How Long Ago Did the Plant Die Using Carbon-14 Dating?

In summary, the half-life of carbon-14 is 5730 years and a living matter produces 15.3 disintegrations per minute per gram of carbon it contains. A 1g sample from an excavation of a plant showed 7 disintegrations per minute of carbon-14. By solving for the concentration using the equation [A] = [Ao]exp(-kt), it can be determined that the plant died approximately 6465.5 years ago.
  • #1
yan__90
2
0

Homework Statement


half life of carbon 14 is 5730 years. living matter produces 15.3 disintegrations per min per gram of carbon it contains. A 1g sample of a plant from an excavation shows 7 disintegrations per min from carbon-14. how long did the plant die?


Homework Equations


k = 1/ t
t(1/2) = 0.693/k
A=Aoexp(-kt)
R=kt


The Attempt at a Solution


may i know if the disintegration value is to be sub into R or A?
 
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  • #2
welcome to pf!

hi yan__90! welcome to pf! :smile:

(try using the X2 icon just above the Reply box :wink:)
yan__90 said:
half life of carbon 14 is 5730 years. living matter produces 15.3 disintegrations per min per gram of carbon it contains. A 1g sample of a plant from an excavation shows 7 disintegrations per min from carbon-14. how long did the plant die?

may i know if the disintegration value is to be sub into R or A?

hint: what is the meaning of A?

how would you write "7 disintegrations per min" as an equation? :wink:
 
  • #3


tiny-tim said:
hi yan__90! welcome to pf! :smile:

(try using the X2 icon just above the Reply box :wink:)


hint: what is the meaning of A?

how would you write "7 disintegrations per min" as an equation? :wink:

A stands for concentration.
this is my solution:
k = 0.693 / t
= 0.693 / (5730x365x24x60)
= 2.301 x 10 ^ -10

[A] = [Ao]exp(-kt)
15.3 = 7 exp(-2.301 x 10 ^-10 t)
t = 6465.5 years

is it correct?
 
Last edited:
  • #4
yan__90 said:
15.3 = 7 exp(-2.301 x 10 ^-10 t)

how can that be correct? …

the RHS is less than 7 :confused:
 
  • #5


As a scientist, it is important to clarify and understand the given information before attempting to solve the problem. In this case, the disintegration value should be substituted into the rate equation R=kt, where R is the rate of decay, k is the decay constant, and t is time. This will allow you to solve for the time (t) that has passed since the plant died. You can also use the half-life equation, t(1/2) = 0.693/k, to solve for the time it takes for half of the carbon-14 to decay. Both equations use the decay constant (k) which can be calculated using k = 1/t, where t is the half-life of carbon-14. By plugging in the given values, you can determine the approximate time that has passed since the plant died. This type of calculation is important in fields such as archaeology and geology, where carbon-14 dating is used to determine the age of organic materials.
 

Related to How Long Ago Did the Plant Die Using Carbon-14 Dating?

What is the half life of carbon?

The half-life of carbon, specifically carbon-14, is approximately 5,730 years.

Why is carbon used for radiocarbon dating?

Carbon is used for radiocarbon dating because it is present in all living organisms and is constantly replenished through the atmosphere. This allows scientists to accurately determine the age of organic materials.

How is the half life of carbon determined?

The half-life of carbon is determined through a process called radioactive decay. This involves measuring the amount of carbon-14 remaining in a sample and calculating how long it would take for half of the original amount to decay.

What are the limitations of using carbon dating?

While carbon dating is a useful tool for determining the age of organic materials, it has its limitations. It can only be used to date materials up to 50,000 years old and is not accurate for materials that have been contaminated with more recent organic material.

How is the half life of carbon used in other scientific fields?

The concept of half-life is not limited to carbon and is used in many other scientific fields to measure the rate of decay of various elements. For example, it is used in nuclear physics, geology, and archaeology.

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