The Physical and
Chemical Properties of Water
The Water Molecule
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H2O
- dipole structure
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Hydrogen
Bonds
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Solvent
power & high heat capacity
Changes of State
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Temperature
and Heat
Ð
Average
kinetic energy versus total kinetic energy
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The
physical states of water
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Liquid,
solid, and gas
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H
bonds = high heat capacity
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Latent
heat of fusion
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Latent
heat of vaporization
Other consequences
of H bonds
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Cohesion
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Surface
Tension
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Viscosity
H2O
Density
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1
g/cm3
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Temperature
and density
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How
does salinity influence density?
Transmission of
Energy
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Heat
- Conduction, convection, radiation
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Light
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Visible
light
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Refracted,
absorbed, scattered
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Attenuation
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How
far does light penetrate into the ocean
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Photic
Zone
The Chemistry of
Seawater
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Acidity
and alkalinity - H+ and OH-
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pH
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pH
of Seawater = 7.8
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Why
is seawater buffered?
Salinity
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Solvent
power
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Disolved
ions
Salinity
amount of
dissolved ions in seawater..
-> normal
salinity = 3.5% or 35ä parts per thousand (ppt)
Tropics =
lowest salinity->high precip.=> 34.5ä
Subtropics=highest
salinity ->high evaporation => 36ä
Why does this
surface pattern exist?
Salinity
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Where does the salt come
from?
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Why is salinity so
stable?
Chemistry of
Seawater
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Major
constituents
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Trace
elements
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Conservative
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Principle
of Constant Proportion
Chemistry of Seawater
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Gasses
Ð
N2,
O2, and CO2
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Why
are concentration of O2 high but CO2 low in the upper 100
m?
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Why
does O2 reach a minimum between 200 and 800 m?
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Temperature,
salinity, and pressure
CO2
and O2
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The
Carbon Cycle
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The
biological pump - deep ocean = carbon sink
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The
Oxygen Balance
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Photosynthesis
<=> Weathering
Nutrients
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N,
P, and Si
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Nonconservative
elements
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Limiting
elements