Did Silicates Form on Early Earth Without Basic Aqueous Solutions?

  • Thread starter Ferrus
  • Start date
  • Tags
    Earth
In summary, during the period when a gas of silica coalesced into a ball of molten silicon, silicates were formed due to the reaction of metal oxides and acidic anhydride, resulting in a slow but continuous process due to the abundance of geological time. Additionally, the reaction was sped up once the mixture became hot. The detailed mechanism of this reaction is still unknown, but it is believed that the thermodynamic stability of silicates and the ionic nature of metal oxides play a role. More information can be found in Navrotsky's book, "The Physics and Chemistry of Earth Materials."
  • #1
Ferrus
13
0
How did the silicates form during the period in which a gas of silica coalesced into a ball of molten silicon? I thought silicate typically only forms in basic aqueous solutions, which clearly did not exist at this period.
 
Chemistry news on Phys.org
  • #2
One of the ways of synthesizing salts is - metal oxide plus acidic anhydride -> salt. In the presence of metal oxides silica will react creating silicates - slowly, but there was plenty of geological time. Plus, once the mixture got hot, reaction speed up.
 
  • #3
Excellent thank you.

What is mechanism of their reaction? I have seen the mechanisms for oxides on water with both acidic and basic characters, electrostatics, etc... how without the polar molecules of water are they able to mediate a reaction? Is it just a matter of gibbs free energy reduction, along with a large activation energy (hence slow speed under normal conditions) reflecting the very awkward transition molecules?
 
  • #4
No idea about the detailed mechanism, for sure silicates are thermodynamically much more stable than silica/metal oxides mixture. Oxides - especially of first two groups metals - are mostly ionic, which probably plays a role.
 
  • #5
There is quite a lot of useful information in Navrotsky p300ff (The Physics and Chemistry of Earth Materials - Cambridge) in the chapter on high temperatures and high pressures and plenty of references at the end of that chapter.

Go well
 

FAQ: Did Silicates Form on Early Earth Without Basic Aqueous Solutions?

What are silicates and why are they important for early Earth?

Silicates are a type of mineral made up of silicon and oxygen atoms. They are important for early Earth because they make up a large portion of the Earth's crust, providing structural support for the planet and playing a crucial role in the formation of the continents.

How were silicates formed on early Earth?

Silicates were formed through a process called magma differentiation, where molten rock (magma) cools and solidifies, allowing crystals to form. As the magma cooled, silicate minerals such as quartz, feldspar, and mica were formed and eventually became part of the Earth's crust.

Did silicates play a role in the formation of the atmosphere on early Earth?

Yes, silicates played a significant role in the formation of the atmosphere on early Earth. As the Earth's crust formed, volcanoes released gases from the molten magma, including water vapor, carbon dioxide, and nitrogen. These gases eventually formed the Earth's early atmosphere.

How did silicates contribute to the development of life on early Earth?

Silicates provided the building blocks for life on early Earth. As the Earth's crust solidified, it created a stable environment for the development of microbial life. The minerals in silicates also provide essential nutrients for plants and animals, making them crucial for the evolution of complex life forms.

Are silicates still important for Earth today?

Yes, silicates continue to play a vital role in the Earth's geological processes and the development of life. They make up a large part of the Earth's crust and are essential for maintaining a stable atmosphere, supporting plant growth, and regulating the planet's temperature. Silicates also have many practical uses, such as in construction materials and as a source of valuable minerals.

Back
Top