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Percentage of U235 in naturally available uranium is about
01
7
001
10
7
Naturally occurring uranium is primarily composed of three isotopes: U238, U235, and U234. The isotope U235 is the only naturally occurring fissile material, and it constitutes approximately 0.72% (commonly simplified to 0.7%) of natural uranium by mass.
Naturally occurring uranium is primarily composed of three isotopes: U238, U235, and U234. The isotope U235 is the only naturally occurring fissile material, and it constitutes approximately 0.72% (commonly simplified to 0.7%) of natural uranium by mass.
NU235≈0.0072×Ntotal — Atomic fraction of U235 in natural uranium.
Natural uranium is composed of roughly 99.27% U238, 0.72% U235, and trace amounts of U234. Because U235 is the isotope that sustains the chain reaction in nuclear fission reactors, it is often enriched (increasing its concentration to 3–5%) to be used effectively as fuel in Light Water Reactors (LWRs).
Natural uranium consists almost entirely of the isotope U238.
Only U235 is fissile, meaning it can sustain a nuclear chain reaction with thermal neutrons.
Enrichment processes are required for most commercial nuclear reactors to achieve a higher U235 concentration.
Natural uranium is abundant in the Earth's crust.
Used directly in CANDU-type heavy water reactors without enrichment.
Low concentration of fissile U235 necessitates enrichment for light water reactors.
Requires complex chemical separation/enrichment processes for industrial use.
Nuclear power plant fuel cycle.
Research reactors.
Nuclear weapon development (highly enriched).
Standard value: Natural uranium contains ~99.27% U238 and ~0.72% U235.
Option B (0.7) is the standard approximation used in nuclear engineering textbooks.
B is correct — Naturally available uranium contains approximately 0.72% of the fissile isotope U235.
Always distinguish between natural uranium (0.7% U235) and low-enriched uranium (3-5% U235) used in standard light water reactors.