Topic 2: Seawater

The physical and chemical properties of the ocean.

🗺️ Topic 2 Mind Map

2.1 Composition and Salinity

Seawater is a complex solution containing dissolved salts, gases, and other substances. The total dissolved salt content is called salinity.

Composition of Seawater

Ion% of Dissolved Salts
Chloride (Cl⁻)55.0%
Sodium (Na⁺)30.6%
Sulfate (SO₄²⁻)7.7%
Magnesium (Mg²⁺)3.7%
Calcium (Ca²⁺)1.2%
Potassium (K⁺)1.1%
Others0.7%

Factors Affecting Salinity

FactorEffect on SalinityExample
EvaporationIncreases salinity (water leaves, salt stays)Red Sea (~40 ppt) — hot, arid climate
Freshwater inputDecreases salinity (dilution)Baltic Sea (~10 ppt) — many rivers
PrecipitationDecreases salinity (dilution)Equatorial regions with high rainfall
Ice formationIncreases local salinity (salt excluded from ice)Polar regions in winter
Ice meltingDecreases local salinity (freshwater added)Polar regions in spring/summer
Average Ocean Salinity ~35 parts per thousand (ppt) = 35 g salt per 1 kg seawater = 3.5%

2.2 Temperature and Density Relationships

The density of seawater is determined by three factors:

  • Temperature: Colder water = denser (molecules closer together)
  • Salinity: Saltier water = denser (more dissolved material)
  • Pressure: Greater pressure = slightly denser (at depth)
Density Rule Cold + Salty = DENSE (sinks)   |   Warm + Fresh = LESS DENSE (rises)

Diagram: Ocean Depth Profile

0m 200m 1000m 4000m Temperature → Depth → Warm Surface THERMOCLINE Cold Deep Water

Ocean Layering (Stratification)

LayerWhat ChangesDescription
ThermoclineTemperatureRapid temperature decrease with depth (~200-1000m)
HaloclineSalinityRapid salinity change with depth
PycnoclineDensityRapid density change with depth
Learn the prefixes: thermo = temperature, halo = salt, pycno = density. The suffix -cline means a gradient or change.

2.3 pH and Dissolved Gases

pH of Seawater

The pH scale measures how acidic or alkaline a solution is (0-14). Ocean surface water is naturally slightly alkaline at approximately pH 8.1.

Ocean Acidification

Ocean acidification is the decrease in ocean pH caused by the absorption of excess CO₂ from the atmosphere:

Ocean Acidification Reaction CO₂ + H₂O → H₂CO₃ (carbonic acid) → H⁺ + HCO₃⁻

Dissolved Gases

GasSourcesImportance
Oxygen (O₂)Photosynthesis, atmosphereEssential for respiration by marine organisms
Carbon Dioxide (CO₂)Atmosphere, respiration, decompositionUsed in photosynthesis; causes acidification when excess

Dissolved oxygen is highest at the surface (contact with air + phytoplankton) and decreases with depth to an oxygen minimum zone before slightly increasing in cold deep water.

A decrease of just 0.1 pH units represents a ~30% increase in acidity! The pH scale is logarithmic — each whole number change represents a 10x change.

2.4 Effects of Depth on Seawater Properties

As ocean depth increases, several properties change dramatically:

PropertyChange with DepthDetail
TemperatureDecreasesRapid drop at thermocline; deep water ~2-4°C
LightDecreasesPhotic zone (0-200m); aphotic zone below 200m
PressureIncreases+1 atm per 10m depth
Dissolved O₂Decreases then stabilisesMinimum at ~500-1000m; slightly more in cold deep water

Measuring Water Clarity

A Secchi disc is a simple tool used to measure how far light penetrates water. The disc is lowered until it disappears from view — this depth is the Secchi depth. Greater Secchi depth = clearer water.

Factors reducing clarity: sediment, algal blooms, pollution, river runoff.

2.5 Water Cycle and Ocean Interactions

The water cycle (hydrological cycle) describes the continuous movement of water between the oceans, atmosphere, and land.

Key Processes

ProcessDescriptionEffect on Ocean Salinity
EvaporationSun heats ocean surface; water turns to vapourIncreases salinity (salt left behind)
CondensationWater vapour cools and forms cloudsNo direct effect
PrecipitationRain/snow falls on ocean or landDecreases salinity (adds fresh water)
RunoffWater flows from land to ocean via riversDecreases coastal salinity

Diagram: The Water Cycle and the Ocean

Evaporation Precipitation Runoff Condensation Ocean Land
  • The ocean holds ~97% of all water on Earth
  • Evaporation removes water but leaves salt behind, increasing salinity
  • River input and rain dilute seawater, decreasing salinity near coasts

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