Water Flashcards

1
Q

How long did life evolve in water before spreading to land

A

3 billion years

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2
Q

What does hydrogen bonding organise water into

A

a higher level of structural order

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3
Q

water is “held together” by hydrogen bonds

A

Cohesion

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4
Q

What does cohesion allow water to do

A

travel up plants against gravity

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5
Q

How does water travel up plants

A

. Water evaporation from the leaf surface results in a tugging effect, like a chain, due to hydrogen bonding between water molecules

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6
Q

Hydrogen bonding to cell molecules

A

Adhesion

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7
Q

How does hydrogen bonding allow creatures to “walk on water”

A

Surface tension due to hydrogen bonding
between water molecules at the interface
between air and water

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8
Q

How does water moderate air temperature

A

absorbing heat from warm air and releasing stored heat to cooler air

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9
Q

Kinetic energy associated with the movement of atoms and molecules

A

Thermal energy

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10
Q

Calorie

A

Thermal energy transfer from one body to another is called HEAT measured as a CALORIE – the amount of heat it takes to raise the temperature of 1 g of water by 1°C

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11
Q

Thermal energy flow

A

region of higher temperature to region of lower temperature

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12
Q

High specific heat

A

can absorb higher levels off heat relative to most other substances

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13
Q

What does water having a high specific heat mean

A

it will change its temperature LESS than other liquids when it absorbs or loses a given amount of heat

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14
Q

Why is waters high specific heat important to life

A

The water that covers most of the Earth keeps temperature fluctuations on land and in water within limits that permit life,
Living organisms are made primarily of water so they are better able to resist changes in their own temperature

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15
Q

Why does water have a high specific heat

A

hydrogen bonding, extra heat has to be absorbed to break hydrogen bonds or heat is
released when hydrogen bonds form

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16
Q

Heat of vaporisation

A

is the amount of heat a liquid must absorb for 1 g to be converted into a gas (water is high due to hydrogen bonding)

17
Q

Why is a high heat of vaporisation important to moderation of climate

A

Huge amount of solar
heat absorbed by tropical seas is consumed by evaporation.
The moist air then travels polewards, cools and releases
heat as it condenses forming RAIN.

18
Q

Why is a high heat of vaporisation important to stability of temperature in lakes and ponds

A

Evaporative cooling of water contributes to the stability
of temperature in lakes and ponds allowing life to
flourish.

19
Q

Why is a high heat of vaporisation important to terrestrial organisms

A

Prevents terrestrial organisms from overheating eg. evaporation of sweat from human skin; evaporation of water from plant leaves.

20
Q

Why is liquid water more dense than ice

A

As the temperature of water drops from 4°C to 0°C more of its molecules are moving too slowly to break hydrogen bonds.
At 0°C the molecules are locked in crystalline lattice each water molecule H-bonded to 4 others.
This creates uniform ‘spaces’ between the water molecules making ice less dense than water = FLOATS

21
Q

Why is ice floating important to life

A

If ice sank then eventually all ponds, lakes and oceans would freeze. Life on Earth as we know it would be impossible. In summer only the surface would thaw. Now, when an ocean cools in winter the floating ice INSULATES the liquid water below preventing it from freezing and allowing life to exist underneath eg. krill.

Solid habitat for many forms of life.

22
Q

Hydration shell

A

The sphere of water molecules around each dissolved ion

23
Q

Why is water the “solvent of life”

A

Polar compounds and ions are dissolved in biological fluids eg. blood, sap in plants and the cytoplasm of cells.

24
Q

Concentration of H+ in pure water

A

10-7 M (one ten-millionth of a mole of hydrogen ions per L of water)

25
Q

Constant product of H+ and OH-

A

10-14

26
Q

Ocean acidification

A

25% of CO2 is absorbed by the oceans which reactis with water to forn carbonic acid. this dissociates into H+ & HCO3 and the H+ combines with carbonate ions forming more HCO3

27
Q

Effects of ocean acidification

A

Less CO32- is available for calcification – the formation of calcium carbonate – by marine organisms eg. coral, shellfish. Prediction that the carbonate concentration could decrease by 40% by 2100