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Lecture goal: To identify and describe the properties of water that are most important to understanding broader patterns of habitat structure and ecology in freshwater systems. Properties and behavior of H 2 0 1: The specifics
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Molecular Structure Density Temperature Oxygen Light
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The Specifics Molecular Structure Density Temperature Oxygen Light
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Structure of H 2 O Polarity Solvent properties
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Surface Tension
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The Specifics Molecular Structure Density Temperature Oxygen Light
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Temperature and Water Density
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Anchor Ice
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Depth and Water Density Density increases with depth. Influenced by atmospheric pressure and other factors.
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Salinity and Water Density Density (g / ml) Freezing point of sea water (35 g/L) = -2ºC Max density of sea water = -2ºC Salinity of “Freshwater” ranges from 0.01 – 1.0 g/L Saline lake 60 g/L
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The Specifics Molecular Structure Density Temperature Oxygen Light
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Temperature and Water Density
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Specific Heat of Water Specific heat: amount of heat in calories required to raise a unit (i.e., a gram) of the substance by 1 C. Specific heat of water = 1 Latent heat of fusion = 80 Latent heat of vaporization = 540
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Measuring Water Temperature Standard / immediate temperature Seasonal max, min, mean Degree days
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The Specifics Molecular Structure Density Temperature Oxygen Light
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How oxygen gets into water
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How oxygen gets into water…or not
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Pressure and O 2 Solubility
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Temperature and O 2 Solubility Oxygen Solubility (mg / L)
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Salinity and O 2 Solubility
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Oxygen Terminology Saturation or Equilibrium Concentration Amount of DO that can be held by water in equilibrium with the atmosphere at a particular temperature, pressure, and salinity. Supersaturation Anoxia Hypoxia
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The Specifics Molecular Structure Density Temperature Oxygen Light
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Why is light important in aquatic systems? Light is energy, capable of work and being transformed from one form to another. Radiant energy of light transformed to potential energy by biochemical reactions (e.g., photosynthesis). Light provides the majority of energy input to aquatic systems – but getting light INTO aquatic systems is tough.
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More Blue More Red Frequency Wavelength
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How do plants receive light energy? Quanta or photons at specific frequencies
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Controls on light input: season and latitude
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Controls on light input: direct solar radiation
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Other controls on direct solar radiation Time of day Altitude Meteorological conditions Topography
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Controls on light input: indirect solar radiation
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Controls on indirect solar radiation Scattering through atmosphere Solar height
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Controls on light input: reflectivity
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Controls on reflectivity Angle of incidence Surrounding topography Surface conditions of water
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Albedo Ratio of reflected to incident irradiance Increases with reflection at surface and scattering within the lake.
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Albedo
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Light scattering within lakes
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Effect of Salinity on Density and O 2 Solubility Density (g / ml) Anthropogenic Salinization
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