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9) One fun thing to think about is that the SVP of water is
a strong function of temperature. As a relevant example,
70% RH at 70 F corresponds to a dewpoint of 59.76 F as you
can verify at
http://einstein.atmos.colostate.edu/~mcnoldy/Humidity.html
Therefore it seems to me you could have essentially infinite
buffer capacity if you are in equilibrium with a puddle of
water at 59.76 F.