It's called radiometric dating, and it's a convenient way to figure out how old rocks are. Radioactive elements have a "half-life," which means during a specific amount of time, half the atoms in that sample will decay into another element. Half-lives are different for every element; some are a fraction of a second and some are billions of years. Analyzing the ratio between parent element and daughter element (what it decays into) can give you the age of the rock it's in. This is how we know how old the earth is - about 4.6x109 years.
This question cannot be answered unequivocally:
Rocks do not have a half life. Radioactive isotopes of elements have. The half life of the radioactive isotope U235 is 704 million years.
The ratio of the two isotopes of lead 207 and uranium 235 is not enough to constrain an accurate age of a rock, because it might have contained a bit of lead 207 already when it formed.
Assuming that there had been absolutely no lead in the rock when it formed and no later processes like partial melting or recrystallization during metamorphic processes changed the budget of lead and uranium in the rock, one can apply the decay equation for radioactive materials:
C = Co * exp(-t*ln2/T)
With C = concentration of radioactive nuclide left
Co = concentration of radioactive nuclide at the beginning
t = time
T = half life
207 lead is only produced by the decay of U235 so the number of Pb 207 atoms in the rock is exactly equivalent to the number of atoms that completed the whole decay chain from U235 to Pb 207. When the ratio of Pb 207 to U 235 is 0.9 (number of Pb207 divided by number of U235 = 0.9), this means that slightly less than half of the Uranium 235 has decayed. The ratio would be 1 if half was Pb 207 and the other half was U 235.
From the given ratio we can get the ratio of C to Co; this is the amount of U235 atoms still present divided by the number of U 235 atoms at the time of rock formation. This ratio is 1 / (1+0.9) ~ 0.526
Now the only unknown in the decay equation is t (time):
C = Co * exp(-t*ln2/T) -->
C/Co = exp(-t*ln2/T) -->
ln(C/Co) = -t*ln2/T-->
ln(C/Co)/ln2*T = -t
-ln(C/Co)/ln2*T = t
and putting in the numbers results in an age of about 652 million years.
Use the the following formula: 206Pb/238U = eλ238t- 1 where lambda is the hal life of uranium 238 (4,470.109 years) and t is the age.
The age of the meteorite is 4,468.109 years.
its a sample of a mineral!
Blood samples can be held in storage for 17 to 180 days. The length of their storage time depends on which enzymes have been added to the sample.
they must be correct and they must be the right kind of sample
No, as density also depends on the state of matter in the sample of the substance.
10.20 g sample is normal, with a specific gravity of 1.020.
Sample size is the number of samples arawn from a population. If you drew 20 samples, your sample size would be 20.
Variables are variable and samples are samples. Variables are not samples so the question has no meaning.
700 milliion years. The definition of half-life is the period of time during which one-half of the atoms of an element undergo decay into other elements.
A composite sample is taken over a period of time, while a grab sample is a snap shot of what is in your well at the time you take the sample. Homeowner samples are generally grab samples.
Yes, the word 'sample' is a noun (sample, samples), a verb (sample, samples, sampling, sampled), and an adjective.Examples:Would you like to try a sample of our fudge? (noun)Yes, I will sample the fudge. (verb)A sample taste is not enough. I will take a pound. (adjective)
Samples.
its a sample of a mineral!
isaac sample
That is the correct spelling of "sampling" (taking a sample).
Samples may include stool sample, blood sample, or other samples.
The sample mean may differ from the population mean, especially for small samples.
It need not be if: the number of samples is small; the elements within each sample, and the samples themselves are not selected independently.