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Why Oceans Don't Drain Into the Ground

1Introduction: The Ocean Basin as a Container2The Structure of the Seafloor3Permeability and Porosity: The Key Barriers4Hydrostatic Pressure and Equilibrium5The Continental Shelf and Slope6Submarine Groundwater Discharge (SGD)7Tectonic Subduction and Deep Water Cycling8The Global Water Cycle Balance9Common Misconceptions About Gravity and Drains10Conclusion: The Stability of Our Oceans
The Global Water Cycle Balance

Salinity and Density Stability

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Since evaporation leaves the salt behind, the ocean is much denser than the freshwater coming from rivers. This density difference helps keep the layers distinct. It also means that the ocean retains its mass and heat more effectively than freshwater bodies, contributing to its role as the stable core of the global climate system.
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Salt Retention

Because evaporation leaves salt behind, the ocean becomes denser and heavier than freshwater. This density difference helps maintain distinct layers within the ocean and prevents the immediate dilution of seawater by incoming rivers. The high salinity is a key indicator that the ocean is a concentrated reservoir, not a temporary holding area.

Fresh vs. Salt Water

Freshwater (Rivers)

  • Low density
  • Low salinity
  • Flows into ocean

Seawater (Ocean)

  • High density
  • High salinity
  • Retains heat and mass
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