4. [6] The table below gives 210Pb activities in a marine sediment core.
Depth, L(cm)
1.0
1.5
2.0
2.5
3.0
3.5
4.0
4.5
5.0
210Pb activity, AL(Bq kg-1)
247.0
199.0
160.0
123.0
101.0
78.0
62.0
46.0
38.0
Assume the following equation applies
Where AL is the activity at depth L (Bq kg-1), A0 is the activity at zero depth (L = 0 cm), l is the decay constant (0.031 yr-1 for 210Pb), L is the sediment depth (cm) and S is the sediment accumulation rate (cm yr-1).
(a) Transform the above equation into straight line form.
(b) By plotting the data estimate the value of A0 and S.
Let t be the age of a layer. Therefore, "L = tS."
The activity is "A_L = A_0e^{-tl}."
So "A_L = A_0e^{-\\frac{L}{S}l}." It is an exponential curve. If we take logarithm, we'll get
"\\ln A_L = \\ln A_0 - \\frac{L}{S}l = \\ln A_0 - L \\cdot\\dfrac{l}{S}." It is a linear function of L.
From a linear plot we get "\\ln A_0 = 5.9 \\; \\Rightarrow A_0 = e^{5.9} = 365" Bq kg-1 ,"\\frac{l}{S} = 0.475 \\Rightarrow S = 0.065" cm/y.
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