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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
Permeability and Porosity: The Key Barriers

Porosity vs. Permeability

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Let's start with a crucial distinction. Porosity is about storage—it's the empty space inside a material. Permeability is about connection—it's whether those spaces link up to let fluid move. Imagine a sponge versus a solid rock. The sponge soaks up water and lets it pass through. The rock might have tiny holes, but if they're sealed off, water can't get through. For the ocean to drain, the seafloor needs to be permeable, not just porous.
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Defines porosity as storage capacity and permeability as flow connectivity, using the sponge analogy to distinguish between holding water and letting it pass through.

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