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Chapter 3. Chemical & Physical Feature of the Ocean. Atom. The smallest particle an element can be divided into & maintain properties Building block of matter. Molecule. A group of atoms chemically combined that can exist by itself CO 2. Ion. Charged particle Cl -1. Polyatomic Ion.
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Chapter 3 Chemical & Physical Feature of the Ocean
Atom • The smallest particle an element can be divided into & maintain properties • Building block of matter
Molecule • A group of atoms chemically combined that can exist by itself • CO2
Ion • Charged particle • Cl-1
Polyatomic Ion • A group of atoms chemically combined that together have a charge • CO3-2
Bond • A strong attraction between atoms that hold compounds together • Ionic, covalent & metallic
Hydrogen Bond • The weak attraction between hydrogen & a highly electronegative(EN) element when the hydrogen is bound to another EN element
Hydrogen Bonds • H-bonds hold one molecule to another
Water • A small molecule made up of two hydrogen atoms covalently bound to one oxygen • H2O
Properties of Water • Exist in all 3 phases on Earth • Very high MP & BP for size • Very high heat capacity • Very high Heat of Fusion
Very high Heat of Vaporization • Holds heat well • Very good solvent • Transparent • Solid phase (ice) less dense than the liquid phase
Salinity • The amount of salts dissolved in sea water
Salts • Ionic compounds or the ions that dissolve in water • NaCl • K2SO4
Solvation • The process of a substance dissolving • Also called dissociation
Average Salinity • 3.5 % or 3.5 parts per 100 • 35 %o or 35 ppt • Cl-1 = 19 %o • Na+1 = 11 %o
Other Water Properties • As salinity increases, density increases • As temperature increases, density decreases • Pressure increases with depth
Thermocline • The location in the water column where the temperature of water declines rapidly
Coriolis Effect • Due to the rotation of the Earth, fluids tend to veer to form cyclic patterns
Northern Hemisphere: Water veers right to make clockwise cycles • Southern Hemisphere: Water veers left to make counter-clockwise cycles
Convection Currents • Fluids form cyclic flowing patterns due to heat differences • Warm air rises & displaces cooler air which drops
Coriolis Effect if a cannon were fired northward from a point on the Equator, the projectile would land to the east of its due north path because the projectile was moving eastward faster at the Equator than was its target farther north.
All of the Earth’s weather patterns are caused by convection currents the Coriolis Effect and rotational forces.
Trade Winds • Winds that tend to blow in the same direction all the time • Easterlies: wind from east
Gyres • Ocean-wide cyclic surface circulation patterns caused by wind friction & Coriolis Effect
Oceanic Gyres • Huge clockwise cycles in the northern hemisphere • Huge counter-clockwise cycles in the south
Waves • A form of energy transfer • Crest: highest point • Trough: lowest point
Wavelength • The distance between corresponding points • Crest to crest
Period • The time it takes for one wave to pass
Surface Wave • The recognizable wave we see in the ocean • Caused by wind
Wave Height • Determined by wind speed, fetch, and wave reinforcement
Fetch • The distance in which winds flow over the water in the same direction
Wave Reinforcement • When the crests of two or more waves flow simultaneously the height of the wave would be the addition of the two
Seismic Waves • Waves caused by geological activity (earthquakes) • Tsunamis • Tidal waves
Tides • Rhythmic pattern of the rising & falling of the water level in the ocean
Cause of Tides • Gravitational pull of the moon on the Earth • Gravitational pull of the sun on the Earth • Spinning of the Earth