AT2 Depth Study Flashcards
(41 cards)
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.
Evolution of Ship-Building Materials
European ships in 16th century were predominantly timber with metals used for fastenings, anchors or braces.
British ships in 18-19th centuries became iron and then steel when iron began to rust too much.
Ancient Greek Ship
Oldest, intact shipwreck ever found (350-410 BCE).
Water in the Black Sea is either of high salinity (from the Mediterranean) or low salinity (land runoff), and lack of water currents makes these layers distinct.
Deep basin allows ships to be entirely submerged in an anaerobic environment.
The Endurance
Sunk in the Antarctic in 1915.
Ice slowed the ships descent to the ocean floor.
Lack of light and oxygen prevent degrading organisms, such as parasitic worms and bacteria.
Hull of the Titanic
Hull - watertight main body of a ship.
Overlapping steel plates held by iron rivets.
Steel was ten times more brittle than modern steel, especially at freezing temperatures due to higher content of S, O and P and lower Mn.
Iron rivets had high concentrations of slag, prone to fracturing and couldn’t handle the stress.
Superstructure of the Titanic
Superstructure - parts that project above the main deck.
Two timber decks with steel framing and a navigating bridge in between.
Sealant to survive harsh weather.
Decay of the Titanic’s Hull
North Atlantic Ocean has ideal conditions for protobacteria.
Presence of bacteria (Halomonas titanicae) consumed iron in hull and formed rust mounds called rusticles because of the solubility of iron.
Fe2O3 formed a porous layer on the surface, which diffused water into iron metal and increased corrosion rate.
2Fe(s) + O2(g) + H2O(l) → 2Fe2O3(s) + H2O(l)
Sulfate-reducing bacteria is one of the key microbes in metal corrosion, facilitating the reduction of sulfate under anaerobic conditions in the water. It occurs in the following redox reaction:
4Fe(s) + SO4(aq) + 10H(aq) → 4Fe2+(aq) + H2S(g) + 4H2O(l)
Hydrogen sulfide reacts with iron (II) ions to form iron (II) sulfide (rusticles), among other components.
Decay of the Titanic’s Superstructure
Steel framing corroded and broke, collapsing decks on top of each other.
Water pressure and deep currents caused disintegration.
Thick layers of sediment allowed some areas of wood deck to be protected from damp environment and remain intact.
Teredo worm holes found.
Corrosion in Shallow Waters
High oxygen concentration allows aerobic bacteria the thrive and cause concretion, and corrosion reactions on reactive metals.
Higher temperature and acidity, which can cause acid/metal reaction with metal salts and hydrogen gas.