Plutonium-241 (, Pu-241) is an isotope of plutonium formed when plutonium-240 captures a neutron. Like some other plutonium isotopes (especially <sup>239</sup>Pu), <sup>241</sup>Pu is fissile, with a neutron absorption cross section about one-third greater than that of <sup>239</sup>Pu, and a similar probability of fissioning on neutron absorption, around 73%. In the non-fission case, neutron capture produces plutonium-242. In general, isotopes with an odd number of neutrons are both more likely to absorb a neutron and more likely to undergo fission on neutron absorption than isotopes with an even number of neutrons.
Plutonium-241 is a beta emitter with a half-life of 14.33 years, corresponding to a decay of about 5% of <sup>241</sup>Pu nuclei over a one-year period. This decay has a Q-value of only , and does not emit gamma rays. The longer spent nuclear fuel waits before reprocessing, the more <sup>241</sup>Pu decays to americium-241, which is nonfissile (although fissionable by fast neutrons) and an alpha emitter with a half-life of 432.6 years; <sup>241</sup>Am, which does emit gamma rays, is a major contributor to the radioactivity of nuclear waste on a scale of hundreds to thousands of years. In its fully ionized state, the beta-decay half-life of <sup>241</sup>Pu<sup>94+</sup> decreases to 4.2 days, and only bound-state beta decay is possible.
Plutonium-241 also has a rare alpha decay branch to uranium-237, occurring in about 0.0025% of decays. Unlike its usual beta decay, this can emit gamma rays, X-rays, and associated electrons.