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A class of atoms with the same number of protons but different number of neutrons are termed isotopes of that element. The general term grouping the different classes of radioactive elements and isotopes. Expressed as a simple probability; the probability that a radioactive nucleus will decay is expressed as the fraction of the nuclei which will decay in a unit time usually in one year. This probability constant is known as the decay rate lambda l. Conversely, the average life time of a radioactive atom is 1. In the above example, what type of radioactive decay does 40 K undergo?
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Explain which would be the best isotope from the Isotope HalfLife Chart to measure a 3 billion year old specimen. Rubidium isotope would be the best isotope to use for that measurement because it contains the most years that would be needed to measure that span.
Even with the help of this isotope the task would still be rather difficult to make precise.
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Activity 2 Place your data from Activity 1 in the appropriate boxes below. Explain how you obtained the estimated initial value of the carbon content.
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I used the formula that is used for radiocarbon dating using the decay constant. Describe if the age of the each specimen is likely a realistic value.
You will need to use the web to evaluate the approximate age of the oldest specimen that is possible for trees, insects, and bats.
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The oldest specimen is almost 5, years old according to my findings and in conclusion I can see these findings realistic because the earth is about 4. Words: Category: Database Pages: 2.
The decay constant lambda l for 87 Rb is 1. In the above problem you have been given l of 87 Rb, what is its half life in years? Construct a graph showing the decay of 87 Rb assuming an initial concentration of 1. How much of the original 87 Rb is left after 2.
The Palisades Sill is an igneous intrusion that created the cliffs along the southern portion of the Hudson River.
May 31, Atomic Dating Using Isotopes Answer the following questions about the results of this activity. Record your answers in the boxes. Send your completed lab report to your instructor. Dont forget to save your lab report to your computer Reference Isotope HalfLife Chart Isotope ProductHalf LifeCarbonNitrogen years Potassium  40Argon  , million yearsRubidium LAB # 3  RELATIVE AND "ABSOLUTE" GEOLOGICAL TIME. In this lab we will look at: 1) relative stratigraphy, which uses the principles of stratigraphy discussed in class to determine relative age; 2) biostratigraphy, which uses fossils to assess relative age; and 3) radiometric dating, which uses the decay of various isotopes to put a numeric age on the rock of interest. Lab Report #7 Atomic Dating Using Isotopes Answer the following questions about the results of the virtual lab activity. Record your answers in the boxes. Reference: Isotope HalfLife Chart Isotope Product Half Life Carbon Nitrogen years Potassium  40 Argon  40 1, million years Rubidium  87 Strontium 8 7 48, million years Thorium  Lead  14, million years.
Biotite a type of the mineral mica was extracted from a sample taken from one of the exposed areas. A friend of yours was kind enough to tell you that the total decay constant l for 40 K is 5.
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