<blockquote>
<p>the mantle is in a highly reduced state</p>
</blockquote>
<p>This is not entirely correct. The core is in a highly reduced state, but the mantle is not necessarily reduced, and is quite oxidised in some places. The mantle is heterogeneous.</p>
<blockquote>
<p>however I justify its emission because carbon dioxide is continually being fed into the mantle by the subduction of carbonate sediments, is this correct?</p>
</blockquote>
<p>The carbon dioxide in the mantle does not necessarily derive from subduction of carbonates.</p>
<blockquote>
<p>Or is this all wrong, and the gases are being emitted because they are still being degassed from the solid mantle in the process if heterogenous separation which separated the atmosphere from the mantle. If this is the case, why have all other gases been separated but not the two I have mentioned?</p>
</blockquote>
<p>Not entirely accurate. Although it is true that some of the gases in the atmosphere derived from the differentiation of the core-mantle-crust system, a popular theory suggests that many of the gases came after the differentiation through other planetary bodies such as comets and meteorites. You are also implying that carbon dioxide and sulphur dioxide are the only two gases that are emitted from volcanoes. No. Water vapour is also emitted (commonly much more than the other two) and also other gases. It's just that less people care about the water and it gets less publicity, because, well, it's just water. There are other gases that are emitted as well: nitrogen, the noble gases. But they are much less common than the other two. They are not the <em>only</em> gases.</p>
<p>The authors of <a href="http://www.sciencedirect.com/science/article/pii/S0012821X98000867" rel="nofollow noreferrer">Fluxes and sources of volatiles discharged from Kudryavy, a subduction zone volcano, Kurile Islands</a> write:</p>
<blockquote>
<p>Several potential sources for CO<sub>2</sub> can be identified: (1) hotspot-type mantle, (2) MORB-type mantle, (3) subducted oceanic crust (MORB), (4) marine carbonate, (5) organic C from crustal and subducted sediments</p>
</blockquote>
<p>They also give a table which states that in island arc volcanoes, 12% of carbon is sourced from the mantle, 67% is sourced from carbonates and 21% is organic carbon. Note that this only gives the amount degassed from volcanoes in subduction zone arcs. This does not mean that all carbonate-hosted carbon is released from the rocks to be degassed. I read somewhere that only 50% is degassed, and the rest is lost to the deep mantle. I would also expect that MORB magmas will have significantly less carbonate-sourced carbon.</p>
<p>Also, <a href="http://www.sciencedirect.com/science/article/pii/S0012821X10004140" rel="nofollow noreferrer">The deep carbon cycle and melting in Earth's interior</a>
may be of interest.</p>

CC BY-SA 3.0
2014-08-01T18:46:51.203Z
That's really helpful thank you. But I was wondering if the CO_2 emitted is *not* subducted carbonate derived, than surely the amount of CO_2 entering the atmosphere should be increasing over time, as there would be a net surplus of CO_2 leaving the mantle to the surface, as this surely means that there is less CO_2 being subducted back into the mantle than is being degassed out of it.
AlexLipp
CC BY-SA 3.0
2014-08-01T19:04:31.830Z
I edited my original answer with some more info.
Gimelist
CC BY-SA 4.0
2014-08-01T10:55:15.943Z
2022-11-01T20:46:06.073Z
2022-11-01T20:46:06.073Z
Gimelist
<p>From my understanding, the mantle is in a highly reduced state, so I can't understand why a volcano would give off a highly oxidised gas such as sulphur dioxide.</p>
<p>Carbon dioxide is too an oxidised gas which is emitted by volcanoes, however I justify its emission because carbon dioxide is continually being fed into the mantle by the subduction of carbonate sediments, is this correct? If this is true, why is there still carbon dioxide emitted at mid-ocean ridges?</p>
<p>Or is this all wrong, and the gases are being emitted because they are still being degassed from the solid mantle in the process if heterogenous separation which separated the atmosphere from the mantle. If <strong>this</strong> is the case, why have all other gases been separated but not the two I have mentioned?</p>

CC BY-SA 3.0
2014-07-10T22:11:55.177Z
Check out http://en.wikipedia.org/wiki/Volcanic_gas  ... both water and magma are impure... and the magma has to make its way through the crust... lots of sources of volatile substances
f.thorpe
CC BY-SA 3.0
2014-07-10T23:05:36.660Z
@farrenthorpe However the Laki eruption in Iceland was not under any continental crust at all, and was in Fact under essentially a ocean ridge so it's extensive sulphur dioxide levels must have come directly from the mantle.
AlexLipp
<geochemistry><volcanology>
Why do Volcanoes give out so much Sulphur Dioxide and Carbon Dioxide?
AlexLipp
# Why do Volcanoes give out so much Sulphur Dioxide and Carbon Dioxide?

(Asked by: username_0 on 2014-07-10)

From my understanding, the mantle is in a highly reduced state, so I can't understand why a volcano would give off a highly oxidised gas such as sulphur dioxide.

Carbon dioxide is too an oxidised gas which is emitted by volcanoes, however I justify its emission because carbon dioxide is continually being fed into the mantle by the subduction of carbonate sediments, is this correct? If this is true, why is there still carbon dioxide emitted at mid-ocean ridges?

Or is this all wrong, and the gases are being emitted because they are still being degassed from the solid mantle in the process if heterogenous separation which separated the atmosphere from the mantle. If **this** is the case, why have all other gases been separated but not the two I have mentioned?

**Tags:** geochemistry, volcanology

> **Comments:**
> **username_1**: Check out http://en.wikipedia.org/wiki/Volcanic_gas  ... both water and magma are impure... and the magma has to make its way through the crust... lots of sources of volatile substances  
> **username_0**: @farrenthorpe However the Laki eruption in Iceland was not under any continental crust at all, and was in Fact under essentially a ocean ridge so it's extensive sulphur dioxide levels must have come directly from the mantle.  

---

## 1 answers

### Answer by username_2 on 2014-08-01. Score: 13 | Accepted answer

> the mantle is in a highly reduced state

This is not entirely correct. The core is in a highly reduced state, but the mantle is not necessarily reduced, and is quite oxidised in some places. The mantle is heterogeneous.

> however I justify its emission because carbon dioxide is continually being fed into the mantle by the subduction of carbonate sediments, is this correct?

The carbon dioxide in the mantle does not necessarily derive from subduction of carbonates.

> Or is this all wrong, and the gases are being emitted because they are still being degassed from the solid mantle in the process if heterogenous separation which separated the atmosphere from the mantle. If this is the case, why have all other gases been separated but not the two I have mentioned?

Not entirely accurate. Although it is true that some of the gases in the atmosphere derived from the differentiation of the core-mantle-crust system, a popular theory suggests that many of the gases came after the differentiation through other planetary bodies such as comets and meteorites. You are also implying that carbon dioxide and sulphur dioxide are the only two gases that are emitted from volcanoes. No. Water vapour is also emitted (commonly much more than the other two) and also other gases. It's just that less people care about the water and it gets less publicity, because, well, it's just water. There are other gases that are emitted as well: nitrogen, the noble gases. But they are much less common than the other two. They are not the *only* gases.

The authors of [Fluxes and sources of volatiles discharged from Kudryavy, a subduction zone volcano, Kurile Islands](http://www.sciencedirect.com/science/article/pii/S0012821X98000867) write:

> Several potential sources for CO2 can be identified: (1) hotspot-type mantle, (2) MORB-type mantle, (3) subducted oceanic crust (MORB), (4) marine carbonate, (5) organic C from crustal and subducted sediments

They also give a table which states that in island arc volcanoes, 12% of carbon is sourced from the mantle, 67% is sourced from carbonates and 21% is organic carbon. Note that this only gives the amount degassed from volcanoes in subduction zone arcs. This does not mean that all carbonate-hosted carbon is released from the rocks to be degassed. I read somewhere that only 50% is degassed, and the rest is lost to the deep mantle. I would also expect that MORB magmas will have significantly less carbonate-sourced carbon.

Also, [The deep carbon cycle and melting in Earth's interior](http://www.sciencedirect.com/science/article/pii/S0012821X10004140)
may be of interest.

> **Comments:**
> **username_0**: That's really helpful thank you. But I was wondering if the CO_2 emitted is *not* subducted carbonate derived, than surely the amount of CO_2 entering the atmosphere should be increasing over time, as there would be a net surplus of CO_2 leaving the mantle to the surface, as this surely means that there is less CO_2 being subducted back into the mantle than is being degassed out of it.  
> **username_2**: I edited my original answer with some more info.  

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