AT2 Depth Study Flashcards
Effect of Temperature on Solubility of Salts
Solubility is proportional to temperature, but differently for different salts.
Exception is sodium sulphate, which decreases in solubility past the 30°C.
Effect of Temperature on Solubility of Gases
Solubility is indirectly proportional to temperature because increased kinetic energy breaks dispersion forces.
Carbon dioxide is more soluble than other gases because it reacts with the water.
Effect of Gas Pressure on Solubility
Gas pressure is proportional to solubility of gas.
What does gas concentration depend on?
Temperature, depth and salinity
Concentration in sea water and fresh water?
Concentration is sea water is less than in fresh water because the presence of ions interferes with dispersion forces.
Factors that Influence Gas Concentration (8)
Partial pressure of gases in troposphere.
Diffusion rate into water surface.
Temperature of ocean.
Diffusion into deeper layers.
Ocean currents.
Water salinity.
Photosynthesis/Respiration.
Carbonate-hydrogen carbonate equilibria.
Concentrations with increasing depth.
Partial Pressure of Gases in Troposphere
Abundancy in troposphere: N > O > CO2
Proportional to shift in dissolution equilibria.
Diffusion Rate into Water Surface
Affected by water turbulence and temperature.
Droplet created by turbulence increases rate of diffusion.
Temperature of Ocean Water
Temperature is inversely proportional to concentration.
Temperature varies according to proximity to land and cold salt water is denser than warm, meaning that surface water near the poles has higher concentration.
Diffusion into Deeper Layers
Surface and deep water do not mix much.
Ocean Currents
Deep: Currents from Antarctica and Southern Ocean transport cold water.
Surface: Currents move into the Indian Ocean.
Ocean temperature decreases with depth and cold water has higher concentration of gases.
Water Salinity
Solubility is inversely proportional to salinity.
Seawater salinity: 3.0-3.7% (w/w)
Warm currents have lower salinity.
Salinity is proportional to density and water is more saline near the poles.
Photosynthesis and Respiration
The photic zone is the surface 150m where photosynthetic organisms can live.
Oxygen is both consumed and produced in photic zone.
Carbonate-Hydrogen Carbonate Equilibria
Carbon dioxide is constantly dissolving to create carbonic acid, which can be stored in deeper layers of the ocean for thousands of years at a constant concentration, but currents can bring it to the surface.
Some organisms use dissolved CO2 in constructing shells and exoskeletons.
CO2(aq) + H2O(l) → H2CO3 (aq)
Concentrations with Increasing Depth
Oxygen: Higher in surface waters because photosynthesis and diffusion.
Carbon dioxide: Higher in deeper water because respiration and decomposition.
Nitrogen: Not affected by depth but opposite of CO2.
What affects rate of reaction in oceans? (4)
Temperature, depth, oxygen concentration and salinity.