Water Relations Flashcards
water vapor pressure
- low temp, low saturation, low pressure
- pressure increases with higher saturation at higher temperatures
- water usually moves from organisms to atmosphere (approximated by vapour pressure deficit)
vapour pressure deficit
differential between actual vapour pressure and saturation water vapour pressure
- high vpd = low water content in sky and high evaporation from organism
hypo osmotic
high water (low salt)
hyper osmotic
low water (high salt)
osmotic pressure
created by movement of water
- larger osmotic differences between organism and environment - high osmotic pressure
isosmotic
same concentrations
water potential
capacity of water to do work
- flows from high water potential to lower
- pure water has a water potential of 0 (solutes reduce potential)
matric forces
tendency for water to cling to soil particles and plant cell walls which reduces water potential
water regulation on land
terrestrial plants and animals regulate internal water by balancing water acquisition against loss
how do marine creatures balance salt and water?
- may be isosmotic to environment
- may be hyper osmotic
osmoregulation: regulation of internal salt and water by decreasing osmotic gradient between themselves and environment
SIA - water uptake in plants
analysis of relative proportions of stable isotopes
2H and 18O are unusual in water and heavier so less likely to evaporate; more likely to precipitate
- surface water and ground water differ and can tell a plant’s water source