Warning: foreach() argument must be of type array|object, bool given in /var/www/html/web/app/themes/studypress-core-theme/template-parts/header/mobile-offcanvas.php on line 20

The half-life of the uranium isotope U235is 700million years. The earth is approximately localid="1650486537957" 4.5billion years old. How much more U235was there when the earth formed than there is today? Give your answer as the then-to-now ratio.

Short Answer

Expert verified

Then-to-now Ratio of uranium isotope is, NU0NU=86.2

Step by step solution

01

Given information

We are given that,

Time is, t=4500my

And half life is,t12=700my

02

Simplify 

Let, amount of uranium isotope when earth is formed is,NU0

And amount of uranium isotope now is,NU

We know that,

The U235decay is given by,

NU=NU0×12tt12

Now, ratio is,

localid="1650360018817" NU0NU=112tt12=2tt12=24500my700my=86.2

Unlock Step-by-Step Solutions & Ace Your Exams!

  • Full Textbook Solutions

    Get detailed explanations and key concepts

  • Unlimited Al creation

    Al flashcards, explanations, exams and more...

  • Ads-free access

    To over 500 millions flashcards

  • Money-back guarantee

    We refund you if you fail your exam.

Over 30 million students worldwide already upgrade their learning with Vaia!

One App. One Place for Learning.

All the tools & learning materials you need for study success - in one app.

Get started for free

Most popular questions from this chapter

The half-life of the uranium isotope 235 U is 700 million years. The earth is approximately 4.5 billion years old. How much more 235 U was there when the earth formed than there is today? Give your answer as the then-to-now ratio

The technique known as potassium-argon dating is used to date old lava flows. The potassium isotope 40 K has a 1.28-billionyear half-life and is naturally present at very low levels. 40 K decays by two routes: 89% undergo beta-minus decay into 40 Ca while 11% undergo electron capture to become 40 Ar. Argon is a gas, and there is no argon in flowing lava because the gas escapes. Once the lava solidifies, any argon produced in the decay of 40 K is trapped inside and cannot escape. A geologist brings you a piece of solidified lava in which you find the 40 Ar/ 40 K ratio to be 0.013. What is the age of the rock?

a. What are the isotopic symbols of all A = 19 isobars?

b. Which of these are stable nuclei?

c. For those that are not stable, identify both the decay mode and the daughter nucleus.

Beta-plus decay is AXz+YzA+e++n

a. Determine the mass threshold for beta-plus decay. That is, what is the minimum atomic mass mX for which this decay is energetically possible? Your answer will be in terms of the atomic mass mY and the electron mass me.

b. Can 13 N undergo beta-plus decay into 13 C? If so, how much energy is released in the decay?

The activity of a sample of the cesium isotope 157Cs, with a half-life of 30 years, is 2.0×108Bq. Many years later, after the sample has fully decayed, how many beta particles will have been emitted?

See all solutions

Recommended explanations on Physics Textbooks

View all explanations

What do you think about this solution?

We value your feedback to improve our textbook solutions.

Study anywhere. Anytime. Across all devices.

Sign-up for free