Sources of Radionuclides in the Environment

1.1 Nuclear Weapons

Nuclear weapons tests account for a significant proportion of the total activity released into the environment and historically are the major source of radio­nuclides in the atmosphere. An estimated 2 x 108 TBq of radioactivity have been released into the atmosphere as a result of nuclear weapons testing;3 Table 1 lists the radionuclides produced and released by atmospheric nuclear tests.4 Most of the radionuclides released were short-lived, and so atmospheric levels of radioactivity have declined sharply from their peak in the 1960s; further decline in levels of radioactivity will be much slower, as the remaining activity is predominantly due to long-lived 14C.4 Fallout from atmospheric weapons testing will also cause contamination of surface water and terrestrial environments. Fallout can either be local (within a few 100 km of the test site), regional (up to several thousand km from the site) or global, and the spread of fallout will depend on the altitude and latitude of the explosion and the explosive yield.5,6

Although much of the contamination arising from nuclear weapons testing is widely dispersed and at low levels, there are considerable levels of activity at test and production sites. In the USA, there are >70 million m3 of con­taminated soil and > 1800 million m3 of contaminated water at Department of Energy facilities used for weapons production.7 At the Mayak Production Association in the Chelyabinsk region, Russia, weapons-grade plutonium was produced for в 40 years and significant levels of contamination exist at the site and the surrounding area from both production and accidental discharges.8,9 Approximately 105 TBq of radioactivity, as liquid waste, were discharged from the site into the Techa River between 1949 and 1956, with most of the released radioactivity associated with 89+90Sr (20.4%), 137Cs (12.2%), rare earth isotopes (26.8%), 95Zr-95Nb (13.6%) and ruthenium isotopes (25.9%).9,10 At the same site ~ 7.4 x 104 TBq of radioactivity were released as a result of a high level radioactive liquid waste tank exploding, causing the contamination of

Table 1 Radionuclides produced and globally dispersed in atmospheric nuclear tests.4

Global Release Global Release

Radionuclide

Half-life

(PBq)

Radionuclide

Half-life

(PBq)

H-3

12.33 y

186000

Sb-125

2.76 y

741

C-14

5730 y

213

I-131

8.02 d

675000

Mn-54

312.3 d

3980

Ba-140

12.75 d

759000

Fe-56

2.73 y

1530

Ce-141

32.5 d

263000

Sr-89

50.53 d

117000

Ce-144

284.9 d

307000

Sr-90

28.78 y

622

Cs-137

30.07 d

948

Y-91

58.51 d

120000

Pu-239

24110 y

6.52

Zr-95

64.02 d

148000

Pu-240

6583 y

4.35

Ru-103

39.26 d

247000

Pu-241

14.35 y

142

Ru-106

373.6 d

12200

~20 000 km2 at concentrations > 4000 Bq m 2.8,11 Underground weapons test­ing has caused contamination of the subsurface with tritium, fission and acti­vation products and actinides.2,12 At the Nevada Test site, the primary location for nuclear weapons tests in the USA, ~1 x 107TBq of radioactivity was released into the subsurface during 828 tests.13 The decay-corrected radionuclide inven­tory as of 1992 (the year of the last test) is 4.86 x 106 TBq, with the most sig­nificant amounts of radioactivity arising from 3H, 137Cs, 90Sr, 241+239Pu, 85Kr, 152+154Eu and 151Sm.14 The inventory will change, however, as short-lived radionuclides decay and daughter radionuclides appear; with time, the remain­ing radionuclide inventory in the subsurface will be dominated by long-lived radionuclides such as uranium, plutonium, neptunium and americium.14