Uran-Menge in Gesteinsprobe
About points...
We associate a certain number of points with each exercise.
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.
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
\(\LaTeX\)
Need help? Yes, please!
The following quantities appear in the problem:
Zeit \(t\) / Masse \(m\) / molare Masse \(M\) / Stoffmenge \(n\) / Halbwertszeit \(T\) / Anzahl \(N\) /
The following formulas must be used to solve the exercise:
\(t = \frac{T}{\ln 2} \cdot \ln\left(\frac{N_2}{N_1}+1\right) \quad \) \(m = nM \quad \) \(N_t = N_0 \cdot 2^{-\frac{t}{T}} \quad \)
No explanation / solution video to this exercise has yet been created.
Visit our YouTube-Channel to see solutions to other exercises.
Don't forget to subscribe to our channel, like the videos and leave comments!
Visit our YouTube-Channel to see solutions to other exercises.
Don't forget to subscribe to our channel, like the videos and leave comments!
Exercise:
Das natürliche Vorkommen der Blei-Isotope isotopePb isotopePb und isotopePb in der Natur beträgt prcacO prcsiO beziehungsweise prcseO. In einer tO alten Gesteinsprobe findet man mPtO Blei wovon mPsO Blei- sind. Wie viel Masse isotopeU findet man in ihr vor? Uran- hat eine Halbwertszeit von TU.
Solution:
Von den Blei-Isotopen isotopePb und isotopePb ist m_ sscmPb-m_ mPt-mPs mPsa vorhanden. Da das prcsiO+prcacOprcot entspricht müsste man also tilde m_ m_ fracprcseprcot mPse vom Isotop isotopePb im Gestein vorfinden. Das was man mehr findet also m_+ m_ - tilde m_ mPs - mPse mpl stammt von Uran-Zerfällen. In dem Gestein findet man neben dem Blei also noch sscmU m_+ frac left^fractT-right^- mpl frac left^fractTU-right^- mU Uran.
Das natürliche Vorkommen der Blei-Isotope isotopePb isotopePb und isotopePb in der Natur beträgt prcacO prcsiO beziehungsweise prcseO. In einer tO alten Gesteinsprobe findet man mPtO Blei wovon mPsO Blei- sind. Wie viel Masse isotopeU findet man in ihr vor? Uran- hat eine Halbwertszeit von TU.
Solution:
Von den Blei-Isotopen isotopePb und isotopePb ist m_ sscmPb-m_ mPt-mPs mPsa vorhanden. Da das prcsiO+prcacOprcot entspricht müsste man also tilde m_ m_ fracprcseprcot mPse vom Isotop isotopePb im Gestein vorfinden. Das was man mehr findet also m_+ m_ - tilde m_ mPs - mPse mpl stammt von Uran-Zerfällen. In dem Gestein findet man neben dem Blei also noch sscmU m_+ frac left^fractT-right^- mpl frac left^fractTU-right^- mU Uran.
Meta Information
Exercise:
Das natürliche Vorkommen der Blei-Isotope isotopePb isotopePb und isotopePb in der Natur beträgt prcacO prcsiO beziehungsweise prcseO. In einer tO alten Gesteinsprobe findet man mPtO Blei wovon mPsO Blei- sind. Wie viel Masse isotopeU findet man in ihr vor? Uran- hat eine Halbwertszeit von TU.
Solution:
Von den Blei-Isotopen isotopePb und isotopePb ist m_ sscmPb-m_ mPt-mPs mPsa vorhanden. Da das prcsiO+prcacOprcot entspricht müsste man also tilde m_ m_ fracprcseprcot mPse vom Isotop isotopePb im Gestein vorfinden. Das was man mehr findet also m_+ m_ - tilde m_ mPs - mPse mpl stammt von Uran-Zerfällen. In dem Gestein findet man neben dem Blei also noch sscmU m_+ frac left^fractT-right^- mpl frac left^fractTU-right^- mU Uran.
Das natürliche Vorkommen der Blei-Isotope isotopePb isotopePb und isotopePb in der Natur beträgt prcacO prcsiO beziehungsweise prcseO. In einer tO alten Gesteinsprobe findet man mPtO Blei wovon mPsO Blei- sind. Wie viel Masse isotopeU findet man in ihr vor? Uran- hat eine Halbwertszeit von TU.
Solution:
Von den Blei-Isotopen isotopePb und isotopePb ist m_ sscmPb-m_ mPt-mPs mPsa vorhanden. Da das prcsiO+prcacOprcot entspricht müsste man also tilde m_ m_ fracprcseprcot mPse vom Isotop isotopePb im Gestein vorfinden. Das was man mehr findet also m_+ m_ - tilde m_ mPs - mPse mpl stammt von Uran-Zerfällen. In dem Gestein findet man neben dem Blei also noch sscmU m_+ frac left^fractT-right^- mpl frac left^fractTU-right^- mU Uran.
Contained in these collections
-
Uran-Blei-Methode mit zusätzlichem Blei by TeXercises
| Title | Matched on |
|---|---|
| Uran-Blei-Methode an Gesteinsprobe | tagsformula |
| Blei-206-Anteil in Gesteinsprobe | tagsformula |
| Blei-Masse in Gesteinsprobe | tagsformula |
| Uran in Gesteinsprobe | tagstitle |
| Datierung von Gestein | tags |
Similar exercises (18)
| Title | Matched on |
|---|---|
| Uran-Blei-Methode an Gesteinsprobe | tagsformula |
| Blei-206-Anteil in Gesteinsprobe | tagsformula |
| Blei-Masse in Gesteinsprobe | tagsformula |
| Uran in Gesteinsprobe | tagstitle |
| Datierung von Gestein | tags |
| Uran-Menge in altem Gestein | tags |
| Grundlagen der Uran-Blei-Methode | tags |
| Datierung von Gestein | tags |
| Gefundene Holzaxt | tags |
| Schriftrollen vom Toten Meer | tags |
| Uran-Blei-Methode [ug a] | tags |
| Kohlenstoffmasse aus Holzwerkzeug von Fundstätte | tags |
| Höhlenmalerei | tags |
| Allgemeine Fragen | tags |
| Höhle von Lascaux | tags |
| Zerfall von C-14 | tags |
| Aktivität eines Pfeilbogens | tags |
| Âge des peintures rupestres de Lascaux | tags |