ocean chemistry Flashcards

1
Q

whats The Hydrologic Cycle

A

Cycle of Precipitation + evaporation driven by solar radiation
**Water spends a very long time in the ocean before its recycled into the atmosphere

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2
Q

what 2 components is a solution made from

A
  • Solvent – usually a liquid, always the more abundant
  • Solute – often a dissolved solid or gas, always the less abundant
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3
Q

difference between solution and mixture

A
  • true solution has uniform properties (e.g. sugar in well-stirred tea)
  • mixture = different substances retain separate identities
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4
Q

whats an ion

A

an atom/small group of atoms with an unbalanced electrical charge (gained or lost one or more electrons) e.g. Sodium ions (Na + ), chloride ions (Cl- )

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5
Q

one major historical belief to solve pollution

A

“The solution to pollution is dilution”
*water polar property allows it to dissolve many things

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6
Q

what percent of the ocean is dissolved substances

A

3.5% - most are salts

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7
Q

what are trace elements

A

Elements less than one part per million in volume
- Only 14 elements have concentrations in seawater greater than this

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8
Q

what happens to the heat capacity of water with increasing salinity

A

decreases

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9
Q

why does seawater evaporate more slowly than freshwater

A

Osmotic pressure increases - salinity levels

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10
Q

5 Processes That Regulate the Major Constituents in Seawater

A

rain, river discharge, volcanic activities, ridge systems

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11
Q

what is Forchhammer’s principle and how does it relate to the ocean

A

principle of constant proportions
- The Ratio of Dissolved Solids in the Ocean Is Constant
- The total amount of dissolved solids (salinity) may vary among samples, but the ratio of major salts was constant in samples of seawater from many locations (HMS Challenger)
- The ocean is in chemical equilibrium

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12
Q

what is the mixing time of the ocean

A

~ 1,600 years

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13
Q

what are Conservative constituents and how are they determined

A

substances that remain in constant proportions or change very slowly through time (long residence time)
- Residence time > mixing time = Conservative constituents

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14
Q

what are non conservative constituents and how are they determined

A

substances dissolved in seawater that
are tied to biological or seasonal cycles or to very short geological cycles (short residence times)
- Residence time < mixing time = Nonconservative constituents

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15
Q

how is Salinity calculated

A

by Seawater’s Conductivity
- water samples at predetermined depths are collected using a group of sampling bottles
- The bottles are hauled to the surface and their contents analyzed by a salinometer

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16
Q

what parts of the ocean do gases dissolve in more readily

A

in cold water + at the surface

17
Q

top 3 gases dissolved in the ocean

A

N2 – most conc at sea surface
O2
CO2 – most conc in ocean as a whole

18
Q

how does Concentrations of Oxygen + Carbon Dioxide Vary with Depth

A

O2 levels higher at the surface - decrease with depth
CO2 lower at surface - increases with depth

19
Q

what is an acid

A

a substance that releases a hydrogen ion in solution

20
Q

what is a base

A

a substance that combines with a hydrogen ion in solution

21
Q

whats the pH of seawater

22
Q

what form in dissolved CO2 in seawater

A

carbonic acid

23
Q

how does the oceans natural buffer work

A

can turn carbonic acid into bicarbonate + carbonate – reduces its acidity

24
Q

how does pH differ with depth

A

Deep, cold seawater (below 4,500 meters) has a pH of around 7.5 - more acidic as co2 dissolves more readily
- A drop to a pH of 7 can occur at the deep ocean floor when bottom bacteria consume oxygen and produce sulfide

25
Q

why is ocean acidification a problem for organisms with shells

A

carbonate ions from dissolved co2 combines with hydrogen to make carbonic acid instead - organism’s supply of essential carbonate goes down