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Figure 11 shows radioactive decay of one nuclide can be modelled by draining water through a tap from a cylindrical tube - AQA - A-Level Physics - Question 6 - 2018 - Paper 2

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Figure 11 shows radioactive decay of one nuclide can be modelled by draining water through a tap from a cylindrical tube. The water flow-rate is proportional to th... show full transcript

Worked Solution & Example Answer:Figure 11 shows radioactive decay of one nuclide can be modelled by draining water through a tap from a cylindrical tube - AQA - A-Level Physics - Question 6 - 2018 - Paper 2

Step 1

Determine the predicted depth of water when the time is 57 s

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Answer

Using the graph from Figure 12, we first need to identify the trend indicating how the depth of water decreases over time. By observing the graph, we can approximate the depth at 57 seconds. The estimated depth will be approximately 1.6 cm based on the linear extrapolation from the data.

Step 2

Suggest how the apparatus in Figure 11 may be changed to represent a radioactive sample of the same nuclide with a greater number of nuclei

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Answer

To represent a radioactive sample with a greater number of nuclei, we can increase the volume of water used in the cylindrical tube. This allows for a greater number of water molecules to simulate the behavior of a larger sample of the nuclide.

Step 3

Suggest how the apparatus in Figure 11 may be changed to represent a radioactive sample of a nuclide with a smaller decay constant

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Answer

To represent a radioactive sample of a nuclide with a smaller decay constant, we should use a narrower tube or a smaller capillary. This will decrease the rate of flow, simulating a slower decay process.

Step 4

Calculate, in years, the half-life of $^{87}Rb$

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Answer

The half-life (T1/2T_{1/2}) can be calculated using the formula:

T1/2=0.693λT_{1/2} = \frac{0.693}{\lambda}

where λ=1.42×1011year1\lambda = 1.42 \times 10^{-11} year^{-1}. Thus, we calculate:

T1/2=0.6931.42×10114.87×1010years.T_{1/2} = \frac{0.693}{1.42 \times 10^{-11}} \approx 4.87 \times 10^{10} years.

Therefore, the half-life of 87Rb^{87}Rb is approximately 4.87 x 10^10 years.

Step 5

Calculate the mass, in g, of $^{87}Rb$ that the rock sample contained when it was formed 4.47 x 10^9 years ago.

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Answer

We can use the decay formula:

N=N0eλtN = N_0 e^{-\lambda t}

Where:

  • NN = final amount (1.23 mg)
  • N0N_0 = initial amount
  • λ=1.42×1011year1\lambda = 1.42 \times 10^{-11} year^{-1}
  • t=4.47×109yearst = 4.47 \times 10^9 years

First, we rearrange to find N0N_0:

N0=NeλtN_0 = N e^{\lambda t}

Calculating this gives:

N0=1.23mg×e1.42×1011×4.47×109.N_0 = 1.23 mg \times e^{1.42 \times 10^{-11} \times 4.47 \times 10^9}.

Calculating the exponent gives us approximately:

N01.23mg×1.0631.31mg.N_0 \approx 1.23 mg \times 1.063 \approx 1.31 mg.

Thus, the initial mass of 87Rb^{87}Rb was approximately 1.31 mg.

Step 6

Calculate the activity of a sample of $^{87}Rb$ of mass 1.23 mg.

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Answer

The activity (A) can be calculated using the formula:

A=λNA = \lambda N

where:

  • λ=1.42×1011year1\lambda = 1.42 \times 10^{-11} year^{-1}
  • NN = number of nuclei, which can be calculated using:

N=massmassnucleusN = \frac{mass}{mass_{nucleus}}

The mass of one 87Rb^{87}Rb nucleus = 1.44 x 10^-25 kg. Thus, for the sample:

N=1.23×103g1.44×1025kg8.54×1021nuclei.N = \frac{1.23 \times 10^{-3} g}{1.44 \times 10^{-25} kg} \approx 8.54 \times 10^{21} nuclei.

Finally, substituting into activity:

A=(1.42×1011)(8.54×1021)121.07 mBq.A = (1.42 \times 10^{-11}) (8.54 \times 10^{21}) \approx 121.07 \ mBq.

Therefore, the activity is approximately 121.07 mBq.

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