240 likes | 737 Views
Water Availability. Organisms can gain or lose waterPartly determined by concentration gradientWater moves down the gradient. Water Content of Air. Relative Humidity - quantity of water vapor in air RH = Water vapor densityX 100 Saturation water vapor density Water vapor pressure - pressure exerted by water vapor in airVapor pressure deficit - the relative saturation of air with water.
E N D
1. Water, Water, Everywhere and Nary a Drop to Drink The Rime of the Ancient Mariner
Coleridge, 1797
2. Water Availability Organisms can gain or lose water
Partly determined by concentration gradient
Water moves down the gradient
3. Water Content of Air Relative Humidity - quantity of water vapor in air
RH = Water vapor density X 100
Saturation water vapor density
Water vapor pressure - pressure exerted by water vapor in air
Vapor pressure deficit - the relative saturation of air with water
4. Determining the Gradient Terrestrial animals - vapor pressure deficit
Aquatic animals - relative osmolarity
Terrestrial plants - water potential
5. Terrestrial Animals -VPD
7. Terrestrial Plants - Water Potential Plants gain and lose water
Moves along gradient of water potential from high to low
Will go from plant --> air due to vpd
Need it to go
Soil -- Plant -- Air
9. Water Movement in Aquatic Environments Diffusion - move down concentration gradients
Osmosis - diffusion of water across a semipermeable membrane
10. Aquatic Animals - Osmolarity Water still moves down gradient
? solutes in water = ? osmolarity
Water goes low osmolarity to high
Isosmotic - no change
Hypoosmotic - lose water
Hyperosmotic - gain water
11. Aquatic Animals
12. Freshwater vs. Marine Bony Fish
13. Marine Cartilagenous Fish Same problems as marine teleosts
Barely hyperosmotic
urine
15. Water Regulation on Land
16. Water Acquisition by a Desert Beetle
17. Water Acquisition
18. Water Conservation Lower evaporation
19. Water Conservation Increase gain
20. Water Conservation Alter secretions
21. Uric Acid
22. Terrestrial Plants
23. Water Conservation ? Evaporation
24. Water Conservation Increase absorption
25. Water Conservation Less leaf area per length of root
Drop leaves in response to drought
Produce leaves in response to soaking rain the shed them when desert dies out.