396Uto itself. Interpolating between 472Uhq and 293Cn gives a reasonable value for maximum half-life of any nuclides stabilized by a strong N = 258 closure of 0.5 yr. Either alpha decay or beta decay may occur in this band, but fission can be expected to be suppressed.

These are not predictions of decay properties for nuclides in the vicinity of N = 258. This entire exercise is qualitative guesswork. No numbers, but a tantalizing hint of what might be.

OCCURRENCE

FORMATION

Where nuclear drops between the neutron dripline (nominally 492Uto) and 452Uto can be nuclides, they may form. Heavier isotopes may form directly from disintegrating neutron star material, and the remainder may form via beta decay chains from lower-Z nuclides. Since some of these chains may be terminated by short-lived, fission-decaying nuclides, it is not possible to say which isotopes of Uto in this range can form.

Nearly all nuclear drops in the bands 451Uto to 395Uto, 371Uto to 365Uto, and 359Uto are predicted to be nuclides. All are too far from the neutron dripline to form directly. It is possible to simulate the formation of nuclides via decay chains using data from Ref. 3 and assuming an initial distribution close to the neutron dripline. Details of the model are provided in "Nuclear Decay Chains at High A" in this wiki. Per that model, 40 predicted isotopes; 451Uto to 434Uto and 423Uto to 402Uto; can form.

Neutron capture may be able to produce nuclides up to A around 360 before fission attrition stops further growth. It is implausible that neutron capture can form any Uto isotope. A small amount of fission infall may contribute to nuclides up to A = 406 (nominal).

PERSISTENCE

439Uto and heavier isotopes, plus 437Uto will vanish within 1000 sec after a neutron star merger which led to their formation.

438Uto, 436Uto, and 435Uto are predicted to decay by fission, have half-lives in the 1 - 1000 sec range, and be located at the end of beta-decay chains. They can be expected to persist for a time less than 105000 sec.

434Uto lies at the end of a beta-decay chain, but has a half-life of less than 1 sec. It will disappear within 102.5 sec.

433Uto to 418Uto are blocked from forming via beta decay from the dripline by fission at Z < 138.

417Uto through 415Uto, and 413Uto through 403Uto are predicted to be short-lived, beta-decaying species,

414Uto is predicted to decay by fission with a long half-life. This nuclide's decay properties are unlike those of the others in its vicinity. It is probably an artifact. 414Uto probably decays by beta emission and has a half-life in the vicinity of 1 sec.

No other isotopes of Uto persist for a significant time.

Calculations done under maximum half-life assumptions and with all nuclides initially populated still point to all isotopes of Uto vanishing within 105.5 (3.16E05) sec.

N = 258 SHELL CLOSURE

Some studies of the neutron dripline indicate a strong shell closure at N = 258, instead of the relatively weak one occurring in the predictive models, If so, and if peak half-lives in the region do approach 0.5 yr, it is possible that one or more isotopes in the band 396Uto to 377Uto may persist for up to 60 yrs. If so, unlike all nuclides with A > 396, small quantities of nuclides in that band may be injected into a stellar system other than the one in which neutron star merger occurred.

ATOMIC PROPERTIES

Electron structure of Uto has been predicted by several sources (see "Extended Periodic Table" in Wikipedia). However, these predictions should be used with caution. Uto is large enough that nuclear shape may have an effect on electron structure, which might cause different isotopes of Uto to have different electronic structures. (That means it is no longer an element in the chemical sense.)

If this effect is small, Uto will be an active (superactinide) metal of the 8th period. Its electron configuration has been predicted(6) to be [Og] 5g12 6f3 7d1 8s2 8p21/2. (Note the 6f-7d change.)

REFERENCES

1. for example, "Nuclear Energy Density Functionals: What Do We Really Know?"; Aurel Bulgac, Michael McNeil Forbes, and Shi Jin; Researchgate publication 279633220 or arXiv: 1506.09195v1 [nucl-th] 30 Jun 2015.

2. for example "Fission Mechanism of Exotic Nuclei"; Research Group for Heavy Element Nuclear Science; http://asrc.jaea.go.jp/soshiki/gr/HENS-gr/np/research/pageFission_e.html.; 17 Sept 17.

3. "Decay Modes and a Limit of Existence of Nuclei"; H. Koura; 4th Int. Conf. on the Chemistry and Physics of Transactinide Elements; Sept. 2011.

4. "Magic Numbers of Ultraheavy Nuclei"; Vitali Denisov; Physics of Atomic Nuclei; researchgate.net/publications/225734594; July 2005.

5. "Nuclear Properties for Astrophysical Applications"; P. Moller & J. R. Nix; Los Alamos National Laboratory website; search by "LANL, T2", then "Nuclear Properties for Astrophysical Applications".

6. "Extended Periodic Table", Wikipedia.

7. Other references are found in the wiki articles cited.

9-Period Periodic Table of Elements
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
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
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
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
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
8 119
Uue
120
Ubn
121
Ubu
122
Ubb
123
Ubt
124
Ubq
125
Ubp
126
Ubh
127
Ubs
128
Ubo
129
Ube
130
Utn
131
Utu
132
Utb
133
Utt
134
Utq
135
Utp
136
Uth
137
Uts
138
Uto
139
Ute
140
Uqn
141
Uqu
142
Uqb
143
Uqt
144
Uqq
145
Uqp
146
Uqh
147
Uqs
148
Uqo
149
Uqe
150
Upn
151
Upu
152
Upb
153
Upt
154
Upq
155
Upp
156
Uph
157
Ups
158
Upo
159
Upe
160
Uhn
161
Uhu
162
Uhb
163
Uht
164
Uhq
165
Uhp
166
Uhh
167
Uhs
168
Uho
169
Uhe
170
Usn
171
Usu
172
Usb
9 173
Ust
174
Usq
Alkali metal Alkaline earth metal Lanthanide Actinide Superactinide Transition metal Post-transition metal Metalloid Other nonmetal Halogen Noble gas
predicted predicted predicted predicted predicted predicted predicted predicted predicted

(06-29-20)

Infobox References[]

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