Nobelium, No, is the name of element 102. Wikipedia has an article which provides a lot of information about the element. This article will focus on things Wikipedia does not stress: heavy isotopes and formation.
It has the lowest atomic number of any element whose peak in stability lies among predicted, rather than observed, isotopes. Half-lives of No isotopes may range up to 20 days, The longer-lived isotopes may survive long enough to form dust in a supernova or neutron star merger remnant. The quantity would be minute, though, and probably undetectable.
A good deal of is known about the chemistry of No, both theoretically and experimentally. We also can produce atoms at a rate high enough to be described as "production" in Wikipedia.
NUCLEAR PROPERTIES
INFORMATION SOURCES
Japan Atomic Energy Agency (JAEA) maintains an on-line chart of nuclides which includes decay properties of many predicted nuclides(1) - unlike charts published by Korea Atomic Energy Research Institute (KAERI) or the (U.S.) National Nuclear Data Center (NNDC). This chart gives separate numerical values for partial half-lives against fission, beta emission (both b- and b+), and alpha emission. This reference provides the most focused look at the most significant predicted No isotopes.
An independent resource is provided by the U.S.'s Los Alamos National Laboratory (LANL) in interactive tables of contains tabulated partial half-life data for alpha and beta decay(2) for numerous nuclides. The great weakness of this source is that it does not consider fission.
A third source describes decay properties of a large number of nuclides(3). Half-life data in this source are presented via color, which makes specifying a value within an order of magnitude difficult. In addition, only the dominant decay mode is reported. Charts on pp 11 - 13 are the most valuable part of the document.
PREDICTED PROPERTIES
Isotopes from the neutron dripline down to 273No are predicted to decay primarily by beta emission. Half lives increase, as A declines, from around 0.001 sec at the dripline to 1 sec near 290No and peaking under 1000 sec at 274No. Isotopes at the light end of this band are likely to decay by a mixture of beta emission and fission. (Ref. 2 predicts long half-lives between 286No and 282No. In light of shorter beta partial half-lives it predicts at lower A, these results appear to be anomalous.)
Between 272No and 268No, the predominant mode of decay is predicted to be fission, although a beta-decay branch is predicted for odd-N isotopes in this band. Half lives are millisecond-scale, although 269No may have a half-life as high as 10 sec.
267No is predicted to decay by a mixture of beta emission and fission, with a weak alpha branch also present. Its half-life may be as much as 2 hr.
Isotopes in the band 266No to 263No, plus 261No are predicted to decay by a combination of fission and alpha emission, with no beta-decay branches. (261No is predicted to have a (b+) branch.) Half-lives of 266No and 265No are predicted to be up to 20 days, while half-lives of 264No and 263No are predicted to be on the order of a day. Beta stability is predicted for this band, making it possibly the region of greatest stability for No. 261No is predicted to have a half-life on the order of 2 hr.
262No has been observed to decay by fission with a half-life around 0.005 sec. This is far shorter than expected, based on predictions. It calls into question the validity of predictions made above for relatively long fission partial half-lives (and presence of other decay modes) for isotopes in the 270No to 261No band.
Isotopes have been predicted or observed down to 237No. Between 236No and 230No, there is a gap containing nuclides with half-lives in the 10-14 - 10-09 sec range or nuclear drops too short-lived to qualify as nuclides. Decay by fission is to be expected.
Ref. 3 predicts that two set of isotopes with N near 126, 229No to 227No and 223No to 221No will have half-lives exceeding 10-09 sec. All are short lived, with some decaying predominantly by fission and some predominantly by alpha emission.
OCCURRENCE
FORMATION
It appears likely that No isotopes from the neutron dripline down to 269No can form. Some losses due to fission in beta-decay chains leading to No is likely, but are not expected to be severe.
It appears likely that 268No cannot form, due to lack of a beta decay branch in 268Fm.
Although fission reduces the amount which can form, it appears to be possible that isotopes in the band 267No to 263No can form.
262No cannot form because 262Fm does not have a beta-decay branch. 261No cannot form because 261Md has no beta decay branch. 260No to 258No cannot form due to rapid fission in 260Fm to 258Fm. It is unlikely that lighter isotopes can form.
Both neutron star mergers and supernovae contribute to the production of all No isotopes which can form. Slow neutron capture cannot produce any isotopes of No.
PERSISTENCE
The longest-lived isotopes, 266No and 265No may persist, in principle, for up to 8 yrs after a supernova, neutron star merger, or other event which led to their formation. These will survive to become part of the resulting diffuse remnant, although probably not in detectable amounts. Of the remaining isotopes, 267No, 264No, and 263No may persist, in principle, for a few months.
ATOMIC PROPERTIES
Wikipedia's article "Nobelium" addresses the element's atomic properties and chemistry in some detail. It is possible that No 266 and No 265 may persist long enough to interact chemically.
REFERENCES
1. "Chart of the Nuclides, 2014", Japan Atomic Energy Agency; website available using "chart of nuclides" and "JAEA" as internet search terms.
2. "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".
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. "Isotopes of Nobelium", Wikipedia article.
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| 1 | 1 H |
2 He | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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| 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 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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(11-17-20)