Luftblase
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:
Temperatur \(T\) / Volumen \(V\) / Druck \(p\) / Ortsfaktor \(g\) / Höhe \(h\) / Stoffmenge \(n\) / Dichte \(\varrho\) /
The following formulas must be used to solve the exercise:
\(p = \varrho g h \quad \) \(pV = nRT \quad \)
No explanation / solution video to this exercise has yet been created.
Visit our YouTube-Channel to see solutions to other exercises.
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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:
Eine Luftblase cubiccentimeter steige vom m tiefen Grund .celsius eines Sees an die celsius warme Oberfläche hPa. Wie gross ist ihr Volumen nun?
Solution:
newqtyVeocubiccentimeter newqtyVeVeon cubicmeter newqtyhm newqtyTeo.celsius newqtyTe.K newqtyrkgpcm newqtyTzocelsius newqtyTz.K newqtypzohPa newqtypzpzon ePa % Geg V_ Veo Ve h h theta_ Teo pf T_ Te textSee pf rho r theta_ Tzo pf T_ Tz p_ pzo pz % GesVolumenV_ sicubicmeter % Der Druck in h Tiefe beträgt bei pz Oberflächruck solqtyperho gh + p_rn*ncgn*hn + pznPa al p_ pef r ncg h + pz pe. Für das Volumen kurz vor dem Austritt aus dem Wasser gilt: solqtyVzfracpefV_T_ fracT_p_pen*Ven/Ten*Tzn/pzncubicmeter al fracp_V_T_ fracp_V_T_ V_ fracp_V_T_ fracT_p_ Vzf fracpe VeTe fracTzpz Vz. % V_ Vzf VzII
Eine Luftblase cubiccentimeter steige vom m tiefen Grund .celsius eines Sees an die celsius warme Oberfläche hPa. Wie gross ist ihr Volumen nun?
Solution:
newqtyVeocubiccentimeter newqtyVeVeon cubicmeter newqtyhm newqtyTeo.celsius newqtyTe.K newqtyrkgpcm newqtyTzocelsius newqtyTz.K newqtypzohPa newqtypzpzon ePa % Geg V_ Veo Ve h h theta_ Teo pf T_ Te textSee pf rho r theta_ Tzo pf T_ Tz p_ pzo pz % GesVolumenV_ sicubicmeter % Der Druck in h Tiefe beträgt bei pz Oberflächruck solqtyperho gh + p_rn*ncgn*hn + pznPa al p_ pef r ncg h + pz pe. Für das Volumen kurz vor dem Austritt aus dem Wasser gilt: solqtyVzfracpefV_T_ fracT_p_pen*Ven/Ten*Tzn/pzncubicmeter al fracp_V_T_ fracp_V_T_ V_ fracp_V_T_ fracT_p_ Vzf fracpe VeTe fracTzpz Vz. % V_ Vzf VzII
Meta Information
Exercise:
Eine Luftblase cubiccentimeter steige vom m tiefen Grund .celsius eines Sees an die celsius warme Oberfläche hPa. Wie gross ist ihr Volumen nun?
Solution:
newqtyVeocubiccentimeter newqtyVeVeon cubicmeter newqtyhm newqtyTeo.celsius newqtyTe.K newqtyrkgpcm newqtyTzocelsius newqtyTz.K newqtypzohPa newqtypzpzon ePa % Geg V_ Veo Ve h h theta_ Teo pf T_ Te textSee pf rho r theta_ Tzo pf T_ Tz p_ pzo pz % GesVolumenV_ sicubicmeter % Der Druck in h Tiefe beträgt bei pz Oberflächruck solqtyperho gh + p_rn*ncgn*hn + pznPa al p_ pef r ncg h + pz pe. Für das Volumen kurz vor dem Austritt aus dem Wasser gilt: solqtyVzfracpefV_T_ fracT_p_pen*Ven/Ten*Tzn/pzncubicmeter al fracp_V_T_ fracp_V_T_ V_ fracp_V_T_ fracT_p_ Vzf fracpe VeTe fracTzpz Vz. % V_ Vzf VzII
Eine Luftblase cubiccentimeter steige vom m tiefen Grund .celsius eines Sees an die celsius warme Oberfläche hPa. Wie gross ist ihr Volumen nun?
Solution:
newqtyVeocubiccentimeter newqtyVeVeon cubicmeter newqtyhm newqtyTeo.celsius newqtyTe.K newqtyrkgpcm newqtyTzocelsius newqtyTz.K newqtypzohPa newqtypzpzon ePa % Geg V_ Veo Ve h h theta_ Teo pf T_ Te textSee pf rho r theta_ Tzo pf T_ Tz p_ pzo pz % GesVolumenV_ sicubicmeter % Der Druck in h Tiefe beträgt bei pz Oberflächruck solqtyperho gh + p_rn*ncgn*hn + pznPa al p_ pef r ncg h + pz pe. Für das Volumen kurz vor dem Austritt aus dem Wasser gilt: solqtyVzfracpefV_T_ fracT_p_pen*Ven/Ten*Tzn/pzncubicmeter al fracp_V_T_ fracp_V_T_ V_ fracp_V_T_ fracT_p_ Vzf fracpe VeTe fracTzpz Vz. % V_ Vzf VzII
Contained in these collections:
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Universelle Gasgleichung by pw
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Luftblase mit T by TeXercises
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Universelle Gasgleichung by uz
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Ideale Gasgleichung by aej
Asked Quantity:
Volumen \(V\)
in
Kubikmeter \(\rm m^3\)
Physical Quantity
Rauminhalt
Unit
Kubikmeter (\(\rm m^3\))
Base?
SI?
Metric?
Coherent?
Imperial?