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Properties of Ocean Water
Oceanography Properties of Ocean Water
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1. Chemical Properties/Composition
400 billion kg of dissolved solids are carried by rivers into the ocean. Mostly dissolved salts As water evaporates salts and minerals are left behind
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Elements in Ocean Water
Na – sodium Cl – Chlorine Mg – Magnesium Ca – Calcium K- Potassium Oxygen Gas Nitrogen Gas Carbon Dioxide Trace Minerals 78% of ocean water is NaCl – Sodium Chloride/Table Salt
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Salinity The amount of dissolved solids in ocean water 1kg = 1000g
1kg ocean water = 35g of dissolved solids 35 parts of salt per 1000 parts of ocean water is 35% salinity
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Changing Salinity 1- freezing 2- evaporation Lower Salinity
When evaporation is high, salinity increases Tropical Waters have a higher salinity because of high evaporation
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Other Factors of Salinity
Depth Surface has more evaporation and higher salinity. Avg. global surface salinity 34.7% Climate Hot and dry Red Sea – 40% Low temp., low evaporation, runoff, melt, and river drainage Baltic Sea – 20% Arctic Ocean has low salinity
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2. Temperature Gases dissolve best in COLDER temperatures
Solids dissolve best in WARMER temperatures Surface Water – varies with seasons Thermocline – area of rapid temperature change
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Temperature of Ocean Water
Absorbs long infrared wavelengths Upper zone – completely absorbed Deep zone – only about 2o C Freezing point of salt water is - 2o C
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3. Density Temperature affects density of ocean water D=M/V
Colder – More Dense Warmer – Less Dense D=M/V Dissolved Substances and density of ocean water Large amount = greater density Small amount = less density
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Ocean Resources Minerals Food Fresh Water
Distillation – one method of desalination
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Ocean Pollution
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