Unique Nature of Pure Water (Section 1)
Physical Properties of Sea Water (Section 2)
Chemical Properties of Sea Water (Section 2)
Ocean Acidification/Carbon Cycle (Section 3)
Ocean Layers (Section 3)
100

Cohesion is the sticking together of particles of the____ substance.

Same

100

This physical property determines how far sunlight can penetrate the ocean.

Transparency

100

Name the two most abundant ions in seawater.

Sodium And chloride

100

The carbon that forms the backbone of all organic

molecules starts in the ____ as carbon

dioxide and then it dissolves in the ocean at the

surface. 

atmosphere

100

This layer is the only one where photosynthesis occurs.

epipelagic zone?

200

What is the sticking together of particles of the same substance.

Cohesion

200

Pressure increases by this amount for every 10 meters of depth.

An Atmosphere 

200

Ocean water typically has a pH between these values.

8.1-8.3

200

This gas dissolves in seawater and forms carbonic acid.

Carbon dioxide

200

This is the second layer and it is known to be the Twilight Zone. There are no plants in this zone because there is not enough sunlight.


Mesopelagic Zone


300

Water’s polarity makes it excellent at dissolving salts and minerals. What is this property called?

Universal Solvent

300

Which color of light is absorbed first as you go deeper into the ocean?

Red light

300

Name one major source of ions entering seawater.

Rivers, volcanoes or hydrothermal vents

300

When carbonic acid forms, it releases hydrogen ions. What happens to ocean pH?

Decrease

300

Animals such as whales, shrimps, octopuses live in this zone. Sponges or sessile (non-moving) animals could also be found here.


Mesopolegic zone

400

Unlike most substances, water becomes less dense when it freezes. What structural change causes this?

Stable Hydrogen Bonds

400

Sound travels faster in water than air. Name one reason why

The water is denser

400

Marine snow plays a role in nutrient cycling. What is marine snow made of?

Dead organisms, fecal pellets, mucus, and organic particles

400

Explain how increased CO₂ levels affect carbonate ion availabilitY

carbonate ions get used up

400

Some species live in this zone, such as rat-tail fish, liparid fish, amphipods, and decapods. Most animals are unable to see because it’s pitch black.


Hadalpelagic Zone


500

Explain why coastal climates stay more stable than inland climates.

High Heat capacity

500

Explain why the thermocline forms in the ocean.

temperature decreases rapidly with depth

500

Explain why salinity varies between different parts of the ocean.

evaporation, precipitation, river input, freezing/melting of ice, and circulation patterns.

500

Describe the full chemical reaction sequence when CO₂ dissolves in seawater.

carbonic acid (H₂CO₃) → bicarbonate (HCO₃⁻) → hydrogen ions (H⁺) → reduced carbonate (CO₃²⁻).

500

This layer is also known as the Lower Midnight Zone. Conditions in this zone are extremely dark and the temperatures are very cold.


Abyssopelagic Zone


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