Skip to main content
. 2001 Jan 30;98(3):827–830. doi: 10.1073/pnas.98.3.827

Figure 1.

Figure 1

The log of the globally averaged depth of water stored in the Martian crust today (H1) and at early times Ho for two values of ρ, the ratio of D/H in today's atmospheric water vapor to the primordial ratio (2.6 and 5.2). These results are for a simple unconstrained escape of hydrogen with a constant ratio of escape flux to H, the depth of the hydrogen supply.