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  2. Marine biogenic calcification - Wikipedia

    en.wikipedia.org/wiki/Marine_biogenic_calcification

    The surface ocean engages in air-sea interactions and absorbs carbon dioxide (CO 2) from the atmosphere, making the ocean the Earth's largest sink for atmospheric CO 2. Carbon dioxide dissolves in and reacts with seawater to form carbonic acid. Subsequent reactions then produce carbonate (CO 3 2−), bicarbonate (HCO 3 −), and hydrogen (H ...

  3. Oceanic carbon cycle - Wikipedia

    en.wikipedia.org/wiki/Oceanic_carbon_cycle

    The air-sea CO 2 flux induced by a marine biological community can be determined by the rain ratio - the proportion of carbon from calcium carbonate compared to that from organic carbon in particulate matter sinking to the ocean floor, (PIC/POC). [19] The carbonate pump acts as a negative feedback on CO 2 taken into the ocean by the solubility ...

  4. Protect Your Home From Water Damage With These 5 Flood ... - AOL

    www.aol.com/lifestyle/protect-home-water-damage...

    Sandbags are designed to divert and halt water before it can reach a building. We only recommend using sandbags outside of buildings as they aren’t effective indoors—plus they slowly leak and ...

  5. Can you take sand from these SC beaches? Here’s what to know

    www.aol.com/sand-sc-beaches-know-130000974.html

    To keep the beaches wide for visitors and the dunes healthy, crews move sand from the ocean floor to the beach, a process called renourishment. $100 million in federal money have gone into ...

  6. How seawalls protect houses and hotels at the expense of the ...

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  7. Sandbag - Wikipedia

    en.wikipedia.org/wiki/Sandbag

    Sandbag structures do not prevent water seepage and therefore should be built with the central purpose of diverting flood water around or away from buildings. Properly filled sandbags for flood control are filled one-half to two-thirds full with clean washed sand.

  8. Marine chemistry - Wikipedia

    en.wikipedia.org/wiki/Marine_chemistry

    Warmer ocean water holds less oxygen and is more buoyant than cooler water. This leads to reduced mixing of oxygenated water near the surface with deeper water, which naturally contains less oxygen. Warmer water also raises oxygen demand from living organisms; as a result, less oxygen is available for marine life. [40]

  9. Ocean stratification - Wikipedia

    en.wikipedia.org/wiki/Ocean_stratification

    Even though approximately 70% of the Earth's surface consists of water, more than 75% of the water exchange between the Earth's surface and the atmosphere occurs over the oceans. The ocean absorbs part of the energy from sunlight as heat and is initially absorbed by the surface. [13] Eventually a part of this heat also spreads to deeper water.

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