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Identify the correct sequence of concentration in increasing order of the following uranium isotopes in naturally occurring uranium: (A) U-233 (B) U-2
Question

Identify the correct sequence of concentration in increasing order of the following uranium isotopes in naturally occurring uranium:

(A) U-233

(B) U-234

(C) U-235

(D) U-238

Choose the correct answer from the options given below:

A.

(A), (B), (C), (D)

B.

(A), (B), (D), (C)

C.

(D), (C), (B), (A)

D.

(D), (C), (A), (B)

Correct option is A

Introduction:

  • Uranium (U), atomic number 92) is a primordial, naturally occurring radioactive element.
  •  Natural uranium is a mixture of three major isotopes, all of which are radioactive: Uranium-238(3238U),Uranium235(4235U (3\text{}^{238}\text{U}), Uranium-235 (4\text{}^{235}\text{U}(5234U)(5\text{}^{234}\text{U})​, and a trace amount of Uranium-234.
  • The difference in their natural abundance is primarily due to their respective half-lives and their role in the long-term radioactive decay chains.
  • The question includes Uranium-233 (233U\text{}^{233}\text{U}​), which is not a naturally abundant isotope, making the sequence largely determined by comparing a synthetic isotope with three natural ones.
  • The sequence is based on the approximate natural abundance (by atom percent) of each isotope:
IsotopeSymbolApproximate Natural Abundance (%)Origin / Status
U-233233U(A)\text{}^{233}\text{U} (A)​​Trace/0%Trace / \approx 0\%Synthetic/Man-made. Produced from Thorium-232 in reactors. Virtually non-existent in natural uranium.
U-234234U(B)\text{}^{234}\text{U} (B)​​0.005%\approx 0.005\%Natural Decay Product. Part of the 238U\text{}^{238}\text{U}​ decay chain; found in secular equilibrium with its parent.
U-235235U(C)\text{}^{235}\text{U} (C)​​0.72%\approx 0.72\%Primordial. The only naturally occurring fissile isotope.
U-238238U(D)\text{}^{238}\text{U} (D)​​99.27%\approx 99.27\%Primordial. The most abundant and stable natural uranium isotope.


  • U-233 : Because 233U\text{}^{233}\text{U}​ is an artificial isotope produced in the Thorium fuel cycle (232Th233Th233Pa233U\text{}^{232}\text{Th} \rightarrow \text{}^{233}\text{Th} \rightarrow \text{}^{233}\text{Pa} \rightarrow \text{}^{233}\text{U}, its concentration in naturally occurring uranium is essentially zero. It is therefore the lowest in the sequence.

  • U-234: 234U\text{}^{234}\text{U}​ is naturally present not because it is primordial, but because it is a decay product in the long-lived 238Udecaychain(specifically,238Udecaysto234Th\text{}^{238}\text{U} decay chain (specifically, \text{}^{238}\text{U} decays to \text{}^{234}\text{Th}234U).Since234Uisinsecularequilibriumwithitsparent(238U),itsactivityisequalto238U,butduetoitsmuchshorterhalflife(2.45×105years),itsmassabundanceisextremelylow(approximately1/17,325of238U\text{}^{234}\text{U}). Since \text{}^{234}\text{U} is in secular equilibrium with its parent (\text{}^{238}\text{U}), its activity is equal to \text{}^{238}\text{U}, but due to its much shorter half-life (2.45 \times 10^5 years), its mass abundance is extremely low (approximately \text{1}/\text{17,325} of \text{}^{238}\text{U}​, which eventually decays to

  • U-235 : As one of the two primordial isotopes,235U \text{}^{235}\text{U}​ has a much greater abundance than the trace decay product 234U\text{}^{234}\text{U}​. Its concentration is critical as it is the fuel for most commercial nuclear reactors.

  • U-238: This isotope, with a half-life nearly equal to the age of the Earth, is the dominant component of natural uranium.


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