Lecture 13: Water on Earth Flashcards

(11 cards)

1
Q

How much water is present in the hydrosphere?

A

Hydrosphere = 1.4 x 10^9 km3

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2
Q

Where is the water on earth stored?

A

Water in air and soil moisture - 0.001%

Surface water (lake, rivers) - 0.022 %

Groundwater - 0.400 %

Icecaps and glaciers - 2.380 %

TOTAL FRESHWATER - 2.8%

What’s the rest, then? - 97.2% Ocean

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3
Q

Describe waters covalent bonding:

A

Hydrogen bonds are about 10% as strong as covalent ones

Results: surface tension, capillarity, adhesion, and blue colour

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4
Q

what is cohesion?

A

Cohesion is the tendency for like particles to stick together

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5
Q

What is adhesion?

A

Adhesion is the tendency for unlike particles to stick together

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6
Q

Describe water tension:

A

the attraction of water molecules to each other (cohesion) …

is greater than their attraction to molecules in the air (adhesion)

Water has a higher surface tension than most liquids

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7
Q

What makes up sea water?

A

Seawater is about 96.5% H2O

Seawater is a soup of chemicals

Cations, anions and compounds

Concentration is determined by: sources, cycles, transport, residence time, chemical reactions

Difference between dissolved and suspended material

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8
Q

Where do these compounds found in seawater come from?

A

From rocks: water is a powerful solvent

DOWN: Weathering of land rocks, transport by water, meteorites, rain, wind-blown

UP: Mid-ocean ridge brines and other hydrothermal vents, underwater lava

So why is the ocean not getting saltier and saltier?

Compounds are removed by: biological activity, settling, precipitation

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9
Q

Do salinity’s differ due to different salts?

A

No matter where you collect seawater, and no matter what its overall salinity is, the proportions of major salts are about the same

They are called “conservative elements”
Cl- Na+ SO42-
Mg2+ Ca2+ K+

Mixing is faster than changing inputs/outputs

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10
Q

Overall describe fresh water in terms of freezing point, cooling and evaporation, Density, material and ph.

A

Freshwater

Freezing point = 0°C

Cooling freshwater increases in density to 4°C, then decreases, then freezes

Freshwater evaporates quickly

Density is determined by T
and P

A predictable and
homogeneous material

pH = about 7

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11
Q

Overall describe sea water in terms of freezing point, cooling and evaporation, Density, material and ph.

A

Seawater

Freezing point typically about -1.9 °C

Cooling seawater increases in density till it freezes

Seawater evaporates more slowly than freshwater

Density is determined by T, S and P

A very mixed soup of chemicals

pH = about 8.1

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