The escape speed from the Earth is \({\bf{1}}{\bf{.12 \times 1}}{{\bf{0}}^{\bf{4}}}\;{\bf{m/s}}\),that is, a gas molecule traveling away from Earth near the outer boundary of the Earth’s atmosphere would, at this speed, be able to escape from the Earth’s gravitational field and be lost in the atmosphere. At what temperature is the RMS speed of (a) oxygen molecules and (b) helium atoms equal to \({\bf{1}}{\bf{.12 \times 1}}{{\bf{0}}^{\bf{4}}}\;{\bf{m/s}}\)? (c) Can you explain why our atmosphere contains oxygen but not helium?

Short Answer

Expert verified

(a) The RMS speed of oxygen molecules is equal to \(1.12 \times {10^4}\;{\rm{m/s}}\)at a temperature of\(1.61\; \times {10^5}\;{\rm{K}}\).

(b) The RMS speed of helium atoms is equal to \(1.12 \times {10^4}\;{\rm{m/s}}\)at a temperature of\(2.01\; \times {10^4}\;{\rm{K}}\).

(c) Earth’s atmosphere contains oxygen but not helium because the temperature at which oxygen molecules can escape the Earth’s atmosphere is very much higher than that of helium atoms.

Step by step solution

01

Step 1:Understanding of root-mean square (RMS) speed

The square root of the mean of the square of the molecules’ speedin a gas at a certain temperature Tis termed as the root-mean square speed of that gas.

The RMS speed is given as

\({v_{{\rm{rms}}}} = \sqrt {\frac{{3kT}}{m}} \). …… (i)

Here, \(k\)is the Boltzmann’s constant, T is the temperature,and m is the mass of each molecule.

02

Given Data

The RMS speed of oxygen molecules and helium atoms is\({v_{{\rm{rms}}}} = 1.12 \times {10^4}\;{\rm{m/s}}\).

The molecular mass of oxygen is 32 u.

The atomic mass of the helium atom is 4 u.

03

(a) Determination of temperature of oxygen molecules

The mass of the oxygen molecule can be calculated in the following manner:

\(\begin{aligned}m &= 32\;{\rm{u}} \times \frac{{1.66 \times {{10}^{ - 27}}\;{\rm{kg}}}}{{1\;{\rm{u}}}}\\m &= 53.12 \times {10^{ - 27}}\;{\rm{kg}}\end{aligned}\)

From equation (i), the temperature is given by

\(T = \frac{{mv_{{\rm{rms}}}^2}}{{3k}}\). …… (ii)

Substitute the values into the above equation.

\(\begin{aligned}T &= \frac{{\left( {53.12\; \times {{10}^{ - 27}}\;{\rm{kg}}} \right){{\left( {1.12 \times {{10}^4}\;{\rm{m/s}}} \right)}^2}}}{{3\left( {1.38 \times {{10}^{ - 23}}\;{\rm{J/K}}} \right)}}\\ &= 1.61\; \times {10^5}\;{\rm{K}}\end{aligned}\)

Thus, the RMS speed of oxygen molecules is equal to \(1.12 \times {10^4}\;{\rm{m/s}}\)at the temperature of\(1.61\; \times {10^5}\;{\rm{K}}\).

04

(b) Determination of temperature of helium atoms

The mass of the helium atom can be calculated in the following manner:

\(\begin{aligned}m &= 4\;{\rm{u}} \times \frac{{1.66 \times {{10}^{ - 27}}\;{\rm{kg}}}}{{1\;{\rm{u}}}}\\m &= 6.64 \times {10^{ - 27}}\;{\rm{kg}}\end{aligned}\)

From equation (ii), the temperature of helium atoms can be calculated in the following manner:

\(\begin{aligned}T &= \frac{{\left( {6.64\; \times {{10}^{ - 27}}\;{\rm{kg}}} \right){{\left( {1.12 \times {{10}^4}\;{\rm{m/s}}} \right)}^2}}}{{3\left( {1.38 \times {{10}^{ - 23}}\;{\rm{J/K}}} \right)}}\\ &= 2.01\; \times {10^4}\;{\rm{K}}\end{aligned}\)

Thus, the RMS speed of helium atoms is equal to \(1.12 \times {10^4}\;{\rm{m/s}}\)at the temperature of\(2.01\; \times {10^4}\;{\rm{K}}\).

05

(c) Explanation of presence of oxygen and absence of helium in the atmosphere

The temperature at which oxygen molecules can escape the Earth’s atmosphere is \(1.61 \times {10^5}\;{\rm{m/s}}\) while the temperature at which helium atoms can escape the Earth’s atmosphere is \(2.01 \times {10^4}\;{\rm{m/s}}\). It can be seen that oxygen molecules require a much higher temperature in order to escape the Earth’s surface as compared to helium atoms. So, it is very difficult for oxygen molecules to leave the Earth’s atmosphere.

However, the temperature of the Earth during its formation was much higher, which is comparable to the temperature at which helium atoms can escape.In that case, the helium atoms being at a much lower temperature than the oxygen molecules might have escaped from the atmosphere.

Therefore, our atmosphere contains oxygen but not helium.

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Most popular questions from this chapter

Question:(II) A certain car has 14.0 L of liquid coolant circulating at a temperature of 93°C through the engine’s cooling system. Assume that, in this normal condition, the coolant completely fills the 3.5-L volume of the aluminum radiator and the 10.5-L internal cavities within the aluminum engine. When a car overheats, the radiator, engine, and coolant expand and a small reservoir connected to the radiator catches any resultant coolant overflow. Estimate how much coolant overflows to the reservoir if the system goes from 93°C to 105°C. Model the radiator and engine as hollow shells of aluminum. The coefficient of volume expansion for coolant is\({\bf{410}} \times {\bf{1}}{{\bf{0}}^{{\bf{ - 6}}}}\;{\bf{/^\circ C}}\).

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Question:(II) It is observed that 55.50 mL of water at 20°C completely fills a container to the brim. When the container and the water are heated to 60°C, 0.35 g of water is lost. (a) What is the coefficient of volume expansion of the container? (b) What is the most likely material of the container? Density of water at 60°C is 0.98324 g/mL.

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