Age of the Solar System determined by Zircon Dating
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When you click an exercise into a collection, this number will be taken as points for the exercise, kind of "by default".
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That being said... How many "default points" should you associate with an exercise upon creation?
As with difficulty, there is no straight forward and generally accepted way.
But as a guideline, we tend to give as many points by default as there are mathematical steps to do in the exercise.
Again, very vague... But the number should kind of represent the "work" required.
When you click an exercise into a collection, this number will be taken as points for the exercise, kind of "by default".
But once the exercise is on the collection, you can edit the number of points for the exercise in the collection independently, without any effect on "points by default" as represented by the number here.
That being said... How many "default points" should you associate with an exercise upon creation?
As with difficulty, there is no straight forward and generally accepted way.
But as a guideline, we tend to give as many points by default as there are mathematical steps to do in the exercise.
Again, very vague... But the number should kind of represent the "work" required.
About difficulty...
We associate a certain difficulty with each exercise.
When you click an exercise into a collection, this number will be taken as difficulty for the exercise, kind of "by default".
But once the exercise is on the collection, you can edit its difficulty in the collection independently, without any effect on the "difficulty by default" here.
Why we use chess pieces? Well... we like chess, we like playing around with \(\LaTeX\)-fonts, we wanted symbols that need less space than six stars in a table-column... But in your layouts, you are of course free to indicate the difficulty of the exercise the way you want.
That being said... How "difficult" is an exercise? It depends on many factors, like what was being taught etc.
In physics exercises, we try to follow this pattern:
Level 1 - One formula (one you would find in a reference book) is enough to solve the exercise. Example exercise
Level 2 - Two formulas are needed, it's possible to compute an "in-between" solution, i.e. no algebraic equation needed. Example exercise
Level 3 - "Chain-computations" like on level 2, but 3+ calculations. Still, no equations, i.e. you are not forced to solve it in an algebraic manner. Example exercise
Level 4 - Exercise needs to be solved by algebraic equations, not possible to calculate numerical "in-between" results. Example exercise
Level 5 -
Level 6 -
When you click an exercise into a collection, this number will be taken as difficulty for the exercise, kind of "by default".
But once the exercise is on the collection, you can edit its difficulty in the collection independently, without any effect on the "difficulty by default" here.
Why we use chess pieces? Well... we like chess, we like playing around with \(\LaTeX\)-fonts, we wanted symbols that need less space than six stars in a table-column... But in your layouts, you are of course free to indicate the difficulty of the exercise the way you want.
That being said... How "difficult" is an exercise? It depends on many factors, like what was being taught etc.
In physics exercises, we try to follow this pattern:
Level 1 - One formula (one you would find in a reference book) is enough to solve the exercise. Example exercise
Level 2 - Two formulas are needed, it's possible to compute an "in-between" solution, i.e. no algebraic equation needed. Example exercise
Level 3 - "Chain-computations" like on level 2, but 3+ calculations. Still, no equations, i.e. you are not forced to solve it in an algebraic manner. Example exercise
Level 4 - Exercise needs to be solved by algebraic equations, not possible to calculate numerical "in-between" results. Example exercise
Level 5 -
Level 6 -
Question
Solution
Short
Video
\(\LaTeX\)
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The following quantities appear in the problem:
Zeit \(t\) / Halbwertszeit \(T\) / Anzahl \(N\) /
The following formulas must be used to solve the exercise:
\(t = \frac{T}{\ln 2} \cdot \ln\left(\frac{N_2}{N_1}+1\right) \quad \)
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Exercise:
The mineral ObjectNamezircon when formed is easily contaminated with uranium but never with lead. In PersonNameClair Cameron Patterson used this mineral to determine the age of our solar system. The ratio of isotopeU to isotopePb he measured was ntO. What age did he calculate from this? The half-life of uranium- is TO.
Solution:
If no lead was present initially all lead comes from the decay of uranium; the number of lead isotopes after a certain time is therefore N_t' N_ - N_t N_t ^+fractT -N_t N_t left^+fractT-right which corresponds to the difference in the number of uranium isotopes at the ning and . For the ratio of lead to uranium we therefore have fracsscNPbsscNU eta_t fracN'_tN_t fracN_t left^+fractT-rightN_t ^+fractT-. The mineral is therefore t T lblefteta_t +right T fraclneta_t +ln T lbleftnt +right t ta old. t T lblefteta_t +right T fraclneta_t +ln t taP
The mineral ObjectNamezircon when formed is easily contaminated with uranium but never with lead. In PersonNameClair Cameron Patterson used this mineral to determine the age of our solar system. The ratio of isotopeU to isotopePb he measured was ntO. What age did he calculate from this? The half-life of uranium- is TO.
Solution:
If no lead was present initially all lead comes from the decay of uranium; the number of lead isotopes after a certain time is therefore N_t' N_ - N_t N_t ^+fractT -N_t N_t left^+fractT-right which corresponds to the difference in the number of uranium isotopes at the ning and . For the ratio of lead to uranium we therefore have fracsscNPbsscNU eta_t fracN'_tN_t fracN_t left^+fractT-rightN_t ^+fractT-. The mineral is therefore t T lblefteta_t +right T fraclneta_t +ln T lbleftnt +right t ta old. t T lblefteta_t +right T fraclneta_t +ln t taP
Meta Information
Exercise:
The mineral ObjectNamezircon when formed is easily contaminated with uranium but never with lead. In PersonNameClair Cameron Patterson used this mineral to determine the age of our solar system. The ratio of isotopeU to isotopePb he measured was ntO. What age did he calculate from this? The half-life of uranium- is TO.
Solution:
If no lead was present initially all lead comes from the decay of uranium; the number of lead isotopes after a certain time is therefore N_t' N_ - N_t N_t ^+fractT -N_t N_t left^+fractT-right which corresponds to the difference in the number of uranium isotopes at the ning and . For the ratio of lead to uranium we therefore have fracsscNPbsscNU eta_t fracN'_tN_t fracN_t left^+fractT-rightN_t ^+fractT-. The mineral is therefore t T lblefteta_t +right T fraclneta_t +ln T lbleftnt +right t ta old. t T lblefteta_t +right T fraclneta_t +ln t taP
The mineral ObjectNamezircon when formed is easily contaminated with uranium but never with lead. In PersonNameClair Cameron Patterson used this mineral to determine the age of our solar system. The ratio of isotopeU to isotopePb he measured was ntO. What age did he calculate from this? The half-life of uranium- is TO.
Solution:
If no lead was present initially all lead comes from the decay of uranium; the number of lead isotopes after a certain time is therefore N_t' N_ - N_t N_t ^+fractT -N_t N_t left^+fractT-right which corresponds to the difference in the number of uranium isotopes at the ning and . For the ratio of lead to uranium we therefore have fracsscNPbsscNU eta_t fracN'_tN_t fracN_t left^+fractT-rightN_t ^+fractT-. The mineral is therefore t T lblefteta_t +right T fraclneta_t +ln T lbleftnt +right t ta old. t T lblefteta_t +right T fraclneta_t +ln t taP
Contained in these collections:
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Isotopendifferenz mit einer Halbwertszeit by TeXercises
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Radiometrische Datierung by uz
Asked Quantity:
Zeit \(t\)
in
Sekunde \(\rm s\)
Physical Quantity
Die Zeit beschreibt die Abfolge von Ereignissen, hat also eine eindeutige, nicht umkehrbare Richtung.
Unit
Seit 1967 ist eine Sekunde das 9.192.631.770-fache der Periodendauer der Strahlung, die dem Übergang zwischen den beiden Hyperfeinstrukturniveaus des Grundzustandes von Atomen des Nuklids 133Cs entspricht.
Base?
SI?
Metric?
Coherent?
Imperial?

