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Spent fuel is mostly U238 in the form of UO2. In modern fuel cycles, the content of U235 varies between 4-5%, so 95-96% of U is U238.
During operation in a LWR core, two things happen with the U, 1) the U-235 fissions producing two fission products, and 2) U-238 absorbs neutrons to eventually produce Pu-239 (and other isotopes of Pu, Am, Cm, with the latter two being in low levels).
At discharge, modern fuel with have a burnup (energy produced/unit mass of U) of 50-60 GWd/tU. This is roughly equivalent to 5-6% of initial U consumed, which is now in the form of highly radioactive fission products. Also, part of the fissioning occurs in the Pu-239 that is produced by conversion of U-238, as Morbius pointed out elsewhere, and in high burnup fuel, as much as half the fissions are in Pu-239.
Mine tailings have 'natural' amounts of radioactive elements (related to the decay of U-235 and U-238), which are left after the U ore has been extracted.
Every mining operation (for copper, gold, silver, iron, lead, zinc, molybdenum, etc) leaves tailings which release heavy metals into the environment - so it is not just U mining that causes hazards, although due to their nature, U mine tailings would have higher level of radioactivity.
"According to the National Council on Radiation Protection and Measurements, sedimentary rocks such as shale and sandstone (quarts) contain about one (1) to four (4) micrograms of uranium per gram of rock. Beach sands contain about three (3) micrograms of uranium per gram of sand. And soil contains, on average, one (1) to three (3) micrograms of uranium per gram.
Igneous rocks, such as basalt, salic and granite, can contain from 0.5 to four (4) micrograms of uranium per gram of rock. However, there can be wide variations in this range in certain regions of the world. Because of the way these rocks were formed during the cooling of magma, light-colored igneous rocks tend to have the highest concentrations of radioactivity." from http://www.iem-inc.com/askq32r.html
So radioactivity is not unique to U-mine tailings, although there is somewhat higher levels than the examples just stated.
During operation in a LWR core, two things happen with the U, 1) the U-235 fissions producing two fission products, and 2) U-238 absorbs neutrons to eventually produce Pu-239 (and other isotopes of Pu, Am, Cm, with the latter two being in low levels).
At discharge, modern fuel with have a burnup (energy produced/unit mass of U) of 50-60 GWd/tU. This is roughly equivalent to 5-6% of initial U consumed, which is now in the form of highly radioactive fission products. Also, part of the fissioning occurs in the Pu-239 that is produced by conversion of U-238, as Morbius pointed out elsewhere, and in high burnup fuel, as much as half the fissions are in Pu-239.
Mine tailings have 'natural' amounts of radioactive elements (related to the decay of U-235 and U-238), which are left after the U ore has been extracted.
Every mining operation (for copper, gold, silver, iron, lead, zinc, molybdenum, etc) leaves tailings which release heavy metals into the environment - so it is not just U mining that causes hazards, although due to their nature, U mine tailings would have higher level of radioactivity.
"According to the National Council on Radiation Protection and Measurements, sedimentary rocks such as shale and sandstone (quarts) contain about one (1) to four (4) micrograms of uranium per gram of rock. Beach sands contain about three (3) micrograms of uranium per gram of sand. And soil contains, on average, one (1) to three (3) micrograms of uranium per gram.
Igneous rocks, such as basalt, salic and granite, can contain from 0.5 to four (4) micrograms of uranium per gram of rock. However, there can be wide variations in this range in certain regions of the world. Because of the way these rocks were formed during the cooling of magma, light-colored igneous rocks tend to have the highest concentrations of radioactivity." from http://www.iem-inc.com/askq32r.html
So radioactivity is not unique to U-mine tailings, although there is somewhat higher levels than the examples just stated.
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