by burzum » Sun Jul 24, 2005 8:28 am
William Hartmann wrote an excellent book,
The Traveler's Guide to Mars, that goes over many theories on how Mars aquired and lost its water. This book was written prior to the Mars Exploration Rover mission, but its conclusions are still relevant. Hartmann and other planetary scientists deduced correctly from various satellite photos that Mars was once a water covered planet, and that water was responsible for many surface features, some more recent than you might expect.
A quick summary is that Mars, like the Earth aquired water either from volcanism, comets, or both. Mars lost its water due to the fact that its planetary magnetic field failed about a billion years after the planet formed. Unlike Earth which is protected from the solar wind by our planetary magnetic field, the solar wind was able to slowly strip away the atmosphere on Mars. As more of the atmosphere was stripped away, the atmospheric pressure dropped. This caused two things to occur: the greenhouse effect on Mars ceased to function causing the planet to cool down, and water either evaporated or sublimed into the atmophere where it was eventually stripped away. This is what has created the dead planet we see today.
The reason for the failure of the planetary magnetic field is uncertain, but it probably relates to the surface to volume ratio of Mars. Having a greater surface to volume ratio, Mars cooled down from its initially hot primordial matter. This eventually caused part or all of an iron core to solidify which stopped the magneto effect creating the planetary magnetic field. The reason this hasn't happened on Earth is that we have a balance between the lesser cooling due to the surface to volume ratio of our planet and the very small heat generation rate due to very small quanties of natural radioactive isotopes decaying thoughout the volume of our planet. In addition, the crust and the atmophere provide a very good layer of insulation.
Hope this helps. I hope you check out Hartmann's book if only for the beautiful pictures.
William Hartmann wrote an excellent book, [url=http://www.amazon.com/exec/obidos/tg/detail/-/0761126066/qid=1122192447/sr=8-1/ref=sr_8_xs_ap_i1_xgl14/104-8231865-6323164?v=glance&s=books&n=507846]The Traveler's Guide to Mars[/url], that goes over many theories on how Mars aquired and lost its water. This book was written prior to the Mars Exploration Rover mission, but its conclusions are still relevant. Hartmann and other planetary scientists deduced correctly from various satellite photos that Mars was once a water covered planet, and that water was responsible for many surface features, some more recent than you might expect.
A quick summary is that Mars, like the Earth aquired water either from volcanism, comets, or both. Mars lost its water due to the fact that its planetary magnetic field failed about a billion years after the planet formed. Unlike Earth which is protected from the solar wind by our planetary magnetic field, the solar wind was able to slowly strip away the atmosphere on Mars. As more of the atmosphere was stripped away, the atmospheric pressure dropped. This caused two things to occur: the greenhouse effect on Mars ceased to function causing the planet to cool down, and water either evaporated or sublimed into the atmophere where it was eventually stripped away. This is what has created the dead planet we see today.
The reason for the failure of the planetary magnetic field is uncertain, but it probably relates to the surface to volume ratio of Mars. Having a greater surface to volume ratio, Mars cooled down from its initially hot primordial matter. This eventually caused part or all of an iron core to solidify which stopped the magneto effect creating the planetary magnetic field. The reason this hasn't happened on Earth is that we have a balance between the lesser cooling due to the surface to volume ratio of our planet and the very small heat generation rate due to very small quanties of natural radioactive isotopes decaying thoughout the volume of our planet. In addition, the crust and the atmophere provide a very good layer of insulation.
Hope this helps. I hope you check out Hartmann's book if only for the beautiful pictures.