Is water at the bottom of the ocean oxygen deficient?

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Discussion Overview

The discussion revolves around the oxygen levels in water at the bottom of the ocean compared to higher levels, exploring factors that may influence these levels such as density, temperature, and the presence of atmospheric contact. The conversation touches on theoretical and conceptual aspects of oceanography.

Discussion Character

  • Exploratory
  • Technical explanation
  • Conceptual clarification
  • Debate/contested

Main Points Raised

  • Some participants propose that water at the bottom of the ocean is oxygen deficient compared to higher levels due to factors like lack of atmospheric contact and relative scarcity of plants.
  • Others suggest that the density of water at lower levels, particularly at around 4 degrees Celsius, may inhibit the absorption of oxygen through diffusion or convection, although this is not universally accepted.
  • One participant notes that while the density of water does change with depth, the change is relatively minor, suggesting that diffusion may be a significant factor in low oxygen concentration at depth.
  • There is mention of meromictic water, which does not mix with surface water and can be anoxic, promoting anaerobic bacteria growth, indicating that similar conditions may exist in oceanic environments.
  • Participants reference resources and studies related to oxygen levels in ocean water, including discussions on dead zones and the overall oxygen profile of the ocean.

Areas of Agreement / Disagreement

Participants express varying views on the factors affecting oxygen levels at the bottom of the ocean, with no consensus reached on the primary causes or the extent of oxygen deficiency.

Contextual Notes

Some claims rely on assumptions about water density and its effects on gas absorption, which may not be fully resolved. The discussion also touches on specific oceanographic terms and phenomena that may require further clarification.

Who May Find This Useful

Individuals interested in oceanography, environmental science, and the dynamics of aquatic ecosystems may find this discussion relevant.

MulderFBI
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Is water at the bottom of the ocean oxygen deficient? Compared to water at the higher levels.
 
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MulderFBI said:
Is water at the bottom of the ocean oxygen deficient? Compared to water at the higher levels.
I am not entirely sure, but I think I've read somewhere that it is. Intuitively speaking, it does sound plausible. The only factor that may increase the oxygen concentration at lower level of ocean is water pressure. I think every other factors (such as lack of atmospheric contact, water temperature although it won't go below 4 deg, relative lack of plants, etc.) decreases the oxygen concentration at lower ocean level.
 
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Thank you, I wanted to verify that claim. One of the explanations I've found is that it's because water at the bottom is very dense (especially at the 4 deg layer). That density stops it from absorbing oxygen (and other gases) through for example diffusion or convection but I'm not sure it's true.
 
MulderFBI said:
Thank you, I wanted to verify that claim. One of the explanations I've found is that it's because water at the bottom is very dense (especially at the 4 deg layer). That density stops it from absorbing oxygen (and other gases) through for example diffusion or convection but I'm not sure it's true.
I am not an expert, but I wouldn't be surprised if that was true.

EDIT: The density of water don't change that much, even comparing between sea level and bottom of the ocean. And at 4 deg layer, it remains pretty much the same. Nonetheless, diffusion indeed may be one of the biggest reason for the low oxygen concentration at low ocean depth.
 
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Why is that? I'm pretty sure water at 4deg is at the most dense point so I would say it is denser than on higher levels when temperature rises.
 
MulderFBI said:
Why is that? I'm pretty sure water at 4deg is at the most dense point so I would say it is denser than on higher levels when temperature rises.
Well, I said "don't change that much", which means it still does change a little. It probably changes around 0.01 g/cm3 comparing sea level and the bottom of the ocean, if not, less. Density of sea water is around 1.025 - 1.027 at sea level. So a 1% difference (or less) is a minor difference to me.
 
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You are right the difference is not that big:
density_depth.jpg

"This is a simple density-depth ocean water profile. You can see density increases with increasing depth. The pycnocline are layers of water where the water density changes rapidly with depth. This density-depth profile is typical of what you might expect to find at a latitude of 30-40 degrees south.
Windows to the Universe original image"
 

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Meromictic water, water that never intermixes with surface water is anoxic, promoting the growth of anaerobic bacteria - the kind of bacteria that were common on Earth prior to an oxygen atmosphere. This can happen in deep lakes, and is often found at the bottom of fjords. Hadalpelagic is the term more often used for ocean basin closed canyons
Discussion on lakes: https://en.wikipedia.org/wiki/Meromictic_lake

There is a whole lot more to this topic- dead zones and so on. This talks about O2 in the entire water column of the ocean.
http://www.fondriest.com/environmental-measurements/parameters/water-quality/dissolved-oxygen/

Is a great resource it has interesting discussions and graphics.
 
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Thank you for great resources!
 

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