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97

Berkelium, Bk, is the name of element 97. It has the highest atomic number of any element for which fission is not significant.

Wikipedia has an article which provides a lot of information about the element.  This article will focus on things Wikipedia does not stress: formation and the element's natural presence on earth..

249Bk and heavier isotopes form in supernovae and neutron star mergers via rapid neutron capture followed by chains of beta decays. All are short-lived, but 249Bk may be present in young supernova or kilonova (neutron star merger) remnants. It will likely participate in dust formation..

On earth, neutrons from 238U spontaneous fission drive a slow process of neutron capture followed by beta decay followed by another capture. This process builds from 238U itself, and produces the isotopes 249Bk and heavier.

Its longest-lived isotope, 247Bk, has a half-life of 1380 yr, but does not form in quantity.

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 Bk isotopes. Other references used are cited.

PREDICTED AND OBSERVED PROPERTIES

Isotopes from the neutron dripline down to 254Bk are predicted to decay primarily by beta emission. Half lives are predicted to increase, as A declines, from around 0.001 sec at the dripline to 1 min at 257Bk and peaking around 20 min at 255Bk.

Beta decay is observed to continue down to 249Bk. Fission is negligible and alpha decay is a very minor branch. Half-lives increase to 1 hr at 251Bk, to 3 hr at 250Bk, and 330 days at 249Bk.

248Bk has an isomer, 248mBk, which beta decays. It is possible that neutron capture by 247Bk may produce this isomer. The ground state decays by alpha emission with a 300 yr half-life. It has not been observed to fission.

247Bk has a half-life of 1380 yr and nearly always alpha-decays. It is by a wide margin the most long-lived isotope of Bk.

Positive beta decay sets in at 246Bk. Half-lives drop from a few hours to seconds by 233Bk, the lightest reported isotope.

Ref 1 predicts isotopes as light as 224Bk. Ref 3 predicts isotopes with half-lives > 10-09 sec down to 219Bk. All these predicted isotopes are short lived, with half-lives under 0.001 sec. That they are possible at all indicates stabilization by the N = 126 neutron shell closure.

OCCURRENCE

FORMATION

a) Outside Earth

It appears likely that Bk isotopes from the neutron dripline down to 249Bk can form, with the possible exception of 252Bk. (252Cm is not predicted to have a beta-decay branch, but there may be a weak beta-decay branch. See "Californium", this wiki.)

Half-lives of isotopes that can form range from 0.001 sec near the neutron dripline to an hour at 251Bk, then to 3 hrs at 250Bk, and 330 +/- 4 days at 249Bk.

248Bk and lighter isotopes are blocked from forming via rapid neutron capture & beta decay(4), significantly by lack of a beta-decay branch in isotopes between 248Cm to 244Cm and presence of positive beta decay at 243Cm.

Berkelium's longest-lived isotope, 247Bk cannot form in quantity either because all neutron-capture / beta-decay processes (r-process, s-process, or reactor irradiation) are blocked by 247Cm which does not beta decay. Alpha bombardment of 243Am does produce some 247Bk both in the laboratory and "in the wild" (including earth's upper atmosphere), but quantities are minute.

Both high-A nuclides ejected during a neutron star merger and rapid neutron capture contribute to the production of those Bk isotopes which can form. Slow neutron capture can also contribute to the amount of Bk produced, but does not produce any isotopes not formed by rapid capture.

b) On Earth

While Bk is produced in some quantity in neutron star mergers and supernovae, those nuclides will decay quickly. After a short time, the only Bk remaining in a body will be what is produced continuously by slow neutron capture. Spontaneous fission of 238U produces free neutrons. This small flux of neutrons will produce a small amount of 249Bk and 250Bk. The short half-life of 250Bk means that, for all practical purposes, heavier isotopes don't form. Concentration of Bk will be many orders of magnitude smaller than uranium concentration; so only geologically-active rocky bodies like the earth, which can concentrate uranium, will contain potentially-detectable quantities of Bk.

PERSISTENCE

The amount of Bk produced during a supernova, neutron star merger, or comparable event will only be a few orders of magnitude less than the amount of uranium produced. Most of it decays until it either vanishes or comes into equilibrium with the continuous, slow production resulting from 238U fission.

249Bk, with its half-life close to a year may persist, in principle, over 150 years after the supernova, neutron star merger, or other event which led to its formation. The amount will be negligible for most of that time. It will persist long enough to exist in potentially detectable amounts in very young supernova or kilonova remnants.

249Bk persists long enough to participate in dust formation.

Slow neutron capture in rocky bodies active enough to concentrate uranium can produce 249Bk and heavier Bk isotopes. This production continues as long as U remains.

ATOMIC PROPERTIES

Wikipedia's article "Berkelium" addresses the element's atomic properties and chemistry in some detail. Chemistry of Bk is not quite limited to the laboratory.

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 Californium", Wikipedia article.

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

(11-23-20)