To determine the temperature at which the root mean square (rms) speed of oxygen molecules is sufficient for escaping Earth's atmosphere, we need to equate the rms speed to the escape speed of the Earth. Let's break down the solution step-by-step:
Thus, the temperature at which the rms speed of oxygen molecules becomes just sufficient for escaping from Earth's atmosphere is 8.360 \times 10^4 \, K, which matches option $8.360 \times 10^4 K $.