An ideal diatomic gas has an initial pressure of 1.00×10°Pa , an initial volume of 2.00m° , and an initial temperature of 300K. (This is point 1 on the pV-diagram.) The gas has an isochoric increase in pressure to 2.00×10° Pa. (This is point 2 on the pV-diagram.) The gas then has an isothermal expansion to a volume of 3.00m' . (This is point 3 on the pV-diagram.) The pressure is then reduced adiabatically back down to its original pressure of 1.00×10°P.. (This is point 4 on the pV-diagram.) Finally, the gas has an isobaric decrease in volume to its original volume of 2.00m. (The gas is back to point 1 on the pV-diagram.) Fill in the missing values on the following table. а. Point Volume Pressure. Temnerature
An ideal diatomic gas has an initial pressure of 1.00×10°Pa , an initial volume of 2.00m° , and an initial temperature of 300K. (This is point 1 on the pV-diagram.) The gas has an isochoric increase in pressure to 2.00×10° Pa. (This is point 2 on the pV-diagram.) The gas then has an isothermal expansion to a volume of 3.00m' . (This is point 3 on the pV-diagram.) The pressure is then reduced adiabatically back down to its original pressure of 1.00×10°P.. (This is point 4 on the pV-diagram.) Finally, the gas has an isobaric decrease in volume to its original volume of 2.00m. (The gas is back to point 1 on the pV-diagram.) Fill in the missing values on the following table. а. Point Volume Pressure. Temnerature
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