What is the dating ratio of a rock sample that contains 87Rb and 86Sr?

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SUMMARY

The discussion centers on calculating the dating ratio of a rock sample containing isotopes 87Rb and 86Sr, formed 3.6 billion years ago. The initial ratios provided are N0[87Rb]/N0[86Sr] = 0.2 and N0[87Sr]/N0[86Sr] = 0.7, with 87Rb decaying into 87Sr at a half-life of 48.8 billion years. Participants emphasize the importance of using governing equations to express the time development of each isotope and suggest that solving these equations will yield the current ratios of isotopes in the sample.

PREREQUISITES
  • Understanding of radioactive decay and half-life concepts
  • Familiarity with isotopic ratios in geochronology
  • Knowledge of exponential functions and their applications in decay equations
  • Ability to manipulate algebraic expressions involving multiple variables
NEXT STEPS
  • Study the equations governing radioactive decay, specifically for isotopes like 87Rb and 87Sr
  • Learn how to derive and solve equations for isotopic ratios over time
  • Explore the application of the decay constant in calculating remaining isotopes
  • Investigate the use of geochronology tools for dating rock samples
USEFUL FOR

This discussion is beneficial for geologists, geochemists, and students studying radiometric dating techniques, particularly those interested in understanding isotopic ratios and their implications in geological time scales.

Granger
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Suppose a rock sample at the time of its formation 3.6 × 10^9 years ago contained N0[87Rb] rubidium atoms 87 (87Rb), N0[87Sr] strontium atoms 87 (87Sr) and N0[86Sr] strontium atoms 86 (86Sr). From the relative abundance of the three species at the height of the rock formation yielded the following ratios: N0 [87Rb] / N0 [86Sr] = 0.2 and N0 [87Sr] / N0 [86Sr] = 0.7. The 87Rb decays into 87Sr with a half-life of 48.8 × 109 years. Turn the 86Sr and 87Sr are stable.

Determine the percentage of 87Rb atoms that have survived to this day and Determine the ratio N [87Rb] / N [86Sr] that currently exists in this sample of rock ..Can someone explain me how this thing of the ratio works? I don't understand what they want in the question?
 
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Hi Granger, welcome to PF :smile: !

You'll get used to the culture around here. read the guidelines to see why we impose the use of the template. It's really useful.
Good thing you separate your questions in one exercise per thread.

You already posted the governing relevant equations. Once you have the right set of equations, all exercises aren't really that much physics any more, but mathematics. Solving m equations with m unknowns mostly.

This exercise expands on the governing equations you already posted: now it's about ratios. Simply write down the equations for the time development of each species. Ratios gve you expressions of the type ## A_1 \, e^{t/\tau_1} / A_2 \, e^{t/\tau_2} ## and that can be written as ## B \, e^{t/\tau_3} ##, and then you're back on familiar terrain. Good luck !
 

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