Ocean Chemistry Chemical Properties Physical Properties
Foundations Aristotle Robert Boyle Edmund Halley Count Luigi Ferdinando Marsigli Antoine Laurent Lavosier Joseph Louis Gay-Lussac Alexander Marcet Johann Georg Forchhammer William Dittmar Justus von Liebig James Johnstone Vladimir Ivanovich Vernadsky Alfred Redfield
Forms of Matter
The Water Molecule
Dissolving Ability Universal solvent Polar nature & hydrogen bonding
Conservative ions Major constituents have very constant ratios to one another Not generally removed or added by living organisms Nonconservative ions Change concentrations depending on season, locale and biological processes
Dissolved Gases The most abundant gases in the atmosphere and in the oceans: Nitrogen (N 2 ) Oxygen (O 2 ) Carbon dioxide (CO 2 )
Dissolved Gases Saturation concentration The maximum amount of any gas that can be held in solution Temp, salinity & pressure Solubility has an inverse relationship with temp and salinity Solubility has a direct relationship with pressure
Distribution with Depth Photosynthesis Sunlight + H 2 O + CO 2 C 6 H 12 O 6 + O 2 Respiration Organics + O 2 CO 2 + H 2 O + Energy Decomposition Uses up oxygen
O2O2 Hypoxic Anoxic Anaerobic
O 2 and CO 2 CO 2 45 – 54 mL/L Oxygen minimum zone
Sources of Salt Continental weathering Riverine input Volcanic gases
Source (& Sink) of Salt Hydrothermal vents Discovered in 1977 Geyser on the seafloor Spews super-hot, mineral-rich water Very biodiverse
Source (& Sink) of Salts Hydrothermal vents Black Smokers Hottest of the vents Spew iron and sulfide, which combine to form iron monosulfide (FeS) White Smokers Cooler temp Barium, Calcium and Silicon
Regulating the Salt Balance - Sources & Sinks
Residence Time RT = Amount of ion Rate of input or removal
CO 2 and The World Ocean
The pH of Seawater H+ Hydrogen cation OH- Hydroxide anion H + = OH - H + < OH - H + > OH - NeutralAlkalineAcidic
Buffering Capacity of CO 2 Buffer Substance that prevents sudden, or large, changes in acidity or alkalinity of a solution CO 2 + H 2 O H 2 CO 3 H + + HCO 3 - 2H + + CO 3 2-
Fig. 6.18
Fig. 6.19
Fig. 6.20
Fig. 6.21
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