Apply independently
In these tasks nobody tells you which formula to use. Decide yourself which phenomena and models belong to the situation, solve the task on paper and justify your solution, as in the matriculation examination.
Three problems bring together the phenomena of energy, changes of state and gases from the module. In each one, you decide which phenomena and models apply to the situation.
Solve the task yourself first, on paper or on a computer. You may use a calculator, a data booklet and graphing software. Write out your reasoning, formulas, substitutions and answers with units.
Check the concepts before the tasks
These cards of the module are in your review deck. Go through them before you start the tasks.
Solar collector 15 points
Made-up example data · The data is calculated from a model and rounded as in a measurement. It is not the result of a real measurement.
Students built a solar collector: a shallow black box with a glass plate on top. The box contains $4.00\,\text{kg}$ of water. The collector is turned towards the Sun. According to the meter, the power of the solar radiation is $800\,\text{W/m}^2$, that is, $800\,\text{W}$ for every square metre perpendicular to the direction of the Sun, and the area of the collector in this direction is $0.50\,\text{m}^2$. The water is stirred all the time, and its temperature is measured every $5\,\text{min}$. The air temperature is $20.0\,{}^\circ\text{C}$.
| $t\ (\text{min})$ | $T\ ({}^\circ\text{C})$ |
|---|---|
| $0$ | $20.0$ |
| $5$ | $24.1$ |
| $10$ | $28.0$ |
| $15$ | $31.6$ |
| $20$ | $35.0$ |
| $25$ | $38.0$ |
| $30$ | $40.9$ |
| $35$ | $43.8$ |
| $40$ | $46.2$ |
| $45$ | $48.5$ |
| $50$ | $50.7$ |
| $55$ | $52.8$ |
| $60$ | $54.7$ |
- a) Draw a $(t, T)$ graph of the data and fit a model to the points. 3 p
- b) Determine the power at which the water receives energy from the solar radiation. Justify which part of the graph you use to determine it. 4 p
- c) Calculate the efficiency of the collector at the start of the measurement, when the water is still at air temperature. 2 p
- d) Why does the rise in temperature slow down? Determine the power of the heat loss at $50\,\text{min}$. 4 p
- e) Evaluate two assumptions you used in parts b–d. In which direction does each one affect the results? 2 p
Show the model answer and marking Open only when your own solution is ready.
Model answer
a)
Find
the $(t, T)$ graph of the data
Graph
The horizontal axis shows time $t\ (\text{min})$ and the vertical axis shows the temperature of the water $T\ ({}^\circ\text{C})$. The vertical axis does not have to start from zero. Each row is one separate point.
Model answer
The points are not on a straight line: at first the temperature rises by about $0.8\,\text{K}$ per minute, but at the end only by about $0.4\,\text{K}$ per minute. So a smooth, levelling-off curve is drawn through the points, not a straight line or a broken line. The auxiliary lines for parts b and d are also drawn in the figure.
b)
Given
mass of the water $m = 4.00\,\text{kg}$, specific heat capacity of water $c = 4190\,\tfrac{\text{J}}{\text{kg}\cdot\text{K}}$ and the graph from part a
Find
the power $P$ at which the water receives energy from the solar radiation
Principle
The power the water receives shows in how fast its temperature rises: the quantity of heat is $Q = cm\Delta T$ and the power is $P = Q : \Delta t$. The warmer the water is compared with the air, the more heat is conducted and radiated to the surroundings. At the start of the measurement the water is at air temperature, so then almost all the power received from the Sun heats the water. So the power is determined from the start of the graph, not from the average rise over the whole measurement.
Reading the graph
A tangent is drawn to the curve at $0\,\text{min}$. It passes through the points $(0\,\text{min}$; $20.0\,{}^\circ\text{C})$ and $(10\,\text{min}$; $28.5\,{}^\circ\text{C})$, so the initial rate of warming is
Formula
Conversions
A change in temperature is the same in degrees Celsius and in kelvins.
Substitution
Answer
$P \approx 240\,\text{W}$
Two significant figures, because the slope of the tangent is read from the graph to about two figures.
Reasonableness
The radiation arriving at the collector is $800\,\text{W/m}^2 \cdot 0.50\,\text{m}^2 = 400\,\text{W}$, so the water receives a little over half of it. The rise of $4.1\,\text{K}$ in the first five minutes gives almost the same power:
c)
Given
power received by the water $P \approx 237\,\text{W}$, radiation power per area $800\,\text{W/m}^2$ and area $A = 0.50\,\text{m}^2$
Find
the efficiency $\eta$ of the collector at the start of the measurement, when there are no losses yet
Principle
Efficiency is the ratio of useful power to incoming power. The useful power is the power from part b that the water receives at the start before losses, and the incoming power is the power of the radiation hitting the surface of the collector.
Formula
$P_\text{in} = 800\,\text{W/m}^2 \cdot A$ and $\eta = \dfrac{P}{P_\text{in}}$
Conversions
Not needed, the powers are in watts.
Substitution
Answer
$\eta \approx 0.59$
That is, about $60\,\%$, two significant figures as in the power from part b.
Reasonableness
The efficiency is at most one, because the water cannot receive more power than arrives at the collector. In a real collector it stays below one, because part of the radiation is reflected from the glass and the box, so about $60\,\%$ is believable for a simple collector.
d)
Given
power received from the Sun $P \approx 237\,\text{W}$ and the graph from part a
Find
why the warming slows down and the power of the heat loss $P_\text{loss}$ at $50\,\text{min}$
Principle
Heat is conducted through the walls of the box and the glass at a higher power, the greater the temperature difference between the water and the air ($P = UA\Delta T$), and a warm box also radiates more. As the water warms up, the loss grows, so a smaller and smaller part of the power received from the Sun is left for the water and the temperature rises more and more slowly. The power received from the Sun stays the same, so the loss is the difference between it and the power left for the water.
Reading the graph
The slope at $50\,\text{min}$ is read from the line through the points at $40\,\text{min}$ and $60\,\text{min}$, which is almost parallel to the tangent of the curve:
Formula
$P_\text{loss} = P - P_\text{water}$
Conversions
Substitution
Answer
$P_\text{loss} \approx 120\,\text{W}$
Two significant figures, because both slopes are read from the graph.
Reasonableness
At $50\,\text{min}$ the water is about $31\,\text{K}$ warmer than the air, and the loss is about half of the power received from the Sun. If it continued at the same rate, the loss would grow equal to the power received when the temperature difference is about $60\,\text{K}$. Then the temperature of the water would stop rising at about $80\,{}^\circ\text{C}$, which is believable for a simple collector.
e)
Find
two assumptions of parts b–d and the direction of their effect
Principle
An assumption is good if its error is small compared with the uncertainty of reading. For each assumption, you think about whether the water would in reality receive more or less energy than was calculated.
Model answer
Any two, with justification:
- The warming of the box and the glass has been left out. Part of the energy received from the Sun also heats the box, so the real power of the collector is slightly higher than calculated.
- No losses were assumed at the start. Losses begin as soon as the water becomes warmer than the air. If the slope is read from a line through the first points and not from the tangent at the start, it is too small, and the power comes out slightly too small.
- The meter reading $800\,\text{W/m}^2$ was assumed to stay the same for the whole hour. If a cloud or the change in the height of the Sun reduced the radiation during the measurement, part of the slowing of the warming is due to that and not to losses, and the loss in part d is too large.
Common mistakes
- A straight line is fitted through all the points, and the whole-measurement average of $0.58\,\text{K/min}$ is used as the rate of warming. Then the power is too small, because later part of the power goes into losses.
- The slope is left in the unit $\text{K/min}$, and the power comes out $60$ times too large.
- In the efficiency, the energy received by the water during the whole hour is compared with the incoming radiation, even though the losses keep changing.
- In part d, the slowing is explained only with the word "losses" without saying why they grow as the temperature rises.
Marking and self-assessment
Compare your solution with the model answer and, for each item, choose the points you think your solution earns. Part marks are possible, and any other physically correct method is accepted too.
a)3 p
b)4 p
c)2 p
d)4 p
e)2 p
Self-assessed points: 0 / 15 (15 items not assessed)
The points are your own estimate, not a checked grade. The marking is Ruukkilabra's own, written according to the features of a good matriculation examination answer, and it is not official marking by the Matriculation Examination Board (YTL).
Practise more:
- Graphs and data analysis: Determining absolute zero
- Mathematical solution: Heating and cooling of matter: $Q = cm\Delta T$
- Conceptual understanding: Heat transfer, energy balance and climate change
- Choosing and applying a model: Heating and cooling of matter: $Q = cm\Delta T$
- Experimental reasoning: Determining absolute zero
Pressure cooker 15 points
The values in the table are measured boiling temperatures of water from data books, rounded.
The lid of a pressure cooker closes tightly. When the water heats up, the pressure in the cooker rises until the valve starts to let steam out. The valve keeps the pressure in the cooker $80\,\text{kPa}$ higher than the outside air pressure of $101\,\text{kPa}$. The air left the cooker with the steam during heating, so there is only water vapour under the lid.
| $p\ (\text{kPa})$ | $T_\text{b}\ ({}^\circ\text{C})$ |
|---|---|
| $70.2$ | $90$ |
| $84.6$ | $95$ |
| $101.3$ | $100$ |
| $120.9$ | $105$ |
| $143.4$ | $110$ |
| $169.2$ | $115$ |
| $198.7$ | $120$ |
| $232.3$ | $125$ |
The table gives the boiling temperature $T_\text{b}$ of water at different pressures $p$.
- a) What is the temperature of the water in the cooker when the valve lets steam out? 3 p
- b) Explain why water boils at a higher temperature in a pressure cooker than in an open pot, and why food cooks faster in it. 3 p
- c) The cooker contains $1.50\,\text{kg}$ of water and also potatoes. When the valve hisses, the power of the hob is set to $300\,\text{W}$. Of this, $80\,\%$ is transferred to the contents of the cooker and the rest to the surroundings. The potatoes have already warmed through to the temperature of the cooker. How much water vaporises in $20$ minutes? 4 p
- d) After cooking, someone opens the lid straight away, even though the pressure has not yet dropped. Explain what happens in the cooker. What fraction of the water vaporises? 5 p
Show the model answer and marking Open only when your own solution is ready.
Model answer
a)
Given
the valve keeps a gauge pressure of $80\,\text{kPa}$, outside air pressure $101\,\text{kPa}$ and the boiling temperatures in the table
Find
the temperature $T$ of the water when the valve lets steam out
Principle
Water boils at the temperature that corresponds to the total pressure acting on the surface of the water. When the valve lets steam out, the total pressure in the cooker is the outside air pressure and the gauge pressure of the valve together. The air has already left, so under the lid there is only water vapour and the whole pressure is the pressure of the vapour. The table gives the boiling temperature only at intervals of $5\,{}^\circ\text{C}$, so a value in between is interpolated between the two nearest rows, assuming that the temperature changes evenly between them.
Formula
Conversions
Not needed, all pressures are in kilopascals.
Substitution
which is between the rows $169.2\,\text{kPa}$ and $198.7\,\text{kPa}$.
Answer
$T \approx 117\,{}^\circ\text{C}$
To the nearest degree: the gauge pressure of the valve is given to two figures, and between the values of the table the curve bends slightly.
Reasonableness
The temperature is between $115\,{}^\circ\text{C}$ and $120\,{}^\circ\text{C}$ of the table and closer to $115\,{}^\circ\text{C}$, just like the pressure lies between theirs. If the gauge pressure $80\,\text{kPa}$ had been read from the table as such, the boiling temperature would have come out below $95\,{}^\circ\text{C}$, which is impossible for a cooker whose pressure is higher than the outside air.
b)
Find
why the boiling temperature is higher and why food cooks faster
Principle
The table shows that the boiling temperature of water increases as pressure increases. The same information is in the vaporisation curve of the phase diagram, but the table is enough for the answer.
Model answer
When it boils, water vaporises as bubbles throughout the liquid. A vapour bubble exists only if the pressure of the vapour inside it is equal to the pressure of the surrounding liquid, which is affected by the pressure at the surface. The vapour pressure increases as the temperature rises, because faster particles leave the liquid more often and hit the wall of the bubble harder. The higher the pressure at the surface, the higher the temperature must be before bubbles can form. In the pressure cooker the pressure is about $1.8$ times the outside air pressure, so the water boils only at about $117\,{}^\circ\text{C}$.
Food cooks when its inner parts get warm enough. Because the water is $17\,{}^\circ\text{C}$ hotter than in an open pot, the temperature difference to the surface of the food is greater. Then heat is conducted into the food faster, and at a higher temperature the changes of cooking also happen faster.
c)
Given
power of the hob $P = 300\,\text{W}$, of which $\eta = 0.80$ is transferred to the contents of the cooker, time $t = 20\,\text{min}$ and specific latent heat of vaporisation of water $r = 2260\,\text{kJ/kg}$
Find
the mass $m$ of the water that vaporises
Principle
The valve keeps the pressure constant, so the contents of the cooker stay at the boiling temperature. The temperature does not rise, and the potatoes are assumed to be already at the temperature of the cooker, so all the energy transferred to the contents is used to vaporise water, and the steam produced escapes through the valve. The mass of the water and the potatoes is not needed: it only determines how long the water lasts.
Formula
$\eta P t = rm$, so $m = \dfrac{\eta P t}{r}$
Conversions
Substitution
Answer
$m \approx 0.13\,\text{kg}$
Two significant figures as in the fraction $0.80$ and the time $20\,\text{min}$.
Reasonableness
Less than a tenth of the water vaporises, so there is plenty left. The value of $r$ from the table is measured at $100\,{}^\circ\text{C}$, and at $117\,{}^\circ\text{C}$ it is slightly smaller (about $2.21 \cdot 10^6\,\text{J/kg}$). The result $0.13\,\text{kg}$ still does not change.
d)
Given
temperature of the water $117\,{}^\circ\text{C}$, boiling temperature at outside air pressure $100\,{}^\circ\text{C}$, $c = 4190\,\tfrac{\text{J}}{\text{kg}\cdot\text{K}}$ and $r = 2.26 \cdot 10^6\,\text{J/kg}$
Find
what happens and what fraction $\dfrac{m_\text{v}}{m}$ of the water vaporises
Principle
When the lid is opened, the pressure in the cooker drops straight to the outside air pressure, so the boiling temperature drops to $100\,{}^\circ\text{C}$. The water is $17\,{}^\circ\text{C}$ hotter than its boiling temperature, so it boils violently throughout its volume until it has cooled to $100\,{}^\circ\text{C}$. Energy is conserved: the energy needed for the vaporisation comes from the cooling of the water itself. The part that vaporises is small, so the whole mass $m$ can be used as the mass of the cooling water.
Formula
$c m \Delta T = r m_\text{v}$, so
Conversions
$r = 2.26 \cdot 10^6\,\text{J/kg}$
Substitution
Answer
about $3\,\%$ of the water vaporises in an instant. One significant figure is enough, because the heat of the potatoes and the cooker was left out of the calculation. They also cool down and vaporise more water, so the real fraction is slightly larger.
Reasonableness
After part c there is about $1.4\,\text{kg}$ of water, and about $40\,\text{g}$ of it vaporises. That is about $2.4\,\text{mol}$, and as an ideal gas at $100\,{}^\circ\text{C}$ and a pressure of $101\,\text{kPa}$ it takes up a volume of
Tens of litres of hot steam and boiling splashes are released at once, and steam burns worse as it condenses than water at the same temperature. So a pressure cooker may be opened only after the pressure has dropped.
Also accepted
- In parts c and d the value $r \approx 2.21 \cdot 10^6\,\text{J/kg}$ for $117\,{}^\circ\text{C}$ can be used; the results do not change.
- If the boiling temperature in part a is read slightly differently (for example $116$–$118\,{}^\circ\text{C}$), part d is marked using that value.
Common mistakes
- The temperature corresponding to the gauge pressure $80\,\text{kPa}$ is read from the table, even though the boiling temperature depends on the total pressure.
- In part c the warming of the water is calculated with the formula $Q = cm\Delta T$, even though the temperature does not change, or the whole power of the hob, $300\,\text{W}$, is used.
- In part d it is assumed that more heat is needed for the boiling, even though the energy comes from the cooling of the water itself.
- In part b it is only stated that "pressure raises the boiling point", without explaining why.
Marking and self-assessment
Compare your solution with the model answer and, for each item, choose the points you think your solution earns. Part marks are possible, and any other physically correct method is accepted too.
a)3 p
b)3 p
c)4 p
d)5 p
Self-assessed points: 0 / 15 (15 items not assessed)
The points are your own estimate, not a checked grade. The marking is Ruukkilabra's own, written according to the features of a good matriculation examination answer, and it is not official marking by the Matriculation Examination Board (YTL).
Practise more:
- Conceptual understanding: Changes of state
- Graphs and data analysis: Determining absolute zero
- Choosing and applying a model: Thermal balance during a change of state
- Mathematical solution: Thermal balance during a change of state
- Explaining physics: Changes of state
Diving 15 points
A diver is at a depth of $15.0\,\text{m}$ in a lake. There the temperature of the water is $6.0\,{}^\circ\text{C}$, and at the surface it is $20.0\,{}^\circ\text{C}$. The atmospheric pressure is $101\,\text{kPa}$. The diver breathes from a tank through a regulator: the regulator supplies air at the same pressure as in the surrounding water.
- a) The volume of an air bubble breathed out by the diver is $4.0\,\text{cm}^3$ at the bottom. What is its volume at the surface? 4 p
- b) At a depth of $15.0\,\text{m}$ the diver fills their lungs with $6.0\,\text{l}$ of air. Why is it dangerous to rise to the surface holding your breath? Justify with a calculation. 3 p
- c) The volume of the diver's tank is $12.0\,\text{l}$, and its pressure gauge shows a gauge pressure of $200\,\text{bar}$, where $1\,\text{bar} = 100\,\text{kPa}$. At a depth of $15.0\,\text{m}$ the diver uses $20\,\text{l}$ of air per minute at the pressure of that depth. The ascent is started when the gauge shows $50\,\text{bar}$. Assume that the air is equally warm in the tank and in the lungs. How long can the diver stay at this depth? 5 p
- d) Evaluate two assumptions of the calculation in part c. Is the real time likely to be shorter or longer than the calculated one? How should the result be used? 3 p
Show the model answer and marking Open only when your own solution is ready.
Model answer
a)
Given
volume of the bubble at the bottom $V_1 = 4.0\,\text{cm}^3$, depth $h = 15.0\,\text{m}$, temperatures $T_1 = 6.0\,{}^\circ\text{C}$ and $T_2 = 20.0\,{}^\circ\text{C}$, atmospheric pressure $p_0 = 101\,\text{kPa}$, density of water $\rho = 1000\,\text{kg/m}^3$ and $g = 9.81\,\text{m/s}^2$
Find
the volume $V_2$ of the bubble at the surface
Principle
The amount of air in the bubble stays the same. The bubble is small, so it is always at the temperature of the surrounding water, and its pressure is the pressure of the water at that depth: atmospheric pressure and hydrostatic pressure together. From the equation of state of an ideal gas $pV = nRT$ it follows that when $n$ is constant, $\dfrac{pV}{T}$ stays the same. Both pressure and temperature change, so neither can be left out.
Formula
so
where at the surface $p_2 = p_0$
Conversions
The volume can stay in cubic centimetres, because the equation has a ratio of volumes.
Substitution
Answer
$V_2 \approx 10\,\text{cm}^3$
Two significant figures as in the volume $4.0\,\text{cm}^3$.
Reasonableness
The pressure falls by a factor of about $2.5$ as the bubble rises, so the volume grows to about $2.5$ times, and the warming increases it by about $5\,\%$ more. The growth of bubbles as they rise can also be seen in diving videos.
b)
Given
lungs full of air, $V_1 = 6.0\,\text{l}$, at pressure $p_1 = 248\,\text{kPa}$ and pressure at the surface $p_2 = 101\,\text{kPa}$
Find
the volume of the air at the surface and why rising while holding your breath is dangerous
Principle
The amount of air stays the same when you hold your breath. The air in the lungs is at body temperature, about $37\,{}^\circ\text{C}$, regardless of depth and the temperature of the water. So the temperature stays constant, and the volume changes according to Boyle's law.
Formula
$p_1 V_1 = p_2 V_2$, so $V_2 = V_1 \cdot \dfrac{p_1}{p_2}$
Conversions
Not needed, the units cancel in the ratio of the pressures.
Substitution
Answer
The air would expand to about $15\,\text{l}$ (two significant figures as in $6.0\,\text{l}$). The lungs can hold only the $6.0\,\text{l}$ given in the problem, so the trapped air would stretch them and could tear the lung tissue. While rising, you must never hold your breath: you breathe normally throughout the ascent, so that the expanding air can escape from the lungs.
Reasonableness
The volume grows in the same ratio as the bubble in part a, except for the share due to warming: the temperature of the lungs does not change.
c)
Given
volume of the tank $V_\text{tank} = 12.0\,\text{l}$, gauge readings $200\,\text{bar}$ and $50\,\text{bar}$ of gauge pressure, consumption $q = 20\,\text{l/min}$ at the pressure of the depth $p = 248\,\text{kPa}$
Find
the time $t$ the diver can stay at a depth of $15.0\,\text{m}$
Principle
According to the problem, the temperature of the air is the same in the tank and in the lungs (part d) estimates the effect of warming), so the amount of air is proportional to the product of pressure and volume (Boyle's law). The air used from the tank takes up, at the pressure of the depth, the volume that is breathed. The gauge shows gauge pressure. However, the difference of the total pressures is the same as the difference of the gauge pressures, because the atmospheric pressure cancels.
Formula
$\Delta p_\text{tank} V_\text{tank} = p V$, so
and $t = \dfrac{V}{q}$
Conversions
The volumes can stay in litres.
Substitution
Answer
$t \approx 36\,\text{min}$
Two significant figures as in the consumption $20\,\text{l/min}$.
Reasonableness
At the surface the same air would last $2.5$ times longer, about $89\,\text{min}$, because each breath takes $2.5$ times the amount of air at depth. A dive of about half an hour matches ordinary recreational dives.
d)
Find
two assumptions, the direction of their effect and the use of the result
Principle
The calculation is a model. For each assumption, you think about whether in reality more or less air is used than in the model.
Model answer
Any two, with justification:
- The consumption is steady. Exertion, cold water and nervousness increase breathing, so the real time is often shorter.
- The whole time is spent at a depth of $15.0\,\text{m}$. During the descent and the ascent the pressure is lower and less air is used, so in this respect the time is longer.
- The temperature stays the same. The air in the tank is at the temperature of the water, but the consumption $20\,\text{l/min}$ is measured in the lungs at body temperature. When it warms up, the same amount of air takes up about $10\,\%$ more space, so less of the tank air is used per minute and the time is about $10\,\%$ longer.
An additional note: at very high pressure air is no longer exactly an ideal gas, and the tank contains slightly less air than the model gives. This is not required in upper secondary school.
The calculated time is a rough estimate, not a guarantee. A dive is planned so that some air is left in reserve, and the ascent is started by the reading of the gauge and not by the clock.
Common mistakes
- Only the hydrostatic pressure $\rho g h \approx 147\,\text{kPa}$ is used as the pressure, without the atmospheric pressure.
- In part a, the temperatures are substituted in degrees Celsius, or the change in temperature is ignored without justification.
- In part b, the temperature of the water is used as the temperature, even though the air in the lungs is at body temperature.
- In part c, the air in the tank is compared with the pressure at the surface, so the time comes out about $89\,\text{min}$, more than double.
Marking and self-assessment
Compare your solution with the model answer and, for each item, choose the points you think your solution earns. Part marks are possible, and any other physically correct method is accepted too.
a)4 p
b)3 p
c)5 p
d)3 p
Self-assessed points: 0 / 15 (15 items not assessed)
The points are your own estimate, not a checked grade. The marking is Ruukkilabra's own, written according to the features of a good matriculation examination answer, and it is not official marking by the Matriculation Examination Board (YTL).
Practise more:
- Choosing and applying a model: Ideal gas law $pV = nRT$
- Mathematical solution: Pressure and hydrostatic pressure
- Conceptual understanding: Changes of state of a gas and Boyle's law
- Explaining physics: Changes of state of a gas and Boyle's law