What would be the final temperature of 1 m3 of atmosphere

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Reference no: EM13603663

The atmosphere on Maris is comprised of mostly carbon dioxide at a pressure of 600 Pa (that is not a mistake, it is in Pa). The earth's average atmospheric pressure, on the other hand, is about 101. 3 kPa. Starting from the same temperature of 250 K and assuming both air and carbon dioxide behave as ideal gasses with constant specific heats (use the value at the initial state) what would be the final temperature of 1 m³ of atmosphere from each of these planets if 1000 J of energy from the sun was absorbed. (Hint: this is a constant presssure process and thus boundary work could occur as the gas expands).

Reference no: EM13603663

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