The concentration of CO 2 gas in atmosphere is given to be 390 ppm . The mole fraction of the CO 2 in the atmosphere is to be calculated. Concept introduction: The mole fraction is calculated by the number of moles of a component in a solution divided by the total number of moles of a solution. It is used to calculate the quantity of the substance in a solution. This concept is based on the Avogadro’s Law . Avogadro’s law states that equal volume of gases contains equal number of molecules at the condition of the same temperature and pressure. To determine: The mole fraction of the CO 2 in the atmosphere.
The concentration of CO 2 gas in atmosphere is given to be 390 ppm . The mole fraction of the CO 2 in the atmosphere is to be calculated. Concept introduction: The mole fraction is calculated by the number of moles of a component in a solution divided by the total number of moles of a solution. It is used to calculate the quantity of the substance in a solution. This concept is based on the Avogadro’s Law . Avogadro’s law states that equal volume of gases contains equal number of molecules at the condition of the same temperature and pressure. To determine: The mole fraction of the CO 2 in the atmosphere.
Definition Definition Number of atoms/molecules present in one mole of any substance. Avogadro's number is a constant. Its value is 6.02214076 × 10 23 per mole.
Chapter 10, Problem 65E
Interpretation Introduction
Interpretation:
The concentration of CO2 gas in atmosphere is given to be 390ppm . The mole fraction of the CO2 in the atmosphere is to be calculated.
Concept introduction: The mole fraction is calculated by the number of moles of a component in a solution divided by the total number of moles of a solution. It is used to calculate the quantity of the substance in a solution. This concept is based on the Avogadro’s Law. Avogadro’s law states that equal volume of gases contains equal number of molecules at the condition of the same temperature and pressure.
To determine: The mole fraction of the CO2 in the atmosphere.
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