7_Ocean Water Chemistry

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    Ocean Water Chemistry

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    http://www.nhptv.org/

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    Distribution of Earths Water

    Oceans 97.2 %

    Ice Caps and Glaciers 2.15 %

    Atmosphere 0.001 % Rivers and Lakes 0.009 %

    Inland Seas 0.008 %

    Groundwater 0.625 %

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    Ocean Water is SALTY

    Salinity: Total amount of dissolved solids Units: o/oo = 1/1000

    Range: 33 37 o/oo

    Increase in salinity: Increase in Density Decrease in Freezing Point Decrease in Vapor Pressure Increase in Osmotic Pressure

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    Origin of Salts in Oceans

    Rivers(largest transport of chemicals to ocean)

    Rain + CO2 H2CO3 Si, Al, Na, K, Mg

    Volcanoes Cl, S, CO2

    Dust / Rain Fe, Si

    Anthropogenic CO2, P

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    Example Geochemical Cycle

    Concept of Steady State

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    Example 2 Geochemical Cycle

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    Residence Time(T = Ocean amount/Output rate)

    Concentration of elements in seawater isdetermined by their removal rate

    Conservative elements:

    Major Elements: Cl, Na, SO4, Mg, Ca, K- Minor Elements: Br, Sr, B, C, F

    Non Conservative Elements

    Nutrients: N, P, Si Dissolved gases: O2, CO2, N2 Trace Elements: Fe, Al, Mn Organic Compounds

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    Residence Time - Concentration

    Element Res. Time (yrs)

    Na 60 000 000

    Cl 80 000 000Mg 10 000 000

    K 6 000 000

    SO4 9 000 000Ca 1 000 000

    Mn 7 000

    Fe 100

    ConcentrationCrust (%) Ocean (mg/l)

    2.4 10 770

    0.013 19 5002.3 1 290

    2.1 380

    0.026 9054.1 412

    0.5 0.0002

    2.4 0.002

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    Dissolved Gases

    Gas Solubility:Decreases with Temp. and Salinity

    Increases with Pressure

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    Gases in Atmosphere & Oceans

    Percent Gas Phase by Volume

    Gas Atmosphere Surface Ocean Total Ocean

    N2 79% 48% 11%

    O2 21% 36% 6%

    CO2 0.04% 15% 83%

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    Seawater pH

    Pure water pH = 7

    Seawater pH = 7.5 8.1

    Seawater is very well buffered!

    CO2(gas)+H2OH2CO3H++HCO32H

    ++CO32

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    H2O: Universal Polar Solvent

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    H20: Temperature and Density

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    H2O: Frozen & Liquid density

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    H2O: Heat Capacity

    Heat Capacity: heat needed to changethe temperature of a substance

    Water has higher heat capacity than:

    All solids All liquids, except liquid ammonia

    Latent heat of Vaporization: heatneeded to evaporate a liquid Water has the highest of all substances

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    Seawater: Temperature and Density

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    Seawater: Temperature and salinity

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    Seawater: Ice Formation

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    Electromagnetic wave penetration

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    Open water(low productivity)

    Coastal and Estuarine waters

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    Coastal and Estuarine waters(high productivity)

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    Nuclear Missile Submarine

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    http://www.nhptv.org/

    H d m s li ht p n t ti n?

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    How do we measure light penetration?

    Secchi Disc

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    Water Refraction

    Eschrichtius robustus

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    Sound Velocity

    Influenced by Salinity, Temperatureand Pressure Increases with Salinity

    Increases with Temperature Increases with Pressure

    Concept of Midwater Sound Channel

    Study in Detail Fig 5-19!

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    Sound Channel

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    H b k Wh l

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    Humpback WhalesMegaptera novaeangliae

    G Wh l & S P s l

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    Gray Whale & Sonar Proposal

    Eschrichtius robustus

    G Wh l Mi i

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    Gray Whale Migration

    A i P ll i

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    Acoustic Pollution

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