Nuklida · radioaktif · alami

Uranium-235 (²³⁵U)

Uranium-235 (²³⁵U) adalah isotop radioaktif uranium dengan 92 proton dan 143 neutron (nomor massa 235). Waktu paruhnya 704 juta tahun (± 1 juta tahun), meluruh terutama lewat peluruhan alfa (α). Kelimpahan alaminya 0.007 204(6).

Data nuklida

Unsur
Uranium (U, Z = 92)
Nomor massa (A)
235
Proton (Z)
92
Neutron (N)
143
Massa atom
235.043928117 ± 0.000001198 u
Waktu paruh
704 juta tahun (± 1 juta tahun)
Mode peluruhan
Peluruhan alfa (α) ( 100 %)
Inti anak
Torium-231 (²³¹Th)
Kelimpahan alami
0.007 204(6)
Tahun penemuan
1935
Sumber data
IAEA Atomic Mass Data Center (NUBASE) and IUPAC CIAAW, via PubChem

Kegunaan isotop uranium

  • The three natural radioactive decay chains beginning with 238U, 235U, and 232Th each have comparable half-lives that are much longer than the radioactive isotopes that follow until the production of stable isotopes of 206Pb, 207Pb, and 208Pb, respectively. When undisturbed, the activities of daughter isotopes in each decay chain are equal to their parents and one can measure the accumulation of the stable isotopes of lead to date the time that has elapsed since a mineral became a closed system (a system that does not exchange matter with its surroundings). Rocks formed hundreds of millions to billions of years ago can be dated using this technique. If a mineral is disturbed at some point during the decay and isotopes in the decay chain are preferentially removed from the system, the equilibria in a decay sequence will be disturbed. For example, one can measure the excess of 230Th (with a half-life of 7.56×104 years) relative to the 234U parent radionuclide to date carbonates (speleothems or corals) that are less than 5×105 years old.
  • Nuclei of 235U are split when bombarded by thermal neutrons. The process is known as nuclear fission and can release tremendous amounts of energy per uranium nucleus. The nucleus that splits will release additional neutrons that, if slowed down sufficiently, can cause subsequent fission events. When properly controlled, 235U fission can be used to generate heat to drive steam turbines, which in turn produces electricity (Fig. IUPAC.92.1). If the fission process is not controlled, then a rapid and explosive release of energy will occur, similar to that of nuclear weapons. Uranium depleted in 235U by fission in nuclear reactors (and hence greatly enriched in 238U compared to “natural” uranium) is used in the manufacture of DUCRETE concrete (Fig. IUPAC.92.2). The incorporation of the large 238U nuclei makes this material an effective absorber of neutrons and gamma rays, and DUCRETE concrete is used to reduce fluxes of neutrons and high-energy photons. The alpha particles produced by the decay of 238U are effectively absorbed by the concrete and do not pose a health risk. DUCRETE is being proposed as a suitable material for the storage of radioactive waste,.

Reaksi inti

Isotop uranium lainnya

²¹⁵U, ²¹⁶U, ²¹⁷U, ²¹⁸U, ²¹⁹U, ²²⁰U, ²²¹U, ²²²U, ²²³U, ²²⁴U, ²²⁵U, ²²⁶U, ²²⁷U, ²²⁸U, ²²⁹U, ²³⁰U, ²³¹U, ²³²U, ²³³U, ²³⁴U, ²³⁶U, ²³⁷U, ²³⁸U, ²³⁹U, ²⁴⁰U, ²⁴¹U, ²⁴²U, ²⁴³U

Pelajari

Kimia inti Simulasi peluruhan ²³⁵U Bagan nuklida