Thorium, Th, is the name of element 90. It is an actinide, a seventh-period f-block element. Thorium is common enough for minerals in which Th is the predominant metal to exist. It is also radioactive, but its principal isotope, 232Th, has a half-life exceeding 14 billion years, which means slightly less than half of any 232Th which formed in the early universe still exists. This element is of interest both for its chemistry and its physics.
NUCLEAR PROPERTIES
Aside from 232Th, three Th isotopes have half-lives exceeding one year. They are, in order of decreasing half-life: 230Th [between 75080 and 75680 yrs(1)], 229Th [7180 to 7500 yrs], and 228Th [1.9100 to 1.9132 yr]. All these long-lived isotopes are present on earth today because they are daughters of long-lived ancestors: 238U, 238U via its fission channel, and 232Th, respectively. The half-life of 232Th itself is between 1.411E10 yrs and 1.399E10 yrs, with a mean at 1.405E10 yrs so most of the 232Th ever formed is still around.
Three more short-lived isotopes are present on earth today. Two of them, 227Th [18.68+/-0.09 days] and 231Th [25.51+/-0.01 hrs], descend from 235U. The third, 234Th [24.10+/-0.03 days], is the alpha daughter of 238U.
Thirty-four isotopes of Th have been reported, which is about a quarter of the total number predicted to exist(2). Most of the predicted ones are neutron-rich, so they will form in quantity in something like a supernova or neutron star merger. With the exception of the seven listed above, Th isotopes disappear within days of the event which formed them.
231Th and 234Th decay exclusively through beta emission. The five other remaining isotopes all decay by alpha emission. Physicists have observed spontaneous fission in 230Th and 232Th, but it is so rare that these isotopes aren't significant as a neutron source in the way 238U is. Interestingly, Th has only one isotope whose half-life exceeds 100000 yrs, while U has five and Pu has two. Thorium's lighter isotopes are heavily affected by instability of nuclei with slightly more than 126 neutrons, so no isotopes comparable to 233U exist.
ATOMIC PROPERTIES
Thorium is an actinide. Comparison of the physical and chemical properties of Th with those of U reveals substantial differences, differences great enough so that Th and U are often found in different minerals. These comparatively large differences between two elements so close together is different from what happens in the lanthanides. Partly, this is the result of relativistic effects and the greater similarity between f and d energies than is true in lanthanides. In experimental work, though, radioactivity makes close measurement of actinides difficult, both by damaging crystal structure and by introducing impurities into a sample.
REFERENCES
- "Isotopes of Thorium", Wikipedia
- "Decay Modes and a Limit of Existence of Nuclei"; H. Koura; 4th Int. Conf. on the Chemistry and Physics of Transactinide Elements; Sept. 2011.
| 9-Period Periodic Table of Elements | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| 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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