Iron meteorite
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:
Masse \(m\) / Temperatur \(T\) / Energie \(E\) / Wärme \(Q\) / spezifische latente Wärme \(L\) / Wärmekapazität \(c\) /
The following formulas must be used to solve the exercise:
\(\sum E_{\scriptscriptstyle\rm tot} \stackrel{!}{=} \sum E_{\scriptscriptstyle\rm tot}' \quad \) \(Q = c \cdot m \cdot \Delta\vartheta \quad \) \(E_{\rm \scriptscriptstyle kin} = \dfrac12 mv^2 \quad \) \(Q = m \cdot L_{\scriptscriptstyle\rm f} \quad \)
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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:
An iron meteorite melts when it enters the Earth's atmosphere. If its initial temperature was -degreeCelsius outside of Earth's atmosphere calculate the minimum velocity the meteorite must have had before it entered Earth's atmosphere. FormelbuchIron melts at degreeCelsius its specific heat is jouleperkilogramperkelvin and its latent heat of fusion .ejouleperkilogram.
Solution:
If the iron meteorite melts it must be heaten up to irons melting po theta_fdegreeCelsius and then be melted. The energy for these two processes comes from the meteorites speed. % EnergieSchritte PGleichungsscEkin Q + ssctilde Qf PGleichungfracmv^ c m Delta theta + msscLf PGleichungfracmv^ c m sscthetaf - theta + msscLf AlgebraSchritte MGleichungmv^ c m sscthetaf - theta + msscLf MGleichungv^ c sscthetaf - theta + sscLf PHYSMATH % The speed is al v sqrtc sscthetaf - theta + sscLf sqrt JpkgK celsius - -celsius + .eJpkg .kilo.
An iron meteorite melts when it enters the Earth's atmosphere. If its initial temperature was -degreeCelsius outside of Earth's atmosphere calculate the minimum velocity the meteorite must have had before it entered Earth's atmosphere. FormelbuchIron melts at degreeCelsius its specific heat is jouleperkilogramperkelvin and its latent heat of fusion .ejouleperkilogram.
Solution:
If the iron meteorite melts it must be heaten up to irons melting po theta_fdegreeCelsius and then be melted. The energy for these two processes comes from the meteorites speed. % EnergieSchritte PGleichungsscEkin Q + ssctilde Qf PGleichungfracmv^ c m Delta theta + msscLf PGleichungfracmv^ c m sscthetaf - theta + msscLf AlgebraSchritte MGleichungmv^ c m sscthetaf - theta + msscLf MGleichungv^ c sscthetaf - theta + sscLf PHYSMATH % The speed is al v sqrtc sscthetaf - theta + sscLf sqrt JpkgK celsius - -celsius + .eJpkg .kilo.
Meta Information
Exercise:
An iron meteorite melts when it enters the Earth's atmosphere. If its initial temperature was -degreeCelsius outside of Earth's atmosphere calculate the minimum velocity the meteorite must have had before it entered Earth's atmosphere. FormelbuchIron melts at degreeCelsius its specific heat is jouleperkilogramperkelvin and its latent heat of fusion .ejouleperkilogram.
Solution:
If the iron meteorite melts it must be heaten up to irons melting po theta_fdegreeCelsius and then be melted. The energy for these two processes comes from the meteorites speed. % EnergieSchritte PGleichungsscEkin Q + ssctilde Qf PGleichungfracmv^ c m Delta theta + msscLf PGleichungfracmv^ c m sscthetaf - theta + msscLf AlgebraSchritte MGleichungmv^ c m sscthetaf - theta + msscLf MGleichungv^ c sscthetaf - theta + sscLf PHYSMATH % The speed is al v sqrtc sscthetaf - theta + sscLf sqrt JpkgK celsius - -celsius + .eJpkg .kilo.
An iron meteorite melts when it enters the Earth's atmosphere. If its initial temperature was -degreeCelsius outside of Earth's atmosphere calculate the minimum velocity the meteorite must have had before it entered Earth's atmosphere. FormelbuchIron melts at degreeCelsius its specific heat is jouleperkilogramperkelvin and its latent heat of fusion .ejouleperkilogram.
Solution:
If the iron meteorite melts it must be heaten up to irons melting po theta_fdegreeCelsius and then be melted. The energy for these two processes comes from the meteorites speed. % EnergieSchritte PGleichungsscEkin Q + ssctilde Qf PGleichungfracmv^ c m Delta theta + msscLf PGleichungfracmv^ c m sscthetaf - theta + msscLf AlgebraSchritte MGleichungmv^ c m sscthetaf - theta + msscLf MGleichungv^ c sscthetaf - theta + sscLf PHYSMATH % The speed is al v sqrtc sscthetaf - theta + sscLf sqrt JpkgK celsius - -celsius + .eJpkg .kilo.
Contained in these collections:
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Latente Wärme by pw
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Latente Wärme und Energiesatz by TeXercises
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Latente Wärme 1 by uz
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Latente Wärmen by aej