So let's consider a scenario where we want to send a balloon carrying a payload weighting 800g to an altitude of 30000 meters (30Km). From the Kaymont balloons manufacturer site lets choose the HAB-600 balloon. This is a 600 grams balloon recommended for individuals or groups launching a photographic mission for the first time. This balloon is recommended for payloads with a weight between 500 and 1000 grams.
Then lets use the CUSF balloon burst calculator and set the following (be sure that the selected gas is Helium):
- Payload mass (g): 800g
- Balloon mass (g): Kaymont - 600
- Target burst altitude (m): 30000
- Burst altitude: 30000m (as we have selected in the inputs for the calculator)
- Time to burst: 134m
- Launch volume: 1.81m3 (1811 L)
- Ascent rate: 3.72 m/s (223.2 m/min)
- Neck lift: 1258g
To summarise we now have a 600-grams balloon at the Earth surface (let's consider at the sea level - 0 meters) filled in with 1811 litres of Helium. How can we then know what will be the size of the balloon at the surface and then at different altitudes?
Well for the size of the balloon let's apply the formula for the volume of a sphere (we are here considering the balloon to be a sphere):
$$Volume= V= \frac{4}{3}\pi r^{3}$$
Where:
$$1.811=\frac{4}{3}3.14r^{3}=4.19r^{3}\Leftrightarrow r^{3}=0.43\Leftrightarrow r=0.75m\Leftrightarrow diameter=d=r*2=1.5m$$
To summarise once again (but with more information), we have a 600-grams balloon at the Earth surface (let's consider at the sea level - 0 meters) filled in with 1811 litres of Helium and with a diameter of 1.5m.
Now let's determine the volume of this same balloon at a different altitude, for instance at 20km. As we have seen before, as the balloon rises, its volume increases and consequently the diameter of the balloon also increases. So let's use the ideal gas law to determine what will be the volume and diameter of the balloon at this altitude of 20km, but let's first deduce a general formula that allows to determine that. As we have seen before:
PV = nRT
Imagine that we have a balloon and that we have two different states, S1 and S2, associated to the balloon. In state 1 (S1) the balloon is at the Earth's surface and in state 2 (S2) the balloon will be at a different altitude, for instance, 20 km.
So now let's draw the ideal gas law for each one of the states S1 and S2:
For S1:
P1V1 = n1RT1
(P1V1)⁄(n1RT1)= 1 (eq. 1)
For S2:
P2V2 = n2RT2
(P2V2)⁄(n2RT2)= 1 (eq. 2)
As the first term of eq. 1 equals 1 and the first term of eq. 2 also equals 1, we can say that those terms are equal to each other:
(P1V1)⁄(n1RT1) = (P2V2)⁄(n2RT2)
But as the amount of gas do not change between S1 and S2, we can say that n = n1 = n2, and consequently:
(P1V1)⁄(nRT1) = (P2V2)⁄(nRT2) <=> nR(P1V1)⁄(nRT1) = nR(P2V2)⁄(nRT2) <=> (P1V1)⁄(T1) = (P2V2)⁄(T2) <=>
$$V_{2}=V_{1}\frac{P_{1}T_{2}}{P_{2}T_{1}} (eq. 3)$$
So the above formula is a general formula that allow us to determine the volume of the balloon in state 2 (S2) given the balloon conditions in state 1 (S1) and given the temperature and pressure of the balloon in state 2 (S2). To make this more concrete let's apply to our example balloon. As we have seen before, in state 1 (S1), we have the 600-grams balloon at sea level (0 meters) filled in with 1811 litres of Helium and with a diameter of 1.5m. Additionally let's consider that for the absolute pressure at sea level we have 101325 Pa and the temperature is 15ºC, as indicated by the International Standard Atmosphere (ISA):
State 1 (S1)
State 2 (S2)
Well for the size of the balloon let's apply the formula for the volume of a sphere (we are here considering the balloon to be a sphere):
$$Volume= V= \frac{4}{3}\pi r^{3}$$
Where:
- π= 3.14
- r= radius= diameter⁄2
$$1.811=\frac{4}{3}3.14r^{3}=4.19r^{3}\Leftrightarrow r^{3}=0.43\Leftrightarrow r=0.75m\Leftrightarrow diameter=d=r*2=1.5m$$
To summarise once again (but with more information), we have a 600-grams balloon at the Earth surface (let's consider at the sea level - 0 meters) filled in with 1811 litres of Helium and with a diameter of 1.5m.
Now let's determine the volume of this same balloon at a different altitude, for instance at 20km. As we have seen before, as the balloon rises, its volume increases and consequently the diameter of the balloon also increases. So let's use the ideal gas law to determine what will be the volume and diameter of the balloon at this altitude of 20km, but let's first deduce a general formula that allows to determine that. As we have seen before:
PV = nRT
Imagine that we have a balloon and that we have two different states, S1 and S2, associated to the balloon. In state 1 (S1) the balloon is at the Earth's surface and in state 2 (S2) the balloon will be at a different altitude, for instance, 20 km.
So now let's draw the ideal gas law for each one of the states S1 and S2:
For S1:
P1V1 = n1RT1
(P1V1)⁄(n1RT1)= 1 (eq. 1)
For S2:
P2V2 = n2RT2
(P2V2)⁄(n2RT2)= 1 (eq. 2)
As the first term of eq. 1 equals 1 and the first term of eq. 2 also equals 1, we can say that those terms are equal to each other:
(P1V1)⁄(n1RT1) = (P2V2)⁄(n2RT2)
But as the amount of gas do not change between S1 and S2, we can say that n = n1 = n2, and consequently:
(P1V1)⁄(nRT1) = (P2V2)⁄(nRT2) <=> nR(P1V1)⁄(nRT1) = nR(P2V2)⁄(nRT2) <=> (P1V1)⁄(T1) = (P2V2)⁄(T2) <=>
$$V_{2}=V_{1}\frac{P_{1}T_{2}}{P_{2}T_{1}} (eq. 3)$$
So the above formula is a general formula that allow us to determine the volume of the balloon in state 2 (S2) given the balloon conditions in state 1 (S1) and given the temperature and pressure of the balloon in state 2 (S2). To make this more concrete let's apply to our example balloon. As we have seen before, in state 1 (S1), we have the 600-grams balloon at sea level (0 meters) filled in with 1811 litres of Helium and with a diameter of 1.5m. Additionally let's consider that for the absolute pressure at sea level we have 101325 Pa and the temperature is 15ºC, as indicated by the International Standard Atmosphere (ISA):
State 1 (S1)
- 600-grams balloon
- Altitude= 0 meters (sea-level)
- Pressure= P1= 101325 Pa
- Temperature= T1= 15 ºC= 288.15 k
- Volume= V1= 1811L= 1.811 m3
- Diameter= 1.5 m
State 2 (S2)
- 600-grams balloon
- Altitude= 20000 meters (20km)
- Pressure= P2= 5474.9 Pa
- Temperature= T2= -56.5 ºC= 216.65 k
- Volume= V2= ?
- Diameter= ?
$$V_{2}=V_{1}\frac{P_{1}T_{2}}{P_{2}T_{1}} <=> V_{2}=1811 \times \frac{101325 \times 216.65}{5474.9 \times 288.15} <=> V_{2}=1811 \times \frac{21952061.25}{1577592.435} <=>$$
$$<=> V_{2}=1811 \times 13.91 <=> V_{2}=25191.01L= 25.2m^{3}$$
And now that we have determined the volume of the balloon at state 2 (S2), it is just a question of determining the new diameter of the balloon:
$$25.2=\frac{4}{3}3.14r^{3}=4.19r^{3}\Leftrightarrow r^{3}=6.01\Leftrightarrow r=1.82m\Leftrightarrow diameter=d=r*2=3.64m$$
Finally let's model a state 3 (S3) of the balloon, where we would like to know the volume and consequently the diameter of the same balloon when at an altitude of 30000 meters. For the pressure and temperature at that altitude let's use again the ISA values but this time retrieved from the Engineering ToolBox site. So let's consider that for the absolute pressure at 30 km we have 0.01197 bar, which corresponds to 1197 Pa, and the temperature is 226.5k:
State 3 (S3)
$$<=> V_{2}=1811 \times 13.91 <=> V_{2}=25191.01L= 25.2m^{3}$$
And now that we have determined the volume of the balloon at state 2 (S2), it is just a question of determining the new diameter of the balloon:
$$25.2=\frac{4}{3}3.14r^{3}=4.19r^{3}\Leftrightarrow r^{3}=6.01\Leftrightarrow r=1.82m\Leftrightarrow diameter=d=r*2=3.64m$$
Finally let's model a state 3 (S3) of the balloon, where we would like to know the volume and consequently the diameter of the same balloon when at an altitude of 30000 meters. For the pressure and temperature at that altitude let's use again the ISA values but this time retrieved from the Engineering ToolBox site. So let's consider that for the absolute pressure at 30 km we have 0.01197 bar, which corresponds to 1197 Pa, and the temperature is 226.5k:
State 3 (S3)
- 600-grams balloon
- Altitude= 30000 meters (30km)
- Pressure= P3= 1197 Pa
- Temperature= T3= 226.5 k
- Volume= V3= ?
- Diameter= ?
$$V_{3}=V_{1}\frac{P_{1}T_{3}}{P_{3}T_{1}} <=> V_{3}=1811 \times \frac{101325 \times 226.5}{1197 \times 288.15} <=> V_{3}=1811 \times \frac{22950112.5}{344915.55} <=>$$
$$<=> V_{3}=1811 \times 66.54 <=> V_{3}=120503.94L= 120.5m^{3}$$
And now that we have determined the volume of the balloon at state 3 (S3), it is just a question of determining the new diameter of the balloon:
$$120.5=\frac{4}{3}3.14r^{3}=4.19r^{3}\Leftrightarrow r^{3}=28.76\Leftrightarrow r=3.06m\Leftrightarrow diameter=d=r*2=6.12m$$
The table bellow summarises the results for the three states, S1, S2, S3:
$$<=> V_{3}=1811 \times 66.54 <=> V_{3}=120503.94L= 120.5m^{3}$$
And now that we have determined the volume of the balloon at state 3 (S3), it is just a question of determining the new diameter of the balloon:
$$120.5=\frac{4}{3}3.14r^{3}=4.19r^{3}\Leftrightarrow r^{3}=28.76\Leftrightarrow r=3.06m\Leftrightarrow diameter=d=r*2=6.12m$$
The table bellow summarises the results for the three states, S1, S2, S3:
S1
|
S2
|
S3
|
|
Type
|
600-grams
|
600-grams
|
600-grams
|
Altitude (m)
|
0
|
20000
|
30000
|
Pressure (Pa)
|
101325
|
5474.9
|
1197
|
Temperature (K)
|
288.15
|
216.65
|
226.5
|
Volume (m3)
|
1.811
|
25.2
|
120.5
|
Diameter (m)
|
1.5
|
3.64
|
6.12
|
If you remember from the beginning of this post, we have used the CUSF balloon burst calculator and set the balloon parameters in such a way that the target burst altitude would be 30000m. Well, from the above calculations we have just determined that at 30000m the balloon will have a diameter of 6.12m. Consequently this means that the diameter of the balloon when bursting will be approximately 6.12m.
These results are very similar to the results presented in the Kaymont balloons manufacturer site regarding the weather forecasting (sounding) 600-grams balloon (with a 250g payload) - it is just a question of converting the units there in order to see that the resulting values are very similar to the ones we have just reached above. This means that we are now equipped to better understand the balloon specifications (and nomenclature) and the different possible configurations of the balloon and its consequences.
These results are very similar to the results presented in the Kaymont balloons manufacturer site regarding the weather forecasting (sounding) 600-grams balloon (with a 250g payload) - it is just a question of converting the units there in order to see that the resulting values are very similar to the ones we have just reached above. This means that we are now equipped to better understand the balloon specifications (and nomenclature) and the different possible configurations of the balloon and its consequences.
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