What is the Earth's composition (by compounds not elements)?

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Discussion Overview

The discussion revolves around the composition of the Earth, specifically focusing on the abundances of compounds rather than elements. Participants explore various aspects of Earth's composition, including the mantle, crust, oceans, and atmosphere, while addressing the challenges in defining and quantifying compounds.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested

Main Points Raised

  • One participant notes the difficulty in finding papers that list the abundance of compounds, as most focus on elemental composition.
  • Another participant highlights that the mantle constitutes 2/3 of Earth's mass and provides references to estimates of its chemical composition, mentioning the complexity of the outer and inner cores.
  • It is pointed out that many minerals are solid solutions, complicating the discussion of compounds, with silicates being suggested as the most common "compounds" in the crust and mantle.
  • One participant asserts that dihydrogen monoxide (H2O) is a plentiful compound due to the Earth's oceans, while others contest this claim, emphasizing the relatively small mass of the oceans compared to the mantle.
  • Another participant provides numerical data indicating that SiO2 constitutes a significant portion of the mantle's mass, greatly exceeding that of H2O in the oceans.
  • There is mention of the uncertainty regarding the hydration of the mantle and the presence of hydrated minerals, suggesting a lack of clarity on the mantle's water content.
  • A participant raises the question of whether the Earth's atmosphere should be included in the discussion of compounds, leading to further exploration of the composition of atmospheric gases.
  • Some participants note the presence of Argon in the atmosphere and crust, discussing its relative abundance compared to other elements.

Areas of Agreement / Disagreement

Participants express disagreement on the significance of dihydrogen monoxide in Earth's overall composition, with some asserting it is not as abundant as suggested. There is no consensus on the inclusion of the atmosphere in the discussion of Earth's compounds, and the conversation remains unresolved regarding the exact composition and definitions of compounds.

Contextual Notes

Participants acknowledge the complexity of defining compounds in the context of solid solutions and the varying contributions of different components to Earth's total mass. There is also recognition of the limitations in current understanding of the mantle's hydration and the role of atmospheric gases.

James Nelson
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I have tried looking for papers on the composition of earth, but none of them seem to list the abundance of compounds. They just list the elements. So, what are the abundances of the most common compounds, by mass and/or percent of Earth?
 
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As the mantle has 2/3 of the mass: Googling "earth mantle chemical composition" gives this article which summarizes several estimates of the chemical composition of the mantle on page 3. The outer core is liquid and doesn't have well-defined molecules, and the inner core should be more like a massive alloy where the concept doesn't make sense either. The crust is complicated, but I guess the main components can be found in some publications as well.
 
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As mfb wrote - the main problem is that in many places it is hard to speak about "compounds". Many minerals are what we call a solid solution - mixture of several compounds forming a continuous solid (one that doesn't have to have a uniform composition!). Most rocks in the crust and mantle are composed mainly of silicates and if anything, I would assume silicates are the most common "compounds".
 
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Since the planet is c.a. 3/4 ocean, I think it is safe to say dihyrogen monoxide is one of the more plentiful compounds.
 
Kevin McHugh said:
Since the planet is c.a. 3/4 ocean

Definitely not.

Kevin McHugh said:
I think it is safe to say dihyrogen monoxide is one of the more plentiful compounds.

Definitely not.
 
Seconding Borek's "definitely not". The oceans are a very thin skin on the surface of the Earth.
 
To add numbers: As 0.45 of the mantle is SiO2 and the mantle is 2/3 of the mass of Earth, 30% of the total mass is SiO2 in the mantle (there is also SiO2 in the crust). The whole crust has 0.5% of the mass of Earth, and the mass of the oceans is just 0.025% of the total mass of Earth.

SiO2 beats H2O by a factor of 1000.
 
Forgot "in the oceans" in my comment.

SiO2 in the mantle beats H2O in the oceans by a factor of 1000.
 
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  • #10
Shouldn't the Earth's atmosphere be considered as well? I'm not saying that the percentage of compounds within the atmosphere would surpass that of the mantle and whatnot--I'm just asking whether the atmosphere should be considered as part of "Earth".
 
  • #11
That's what I would do. Not that it will change things by much (perhaps for the noble gases?).
 
  • #12
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  • #13
Borek said:
Definitely not.
Definitely not.

My bad, I was thinking of the surface, not the whole planet.
 
  • #14
mfb said:
Looks like most of Earth's Argon atoms are gone in the atmosphere. A small contribution is in the crust (still about as much as tin and uranium, for example).
That's what I thought.

Edit: I hope that pun was intended.
 

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