Major: 96.5% Carbon Dioxide (CO2), 3.5% Nitrogen (N2)
Minor (ppm): Sulfur Dioxide (SO2) - 150; Argon (Ar) - 70; Water (H2O) - 20;
Carbon Monoxide (CO) - 17; Helium (He) - 12; Neon (Ne) - 7
That's interesting because if you take away the products of volcanism (a major source of sulfur dioxide and carbon dioxide here on Earth), you're left with... Nitrogen... Argon... Water... and noble gasses. Look familiar?The best thinking right now is that Earth outgassed and held on to a similar volume of gasses as Venus. But since we had a substantial volume of liquid water on the surface, the oceans naturally absorbed CO2 and then deposited it on the sea bottom as carbonate minerals. (Life eventually learned that trick too, leading to things like shells)
So limestone, dolostone, chalks, calcite, marble, etc.... all those carbonates are likely the product of our liquid water oceans drawing out the vast bulk of the C02 in our atmosphere, leaving relict gasses in its place. Same starting point but we ended up with vastly lower pressure and vastly different final composition.
Venus had no such luck. She suffocates forever.
http://nssdc.gsfc.nasa.gov/planetary/factsheet/venusfact.htm...
In short, scientists think there has to be a convecting, rotating, liquid metal core in order to create a substantial magnetosphere. Venus's planetary core is almost certainly missing one, two, or three of those things.
The fact that Venus is extremely hot on the surface (460ºC) is at least partially assisting with creating a "stagnant lid" tectonic regime where no heat-venting plate action is seen. So if the surface of the planet is nearly as hot as the mantle and the mantle is nearly as hot as the core, convection doesn't happen. Wiki "geothermal gradient" for more.
Thus no magnetosphere, thus no electromagnetic deflection of the sun's blast. Not a dealkiller, but certainly not preferable if you'd like to move in someday.
http://spacemonitor.blogspot.com/2007/05/floating-city-on-ve...