Physical Chemistry Barometric Derivation

M/aRT * Integral(dz)In summary, to derive an expression for the barometric equation with temperature dependency, we need to integrate with respect to temperature and substitute dT in the integral. The final expression is p=poe-gMz/aRT ln(p/po) = -gM/aRT * Integral(dz).
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Physical Chemistry Barometric Derivation!

Homework Statement


Derive an expression for the barometric equation that takes the temperature dependency (To=T-az) into account. Where To=ground level temperature, T=temperature at an altitude, a=proportion constant, z=altitdue


Homework Equations


p=poe-gMz/RT


The Attempt at a Solution


I know how to derive the barometric equation formula to get to ln(p/po) which i know has to be part of the final expression. however, I having trouble with the integral on the other side. should i integrate for dz or dT?
 
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And how to i account for the temperature dependency?p=poe-gMz/RTln(p/po) = -gM/RT * Integral(dz or dT)Since we are accounting for temperature, we need to integrate with respect to temperature. The equation for To=T-az implies that dT=dz/a. Therefore, we can substitute dT in the integral to get:ln(p/po) = -gM/RT * Integral(dT)= -gM/RT * Integral(dz/a)= -gM/aRT * Integral(dz)So the final expression for the barometric equation with temperature dependency is: p=poe-gMz/aRT
 
  • #3


I would suggest approaching this problem by first considering the ideal gas law, which relates pressure, volume, and temperature. We can use this law to derive the barometric equation, which describes how pressure changes with altitude in a column of air.

Starting with the ideal gas law, we can rearrange it to isolate pressure (p):

pV = nRT

p = nRT/V

Next, we can consider a column of air of height z, with a cross-sectional area of A. The volume of this column of air can be represented as V = Az, where A is the cross-sectional area and z is the height. We can also assume that the number of moles of air (n) remains constant.

Substituting these values into the ideal gas law, we get:

p = nRT/Az

Next, we can use the fact that density (ρ) is equal to mass (m) divided by volume (V). In this case, the mass of the column of air remains constant, so we can say:

ρ = m/V = constant

Therefore, we can rewrite the ideal gas law as:

p = ρRT/Az

Now, we need to account for the temperature dependency. We can do this by substituting T = To - az, where To is the ground level temperature and a is a proportionality constant, into the ideal gas law. This gives us:

p = ρR(To - az)/Az

Next, we can use the barometric equation to relate pressure at an altitude (p) to pressure at ground level (po):

p = poe^(-gz/RT)

Substituting this into our previous equation, we get:

poe^(-gz/RT) = ρR(To - az)/Az

Solving for p/po, we get:

p/po = ρR(To - az)/Az * e^(gz/RT)

Finally, taking the natural logarithm of both sides, we get the expression for the barometric equation that takes temperature dependency into account:

ln(p/po) = ln(ρR(To - az)/Az * e^(gz/RT))

Therefore, to answer your question about the integral, you would need to integrate for dz because it is the variable that is changing with altitude. I hope this helps in your derivation.
 

1. What is the purpose of barometric derivation in physical chemistry?

Barometric derivation is a mathematical technique used to determine the vapor pressure of a substance at different temperatures. This is important in physical chemistry because it helps us understand the behavior of gases and the factors that influence their vapor pressure.

2. How is barometric derivation performed?

Barometric derivation involves measuring the change in vapor pressure of a substance at different temperatures and using this data to calculate the vapor pressure at any given temperature. This is typically done by placing the substance in a closed container and measuring the pressure of the gas above the liquid at different temperatures.

3. What is the relationship between temperature and vapor pressure in barometric derivation?

According to the ideal gas law, there is an inverse relationship between temperature and vapor pressure. As temperature increases, the vapor pressure of a substance also increases. Barometric derivation allows us to quantify this relationship and determine the vapor pressure at any given temperature.

4. How does barometric derivation differ from other methods of determining vapor pressure?

Barometric derivation is a direct method of determining vapor pressure, as it involves measuring the pressure of the gas directly above the liquid. Other methods, such as the Clausius-Clapeyron equation, use indirect measurements and mathematical equations to determine vapor pressure.

5. What are the applications of barometric derivation in physical chemistry?

Barometric derivation is used in a variety of applications, including the study of atmospheric chemistry, the design of chemical processes, and the development of new materials. It is also an important tool for understanding the behavior of gases and how they interact with other substances.

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