The Physical and Chemical Properties of Water

 

The Water Molecule

¥     H2O - dipole structure

¥     Hydrogen Bonds

 

¥     Solvent power & high heat capacity

Changes of State

¥     Temperature and Heat

Р   Average kinetic energy versus total kinetic energy

 

¥     The physical states of water

Р   Liquid, solid, and gas

Р   H bonds = high heat capacity

Р   Latent heat of fusion

Р   Latent heat of vaporization

Other consequences of H bonds

¥     Cohesion

¥     Surface Tension

¥     Viscosity

H2O Density

¥     1 g/cm3

 

¥     Temperature and density

 

¥     How does salinity influence density?

Transmission of Energy

¥     Heat - Conduction, convection, radiation

¥     Light

¥     Visible light

¥     Refracted, absorbed, scattered

¥     Attenuation

¥     How far does light penetrate into the ocean

¥     Photic Zone

The Chemistry of Seawater

¥            Acidity and alkalinity - H+ and OH-

¥     pH

¥     pH of Seawater = 7.8

 

¥            Why is seawater buffered?

Salinity

¥     Solvent power

 

¥     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

¥     Where does the salt come from?

 

¥     Why is salinity so stable?

 

Chemistry of Seawater

¥     Major constituents

¥     Trace elements

¥     Conservative

¥     Principle of Constant Proportion

Chemistry of Seawater

¥     Gasses

Р       N2, O2, and CO2

 

¥     Why are concentration of O2 high but CO2 low in the upper 100 m?

 

¥     Why does O2 reach a minimum between 200 and 800 m?

 

¥     Temperature, salinity, and pressure

 

 

CO2 and O2

¥     The Carbon Cycle

¥     The biological pump - deep ocean = carbon sink

 

¥     The Oxygen Balance

Р   Photosynthesis <=> Weathering

Nutrients

¥     N, P, and Si

¥     Nonconservative elements

¥     Limiting elements