18. The Hydrosphere Flashcards
What is the hydrosphere composed of? 5
- 97.5% sea water, icl estuaries 2. 2.24% glaciers 3. 0.009% standing/lentic water 4. 0.001% running/lotic water 5. lack of water impacts water security and availability, so has economic and also ecologicial impacts
Why are freshwaters important to the biosphere? 3
- Movement of water between and within ecosystems 2. Transport of natural substances including nutrients 3. Water is provided for the terrestrial system
Why is freshwater important to humans? 3
- transport 2. irrigation 3. waste disposal
What are the types of non-marine water environment? 6
What are the major biological communities that live in freshwaters composed of? 5
1. Plankton – floating and movement depend on currents. less in running water as washed away- can’t move against current
2. Epibenthos – attached or clinging to mcro/macroplants
- Nekton – swimming and able to navigate at will ie. fish
4. Benthos - attached or living on/in bottom sediments
5. Neuston - resting or swimming at surface due to surface tension
What are shredders? 2
- Shred food material eg. dead leaves
- incl Trichoptera (caddis flies), Amphipoda (Gammaridae), Isopoda (Asellidae) Decapoda (various families of crayfish)
What are grazers in the water? 2
- graze on algae etc that is on stones and the like
- incl Ephemeroptera (mayflies), Gastropod molluscs
What are collectors in the water? 3
- collect bits of food eg, parts that have been shredded by shredders
- Those in the water column incl Diptera, Trichoptera
- those on sediment incl. oligochaeta, diptera and bivalve molluscs
What are predators in the water? 2
- May eat directly, may suck blood
- incl Hirudinea (leeches) Trichoptera, Plectoptera (stoneflies), Odonata (dragon/damsel flies), Coleoptera (beetles)
How do freshwater ecosystems form a continua? 6
1. Different organisms occur in different reaches (‘stretches’), river communities grade into one another - ‘river continuum’
- Results in changes in energy transfer
3. shredders/grazers -> collectors of coarse particulates (from above)/grazers -> collectors of fine particulates (as river slows down so larger particles are eroded)
4. Energy: allochthonous (from outside eg. leaf fall) and autochthonous material (aqueous primary production eg. moss, epibenthic algae)
5. Slow-flowing deep river behaves more like a lake – ‘linear lake’.
- get stratificiation
What is stratification? 7
1. Thermal stratification common in deep (>5 m) lakes
- Oxygen depletion due to reduced re-aeration from the atmosphere
- Rivers too fast flowing and shallow for stratification
- However, stratification can occur in slow-flowing deep rivers
- The surface layer, the epilimnion, is warmer, therefore less dense, so creates a distinct layer
- The cooler layer is the lower hypolimnion
- dissolved o2 decreases getting deeper into this, as o2 can’t penetrate and is not replenished when used
What is the significance of the temperature of water? 1
- It is in lquid form all year round
What is the significance of the density of water? 5
- Similarity in density of water and aquatic biota limits the rate of passive sinking (sedimentation)
- allows shells and bouyant organisms to keep position
- Density lower above and below 4 degrees C
- Allows ice to be less dense than water - important as sinking would freeze substrate so no burrowing/feedind
- Above 4deg C: surface warming - thermal stratification in standing and slow moving running waters
What is the significance of the high absoloute viscosity of water? 3
- High viscosity limits:
- mixing of water (slower)
- sedimentation of biota
What is the significance of the low thermal conductivity and high specific heat capacity of water? 3
- slow response to change in air temperature
- So organisms don’t have to adapt to sudden temperature changes
- localised surface heating and hence stratification