| 1. | For a 50m mixed layer, we need to cool 50m 3 of water.
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| 2. | However, it becomes zero at the base of the mixed layer.
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| 3. | Mixed layer clay variations exist for most of the above groups.
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| 4. | Velocities, however, may exhibit significant shears within the mixed layer.
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| 5. | Mixed layer clay minerals which are perfect R1 types often get their own names.
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| 6. | Mixed layer dynamics are quite complicated; however, in some regions some simplifications are possible.
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| 7. | The thermostad is the deep mixed layer that has discrete boundaries and uniform temperature.
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| 8. | With enough mixing, some stable equilibrium is reached and a mixed layer is formed.
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| 9. | It is the remnant of the winter surface mixed layer.
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| 10. | Turbulence again increases below the base of the mixed layer due to shear instabilities.
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