Exam 1 Flashcards
Water
- polar molecule (one side that is positively charged and one that is negative)
- H2O covalent bonds (share electrons); hydrogen bonds causes water molecules to associate in a cluster
- # of molecules per cluster decreases with increase in water temp
- dissolves other substances
- lattice like molecular configuration
Latent Heat of Vaporization
- heat doesn’t cause a change in temp but changes the phase or state; ie liquid to gas
- takes 540 cal/g/C to change a phase
- water is more stable and remarkably resistant to heating due to H+ bonds
Temperature Variation
- Terrestrial ecosystems 10-15 degrees C
- Aquatic ecosystems 1-2 degrees C
Specific Heat
- amount of heat required to raise the temp of 1 gram of water 1 degrees C
- water can hold a great deal of heat
Latent Heat of Fusion
- melting
- heat required to change ice to water with no change in temp.
- don’t need to break all H+ bonds, just some
- takes 80 cal/g/degrees C
Density
- water’s max density at 4 degrees C
- density of ice: 0.917 g cm^3
- density of water: 0.999 cm^3
- ice formation: angle expanded and lattice-like structure forms; ice less dense than water
- thermal expansion is the dominant force
Viscosity
- the state of being thick, sticky, and semifluid in consistency, due to internal friction
- honey has higher viscosity than water
Surface tension
- attraction of the particles in the surface layer by the bulk of the liquid, which tends to minimize surface area
- water has a high surface tension
Normal Conditions
- trade winds blow from east to west
- warm low pressure area around Australia & Asia
- causes upwellings near South America, heavy in nutrients, rich fishery in that area
El Nino
- weak or no trade winds
- warm moist air and water flows toward South America which causes lots of rain there and no upwellings
Lacustrine
relating to lakes
Paulustrine
relating to wetlands
Riverine
relating to rivers
Evapotranspiration
water evaporating from plants and trees out of their stomata
Watershed/ Basin
area surrounding a lake or river that all water drains into
Euphotic
light penetration; top layer
Aphotic
no light and no photosynthesis
Littoral zone
rooted and submerged plants; near shore area
Causes of circulation patterns in lakes
- wind (AKA fetch)
- Topography (hills, mtns can block wind)
- Amount of ions in the water
- Temperature (which relates to density)
- Depth
Lake ecosytems
- highly variable, heterogeneous (patchy) in physical, chemical and biological components
- temp, light, density, currents
- nutrients, ions, contaminants
- populations, growth rates: ie filter feeders at the outlet